\<@37\>Albany Series

\<@32\>The Albany series consists of very deep, somewhat poorly drained
soils that formed in sandy and loamy marine sediments. These soils are
in positions that are depressed relative to surrounding landforms on low
terraces and on broad ridges and knolls, on toeslopes, and on the lower
parts of footslopes. They are in the uplands. The seasonal high water
table is at a depth of 1 to 2-1/2 feet from December through April in
most years. The areas on low terraces are subject to occasional
flooding. Slopes range from 0 to 5 percent. These soils are loamy,
siliceous, subactive, thermic Grossarenic Paleudults.

\<@32\>Albany soils are geographically associated with Bonifay, Eunola,
Lakeland, Pelham, Troup, and Weston soils. The Bonifay, Lakeland, and
Troup soils are on summits and shoulder slopes in higher positions than
the Albany soils. The well drained Bonifay soils have a significant
accumulation of plinthite in the subsoil. The excessively drained
Lakeland soils are sandy throughout. The somewhat excessively drained
Troup soils have a reddish argillic horizon. The moderately well drained
Eunola soils are on stream terraces and do not have a thick, sandy
epipedon. The poorly drained Pelham and Weston soils are in lower
positions than the Albany soils. The Pelham soils have a loamy argillic
horizon at a depth of 20 to 40 inches. The Weston soils do not have a
thick, sandy epipedon.

\<@32\>Typical pedon of Albany sand, 0 to 5 percent slopes; about 100
feet north of Langley Avenue and 3,750 feet east of Ninth Avenue in
Pensacola; about 3,700 feet east and 100 feet north of the southwest
corner of sec. 10, T. 1 S., R. 29 W.

\<@23\>A---0 to 7 inches; very dark grayish brown (10YR 3/2) sand; weak
medium granular structure; very friable; common medium and fine roots;
strongly acid; clear smooth boundary.

\<@33\>E1---7 to 22 inches; brown (10YR 5/3) sand; single grained;
loose; few fine roots; strongly acid; clear wavy boundary.

\<@33\>E2---22 to 42 inches; light yellowish brown (10YR 6/4) sand;
single grained; loose; common medium prominent yellowish red (5YR 5/8)
masses of iron accumulation that have clear boundaries throughout the
matrix; common fine faint pale brown (10YR 6/3) iron depletions that
have clear boundaries throughout the matrix; strongly acid; gradual wavy
boundary.

\<@33\>Eg---42 to 57 inches; light gray (10YR 7/2) sand; single grained;
loose; common fine faint light brownish gray (10YR 6/2) iron depletions
throughout the matrix; strongly acid; clear wavy boundary.

\<@33\>Btg1---57 to 72 inches; light brownish gray (10YR 6/2) sandy
loam; weak medium subangular blocky structure; friable; sand grains
bridged and coated with clay; common medium prominent strong brown
(7.5YR 5/6) masses of iron accumulation that have sharp boundaries
throughout the matrix; strongly acid; gradual wavy boundary.

\<@33\>Btg2---72 to 80 inches; gray (10YR 6/1) sandy clay loam; moderate
medium subangular blocky structure; friable; few faint clay films on
faces of peds; common medium prominent strong brown (7.5YR 5/6) masses
of iron accumulation that have sharp boundaries throughout the matrix;
strongly acid.

\<@8\>The solum is more than 70 inches thick. The sandy epipedon ranges
from 40 to 80 inches in thickness. Reaction ranges from extremely acid
to moderately acid in the A and E horizons, except in areas where lime
has been applied, and from very strongly acid to moderately acid in the
Btg horizon.

\<@32\>The A horizon has hue of 10YR, value of 3 to 5, and chroma of 1
or 2.

\<@32\>The E horizon has hue of 10YR or 2.5Y, value of 5 to 7, and
chroma of 3 or 4. In many pedons, it has thin streaks and pockets of
white or light gray uncoated sand. It has few to many redoximorphic
depletions in shades of gray or brown and redoximorphic accumulations in
shades of red, yellow, and brown. It is sand, fine sand, loamy sand, or
loamy fine sand.

\<@32\>The Eg horizon has hue of 10YR, value of 6 to 8, and chroma of 1
or 2. It has few to many redoximorphic accumulations in shades of
yellow, olive, brown, and red. It is sand, fine sand, loamy sand, or
loamy fine sand.

\<@32\>The Bt horizon, where present, has hue of 10YR or 2.5Y, value of
5 to 7, and chroma of 3 to 8. It has common or many redoximorphic
depletions in shades of brown and gray and redoximorphic accumulations
in shades of red, brown, and yellow. It is sandy loam, fine sandy loam,
or sandy clay loam.

\<@32\>The Btg horizon has hue of 10YR or 2.5Y, value of 5 to 7, and
chroma of 1 or 2; or it does not have a dominant matrix color and is
multicolored in shades of red, yellow, brown and gray. It has common or
many redoximorphic accumulations in shades of red, yellow, and brown. It
is sandy loam, fine sandy loam, or sandy clay loam.

\<@37\>Allanton Series

\<@32\>The Allanton series consists of very deep, very poorly drained
soils that formed in sandy marine sediments. These soils are on broad
flats and in shallow depressions. They are on the coastal lowlands. The
seasonal high water table is within a depth of 1/2 foot from December
through April in most years. Slopes range from 0 to 2 percent. These
soils are sandy, siliceous, thermic Grossarenic Alaquods.

\<@32\>Allanton soils are geographically associated with Hurricane,
Leon, Pelham, Pickney, and Pottsburg soils. The somewhat poorly drained
Hurricane soils are on knolls in slightly higher positions than the
Allanton soils. The poorly drained Leon soils are in areas of flatwoods,
are at slightly higher elevations than the Allanton soils, and have a
spodic horizon within a depth of 30 inches. The poorly drained Pelham
soils are in positions similar to those of the Allanton soils on flats
and have a loamy argillic horizon at a depth of 20 to 40 inches. The
Pickney soils are in positions similar to those of the Allanton soils
and do not have a spodic horizon. The poorly drained Pottsburg soils are
in slightly higher positions than the Allanton soils on flats and do not
have an umbric epipedon.

\<@32\>Typical pedon of Allanton sand, in an area of Allanton-Pottsburg
complex; about 250 feet south and 875 feet west of the northeast corner
of sec. 22, T. 2 S., R. 31 W.

\<@23\>A1---0 to 10 inches; black (10YR 2/1) sand; weak fine granular
structure; very friable; many medium and fine roots; common uncoated
sand grains; very strongly acid; clear wavy boundary.

\<@33\>A2---10 to 17 inches; very dark gray (10YR 3/1) sand; single
grained; loose; few medium and fine roots; common uncoated sand grains;
very strongly acid; clear wavy boundary.

\<@33\>Eg1---17 to 28 inches; grayish brown (10YR 5/2) sand; single
grained; loose; few fine roots; very strongly acid; gradual wavy
boundary.

\<@33\>Eg2---28 to 53 inches; light gray (10YR 7/2) sand; single
grained; loose; very strongly acid; gradual wavy boundary.

\<@33\>Bh1---53 to 65 inches; dark brown (7.5YR 3/2) sand; massive;
friable; about 70 percent of the sand grains are coated with organic
matter; very strongly acid; clear wavy boundary.

\<@33\>Bh2---65 to 80 inches; dark reddish brown (5YR 2.5/2) sand;
massive; friable; about 90 percent of the sand grains are coated with
organic matter; very strongly acid.

\<@8\>The solum is more than 80 inches thick. Reaction is very strongly
acid or strongly acid in the A and Eg horizons and ranges from extremely
acid to strongly acid in the Bh horizon. Depth to the spodic horizon
ranges from 50 to 80 inches. The umbric epipedon ranges from 16 to 30
inches in thickness.

\<@32\>The A horizon has hue of 10YR or 2.5Y, value of 2 or 3, and
chroma of 2 or less.

\<@32\>The Eg horizon has hue of 10YR or 2.5Y, value of 4 to 7, and
chroma of 2 or less. It is sand, fine sand, or loamy sand.

\<@32\>The Bh1 horizon has hue of 7.5YR or 10YR, value of 2 to 5, and
chroma of 2 or less. It is sand, fine sand, or loamy sand.

\<@32\>The Bh2 horizon has hue of 5YR to 10YR, value of 2 to 3, and
chroma of 2 or less. It is sand, fine sand, or loamy sand.

\<@37\>Bama Series

\<@32\>The Bama series consists of very deep, well drained soils that
formed in loamy sediments. These soils are on summits and shoulder
slopes in the uplands. In most years, the seasonal high water table is
below a depth of 6 feet throughout the year. Slopes range from 0 to 5
percent. These soils are fine-loamy, siliceous, subactive, thermic Typic
Paleudults.

\<@32\>Bama soils are geographically associated with Emory, Malbis,
Notcher, and Red Bay soils. The Emory soils are in shallow depressions
and have a dark red argillic horizon. The Malbis and Notcher soils are
in slightly lower positions than the Bama soils, have a brownish
argillic horizon, and have a significant accumulation of plinthite in
the subsoil. The Red Bay soils are in positions similar to those of the
Bama soils and have a dark red argillic horizon.

\<@32\>Typical pedon of Bama fine sandy loam, 0 to 2 percent slopes;
about 300 feet north and 500 feet east of the intersection of County
Highways 97 and 4 in the northern part of the county; 1,300 feet south
and 350 feet east of the northwest corner of sec. 7, T. 5 N., R. 33 W.

\<@23\>Ap---0 to 6 inches; brown (10YR 5/3) fine sandy loam; weak medium
granular structure; friable; common medium, fine, and very fine roots;
moderately acid; clear smooth boundary.

\<@33\>Bt1---6 to 20 inches; reddish yellow (5YR 6/6) sandy clay loam;
weak medium subangular blocky structure; friable; common fine roots; few
faint clay films on faces of peds; few pebbles of ironstone; strongly
acid; clear smooth boundary.

\<@33\>Bt2---20 to 32 inches; yellowish red (5YR 5/8) sandy clay loam;
weak medium subangular blocky structure; friable; few fine roots; few
faint clay films on faces of peds; strongly acid; gradual wavy boundary.

\<@33\>Bt3---32 to 56 inches; red (2.5YR 5/8) sandy clay loam; moderate
medium subangular blocky structure; firm; few faint clay films on faces
of peds; strongly acid; gradual wavy boundary.

\<@33\>Bt4---56 to 80 inches; red (10R 5/8) sandy clay loam; weak medium
subangular block structure; firm; few faint clay films on faces of peds;
strongly acid.

\<@8\>The solum is more than 60 inches thick. The content of ironstone
concretions, quartz gravel, or both ranges from 0 to 15 percent, by
volume, in the solum. Reaction ranges from very strongly acid to
slightly acid in the A and E horizons, except in areas where lime has
been applied, and from very strongly acid to moderately acid in the Bt
horizon.

\<@32\>The A or Ap horizon has hue of 5YR to 10YR, value of 3 to 5, and
chroma of 2 to 4.

\<@32\>The E horizon, where present, has hue of 7.5YR or 10YR, value of
4 to 6, and chroma of 4 to 8. It is fine sandy loam or sandy loam.

\<@32\>The Bt horizon dominantly has hue of 10R to 5YR, value of 4 to 6,
and chroma of 6 to 8. In some pedons, however, below a depth of about 40
inches the Bt horizon has hue of 10R or 2.5YR, value of 3, and chroma of
4 to 6. In the lower part of some pedons, the Bt horizon has
redoximorphic accumulations in shades of brown. These accumulations are
assumed to be relict features. The texture is loam, sandy clay loam, or
clay loam.

\<@37\>Bigbee Series

\<@32\>The Bigbee series consists of very deep, excessively drained
soils that formed in sandy fluvial sediments. These soils are on high
parts of natural levees on flood plains. The seasonal high water table
is within a depth of 3-1/2 to 6 feet from December through April in most
years. These soils are subject to occasional flooding for brief periods.
Slopes range from 0 to 5 percent. These soils are thermic, coated Typic
Quartzipsamments.

\<@32\>Bigbee soils are geographically associated with Fluvaquents and
Garcon, Mantachie, and Yemassee soils. The very poorly drained
Fluvaquents are in depressions on the lower parts of the flood plains.
The somewhat poorly drained Garcon and Yemassee soils are on low
terraces and have loamy subsoil layers. The somewhat poorly drained,
loamy Mantachie soils are on the lower parts of the flood plains.

\<@32\>Typical pedon of Bigbee fine sand, in an area of
Garcon-Bigbee-Yemassee complex, 0 to 5 percent slopes, occasionally
flooded; in the Bristol Park subdivision, about 3,165 feet north and
3,170 feet east of the southwest corner of sec. 3, T. 1 S., R. 31 W.

\<@23\>A---0 to 7 inches; dark grayish brown (10YR 4/2) fine sand; weak
fine granular structure; very friable; common medium and fine roots;
strongly acid; clear wavy boundary.

\<@33\>C1---7 to 18 inches; yellowish brown (10YR 5/4) fine sand; single
grained; loose; strongly acid; gradual wavy boundary.

\<@33\>C2---18 to 25 inches; light yellowish brown (10YR 6/4) fine sand;
single grained; loose; strongly acid; gradual wavy boundary.

\<@33\>C3---25 to 35 inches; light yellowish brown (10YR 6/4) fine sand;
single grained; loose; few faint streaks of clean sand; common medium
prominent reddish yellow (7.5YR 6/6) masses of iron accumulation with
sharp boundaries throughout the matrix; strongly acid; clear wavy
boundary.

\<@33\>C4---35 to 63 inches; white (10YR 8/1) fine sand; single grained;
loose; common medium faint very pale brown (10YR 7/4) masses of iron
accumulation with clear boundaries; strongly acid; gradual wavy
boundary.

\<@33\>C5---63 to 80 inches; light gray (10YR 7/1) fine sand; single
grained; loose; common medium faint gray (10YR 6/1) iron depletions;
strongly acid.

\<@8\>The combined thickness of the sandy sediments is more than 80
inches. Reaction ranges from very strongly acid to moderately acid
throughout the profile, except in areas where lime has been applied.

\<@32\>The A horizon has hue of 10YR, value of 3 to 5, and chroma of 2
to 4.

\<@32\>The upper part of the C horizon has hue of 10YR or 7.5YR, value
of 4 to 7, and chroma of 4 or 5. Redoximorphic features, if present, are
in shades of brown. The texture is sand or fine sand. The lower part of
the C horizon has hue of 10YR, value of 6 to 8, and chroma of 1 to 6. It
has few to many redoximorphic accumulations in shades of brown and
yellow. It has few or common redoximorphic depletions in shades of brown
and gray below a depth of 40 inches. In many pedons, the C horizon has
few or common streaks or pockets of uncoated sand.

\<@37\>Bonifay Series

\<@32\>The Bonifay series consists of very deep, well drained soils that
formed in sandy and loamy marine sediments. These soils are on broad
summits, shoulder slopes, and side slopes in the uplands. The seasonal
high water table is at a depth of 3-1/2 to 5 feet from December through
April in most years. Slopes range from 0 to 8 percent. These soils are
loamy, siliceous, subactive, thermic Grossarenic Plinthic Paleudults.

\<@32\>Bonifay soils are geographically associated with Albany,
Lakeland, and Troup soils. The somewhat poorly drained Albany soils are
in lower positions than the Bonifay soils and do not have a significant
accumulation of plinthite in the subsoil. The excessively drained
Lakeland and somewhat excessively drained Troup soils are in slightly
higher positions than the Bonifay soils and do not have a significant
accumulation of plinthite in the subsoil.

\<@32\>Typical pedon of Bonifay loamy sand, 0 to 5 percent slopes; about
1,000 feet south and 3,170 feet east of the northwest corner of sec. 13,
T. 3 N., R. 33 W.

\<@23\>A---0 to 3 inches; dark grayish brown (10YR 4/2) loamy sand; weak
fine granular structure; very friable; common medium, fine, and very
fine roots; strongly acid; clear smooth boundary.

\<@33\>E1---3 to 16 inches; yellowish brown (10YR 5/6) loamy sand; weak
coarse subangular blocky structure; very friable; few medium and fine
roots; strongly acid; gradual wavy boundary.

\<@33\>E2---16 to 34 inches; brownish yellow (10YR 6/6) loamy sand; weak
coarse subangular blocky structure; very friable; strongly acid; gradual
wavy boundary.

\<@33\>E3---34 to 54 inches; brownish yellow (10YR 6/6) loamy sand; weak
coarse subangular blocky structure; very friable; common medium faint
very pale brown (10YR 7/3) iron depletions; common medium faint
yellowish brown (10YR 5/4) masses of iron accumulation; strongly acid;
clear wavy boundary.

\<@33\>Btv---54 to 80 inches; 25 percent yellow (10YR 7/6), 25 percent
light gray (10YR 7/2), 20 percent strong brown (7.5YR 5/8), 15 percent
pale yellow (2.5Y 7/4), and 15 percent red (10R 4/6) sandy clay loam;
moderate medium subangular blocky structure; firm; few faint clay films
on faces of peds; about 12 percent, by volume, firm and brittle masses
of plinthite; about 4 percent, by volume, rounded quartzite pebbles;
areas of yellow, strong brown, and red are masses of iron accumulation;
areas of light gray are iron depletions; strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction is very strongly
acid or strongly acid throughout the profile, except in areas where lime
has been applied.

\<@32\>The A or Ap horizon has hue of 10YR, value of 3 to 5, and chroma
of 1 to 3.

\<@32\>The E horizon has hue of 10YR, value of 5 to 7, and chroma of 3
to 8. In many pedons, it has few to common, fine to coarse streaks or
pockets of whitish or grayish uncoated sand. It has few or common
redoximorphic accumulations in shades of yellow, olive, brown, and red
in the lower part. The quantity of redoximorphic depletions in shades of
brown and gray ranges from none to common below a depth of 40 inches.
The texture is loamy sand.

\<@32\>The Btv horizon commonly has no dominant matrix color and is
multicolored in shades of brown, red, yellow, and gray. In some pedons,
however, it has hue of 10YR or 7.5YR, value of 5 or 6, and chroma of 4
to 8. It has few to many masses of iron accumulation in shades of
yellow, brown, or red and iron depletions in shades of brown and gray.
It is sandy loam, fine sandy loam, or sandy clay loam.

\<@37\>Corolla Series

\<@32\>The Corolla series consists of very deep, somewhat poorly drained
soils that formed in thick deposits of marine sands that have been
reworked by wind and wave action. These soils are on the lower parts of
dunes and in shallow swales between dunes on the barrier islands and
near the coastal beaches on the mainland. The seasonal high water table
is influenced by daily tidal fluctuations. In most years, it is at a
depth of 1-1/2 to 3 feet throughout the year. These soils are subject to
rare flooding. Slopes range from 2 to 6 percent. These soils are
thermic, uncoated Aquic Quartzipsamments.

\<@32\>Corolla soils are geographically associated with Dirego,
Duckston, Kureb, Newhan, and Resota soils. The very poorly drained
Dirego soils are in tidal marshes and have a thick, histic epipedon. The
poorly drained Duckston soils are in lower positions than the Corolla
soils on flats and in swales between dunes. The excessively drained
Kureb and moderately well drained Resota soils are in the higher
positions and have spodic materials in the subsoil. The excessively
drained Newhan soils are in the higher positions on the dunes.

\<@32\>Typical pedon of Corolla sand, in an area of Newhan-Corolla
complex, rolling, rarely flooded; in Big Lagoon State Recreation Area,
about 2,640 feet south and 675 feet west of the northeast corner of sec.
13, T. 3 S., R. 32 W.

\<@23\>A---0 to 5 inches; grayish brown (10YR 5/2) sand; single grained;
loose; few fine roots; moderately acid; clear wavy boundary.

\<@33\>C1---5 to 28 inches; very pale brown (10YR 7/3) sand; single
grained; loose; common medium distinct brown (10YR 4/3) streaks of
organic stains; moderately acid; clear wavy boundary.

\<@33\>C2---28 to 40 inches; white (N 8/0) sand; single grained; loose;
common fine prominent strong brown (7.5YR 5/8) masses of iron
accumulation with sharp boundaries throughout the matrix; common medium
prominent brown (10YR 4/3) streaks of organic stains; moderately acid;
gradual wavy boundary.

\<@33\>C3---40 to 48 inches; white (10YR 8/1) sand; single grained;
loose; common fine prominent yellowish red (5YR 5/8) masses of iron
accumulation with sharp boundaries throughout the matrix; moderately
acid; gradual wavy boundary.

\<@33\>C4---48 to 80 inches; light gray (10YR 7/1) sand; single grained;
loose; common black sand grains; moderately acid.

\<@8\>The combined thickness of the sandy sediments is more than 80
inches. Reaction ranges from moderately acid to slightly alkaline
throughout the profile. In many pedons, the profile contains dark sand
grains of ilmenite or other dark colored minerals.

\<@32\>The A horizon has hue of 10YR or 2.5Y, value of 3 to 7, and
chroma of 1 to 3; or it is neutral in hue and has value of 3 to 7.

\<@32\>The upper part of the C horizon has hue of 10YR or 2.5Y, value of
4 to 7, and chroma of 3 or 4. It has few or common masses of iron
accumulation in shades of red, yellow, and brown. The lower part has hue
of 10YR or 2.5Y, value of 4 to 8, and chroma of 1 or 2; or it is neutral
in hue and has value of 7 or 8.

\<@37\>Cowarts Series

\<@32\>The Cowarts series consists of very deep, well drained soils that
formed in loamy marine sediments. These soils are on side slopes of
ridges in the uplands. In most years, the seasonal high water table is
below a depth of 6 feet throughout the year. Slopes are short and
complex and range from 12 to 18 percent. These soils are fine-loamy,
kaolinitic, thermic Typic Kanhapludults.

\<@32\>Cowarts soils are geographically associated with Lakeland,
Maubila, Notcher, Poarch, and Troup soils. The Lakeland soils are on
summits and are sandy throughout. The Maubila soils are in positions
similar to those of the Cowarts soils and have a clayey argillic
horizon. The Notcher and Poarch soils are on summits and shoulder slopes
and have significant accumulations of plinthite in the lower part of the
subsoil. Also, Poarch soils are coarse-loamy. The Troup soils are on
summits or in positions similar to those of the Cowarts soils on side
slopes and have a thick, sandy epipedon.

\<@32\>Typical pedon of Cowarts sandy loam, in an area of Cowarts-Troup
complex, 12 to 18 percent slopes; about 1,670 feet south and 2,085 feet
east of the northwest corner of sec. 15, T. 4 N., R. 32 W.

\<@23\>A---0 to 4 inches; dark grayish brown (10YR 4/2) sandy loam; weak
fine granular structure; very friable; many medium and fine roots;
strongly acid; clear wavy boundary.

\<@33\>BE---4 to 9 inches; strong brown (7.5YR 5/6) sandy loam; weak
fine subangular blocky structure; very friable; common medium and fine
roots; strongly acid; clear wavy boundary.

\<@33\>Bt1---9 to 22 inches; strong brown (7.5YR 5/8) sandy clay loam;
moderate medium subangular blocky structure; friable; few medium and
fine roots; few faint clay films on faces of peds; strongly acid;
gradual wavy boundary.

\<@33\>Bt2---22 to 32 inches; strong brown (7.5YR 5/8) sandy clay loam;
moderate medium subangular blocky structure; friable; few faint clay
films on faces of peds; common medium distinct red (2.5YR 4/8) masses of
iron accumulation; common medium distinct light brownish gray (10YR 6/2)
iron depletions; the redoximorphic features are assumed to be relict
features; strongly acid; gradual wavy boundary.

\<@33\>BC---32 to 40 inches; strong brown (7.5YR 5/8) sandy loam; weak
coarse subangular blocky structure; friable; common medium distinct
yellowish red (5YR 5/8) and red (2.5YR 4/8) masses of iron accumulation;
common medium distinct light brownish gray (10YR 6/2) and grayish brown
(10YR 5/2) iron depletions with gradual boundaries throughout the
matrix; strongly acid; gradual wavy boundary.

\<@33\>C---40 to 80 inches; strong brown (7.5YR 5/8) sandy loam;
massive; very friable; common thin strata of loamy sand; common medium
distinct brownish yellow (10YR 6/6), yellowish red (5YR 5/8), and red
(2.5YR 4/8) masses of iron accumulation; common medium distinct light
brownish gray (10YR 6/2) and grayish brown (10YR 5/2) iron depletions
with gradual boundaries throughout the matrix; strongly acid.

\<@8\>The solum ranges from 18 to 40 inches in thickness. Reaction is
very strongly acid or strongly acid throughout the profile, except for
the surface layer in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 7.5YR or 10YR, value of 3 or 4,
and chroma of 2 to 4.

\<@32\>The BE horizon, where present, has hue of 7.5YR or 10YR, value of
5 or 6, and chroma of 4 to 8. It is sandy loam or fine sandy loam.

\<@32\>The Bt horizon commonly has hue of 7.5YR or 10YR, value of 5 or
6, and chroma of 4 to 8. In some pedons, however, it has hue of 5YR,
value of 5 or 6, and chroma of 4 to 8. It is sandy loam, fine sandy
loam, or sandy clay loam. Redoximorphic accumulations, if present, are
in shades of yellow, olive, brown, and red and are assumed to be relict
features.

\<@32\>The BC horizon, where present, has hue of 10YR to 5YR, value of 4
to 8, and chroma of 3 to 8; or it does not have a dominant matrix color
and is multicolored in shades of red, brown, yellow, and gray. The
texture ranges from sandy loam to sandy clay.

\<@32\>The C horizon, or the Cd horizon where present, has the same
range in hue, value, and chroma as the BC horizon. The C horizon is
commonly layered and pocketed with finer- and coarser-textured
sediments. The texture ranges from loamy sand to sandy clay loam.

\<@37\>Croatan Series

\<@32\>The Croatan Series consists of very deep, very poorly drained
soils that formed in highly decomposed plant materials and the
underlying loamy and sandy sediments. These soils are in depressions in
the coastal lowlands. The seasonal high water table ranges from 1 foot
above the surface to a depth of 1/2 foot from December through July in
most years. Slopes are less than 1 percent. These soils are loamy,
siliceous, dysic, thermic Terric Medisaprists.

\<@32\>Croatan soils are geographically associated with Dorovan,
Hurricane, Leon, and Pickney soils in the southwestern part of the
county and with Escambia and Robertsdale soils in the central and
northern parts. All of the associated soils, except the Dorovan soils,
are in higher positions than the Croatan soils and are mineral soils.
The Dorovan soils are in lower positions than the Croatan soils and have
a histic epipedon that is more than 51 inches thick.

\<@32\>Typical pedon of Croatan muck, depressional; about 665 feet west
and 1,985 feet south of the northeast corner of sec. 3, T. 1 S., R. 31
W.

\<@23\>Oa1---0 to 15 inches; black (10YR 2/1) muck, rubbed and unrubbed;
less than 5 percent fiber rubbed and unrubbed; common medium, fine, and
very fine roots; about 95 percent organic matter; extremely acid;
gradual wavy boundary.

\<@33\>Oa2---15 to 25 inches; dark brown (7.5YR 3/2) muck, rubbed and
unrubbed; less than 5 percent fiber rubbed and unrubbed; few medium,
fine, and very fine roots; about 95 percent organic matter; extremely
acid; gradual wavy boundary.

\<@33\>2Ag---25 to 33 inches; dark grayish brown (10YR 4/2) loam;
massive; very friable; estimated 10 percent organic matter; extremely
acid; gradual wavy boundary.

\<@33\>2Cg1---33 to 50 inches; gray (10YR 6/1) sandy loam; massive; very
friable; extremely acid; gradual wavy boundary.

\<@33\>2Cg2---50 to 60 inches; gray (10YR 6/1) loamy sand; massive; very
friable; extremely acid; gradual wavy boundary.

\<@33\>2Cg3---60 to 80 inches; 60 percent gray (10YR 6/1) and 40 percent
dark gray (10YR 4/1) sand; massive; very friable; extremely acid.

\<@8\>The combined thickness of the organic layers ranges from 16 to 51
inches. The O horizon is ultra acid or extremely acid. The 2A and 2C
horizons range from extremely acid to slightly acid. Woody materials
make up less than 10 percent of the O horizon. The content of fiber in
the O horizon ranges from 3 to 30 percent unrubbed and is less than 10
percent rubbed.

\<@32\>The Oa horizon has hue of 10YR or 7.5YR, value of 2 or 3, and
chroma of 1 or 2.

\<@32\>The 2Ag horizon has hue of 10YR or 2.5Y, value of 2 to 7, and
chroma of 1 or 2. It is loam, fine sandy loam, sandy loam, or mucky
sandy loam.

\<@32\>The 2Cg horizon has hue of 10YR, 2.5Y, 5GY, or 5G; value of 2 to
7; and chroma of 1 or 2. The texture ranges from sand to clay loam.

\<@37\>Dirego Series

\<@32\>The Dirego series consists of very deep, very poorly drained
organic soils that formed in highly decomposed plant materials and the
underlying sandy sediments. These soils are in tidal marshes on the
barrier islands and adjacent to the coastline. Dirego soils have a high
water table within a depth of 1/2 foot throughout the year and are
subject to daily flooding by the tides. Slopes are less than 1 percent.
These soils are sandy or sandy-skeletal, siliceous, euic, thermic Terric
Sulfisaprists.

\<@32\>Dirego soils are geographically associated with Corolla,
Duckston, Leon, Newhan, and Pickney soils. All of the associated soils
are in higher positions than the Dirego soils and are mineral soils.

\<@32\>Typical Pedon of Dirego muck, in an area of Dirego muck, tidal;
on Santa Rosa Island, about 2.0 miles east of Big Sabine Point and 0.7
mile north of County Road 399; lat. 30 degrees 21 minutes 32 seconds N.
and long. 87 degrees 00 minutes 51 seconds W.

\<@23\>Oa1---0 to 8 inches; very dark brown (10YR 2/2) muck; less than
10 percent fiber rubbed and unrubbed; many medium and fine roots; strong
odor of hydrogen sulfide; slightly acid when wet, extremely acid when
dry; gradual smooth boundary.

\<@33\>Oa2---8 to 35 inches; black (10YR 2/1) muck; less than 5 percent
fiber rubbed and unrubbed; slightly acid when wet, extremely acid when
dry; clear smooth boundary.

\<@33\>2Cg1---35 to 43 inches; dark grayish brown (10YR 4/2) fine sand;
single grained; loose; slightly acid when wet, extremely acid when dry;
gradual wavy boundary.

\<@33\>2Cg2---43 to 80 inches; grayish brown (10YR 5/2) fine sand;
single grained; loose; slightly acid when wet, extremely acid when dry.

\<@8\>The organic material is dominantly sapric. When the Oa horizon is
in its natural wet condition, reaction is slightly acid or neutral. When
it is dry, reaction is extremely acid or ultra acid. The 2Cg horizon is
moderately acid or slightly acid when wet.

\<@32\>The Oa horizon has hue of 5YR to 10YR, value of 2 or 3, and
chroma of 1 or 2; or it is neutral in hue and has value of 2 or 3.

\<@32\>The 2Cg horizon has hue of 7.5YR to 5Y, value of 2 to 7, and
chroma of 1 or 2; or it is neutral in hue and has value of 2 to 8. It is
loamy fine sand, fine sand, sand, mucky fine sand, or mucky sand. In
some pedons, the horizon has thin subhorizons of fine sandy loam; but
the average texture of the mineral part of the control section is loamy
fine sand or fine sand.

\<@37\>Dorovan Series

\<@32\>The Dorovan series consists of very deep, very poorly drained
organic soils that formed in highly decomposed remains of woody and
herbaceous plants. These soils are in depressions on nearly level flood
plains along streams and rivers. The seasonal high water table ranges
from 2 feet above the surface to a depth of 1/2 foot from December
through July in most years. Slopes are less than 1 percent. These soils
are dysic, thermic Typic Medisaprists.

\<@32\>Dorovan soils are geographically associated with Fluvaquents and
Croatan, Mantachie, Pelham, and Yemassee soils. The Croatan soils are in
positions similar to those of the Dorovan soils and have loamy or sandy
sediments within a depth of 51 inches. The Fluvaquents and Mantachie
soils are in slightly higher positions than the Dorovan soils on flood
plains and are mineral soils. The Pelham and Yemassee soils are in
higher positions than the Dorovan soils on terraces and are mineral
soils.

\<@32\>Typical pedon of Dorovan muck, in an area of Dorovan muck and
Fluvaquents, frequently flooded; on the flood plains along the Escambia
River, about 1,500 feet south and 1,170 feet east of the northwest
corner of sec. 19, T. 2 N., R. 30 W.

\<@23\>Oa1---0 to 8 inches; dark reddish brown (5YR 3/2) muck; about 25
percent fiber unrubbed, 5 percent rubbed; many medium and fine roots;
very strongly acid; gradual wavy boundary.

\<@33\>Oa2---8 to 45 inches; black (5YR 2/1) muck; about 10 percent
fiber unrubbed, 2 percent rubbed; common medium and fine roots; very
strongly acid; gradual wavy boundary.

\<@33\>Oa3---45 to 80 inches; black (N 2/0) muck; about 10 percent fiber
unrubbed, 2 percent rubbed; very strongly acid.

\<@8\>The combined thickness of the organic material ranges from 51 to
more than 80 inches. Reaction is extremely acid or very strongly acid
throughout the profile.

\<@32\>The Oa horizon has hue of 5YR to 10YR, value of 2 or 3, and
chroma of 1 to 3; or it is neutral in hue and has value of 2 or 3. The
content of fiber is generally less than 30 percent unrubbed and less
than 15 percent rubbed.

\<@32\>The 2Cg horizon, where present, is neutral in hue and has value
of 2.5 to 6; or it has hue of 10YR, 2.5Y, or 5Y, value of 2 to 5, and
chroma of 1 or 2. It is sand, fine sand, loamy sand, loamy fine sand,
sandy loam, fine sandy loam, clay, or their mucky analogues.

\<@37\>Duckston Series

\<@32\>The Duckston series consists of very deep, poorly drained soils
that formed in sandy marine sediments. These soils are on flats and in
swales between dunes. They are on the barrier islands and adjacent to
the coastal beaches on the mainland. The seasonal high water table is
influenced by daily tidal fluctuations. In most years, it is within a
depth of 1/2 foot throughout the year. Duckston soils are subject to
occasional or frequent flooding for brief periods throughout the year.
Slopes range from 0 to 2 percent. These soils are siliceous, thermic
Typic Psammaquents.

\<@32\>Duckston soils are geographically associated with Corolla,
Dirego, and Newhan soils. The somewhat poorly drained Corolla and
excessively drained Newhan soils are in higher positions than the
Duckston soils on dunes adjacent to the Duckston soils. The very poorly
drained Dirego soils are in tidal marshes and are organic soils.

\<@32\>Typical pedon of Duckston sand, frequently flooded; in Big Lagoon
State Recreation Area, about 2,670 feet south and 670 feet west of the
northeast corner of sec. 13, T. 3 S., R. 32 W.

\<@23\>Oa---0 to 1 inch; black (10YR 2/1) muck; less than 5 percent
fiber rubbed and unrubbed; common fine roots; slightly acid; clear wavy
boundary.

\<@33\>A---1 to 4 inches; very dark gray (10YR 3/1) sand; weak medium
granular structure; very friable; common fine roots; common medium faint
very dark grayish brown (10YR 3/2) streaks of organic stains; common
thin streaks and pockets of light gray (10YR 7/1) clean sand; slightly
acid; clear wavy boundary.

\<@33\>Cg1---4 to 12 inches; light gray (10YR 7/2) sand; single grained;
loose; many coarse faint pale brown (10YR 6/3) masses of iron
accumulation; strong odor of hydrogen sulfide; slightly acid; gradual
wavy boundary.

\<@33\>Cg2---12 to 50 inches; light gray (10YR 7/2) sand; single
grained; loose; slightly acid; gradual wavy boundary.

\<@33\>Cg3---50 to 80 inches; white (10YR 8/2) sand; single grained;
loose; common black sand grains; slightly acid.

\<@8\>The combined thickness of the sandy sediments is more than 80
inches. Reaction ranges from extremely acid to moderately alkaline
throughout the profile. Small fragments of mollusk shells are in some
pedons.

\<@32\>The Oa horizon, or the Oe horizon where present, has hue of 10YR,
value of 2 or 3, and chroma of 1 or 2. It is less than 8 inches thick.

\<@32\>The A horizon has hue of 10YR to 5Y, value of 3 to 5, and chroma
of 1 or 2; or it is neutral in hue and has value of 2.5 to 5.

\<@32\>The Cg horizon commonly has hue of 10YR to 5Y, value of 5 to 8,
and chroma of 1 or 2. In some pedons, however, it has hue of 5GY, value
of 5 or 6, and chroma of 1. In some pedons, it has redoximorphic
accumulations in shades of yellow, olive, brown, and red and
redoximorphic depletions in shades of brown and gray.

\<@37\>Emory Series

\<@32\>The Emory series consists of very deep, well drained soils that
formed in loamy sediments. These soils are in shallow depressions on
broad, nearly level summits in the uplands. The seasonal high water
table is below a depth of 6 feet. Most areas, however, are subject to
ponding for 2 to 7 days following periods of heavy rainfall. Slopes are
0 to 1 percent.

\<@32\>The Emory soils in this survey area are taxadjuncts to the Emory
series because they do not have the high content of silt and dark
surface colors that are definitive for the series. These differences,
however, do not significantly affect the use, management, or
interpretations of the soils. The soils of the Emory series are
classified as fine-silty, siliceous, active, thermic Fluventic Umbric
Dystrochrepts. In this survey area, the Emory soils are fine-loamy,
siliceous, subactive, thermic Rhodic Paleudults.

\<@32\>Emory soils are geographically associated with Bama, Perdido,
Poarch, and Red Bay soils. The Bama and Red Bay soils are in slightly
higher, more convex positions than the Emory soils and are not subject
to ponding. The Perdido and Poarch soils are in higher, more convex
positions, are coarse-loamy, and have a significant accumulation of
plinthite in the lower part of the subsoil.

\<@32\>Typical pedon of Emory fine sandy loam, ponded; about 200 feet
east and 600 feet north of the southwest corner of sec. 14, T. 5 N., R.
32 W.

\<@23\>Ap---0 to 10 inches; brown (7.5YR 4/4) fine sandy loam; moderate
fine granular structure; very friable; common medium roots and many fine
and very fine roots; strongly acid; clear wavy boundary.

\<@33\>Bt1---10 to 15 inches; dusky red (10R 3/4) sandy clay loam; weak
medium subangular blocky structure; friable; common medium roots and
many fine and very fine roots; few faint clay films on faces of peds;
strongly acid; clear wavy boundary.

\<@33\>Bt2---15 to 24 inches; dark red (10R 3/6) sandy clay loam;
moderate medium subangular blocky structure; friable; few fine roots;
few faint clay films on faces of peds; extremely acid; gradual wavy
boundary.

\<@33\>Bt3---24 to 80 inches; dark red (10R 3/6) sandy clay loam;
moderate medium subangular blocky structure; friable; few fine roots;
few faint clay films on faces of peds; extremely acid.

\<@8\>The solum is more than 60 inches thick. Reaction ranges from
extremely acid to moderately acid in the Ap horizon, except in areas
where lime has been applied, and from extremely acid to strongly acid in
the Bt horizon.

\<@32\>The Ap horizon has hue of 2.5YR to 10YR, value of 3 or 4, and
chroma of 2 to 4.

\<@32\>The BA horizon, where present, has hue of 2.5YR to 7.5YR, value
of 3 or 4, and chroma of 4 to 6. It is sandy loam or sandy clay loam.

\<@32\>The Bt horizon has hue of 10R or 2.5YR, value of 3, and chroma of
4 to 6. It is commonly sandy clay loam; in some pedons, however, it is
sandy clay in the lower part. Also, in some pedons, it has a thin
subhorizon of sandy loam in the upper part.

\<@37\>Escambia Series

\<@32\>The Escambia series consists of very deep, somewhat poorly
drained soils that formed in loamy sediments. These soils are in
slightly convex positions on broad, nearly level flats and summits. The
seasonal high water table is at a depth of 1-1/2 to 2-1/2 feet from
December through April in most years. Slopes range from 0 to 2 percent.
These soils are coarse-loamy, siliceous, semiactive, thermic Plinthaquic
Paleudults.

\<@32\>Escambia soils are geographically associated with Grady, Notcher,
Poarch, and Robertsdale soils. The poorly drained Grady soils are in
depressions and have a clayey argillic horizon. The moderately well
drained Notcher and well drained Poarch soils are in slightly higher
positions than the Escambia soils. Robertsdale soils are in positions
similar to those of the Escambia soils and are fine-loamy.

\<@32\>Typical pedon of Escambia fine sandy loam, 0 to 2 percent slopes;
about 415 feet north and 2,085 feet east of the southwest corner of sec.
25, T. 1 S., R. 31 W.

\<@23\>A---0 to 5 inches; very dark grayish brown (2.5Y 3/2) fine sandy
loam; weak medium granular structure; very friable; common medium and
fine roots; very strongly acid; clear smooth boundary.

\<@33\>E---5 to 10 inches; grayish brown (2.5Y 5/2) fine sandy loam;
weak medium granular structure; very friable; common medium and fine
roots; common medium distinct light yellowish brown (10YR 6/4) masses of
iron accumulation; very strongly acid; clear smooth boundary.

\<@33\>Bt---10 to 24 inches; light yellowish brown (10YR 6/4) fine sandy
loam; weak medium subangular blocky structure; very friable; common fine
roots; few faint clay films on faces of peds; common medium faint light
brownish gray (10YR 6/2) iron depletions; few medium prominent strong
brown (7.5YR 5/8) masses of iron accumulation with sharp boundaries
throughout the matrix; very strongly acid; gradual wavy boundary.

\<@33\>Btv1---24 to 48 inches; light yellowish brown (10YR 6/4) fine
sandy loam; weak medium subangular blocky structure; very friable; few
faint clay films on faces of peds; about 3 percent firm and brittle
masses of dark red (2.5YR 3/6) plinthite; common medium faint very pale
brown (10YR 7/4), common medium prominent strong brown (7.5YR 5/8), and
common medium faint brownish yellow (10YR 6/6) masses of iron
accumulation; common medium faint light gray (10YR 7/2) irregularly
shaped iron depletions; very strongly acid; gradual wavy boundary.

\<@33\>Btv2---48 to 60 inches; 35 percent light gray (10YR 7/2), 35
percent brownish yellow (10YR 6/6), and 30 percent strong brown (7.5YR
5/8) fine sandy loam; weak medium subangular blocky structure; very
friable; common faint clay films on faces of peds; about 7 percent firm
and brittle masses of dark red (2.5YR 3/6) plinthite; areas of brownish
yellow and strong brown are masses of iron accumulation; areas of light
gray are iron depletions; very strongly acid; gradual wavy boundary.

\<@33\>Btv3---60 to 80 inches; 30 percent light gray (10YR 7/2), 25
percent brownish yellow (10YR 6/8), 25 percent strong brown (7.5YR 5/8),
and 20 percent red (2.5YR 5/8) fine sandy loam; weak coarse subangular
blocky structure; firm; few faint clay films on faces of peds; about 12
percent firm and brittle masses of dark red (2.5YR 3/6) plinthite; areas
of brownish yellow, strong brown, and red are masses of iron
accumulation; areas of light gray are iron depletions; very strongly
acid.

\<@8\>The solum is more than 60 inches thick. Depth to horizons that
have more than 5 percent plinthite ranges from 20 to 48 inches. Reaction
ranges from extremely acid to strongly acid throughout the profile,
except for surface layer in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 10YR or 2.5Y, value of 3 or 4, and
chroma of 1 or 2.

\<@32\>The E horizon has hue of 10YR or 2.5Y, value of 5 or 6, and
chroma of 2 to 4. It is sandy loam, fine sandy loam, or loam.

\<@32\>The upper part of the Bt horizon has hue of 10YR or 2.5Y, value
of 5 or 6, and chroma of 3 to 8. It has few to many redoximorphic
accumulations in shades of yellow, olive, brown, and red and
redoximorphic depletions in shades of brown and gray. It is fine sandy
loam, sandy loam, or loam.

\<@32\>The lower part of the Bt horizon commonly has no dominant matrix
color and is multicolored in shades of brown, gray, olive, and red; or
it has hue of 10YR to 5Y, value of 5 to 7, and chroma of 3 to 8. It has
common or many redoximorphic accumulations in shades of brown, yellow,
and olive and redoximorphic depletions in shades of brown and gray. It
is fine sandy loam, loam, or sandy clay loam. The content of plinthite
ranges from 5 to about 25 percent, by volume.

\<@37\>Eunola Series

\<@32\>The Eunola series consists of very deep, moderately well drained
soils that formed in loamy and sandy fluvial sediments. These soils are
on low terraces adjacent to major streams and rivers. The seasonal high
water table is at a depth of 1-1/2 to 2-1/2 feet from December through
April in most years. These soils are subject to occasional flooding.
Slopes range from 0 to 5 percent. These soils are fine-loamy, siliceous,
semiactive, thermic Aquic Hapludults.

\<@32\>Eunola soils are geographically associated with Albany, Izagora,
Weston, and Yemassee soils. The Albany, Izagora, and Yemassee soils are
in positions similar to those of the Eunola soils on low terraces. The
Albany soils are somewhat poorly drained and have a thick, sandy
epipedon. The Izagora soils do not have a significant decrease in clay
content within a depth of 60 inches. The Yemassee soils are somewhat
poorly drained. The poorly drained Weston soils are in shallow
drainageways.

\<@32\>Typical pedon of Eunola fine sandy loam, 0 to 2 percent slopes,
occasionally flooded; about 625 feet south of Fletcher Creek and 935
feet east of the railroad tracks, in a wooded area near Cotton Lake
Road; about 1.25 miles east and 1.8 miles south of the northwest corner
of Spanish Land Grant 2, T. 3 N., R. 31 W.

\<@23\>A---0 to 5 inches; dark brown (10YR 3/3) fine sandy loam;
moderate medium granular structure; very friable; common medium and fine
roots; strongly acid; clear smooth boundary.

\<@33\>BE---5 to 10 inches; yellowish brown (10YR 5/4) fine sandy loam;
weak fine subangular blocky structure; very friable; common medium and
fine roots; strongly acid; clear smooth boundary.

\<@33\>Bt1---10 to 18 inches; yellowish brown (10YR 5/6) sandy loam;
moderate medium subangular blocky structure; friable; common fine roots;
few faint clay films on faces of peds; strongly acid; clear smooth
boundary.

\<@33\>Bt2---18 to 28 inches; yellowish brown (10YR 5/6) sandy clay
loam; moderate medium subangular blocky structure; friable; few fine
roots; few faint clay films on faces of peds; common coarse distinct
very pale brown (10YR 7/3) and common medium distinct light gray (10YR
7/2) areas of iron depletion with sharp boundaries throughout the
matrix; strongly acid; clear wavy boundary.

\<@33\>Bt3---28 to 38 inches; yellowish brown (10YR 5/8) sandy clay
loam; moderate medium subangular blocky structure; friable; few faint
clay films on faces of peds; common medium distinct very pale brown
(10YR 7/3) and common medium distinct light gray (10YR 7/2) areas of
iron depletion with sharp boundaries throughout the matrix; strongly
acid; gradual wavy boundary.

\<@33\>Bt4---38 to 50 inches; yellowish brown (10YR 5/6) sandy clay
loam; moderate medium subangular blocky structure; friable; few faint
clay films on faces of peds; common medium distinct strong brown (7.5YR
5/8) masses of iron accumulation; common medium distinct very pale brown
(10YR 7/3) and light gray (10YR 7/2) irregularly shaped iron depletions
with sharp boundaries throughout the matrix; strongly acid; clear wavy
boundary.

\<@33\>2C1---50 to 58 inches; yellowish brown (10YR 5/6) loamy sand;
massive; very friable; common medium distinct strong brown (7.5YR 5/8)
masses of iron accumulation with sharp boundaries throughout the matrix;
strongly acid; gradual wavy boundary.

\<@33\>2C2---58 to 80 inches; yellowish brown (10YR 5/6) sand; single
grained; loose; common medium distinct strong brown (7.5YR 5/8) masses
of iron accumulation; common medium faint pale brown (10YR 6/3)
irregularly shaped iron depletions with sharp boundaries throughout the
matrix; strongly acid.

\<@8\>The solum is more than 40 inches thick. Reaction is very strongly
acid or strongly acid throughout the profile, except for the surface
layer in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 10YR or 2.5Y, value of 3 or 4, and
chroma of 1 to 4.

\<@32\>The BE horizon, which is present in most pedons, has hue of 7.5YR
or 10YR, value of 5 or 6, and chroma of 4 to 8. It is sandy loam or fine
sandy loam.

\<@32\>The upper part of the Bt horizon has hue of 7.5YR or 10YR, value
of 5 or 6, and chroma of 4 to 8. The quantity of redoximorphic
accumulations in shades of yellow, olive, brown, and red and
redoximorphic depletions in shades of brown and gray ranges from none to
common. The texture is sandy loam, sandy clay loam, or clay loam.

\<@32\>The lower part of the Bt horizon has hue of 10YR or 2.5Y, value
of 4 to 6, and chroma of 4 to 8; or it has no dominant matrix color and
is multicolored in shades of brown, yellow, gray, and red. It has few to
many redoximorphic accumulations in shades of brown, yellow, or red and
redoximorphic depletions in shades of brown or gray. It is sandy clay
loam, clay loam, or sandy clay.

\<@32\>The 2C horizon has a range in color similar to that of the lower
part of the Bt horizon. The texture is sand, loamy sand, sandy loam, or
fine sandy loam. In many pedons, the 2C horizon has strata of finer- and
coarser-textured sediments.

\<@37\>Foxworth Series

\<@32\>The Foxworth series consists of very deep, moderately well
drained soils that formed in sandy sediments. These soils are on low
ridges and on knolls. They are in the coastal lowlands. The seasonal
high water table is at a depth of 3-1/2 to 6 feet from December through
April in most years. Slopes range from 0 to 5 percent. These soils are
thermic, coated Typic Quartzipsamments.

\<@32\>Foxworth soils are geographically associated with Albany,
Hurricane, and Lakeland soils. The somewhat poorly drained Albany and
Hurricane soils are in slightly lower positions than the Foxworth soils.
The Albany soils have a loamy argillic horizon within a depth of 40 to
80 inches. The Hurricane soils have a spodic horizon below a depth of 50
inches. The excessively drained Lakeland soils are in slightly higher
positions than the Foxworth soils.

\<@32\>Typical pedon of Foxworth sand, 0 to 5 percent slopes; about 50
feet north and 50 feet west of the southeast corner of sec. 7, T. 3 S.,
R. 32 W.

\<@23\>A---0 to 6 inches; dark brown (10YR 3/3) sand; weak fine granular
structure; very friable; common medium and fine roots; very strongly
acid; clear smooth boundary.

\<@33\>C1---6 to 15 inches; yellowish brown (10YR 5/6) sand; single
grained; loose; common medium and fine roots; few thin streaks and fine
pockets of uncoated sand; very strongly acid; clear smooth boundary.

\<@33\>C2---15 to 45 inches; yellowish brown (10YR 5/6) sand; single
grained; loose; few thin streaks and fine pockets of uncoated sand; very
strongly acid; gradual wavy boundary.

\<@33\>C3---45 to 55 inches; light yellowish brown (10YR 6/4) sand;
single grained; loose; common medium prominent yellowish red (5YR 5/8)
masses of iron accumulation; few medium faint light brownish gray (10YR
6/2) iron depletions with gradual boundaries throughout the matrix; very
strongly acid; gradual wavy boundary.

\<@33\>C4---55 to 80 inches; white (10YR 8/2) sand; single grained;
loose; common medium prominent yellowish red (5YR 5/8) masses of iron
accumulation; very strongly acid.

\<@8\>Reaction ranges from very strongly acid to slightly acid
throughout the profile, except in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 7.5YR or 10YR, value of 3 or 4,
and chroma of 1 to 3.

\<@32\>The upper part of the C horizon has hue of 7.5YR or 10YR, value
of 5 or 6, and chroma of 3 to 8. It is sand or fine sand. The lower part
has hue of 7.5YR or 10YR, value of 5 to 8, and chroma of 1 to 6 and has
few or common redoximorphic accumulations in shades of yellow, olive,
brown, and red and redoximorphic depletions in shades of brown and gray.
It is sand or fine sand.

\<@37\>Garcon Series

\<@32\>The Garcon series consists of very deep, somewhat poorly drained
soils that formed in sandy and loamy fluvial sediments. These soils are
on low terraces adjacent to major streams and rivers. The seasonal high
water table is at a depth of 1-1/2 to 3 feet from December through April
in most years. These soils are subject to occasional flooding. Slopes
commonly are less than 2 percent but range from 0 to 5 percent. These
soils are loamy, siliceous, semiactive, thermic Aquic Arenic Hapludults.

\<@32\>Garcon soils are geographically associated with Fluvaquents and
Bigbee, Mantachie, and Yemassee soils. Bigbee soils are on high parts of
natural levees and are sandy throughout the profile. The very poorly
drained Fluvaquents and the loamy Mantachie soils are on flood plains
adjacent to the Garcon soils. The Yemassee soils are in positions
similar to those of the Garcon soils and do not have a thick, sandy
epipedon.

\<@32\>Typical pedon of Garcon loamy fine sand, in an area of
Garcon-Bigbee-Yemassee complex, 0 to 5 percent slopes, occasionally
flooded; about 2,100 feet north and 2,700 feet east of the southwest
corner of sec. 3, T. 1 S., R. 31 W.

\<@23\>A---0 to 5 inches; very dark gray (10YR 3/1) loamy fine sand;
weak fine granular structure; very friable; common medium and fine
roots; strongly acid; abrupt wavy boundary.

\<@33\>E1---5 to 14 inches; light yellowish brown (2.5Y 6/4) loamy fine
sand; weak coarse subangular blocky structure; very friable; common fine
roots; few fine prominent strong brown (7.5YR 5/6) masses of iron
accumulation; strongly acid; clear smooth boundary.

\<@33\>E2---14 to 27 inches; light yellowish brown (2.5Y 6/4) loamy fine
sand; weak coarse subangular blocky structure; very friable; few fine
roots; common medium prominent strong brown (7.5YR 5/6) masses of iron
accumulation; common medium distinct light gray (10YR 7/2) irregularly
shaped iron depletions with sharp boundaries throughout the matrix;
strongly acid; clear smooth boundary.

\<@33\>Bt---27 to 38 inches; brownish yellow (10YR 6/6) fine sandy loam;
weak medium subangular blocky structure; friable; few faint clay films
on faces of peds; common medium prominent strong brown (7.5YR 5/6)
masses of iron accumulation; common medium distinct light gray (10YR
7/2) irregularly shaped iron depletions with diffuse boundaries
throughout the matrix; strongly acid; clear wavy boundary.

\<@33\>Btg1---38 to 47 inches; light brownish gray (10YR 6/2) sandy clay
loam; moderate medium subangular blocky structure; friable; few faint
clay films on faces of peds; many medium faint light gray (10YR 7/2) and
gray (10YR 5/1) irregularly shaped iron depletions with diffuse
boundaries; common medium distinct dark yellowish brown (10YR 4/4) and
common medium prominent strong brown (7.5YR 5/6) masses of iron
accumulation with diffuse boundaries; strongly acid; gradual wavy
boundary.

\<@33\>Btg2---47 to 57 inches; light brownish gray (10YR 6/2) fine sandy
loam; weak coarse subangular blocky structure; friable; few faint clay
films on faces of peds; many medium faint light gray (10YR 7/2) and gray
(10YR 5/1) irregularly shaped iron depletions with diffuse boundaries;
common medium distinct dark yellowish brown (10YR 4/4) and common medium
prominent strong brown (7.5YR 5/6) masses of iron accumulation with
diffuse boundaries; strongly acid; clear wavy boundary.

\<@33\>Cg---57 to 80 inches; white (10YR 8/1) fine sand; single grained;
loose; common medium prominent brownish yellow (10YR 6/6) masses of iron
accumulation with diffuse boundaries throughout the matrix; strongly
acid.

\<@8\>The solum ranges from 45 to 60 inches in thickness. Reaction is
very strongly acid or strongly acid throughout the profile, except in
areas where lime has been applied.

\<@32\>The A horizon has hue of 10YR, value of 2 to 4, and chroma of 1
or 2.

\<@32\>The E horizon has hue of 10YR or 2.5Y, value of 5 to 7, and
chroma of 3 to 6. It has few or common redoximorphic accumulations in
shades of brown, yellow, and red and redoximorphic depletions in shades
of brown and gray. It is fine sand, loamy fine sand, or loamy sand.

\<@32\>The Bt horizon has hue of 10YR or 2.5Y, value of 5 or 6, and
chroma of 3 to 6. It has few or common redoximorphic accumulations in
shades of brown, yellow, and red and redoximorphic depletions in shades
of brown and gray. It is sandy loam, fine sandy loam, or sandy clay
loam.

\<@32\>The Btg horizon has hue of 10YR or 2.5Y, value of 5 or 6, and
chroma of 1 or 2. It has common or many redoximorphic accumulations in
shades of brown, yellow, and red and redoximorphic depletions in shades
of brown and gray. It is sandy loam, fine sandy loam, or sandy clay
loam.

\<@32\>The Cg horizon has hue of 10YR or 2.5Y, value of 6 to 8, and
chroma of 1 or 2. It has few to many redoximorphic accumulations in
shades of brown, yellow, and red and redoximorphic depletions in shades
of brown and gray. It is sand or fine sand.

\<@37\>Grady Series

\<@32\>The Grady series consists of very deep, poorly drained soils that
formed in clayey sediments. These soils are in depressions on broad,
nearly level summits in the uplands. The seasonal high water table
ranges from 2 feet above the surface to a depth of 1 foot from December
through July in most years, except in areas that have been drained.
Slopes are 0 to 1 percent. These soils are fine, kaolinitic, thermic
Typic Paleaquults.

\<@32\>Grady soils are geographically associated with Bama, Escambia,
Malbis, and Red Bay soils. The well drained Bama, Malbis, and Red Bay
soils are on convex summits at slightly higher elevations than the Grady
soils. The somewhat poorly drained Escambia soils are in slightly
higher, more convex positions than the Grady soils and are coarse-loamy.

\<@32\>Typical pedon of Grady loam; about 2,700 feet south and 2,580
feet west of the northeast corner of Spanish Land Grant 38, T. 1 S., R.
31 W.

\<@23\>A---0 to 5 inches; very dark grayish brown (10YR 3/2) loam; weak
fine granular structure; very friable; common medium and fine roots;
very strongly acid; clear smooth boundary.

\<@33\>BE---5 to 11 inches; dark grayish brown (10YR 4/2) clay loam;
weak fine subangular blocky structure; friable; few fine roots; common
fine prominent reddish brown (5YR 4/4) masses of iron accumulation with
gradual boundaries; very strongly acid; clear smooth boundary.

\<@33\>Btg1---11 to 26 inches; dark gray (10YR 4/1) clay; moderate
medium subangular blocky structure; firm; few faint clay films on faces
of peds; few fine prominent strong brown (7.5YR 4/6) masses of iron
accumulation with sharp boundaries; very strongly acid; clear wavy
boundary.

\<@33\>Btg2---26 to 47 inches; grayish brown (10YR 5/2) clay; moderate
medium subangular blocky structure; firm; few faint clay films on faces
of peds; common fine prominent strong brown (7.5YR 5/6) masses of iron
accumulation with sharp boundaries; many medium faint light brownish
gray (10YR 6/2) iron depletions with diffuse boundaries throughout the
matrix; very strongly acid; gradual wavy boundary.

\<@33\>Btg3---47 to 54 inches; light brownish gray (2.5Y 6/2) clay;
moderate medium subangular blocky structure; firm; few faint clay films
on faces of peds; common medium faint light gray (5Y 7/2) irregularly
shaped iron depletions with clear boundaries throughout the matrix; very
strongly acid; gradual wavy boundary.

\<@33\>Btg4---54 to 80 inches; light gray (2.5Y 7/2) clay; moderate
medium subangular blocky structure; firm; few faint clay films on faces
of peds; many medium prominent yellowish red (5YR 5/6) and common medium
prominent brown (7.5YR 4/4) masses of iron accumulation with sharp
boundaries; very strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction ranges from
extremely acid to strongly acid throughout the profile, except for the
surface layer in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 10YR to 5Y, value of 2 to 4, and
chroma of 1 or 2; or it is neutral in hue and has value of 2 to 4.

\<@32\>The Eg horizon, where present, has hue of 10YR to 5Y, value of 5
to 7, and chroma of 1 or 2. It is sandy loam, fine sandy loam, or loam.

\<@32\>The BE horizon, where present, has hue of 10YR to 5Y, value of 4
to 6, and chroma of 1 or 2; or it is neutral in hue and has value of 4
to 6. It is sandy clay loam or clay loam.

\<@32\>The Btg horizon has hue of 10YR to 5Y, value of 4 to 7, and
chroma of 1 or 2; or it is neutral in hue and has value of 4 to 7. It
has few to many redoximorphic accumulations in shades of brown, yellow,
or red and redoximorphic depletions in shades of gray. It is clay or
sandy clay.

\<@37\>Hurricane Series

\<@32\>The Hurricane series consists of very deep, somewhat poorly
drained soils that formed in sandy sediments. These soils are on broad
ridges and knolls in the coastal lowlands and on low terraces adjacent
to major streams and rivers. The seasonal high water table is at a depth
of 1-1/2 to 3-1/2 feet from December through April in most years. The
areas on the low terraces are subject to occasional flooding. Slopes
range from 0 to 5 percent. These soils are sandy, siliceous, thermic
Oxyaquic Alorthods.

\<@32\>Hurricane soils are geographically associated with Albany,
Allanton, Foxworth, Leon, and Pottsburg soils. The Albany soils are in
positions similar to those of the Hurricane soils on terraces and do not
have a spodic horizon. The very poorly drained Allanton and poorly
drained Pottsburg soils are on flats in slightly lower positions than
the Hurricane soils. The moderately well drained Foxworth soils are on
higher, more convex knolls than the Hurricane soils and do not have a
spodic horizon. The poorly drained Leon soils are in areas of flatwoods
and have a spodic horizon within a depth of 30 inches.

\<@32\>Typical pedon of Hurricane sand, 0 to 5 percent slopes; about 750
feet west and 2,375 feet south of the northeast corner of sec. 13, T. 3
S., R. 31 W.

\<@23\>A---0 to 5 inches; very dark grayish brown (10YR 3/2) sand; weak
fine granular structure; very friable; common fine and very fine roots;
strongly acid; clear smooth boundary.

\<@33\>E1---5 to 24 inches; yellowish brown (10YR 5/6) sand; single
grained; loose; very friable; few fine roots; strongly acid; clear wavy
boundary.

\<@33\>E2---24 to 38 inches; yellowish brown (10YR 5/6) sand; single
grained; loose; common medium distinct strong brown (7.5YR 5/8) masses
of iron accumulation; common medium distinct light brownish gray (10YR
6/2) iron depletions with clear boundaries throughout the matrix;
strongly acid; clear wavy boundary.

\<@33\>Eg1---38 to 45 inches; light gray (10YR 7/2) sand; single
grained; loose; common medium faint pale brown (10YR 6/3) and common
medium distinct yellowish brown (10YR 5/6) masses of iron accumulation
with clear boundaries throughout the matrix; strongly acid; gradual wavy
boundary.

\<@33\>Eg2---45 to 58 inches; white (10YR 8/2) sand; single grained;
loose; strongly acid; clear smooth boundary.

\<@33\>Bh1---58 to 68 inches; dark reddish gray (5YR 4/2) sand; massive;
very friable; about 80 percent of the sand grains are coated with
organic matter; very strongly acid; gradual smooth boundary.

\<@33\>Bh2---68 to 80 inches; dark reddish brown (5YR 2.5/2) sand;
massive; very friable; about 95 percent of the sand grains are coated
with organic matter; very strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction ranges from
extremely acid to moderately acid throughout the profile, except in
areas where lime has been applied.

\<@32\>The A horizon has hue of 10YR or 2.5Y, value of 3 to 5, and
chroma of 1 to 3.

\<@32\>The E horizon has hue of 10YR or 2.5Y, value of 5 to 8, and
chroma of 2 to 6. In some pedons, it has redoximorphic accumulations in
shades of yellow, olive, brown, and red below a depth of 24 inches. It
is sand or fine sand.

\<@32\>The Eg horizon has hue of 10YR or 2.5Y, value of 5 to 8, and
chroma of 1 or 2. The quantity of redoximorphic accumulations in shades
of yellow, olive, brown, and red ranges from none to common. The texture
is sand or fine sand.

\<@32\>The Bh horizon has hue of 10YR to 5YR, value of 2 to 4, and
chroma of 1 to 4. It is sand, fine sand, or loamy sand. In some pedons,
it is weakly cemented.

\<@37\>Iuka Series

\<@32\>The Iuka series consists of very deep, moderately well drained
soils that formed in stratified loamy and sandy alluvium. These soils
are on the high and intermediate parts of natural levees along flood
plains. The seasonal high water table is at a depth of 1 to 3 feet from
December through April in most years. These soils are subject to
frequent flooding of brief duration. Slopes range from 0 to 2 percent.
These soils are coarse-loamy, siliceous, active, acid, thermic Aquic
Udifluvents.

\<@32\>Iuka soils are geographically associated with Fluvaquents and
Bigbee, Eunola, and Mantachie soils. The Bigbee soils are on the higher
parts of the natural levees and are sandy throughout the profile. The
Eunola soils are on low terraces adjacent to the Iuka soils and have a
loamy argillic horizon. The very poorly drained Fluvaquents and the
somewhat poorly drained Mantachie soils are on the lower parts of the
flood plain.

\<@32\>Typical pedon of Iuka fine sandy loam, frequently flooded; about
2,670 feet east and 1,585 feet north of the southwest corner of sec. 34,
T. 2 N., R. 31 W.

\<@23\>A---0 to 9 inches; very dark grayish brown (10YR 3/2) fine sandy
loam; weak fine granular structure; very friable; common fine roots;
strongly acid; clear wavy boundary.

\<@33\>C1---9 to 20 inches; dark yellowish brown (10YR 4/4) sandy loam;
massive; very friable; common fine roots; common fine faint yellowish
brown (10YR 5/6) masses of iron accumulation; strongly acid; gradual
wavy boundary.

\<@33\>C2---20 to 32 inches; yellowish brown (10YR 5/6) sandy loam;
massive; very friable; few thin strata of loamy fine sand; common fine
distinct grayish brown (10YR 5/2) and pale brown (10YR 6/3) iron
depletions with clear boundaries throughout the matrix; very strongly
acid; gradual wavy boundary.

\<@33\>C3---32 to 58 inches; yellowish brown (10YR 5/6) sandy loam;
massive; very friable; few thin strata of sand and loamy sand; common
medium distinct light brownish gray (10YR 6/2) iron depletions; common
medium prominent yellowish red (5YR 5/8) masses of iron accumulation
with clear boundaries throughout the matrix; very strongly acid; gradual
wavy boundary.

\<@33\>C4---58 to 80 inches; 20 percent light gray (10YR 7/1), 20
percent light brownish gray (10YR 6/2), 20 percent brownish yellow (10YR
6/6), 20 percent yellowish red (5YR 5/8), and 20 percent red (2.5YR 4/8)
sandy loam; massive; very friable; common thin strata of sand and loamy
sand; areas of light gray and light brownish gray are iron depletions;
areas of brownish yellow, yellowish red, and red are masses of iron
accumulation; very strongly acid.

\<@8\>Reaction ranges from extremely acid to strongly acid throughout
the profile, except for the surface layer in areas where lime has been
applied.

\<@32\>The A horizon has hue of 10YR or 7.5YR, value of 3 or 4, and
chroma of 2 to 4.

\<@32\>The upper part of the C horizon has hue of 10YR or 2.5Y, value of
4 to 6, and chroma of 3 to 8. It has few or common redoximorphic
accumulations in shades of yellow, olive, brown, and red and
redoximorphic depletions in shades of brown and gray. It is fine sandy
loam or sandy loam. The quantity of thin strata of finer- or
coarser-textured sediments ranges from none to common.

\<@32\>The lower part of the C horizon has hue of 10YR or 2.5Y, value of
4 to 6, and chroma of 3 to 8; or it does not have a dominant matrix
color and is multicolored in shades of brown, yellow, and red. It is
fine sandy loam, sandy loam, or loamy sand. It has few or common thin
strata of finer- or coarser-textured sediments.

\<@32\>The Cg horizon, where present, has hue of 10YR or 2.5Y, value of
5 or 6, and chroma of 1 or 2. It is fine sandy loam, sandy loam, or
loamy sand. It has few or common thin strata of finer- or
coarser-textured sediments.

\<@37\>Izagora Series

\<@32\>The Izagora series consists of very deep, moderately well drained
soils that formed in loamy and clayey sediments. These soils are on low
terraces adjacent to major streams and rivers. The seasonal high water
table is at a depth of 1-1/2 to 2-1/2 feet from December through April.
These soils are subject to occasional flooding. Slopes range from 0 to 2
percent. These soils are fine-loamy, siliceous, semiactive, thermic
Aquic Paleudults.

\<@32\>Izagora soils are geographically associated with Dorovan, Eunola,
Yemassee, and Weston soils. The very poorly drained Dorovan soils are in
deep sloughs or other depressions and are organic soils. The Eunola
soils are in positions similar those of the Izagora soils and have sandy
substrata within a depth of 60 inches. The poorly drained Weston and
somewhat poorly drained Yemassee soils are in the slightly lower, less
convex positions on the terraces.

\<@32\>Typical pedon of Izagora fine sandy loam, 0 to 2 percent slopes,
occasionally flooded; about 500 feet east and 170 feet south of the
northwest corner of sec. 3, T. 5 N., R. 30 W.

\<@23\>Ap1---0 to 4 inches; dark grayish brown (2.5Y 4/2) fine sandy
loam; weak fine granular structure; very friable; common medium, fine,
and very fine roots; very strongly acid; clear smooth boundary.

\<@33\>Ap2---4 to 8 inches; grayish brown (2.5Y 5/2) fine sandy loam;
weak medium granular structure; very friable; common medium, fine, and
very fine roots; very strongly acid; clear smooth boundary.

\<@33\>E---8 to 10 inches; light yellowish brown (2.5Y 6/4) fine sandy
loam; weak coarse subangular blocky structure; very friable; common fine
and very fine roots; very strongly acid; clear wavy boundary.

\<@33\>Bt1---10 to 18 inches; brownish yellow (10YR 6/6) loam; moderate
medium subangular blocky structure; friable; few fine roots; few faint
clay films on faces of peds; very strongly acid; clear wavy boundary.

\<@33\>Bt2---18 to 28 inches; brownish yellow (10YR 6/6) loam; moderate
medium subangular blocky structure; friable; few faint clay films on
faces of peds; few fine prominent yellowish red (5YR 5/8) masses of iron
accumulation; few fine faint light gray (10YR 7/2) iron depletions with
clear boundaries throughout the matrix; very strongly acid; clear wavy
boundary.

\<@33\>Bt3---28 to 80 inches; 30 percent light gray (10YR 7/1), 30
percent brownish yellow (10YR 6/8), 20 percent strong brown (7.5YR 5/8),
and 20 percent red (2.5YR 4/8) clay loam; weak coarse prisms that part
to moderate coarse subangular blocky structure; firm; common thin clay
films on faces of peds; areas of brownish yellow, strong brown, and red
are masses of iron accumulation; areas of light gray are iron
depletions; very strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction ranges from very
strongly acid to moderately acid throughout the profile, except for the
surface layer in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 10YR or 2.5Y, value of 3 to 5, and
chroma of 1 to 4.

\<@32\>The E horizon, where present, has hue of 10YR or 2.5Y, value of 5
or 6, and chroma of 2 to 4. It is fine sandy loam or loam.

\<@32\>The upper part of the Bt horizon has hue of 10YR or 2.5Y, value
of 5 or 6, and chroma of 4 to 8. The quantity of redoximorphic
accumulations in shades of brown and red and redoximorphic depletions in
shades of brown and gray ranges from none to common. The texture is loam
or clay loam.

\<@32\>The lower part of the Bt horizon has hue of 10YR or 2.5Y, value
of 5 or 6, and chroma of 3 to 8; or it does not have a dominant matrix
color and is multicolored in shades of brown, yellow, and red. It has
common or many redoximorphic accumulations in shades of brown and red
and redoximorphic depletions in shades of brown and gray. It is clay
loam or clay.

\<@37\>Kureb series

\<@32\>The Kureb series consists of very deep, excessively drained soils
that formed in sandy marine sediments. These soils are on low ridges and
knolls and on old dunes. They are in the coastal lowlands. The seasonal
high water table is below a depth of 6 feet throughout the year. Slopes
range from 0 to 12 percent. These soils are thermic, uncoated Spodic
Quartzipsamments.

\<@32\>Kureb soils are geographically associated with Corolla, Duckston,
Lakeland, Newhan, and Resota soils. The somewhat poorly drained Corolla
and poorly drained Duckston soils are in lower positions than the Kureb
soils. The Lakeland soils are in positions similar to those of the Kureb
soils and do not have spodic materials within the profile. The Newhan
soils are on the less stable dunes that are affected by salt spray and
do not have spodic materials within the profile. The moderately well
drained Resota soils are in lower positions than the Kureb soils.

\<@32\>Typical pedon of Kureb sand, 0 to 8 percent slopes; about 1,600
feet south and 2,900 feet east of the northwest corner of sec. 23, T. 3
S., R. 31 W.

\<@23\>A---0 to 3 inches; very dark gray (10YR 3/1) sand; single
grained; loose; common medium and fine roots; many uncoated sand grains;
very strongly acid; clear wavy boundary.

\<@33\>E---3 to 19 inches; white (N 8/0) sand; single grained; loose;
common medium and fine roots; strongly acid; clear irregular boundary.

\<@33\>C/Bh---19 to 36 inches; 70 percent brownish yellow (10YR 6/8)
sand (C); single grained; loose; few streaks of white (N 8/0) sand; 30
percent dark brown (7.5YR 4/4) sand (Bh) in thin bands at the horizon
contact and bordering the streaks of white sand; single grained; loose;
strongly acid; clear wavy boundary.

\<@33\>C1---36 to 50 inches; brownish yellow (10YR 6/8) sand; single
grained; loose; strongly acid; gradual wavy boundary.

\<@33\>C2---50 to 80 inches; yellow (10YR 7/8) sand; single grained;
loose; strongly acid.

\<@8\>Reaction ranges from very strongly acid to slightly acid
throughout the profile.

\<@32\>The A horizon has hue of 10YR, value of 3 or 4, and chroma of 1
or 2.

\<@32\>The E horizon has hue of 10YR or 2.5Y, value of 5 to 8, and
chroma of 1 to 3; or it is neutral in hue and has value of 8. It is fine
sand or sand.

\<@32\>The Bh part of the C/Bh horizon has hue of 5YR to 10YR, value of
2 to 4, and chroma of 2 to 4. It is fine sand or sand.

\<@32\>The C horizon and the C part of the C/Bh horizon have hue of 10YR
or 2.5Y, value of 5 to 7, and chroma of 1 to 8. The quantity of
redoximorphic accumulations in shades of yellow, olive, brown, and red
ranges from none to common. The texture is fine sand or sand. In many
pedons, the C horizon and the C part of the C/Bh horizon have streaks of
clean or uncoated sand.

\<@37\>Lakeland Series

\<@32\>The Lakeland series consists of very deep, excessively drained
soils that formed in sandy marine sediments. These soils are on the
summits and side slopes of ridges in the uplands and on low ridges and
knolls in the coastal lowlands. The seasonal high water table is below a
depth of 6 feet throughout the year. Slopes range from 0 to 12 percent.
These soils are thermic, coated Typic Quartzipsamments.

\<@32\>Lakeland soils are geographically associated with Albany,
Bonifay, Foxworth, Poarch, and Troup soils. The somewhat poorly drained
Albany soils are on toeslopes and terraces and have a loamy argillic
horizon within a depth of 40 to 80 inches. The Bonifay and Troup soils
are in positions similar to those of the Lakeland soils and have a loamy
argillic horizon within a depth of 40 to 80 inches. The moderately well
drained Foxworth soils are in positions similar to those of the Lakeland
soils but are at lower elevations. The Poarch soils are on summits or
side slopes at slightly higher elevations than the Lakeland soils and
are fine-loamy.

\<@32\>Typical pedon of Lakeland sand, 0 to 5 percent slopes; about
1,100 feet south and 80 feet east of the northwest corner of sec. 13, T.
2 S., R. 30 W.

\<@23\>A---0 to 5 inches; dark grayish brown (10YR 4/2) sand; weak fine
granular structure; very friable; common medium and fine roots; strongly
acid; clear wavy boundary.

\<@33\>C1---5 to 15 inches; yellowish brown (10YR 5/4) sand; single
grained; loose; common medium and fine roots; strongly acid; gradual
wavy boundary.

\<@33\>C2---15 to 58 inches; yellowish brown (10YR 5/6) sand; single
grained; loose; few streaks of clean sand; strongly acid; gradual wavy
boundary.

\<@33\>C3---58 to 80 inches; brownish yellow (10YR 6/6) sand; single
grained; loose; common streaks and pockets of clean sand; strongly acid.

\<@8\>Reaction ranges from very strongly acid to moderately acid
throughout the profile, except in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 10YR, value of 3 to 5, and chroma
of 1 to 4.

\<@32\>The C horizon has hue of 10YR, value of 4 to 7, and chroma of 3
to 8; or it has hue of 7.5YR, value of 5 or 6, and chroma of 6 to 8. In
most pedons, it has streaks and pockets of clean sand.

\<@37\>Leon Series

\<@32\>The Leon series consists of very deep, poorly drained soils that
formed in sandy marine sediments. These soils are in convex or concave
positions in areas of flatwoods in the coastal lowlands. The seasonal
high water table is at a depth of 1/2 to 1-1/2 feet from December
through April in most years. Slopes range from 0 to 2 percent. These
soils are sandy, siliceous, thermic Aeric Alaquods.

\<@32\>Leon soils are geographically associated with Allanton, Croatan,
Hurricane, Pickney, and Pottsburg soils. The very poorly drained
Allanton, Croatan, and Pickney soils are in flats and depressions at
slightly lower elevations than the Leon soils. The Allanton soils do not
have a spodic horizon within a depth of 30 inches. The Croatan soils are
organic soils. The Pickney soils have an umbric epipedon. The somewhat
poorly drained Hurricane soils are in slightly higher positions than the
Leon soils and do not have a spodic horizon within a depth of 30 inches.
The Pottsburg soils are in positions similar to those of the Leon soils
and do not have a spodic horizon within a depth of 30 inches.

\<@32\>Typical pedon of Leon sand; about 500 feet south and 170 feet
east of the northwest corner of Spanish Land Grant 17, T. 3 S., R. 31 W.

\<@23\>A---0 to 5 inches; dark gray (10YR 4/1) sand; weak fine granular
structure; very friable; many medium and fine roots; many clean sand
grains; very strongly acid; clear smooth boundary.

\<@33\>Eg1---5 to 12 inches; gray (10YR 6/1) sand; single grained;
loose; common medium and fine roots; very strongly acid; gradual smooth
boundary.

\<@33\>Eg2---12 to 18 inches; gray (10YR 6/1) sand; single grained;
loose; few fine roots; common medium distinct dark yellowish brown (10YR
4/6) masses of iron accumulation; common faint streaks of gray (10YR
5/1) clean sand; very strongly acid; abrupt smooth boundary.

\<@33\>Bh1---18 to 22 inches; dark reddish brown (5YR 2.5/2) sand; weak
coarse subangular blocky structure; very friable; more than 95 percent
of the sand grains are coated with organic matter; very strongly acid;
clear wavy boundary.

\<@33\>Bh2---22 to 26 inches; dark brown (7.5YR 3/3) sand; weak coarse
subangular blocky structure; very friable; more than 90 percent of the
sand grains are coated with organic matter; very strongly acid; clear
wavy boundary.

\<@33\>E´g1---26 to 38 inches; light brownish gray (10YR 6/2) sand;
single grained; loose; common medium distinct dark brown (7.5YR 3/2)
organic stains in root channels; very strongly acid; gradual wavy
boundary.

\<@33\>E´g2---38 to 65 inches; very pale brown (10YR 8/2) sand; single
grained; loose; common coarse faint pale brown (10YR 6/3) masses of iron
accumulation; very strongly acid; clear wavy boundary.

\<@33\>B´h---65 to 80 inches; very dark brown (10YR 2/2) sand; weak
coarse subangular blocky structure; very friable; more than 90 percent
of the sand grains are coated with organic matter; common medium faint
dark grayish brown (10YR 4/2) iron depletions; very strongly acid.

\<@8\>Reaction ranges from extremely acid to slightly acid throughout
the profile.

\<@32\>The A horizon has hue of 10YR, value of 2 to 4, and chroma of 1
or 2; or it is neutral in hue and has value of 2 to 4.

\<@32\>The Eg and E´g horizons have hue of 10YR or 2.5Y, value of 5 to
8, and chroma of 1 or 2. They are sand or fine sand.

\<@32\>The Bh and B´h horizons have hue of 5YR to 10YR, value of 2 to 4,
and chroma of 1 to 3. They are sand, fine sand, loamy sand, or loamy
fine sand.

\<@32\>The C horizon, where present, has hue of 10YR or 2.5Y, value of 5
to 8, and chroma of 1 to 6. It is sand or fine sand.

\<@37\>Lucy Series

\<@32\>The Lucy series consists of very deep, well drained soils that
formed in sandy and loamy sediments. These soils are on summits,
shoulder slopes, and side slopes of ridges in the uplands. The seasonal
high water table is below a depth of 6 feet throughout the year. Slopes
range from 0 to 8 percent. These soils are loamy, kaolinitic, thermic
Arenic Kandiudults.

\<@32\>Lucy soils are geographically associated with Bama, Bonifay,
Cowarts, Perdido, and Troup soils. The Bama soils are on summits at
slightly higher elevations than the Lucy soils and do not have a thick,
sandy epipedon. The Bonifay and Troup soils are in positions similar to
those of the Lucy soils and have sandy epipedons that range from 40 to
80 inches in thickness. The Cowarts and Perdido soils commonly are in
the lower positions on side slopes and do not have a thick, sandy
epipedon.

\<@32\>Typical pedon of Lucy loamy sand, 0 to 2 percent slopes; about
2,335 feet north and 2,670 feet east of the southwest corner of sec. 21,
T. 2 N., R. 31 W.

\<@23\>A---0 to 6 inches; brown (10YR 4/3) loamy sand; weak medium
granular structure; very friable; many medium, fine, and very fine
roots; strongly acid; clear smooth boundary.

\<@33\>E1---6 to 20 inches; brown (7.5YR 5/4) loamy sand; weak coarse
subangular blocky structure; very friable; common medium and fine roots;
strongly acid; gradual wavy boundary.

\<@33\>E2---20 to 26 inches; brown (7.5YR 4/4) loamy sand; weak coarse
subangular blocky structure; very friable; few medium and fine roots;
strongly acid; clear wavy boundary.

\<@33\>Bt1---26 to 38 inches; red (2.5YR 4/6) sandy loam; weak medium
subangular blocky structure; friable; few medium and fine roots; few
faint clay films on faces of peds; strongly acid; gradual wavy boundary.

\<@33\>Bt2---38 to 65 inches; red (2.5YR 4/6) sandy clay loam; moderate
medium subangular structure; friable; few faint clay films on faces of
peds; strongly acid; gradual wavy boundary.

\<@33\>Bt3---65 to 80 inches; red (2.5YR 4/6) sandy loam; weak medium
subangular blocky structure; friable; few faint clay films on faces of
peds; strongly acid.

\<@8\>The solum is more than 60 inches thick. The combined thickness of
the sandy layers ranges from 20 to 40 inches. Reaction ranges from very
strongly acid to moderately acid in the A and E horizons, except where
lime has been applied, and is very strongly acid or strongly acid in the
Bt horizon. The content of rounded quartz pebbles, ironstone nodules, or
both ranges from 0 to 10 percent, by volume.

\<@32\>The A or Ap horizon has hue of 10YR or 7.5YR, value of 3 to 5,
and chroma of 2 or 3.

\<@32\>The E horizon has hue of 10YR or 7.5YR, value of 4 to 7, and
chroma of 3 to 6. It is sand, loamy sand, or loamy fine sand.

\<@32\>The Bt horizon has hue of 2.5YR or 5YR, value of 4 or 5, and
chroma of 6 to 8. In some pedons, it has redoximorphic features in
shades of brown and gray in the lower part. These features are assumed
to be relict and are not reflective of current hydrology. The texture is
sandy loam, sandy clay loam, or clay loam.

\<@37\>Malbis Series

\<@32\>The Malbis series consists of very deep, moderately well drained
soils that formed in loamy sediments. These soils are on summits and
shoulder slopes in the uplands. The seasonal high water table is at a
depth of 2-1/2 to 4 feet from December through April in most years.
Slopes range from 0 to 8 percent. These soils are fine-loamy, siliceous,
subactive, thermic Plinthic Paleudults.

\<@32\>Malbis soils are geographically associated with Bama, Escambia,
Grady, Notcher, and Poarch soils. The Bama, Notcher, and Poarch soils
are in positions similar to those of the Malbis soils. The Bama soils
have a reddish argillic horizon and do not have a significant
accumulation of plinthite in the subsoil. The Notcher soils have more
than 5 percent ironstone nodules throughout. The Poarch soils are
coarse-loamy. The somewhat poorly drained Escambia soils are in slightly
lower positions than the Malbis soils and are coarse-loamy. The poorly
drained Grady soils are in depressions.

\<@32\>Typical pedon of Malbis sandy loam, 0 to 2 percent slopes; about
1,875 feet east and 50 feet south of the northwest corner of sec. 2, T.
2 S., R. 31 W.

\<@23\>Ap---0 to 7 inches; dark brown (10YR 3/3) sandy loam; moderate
medium granular structure; very friable; many medium, fine, and very
fine roots; strongly acid; abrupt smooth boundary.

\<@33\>Bt---7 to 22 inches; yellowish brown (10YR 5/6) loam; weak medium
subangular blocky structure; friable; few medium and common fine roots;
few faint clay films on faces of peds; strongly acid; clear wavy
boundary.

\<@33\>Btv1---22 to 37 inches; brownish yellow (10YR 6/6) clay loam;
moderate medium subangular blocky structure; friable; common faint clay
films on faces of peds; about 8 percent firm and brittle masses of
plinthite; common medium prominent yellowish red (5YR 5/8) masses of
iron accumulation; common medium distinct brown (10YR 5/3) iron
depletions with sharp boundaries throughout the matrix; very strongly
acid; gradual wavy boundary.

\<@33\>Btv2---37 to 50 inches; brownish yellow (10YR 6/6) clay loam;
moderate medium subangular blocky structure; friable; common faint clay
films on faces of peds; about 12 percent firm and brittle masses of
plinthite; common medium prominent yellowish red (5YR 5/8) masses of
iron accumulation; common medium distinct light gray (2.5Y 7/2) and
brown (10YR 5/3) iron depletions with sharp boundaries throughout the
matrix; very strongly acid; gradual wavy boundary.

\<@33\>Btv3---50 to 62 inches; yellowish brown (10YR 5/4) clay loam;
moderate medium subangular blocky structure; firm; common faint clay
films on faces of peds; about 10 percent firm and brittle masses of
plinthite; many medium prominent yellowish red (5YR 5/8) and many medium
distinct yellowish brown (10YR 5/8) masses of iron accumulation; many
medium distinct light gray (10YR 7/2) iron depletions with sharp
boundaries throughout the matrix; very strongly acid; gradual wavy
boundary.

\<@33\>BC---62 to 80 inches; 25 percent yellowish brown (10YR 5/4), 25
percent light gray (10YR 7/2), 20 percent strong brown (7.5YR 5/8), 15
percent red (2.5YR 4/8), and 15 percent pale yellow (2.5Y 7/3) clay
loam; weak coarse subangular blocky structure; firm; areas of yellowish
brown, strong brown, and red are masses of iron accumulation; areas of
light gray are iron depletions; very strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction ranges from very
strongly acid to moderately acid in the surface layer, except in areas
where lime has been applied, and is very strongly acid or strongly acid
in the subsoil.

\<@32\>The A or Ap horizon has hue of 10YR or 2.5Y, value of 3 to 5, and
chroma of 2 or 3.

\<@32\>The Bt horizon has hue of 10YR or 2.5Y, value of 5 or 6, and
chroma of 4 to 8. The quantity of redoximorphic accumulations in shades
of brown or red is none or few. The texture is loam, sandy clay loam, or
clay loam.

\<@32\>The upper part of the Btv horizon has hue of 10YR or 2.5Y, value
of 5 or 6, and chroma of 4 to 8. It has few or common redoximorphic
accumulations in shades of yellow, olive, brown, and red. It has few to
many redoximorphic depletions in shades of gray below a depth of 30
inches. It is sandy clay loam or clay loam.

\<@32\>The lower part of the Btv horizon has a range in color similar to
that of the upper part; or it has no dominant matrix color and is
multicolored in shades of brown, yellow, red, and gray. It is loam, clay
loam, or sandy clay loam. The content of plinthite ranges from 5 to 15
percent, by volume, in the Btv horizon.

\<@32\>The BC horizon, where present, has no dominant matrix color and
is multicolored in shades of brown, yellow, red, and gray. It is clay
loam, sandy clay loam, or clay.

\<@37\>Mantachie Series

\<@32\>The Mantachie series consists of very deep, somewhat poorly
drained soils that formed in loamy alluvium. These soils are on the
lower parts of natural levees and the higher parts of backswamps on
flood plains along major streams and rivers. The seasonal high water
table is at a depth of 1 to 1-1/2 feet from December through April in
most years. These soils are subject to frequent flooding. Slopes range
from 0 to 2 percent. These soils are fine-loamy, siliceous, active,
acid, thermic Aeric Endoaquepts.

\<@32\>Mantachie soils are geographically associated with Fluvaquents
and Bigbee, Dorovan, Eunola, and Iuka soils. The Bigbee soils are on the
highest parts of the natural levees and are sandy throughout. The very
poorly drained Dorovan soils and Fluvaquents are in depressions on the
flood plains. The moderately well drained Eunola soils are on low
terraces and have a loamy argillic horizon. The moderately well drained
Iuka soils are on the slightly higher parts of the natural levees and
are coarse-loamy.

\<@32\>Typical pedon of Mantachie loam, in an area of
Mantachie-Fluvaquents-Bigbee complex, frequently flooded; on the flood
plains along the Escambia River, about 670 feet north and 1,670 feet
east of the southwest corner of sec. 35, T. 6 N., R. 30 W.

\<@23\>A---0 to 6 inches; dark brown (10YR 3/3) loam; weak medium
granular structure; friable; common medium roots and many fine roots;
few medium and fine concretions of iron and manganese oxides; strongly
acid; gradual smooth boundary.

\<@33\>Bw---6 to 11 inches; brown (10YR 4/3) loam; weak fine subangular
blocky structure; friable; common medium and fine roots; few medium and
fine concretions of iron and manganese oxides; few fine faint dark
yellowish brown (10YR 4/6) masses of iron accumulation; few fine faint
grayish brown (10YR 5/2) iron depletions; strongly acid; clear wavy
boundary.

\<@33\>Bg1---11 to 26 inches; grayish brown (10YR 5/2) clay loam; weak
medium subangular blocky structure; friable; few fine roots; common
medium and fine concretions of iron and manganese oxides; common fine
faint gray (10YR 5/1) iron depletions; common medium prominent strong
brown (7.5YR 5/6) masses of iron accumulation with gradual boundaries
throughout the matrix; strongly acid; gradual wavy boundary.

\<@33\>Bg2---26 to 55 inches; 50 percent gray (10YR 6/1), 20 percent
brownish yellow (10YR 6/6), 20 percent strong brown (7.5YR 5/8), and 10
percent reddish brown (5YR 5/4) sandy clay loam; weak medium subangular
blocky structure; friable; areas of gray are iron depletions; areas of
brownish yellow, strong brown, and reddish brown are masses of iron
accumulation; strongly acid; gradual wavy boundary.

\<@33\>Cg---55 to 80 inches; gray (10YR 5/1) loam; massive; friable;
many fine and medium prominent brownish yellow (10YR 6/8), strong brown
(7.5YR 5/8), and reddish brown (5YR 5/4) masses of iron accumulation;
strongly acid.

\<@8\>The solum ranges from 30 to 65 inches in thickness. Reaction is
very strongly acid or strongly acid throughout the profile, except for
the surface layer in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 10YR or 2.5Y, value of 3 to 5, and
chroma of 2 to 4.

\<@32\>The Bw horizon commonly has hue of 10YR or 2.5Y, value of 4 or 5,
and chroma of 3 to 6. In some pedons, however, it does not have a
dominant matrix color and is multicolored in shades of brown, yellow,
gray, and red. It has few to many redoximorphic accumulations in shades
of yellow, olive, brown, and red and redoximorphic depletions in shades
of gray. It is loam, clay loam, or sandy clay loam.

\<@32\>The Bg horizon commonly has hue of 10YR or 2.5Y, value of 4 to 7,
and chroma of 1 or 2 and has few to many masses of iron accumulation in
shades of yellow, olive, brown, and red. In some pedons, however, it
does not have a dominant matrix color and is multicolored in shades of
brown, yellow, gray, and red. It is loam, clay loam, or sandy clay loam.

\<@32\>The Cg horizon has hue of 10YR or 2.5Y, value of 4 to 7, and
chroma of 1 or 2 and has few to many redoximorphic accumulations in
shades of yellow, olive, brown, and red. It is clay loam, sandy clay
loam, loam, or sandy loam.

\<@37\>Maubila Series

\<@32\>The Maubila series consists of very deep, moderately well drained
soils that formed in clayey marine sediments. These soils are on
summits, shoulder slopes, and side slopes in the uplands. The seasonal
high water table is at a depth of 2 to 3-1/2 feet from December through
April in most years. Slopes range from 2 to 12 percent. These soils are
fine, mixed, subactive, thermic Aquic Hapludults.

\<@32\>Maubila soils are geographically associated with Cowarts,
Notcher, Perdido, Poarch, and Troup soils. The Cowarts, Notcher,
Perdido, and Troup soils are in positions similar to those of the
Maubila soils. The Cowarts soils are fine-loamy. The Notcher soils are
fine-loamy and have a significant accumulation of plinthite in the
subsoil. The Perdido soils are coarse-loamy. The Troup soils have a
thick, sandy epipedon. The Poarch soils are on higher summits than the
Maubila soils and are coarse-loamy.

\<@32\>Typical pedon of Maubila gravelly fine sandy loam, in an area of
Notcher-Maubila complex, 2 to 5 percent slopes; about 170 feet south and
1,835 feet east of the northwest corner of sec. 27, T. 4 N., R. 31 W.

\<@23\>Ap---0 to 4 inches; very dark grayish brown (10YR 3/2) gravelly
fine sandy loam; weak fine granular structure; very friable; many
medium, fine, and very fine roots; 20 percent, by volume, fine and
medium nodules of ironstone; strongly acid; clear smooth boundary.

\<@33\>E---4 to 9 inches; yellowish brown (10YR 5/4) fine sandy loam;
weak fine granular structure; common medium and fine roots; 8 percent,
by volume, fine and medium nodules of ironstone; strongly acid; clear
wavy boundary.

\<@33\>Bt1---9 to 16 inches; reddish yellow (7.5YR 6/8) clay loam; weak
medium subangular blocky structure; few medium and fine roots; few faint
clay films on faces of peds; very strongly acid; clear wavy boundary.

\<@33\>Bt2---16 to 32 inches; strong brown (7.5YR 5/8) clay loam;
moderate medium subangular blocky structure; firm; few fine roots;
common faint clay films on faces of peds; common fine and medium reddish
yellow (5YR 6/8) and red (2.5YR 4/8) masses of iron accumulation; few
medium distinct grayish brown (10YR 5/2) iron depletions; very strongly
acid; gradual wavy boundary.

\<@33\>Bt3---32 to 54 inches; 30 percent reddish yellow (7.5YR 6/8), 30
percent yellowish red (5YR 5/8), 20 percent red (2.5YR 4/8), and 20
percent light gray (10YR 7/1) clay loam; moderate medium subangular
blocky structure; firm; common faint clay films on faces of peds; areas
of reddish yellow, yellowish red, and red are masses of iron
accumulation; areas of light gray are iron depletions; very strongly
acid; gradual wavy boundary.

\<@33\>BC---54 to 80 inches; 25 percent brownish yellow (10YR 6/8), 25
percent reddish yellow (7.5YR 6/8), 25 percent yellowish red (5YR 5/8),
and 25 percent light gray (10YR 7/1) sandy clay loam; massive; firm;
areas of brownish yellow, reddish yellow, and yellowish red are masses
of iron accumulation; areas of light gray are iron depletions; very
strongly acid.

\<@8\>The solum ranges from 40 to 60 inches in thickness. Reaction
ranges from extremely acid to strongly acid throughout the profile,
except for the surface layer in areas where lime has been applied. The
content of coarse fragments, mainly nodules or channers of ironstone,
ranges from 5 to 25 percent, by volume, in the A and E horizons and is
less than 15 percent, by volume, in the Bt, BC, and C horizons.

\<@32\>The A or Ap horizon has hue of 10YR or 7.5YR, value of 3 to 5,
and chroma of 2 to 4.

\<@32\>The E horizon, where present, has hue of 10YR, value of 5 or 6,
and chroma of 2 to 4. It is loamy sand, loamy fine sand, fine sandy
loam, loam, or their gravelly analogues.

\<@32\>The upper part of the Bt horizon commonly has hue of 7.5YR or
10YR, value of 4 to 6, and chroma of 6 to 8. It has few or common
redoximorphic accumulations in shades of yellow, olive, brown, and red
and redoximorphic depletions in shades of brown and gray. The texture
commonly is clay loam or clay. In some pedons, however, it is sandy clay
loam.

\<@32\>The lower part of the Bt horizon has a range in color similar to
that of the upper part, or it does not have a dominant matrix color and
is multicolored in shades of brown, yellow, gray, and red. It has common
or many redoximorphic accumulations in shades of yellow, olive, brown,
and red and redoximorphic depletions in shades of brown and gray. It is
clay loam, clay, or silty clay.

\<@32\>The BC horizon, where present, typically does not have a dominant
matrix color and is multicolored in shades of brown, yellow, gray, and
red. It is sandy clay loam, clay loam, or clay. The quantity of thin
strata or pockets of finer- or coarser-textured sediments ranges from
none to common.

\<@32\>The C horizon, where present, has the same range in color as the
BC horizon. It is firm or very firm and is massive. It is clay loam,
clay, silty clay, or sandy clay loam. Most pedons have one or more thin,
discontinuous strata of ironstone and thin strata or pockets of finer-
or coarser-textured sediments.

\<@37\>Newhan Series

\<@32\>The Newhan series consists of very deep, excessively drained
soils that formed in thick deposits of marine sands that have been
reworked by wind and wave action. These soils are on dunes on the
barrier islands and adjacent to the coastal beaches on the mainland. The
seasonal high water table is below a depth of 6 feet throughout the
year. Slopes range from 2 to 12 percent. These soils are thermic,
uncoated Typic Quartzipsamments.

\<@32\>Newhan soils are geographically associated with Corolla, Dirego,
Duckston, Kureb, and Resota soils. The somewhat poorly drained Corolla
soils are on the lower parts of dunes and in shallow swales between
dunes. The very poorly drained Dirego soils are in tidal marshes and
have a thick histic horizon. The poorly drained Duckston soils are on
flats and in swales between dunes. The Kureb and Resota soils are on
dunes and knolls that are not subject to salt spray. The Kureb soils
have discontinuous spodic horizons. The Resota soils are moderately well
drained.

\<@32\>Typical pedon of Newhan sand, in an area of Newhan-Corolla
complex, rolling, rarely flooded; about 2,500 feet south and 4,850 feet
west of the northeast corner of sec. 34, T. 3 S., R. 32 W.

\<@23\>A---0 to 3 inches; gray (10YR 6/1) sand; single grained; loose;
few fine roots; slightly acid; clear wavy boundary.

\<@33\>C1---3 to 22 inches; light gray (10YR 7/1) sand; single grained;
loose; few fine roots; common black sand grains; slightly acid; gradual
wavy boundary.

\<@33\>C2---22 to 80 inches; white (10YR 8/1) sand; single grained;
loose; common black sand grains; slightly acid.

\<@8\>The combined thickness of the sandy sediments is more than 80
inches. Reaction ranges from extremely acid to slightly alkaline. Up to
35 percent, by volume, of the soil is fragments of mollusk shell, mostly
of sand size. In most pedons, dark sand grains of ilmenite are
throughout the profile.

\<@32\>The A horizon has hue of 10YR or 2.5Y, value of 4 to 7, and
chroma of 1 to 3.

\<@32\>The C horizon has hue of 10YR or 2.5Y, value of 5 to 8, and
chroma of 1 or 2. It is sand or fine sand.

\<@37\>Notcher Series

\<@32\>The Notcher series consists of very deep, moderately well drained
soils that formed in loamy sediments. These soils are on summits,
shoulder slopes, and side slopes in the uplands. The seasonal high water
table is at a depth of 3 to 4 feet from December through April in most
years. Slopes range from 0 to 12 percent. These soils are fine-loamy,
siliceous, subactive, thermic Plinthic Paleudults.

\<@32\>Notcher soils are geographically associated with Bama, Grady,
Malbis, Maubila, and Robertsdale soils. The Bama and Malbis soils are in
positions similar to those of the Notcher soils. The Bama soils have a
reddish argillic horizon and do not have a significant accumulation of
plinthite in the subsoil. The Malbis soils have less than 5 percent, by
volume, nodules of ironstone throughout. The poorly drained Grady soils
are in depressions. The Maubila soils are on side slopes and have a
clayey argillic horizon. The somewhat poorly drained Robertsdale soils
are in slightly lower positions than the Notcher soils.

\<@32\>Typical pedon of Notcher fine sandy loam, 0 to 2 percent slopes;
about 1,670 feet east and 2,250 feet south of the northwest corner of
sec. 33, T. 3 N., R. 31 W.

\<@23\>Ap---0 to 5 inches; dark grayish brown (10YR 4/2) fine sandy
loam; moderate fine granular structure; very friable; common medium,
fine, and very fine roots; about 5 percent, by volume, fine and medium
nodules of ironstone; very strongly acid; clear smooth boundary.

\<@33\>EB---5 to 12 inches; yellowish brown (10YR 5/8) fine sandy loam;
weak fine subangular blocky structure; very friable; common medium and
fine roots; about 7 percent, by volume, medium nodules of ironstone;
very strongly acid; clear wavy boundary.

\<@33\>Btc1---12 to 20 inches; brownish yellow (10YR 6/8) sandy clay
loam; weak medium subangular blocky structure; friable; few faint clay
films on faces of peds; about 10 percent, by volume, fine and medium
nodules of ironstone; very strongly acid; gradual wavy boundary.

\<@33\>Btc2---20 to 34 inches; brownish yellow (10YR 6/8) gravelly sandy
clay loam; moderate medium subangular blocky structure; friable; few
faint clay films on faces of peds; about 20 percent, by volume, fine and
medium nodules of ironstone; few medium prominent yellowish red (5YR
5/8) masses of iron accumulation; few fine distinct grayish brown (10YR
5/2) iron depletions; very strongly acid; gradual wavy boundary.

\<@33\>Btv1---34 to 48 inches; brownish yellow (10YR 6/8) gravelly sandy
clay loam; moderate medium subangular blocky structure; firm; few faint
clay films on faces of peds; about 20 percent, by volume, fine and
medium nodules of ironstone; about 5 percent, by volume, firm and
brittle masses of plinthite; few medium prominent yellowish red (5YR
5/8) and red (2.5YR 5/8) masses of iron accumulation with clear
boundaries throughout the matrix; few fine distinct grayish brown (10YR
5/2) iron depletions; very strongly acid; gradual wavy boundary.

\<@33\>Btv2---48 to 80 inches; brownish yellow (10YR 6/8) sandy clay
loam; moderate medium subangular blocky structure; firm; few faint clay
films on faces of peds; about 10 percent, by volume, fine and medium
nodules of ironstone; about 7 percent, by volume, firm and brittle
masses of plinthite; common medium distinct light gray (10YR 7/2) iron
depletions with sharp boundaries throughout the matrix; common medium
prominent reddish yellow (5YR 6/8) and red (2.5YR 5/8) masses of iron
accumulation with clear boundaries throughout the matrix; very strongly
acid.

\<@8\>The solum is more than 60 inches thick. Reaction ranges from very
strongly acid to moderately acid in the surface layer, except where lime
has been applied, and is very strongly acid or strongly acid in the
subsoil. The content of nodules of ironstone, ranging from 0.25 to 2
inches in diameter, is 5 to 25 percent, by volume, in the A, E, EB, and
Btc horizons.

\<@32\>The A or Ap horizon has hue of 10YR or 2.5Y, value of 3 to 5, and
chroma of 2 or 3.

\<@32\>The EB or BE horizon, where present, has hue of 10YR, value of 5
or 6, and chroma of 3 to 8. It is sandy loam, fine sandy loam, loam, or
their gravelly analogues.

\<@32\>The Btc horizon has hue of 7.5YR or 10YR, value of 5 or 6, and
chroma of 4 to 8. It has few or common redoximorphic accumulations in
shades of yellow, olive, brown, and red and redoximorphic depletions in
shades of brown and gray. It is sandy clay loam, clay loam, loam, or
their gravelly analogues.

\<@32\>The Btv horizon dominantly has a range in color similar to that
of the Btc horizon or has hue of 2.5YR or 5YR, value of 4 or 5, and
chroma of 4 to 8. In some pedons, however, the lower part of the horizon
has no dominant matrix color and is multicolored in shades of red,
brown, yellow, and gray. The texture is sandy clay loam, clay loam,
loam, or their gravelly analogues.

\<@37\>Pelham Series

\<@32\>The Pelham series consists of very deep, poorly drained soils
that formed in sandy and loamy sediments. These soils are on flats in
the coastal lowlands and in slightly depressional positions on low
stream terraces. The seasonal high water table is within a depth of 1/2
foot from December through April in most years. Areas on low terraces
are subject to occasional flooding. Slopes range from 0 to 2 percent.
These soils are loamy, siliceous, subactive, thermic Arenic Paleaquults.

\<@32\>Pelham soils are geographically associated with Albany, Dorovan,
Escambia, and Yemassee soils. The somewhat poorly drained Albany and
Escambia soils are in slightly higher positions than the Pelham soils.
The Albany soils have a sandy epipedon that is 40 to 80 inches thick.
The Escambia soils do not have a thick, sandy epipedon. The very poorly
drained Dorovan soils are in depressions and have a thick histic
epipedon. The somewhat poorly drained Yemassee soils are in positions
similar to those of the Pelham soils on low terraces and do not have a
thick, sandy epipedon.

\<@32\>Typical pedon of Pelham loamy sand, 0 to 2 percent slopes; about
2,500 feet north and 2,500 feet east of the southwest corner of sec. 29,
T. 3 N., R. 32 W.

\<@23\>A---0 to 5 inches; very dark gray (10YR 3/1) loamy sand; weak
fine granular structure; very friable; many medium and fine roots; very
strongly acid; clear wavy boundary.

\<@33\>Eg1---5 to 20 inches; gray (10YR 5/1) loamy sand; weak coarse
subangular blocky structure; very friable; few medium and fine roots;
common fine distinct yellowish brown (10YR 5/6) and brownish yellow
(10YR 6/6) masses of iron accumulation with clear boundaries throughout
the matrix; very strongly acid; clear wavy boundary.

\<@33\>Eg2---20 to 35 inches; gray (10YR 5/1) loamy sand; weak coarse
subangular blocky structure; very friable; common fine prominent strong
brown (7.5YR 5/6) masses of iron accumulation with sharp boundaries
throughout the matrix; very strongly acid; clear wavy boundary.

\<@33\>Btg1---35 to 58 inches; gray (10YR 5/1) sandy loam; weak medium
subangular blocky structure; friable; few faint clay films on faces of
peds; common medium prominent yellowish brown (10YR 5/6) and strong
brown (7.5YR 5/6) masses of iron accumulation with gradual boundaries
throughout the matrix; very strongly acid; gradual wavy boundary.

\<@33\>Btg2---58 to 80 inches; 55 percent gray (10YR 6/1) and 45 percent
light gray (10YR 7/1) sandy clay loam; weak coarse subangular blocky
structure; friable; few faint clay films on faces of peds; common coarse
prominent yellow (10YR 7/6) and strong brown (7.5YR 5/8) masses of iron
accumulation with sharp boundaries throughout the matrix; very strongly
acid.

\<@8\>The solum is more than 60 inches thick. The combined thickness of
the sandy layers ranges from 20 to 40 inches. Reaction ranges from
extremely acid to strongly acid throughout the profile, except in areas
where lime has been applied.

\<@32\>The A horizon has hue of 10YR to 5Y, value of 2 to 5, and chroma
of 1 or 2; or it is neutral in hue and has value of 2 to 4.

\<@32\>The Eg horizon has hue of 10YR to 5Y, value of 4 to 7, and chroma
of 1 or 2. The quantity of redoximorphic accumulations in shades of
yellow, olive, brown, and red ranges from none to common. The texture is
loamy sand, sand, or fine sand.

\<@32\>The Btg horizon has hue of 10YR to 5Y, value of 5 to 7, and
chroma of 1 or 2; or it is neutral in hue and has value of 5 to 7. It
has few to many redoximorphic accumulations in shades of yellow, olive,
brown, and red and redoximorphic depletions in shades of brown and gray.
It is sandy loam, fine sandy loam, or sandy clay loam.

\<@37\>Perdido Series

\<@32\>The Perdido series consists of very deep, well drained soils that
formed in loamy sediments. These soils are on summits, shoulder slopes,
and side slopes in the uplands. The seasonal high water table is at a
depth of 4 to 6 feet from December through April in most years. Slopes
range from 0 to 35 percent. These soils are coarse-loamy, siliceous,
subactive, thermic Plinthic Paleudults.

\<@32\>Perdido soils are geographically associated with Lucy, Maubila,
Notcher, Poarch, and Troup soils. The Lucy soils are in higher positions
than the Perdido soils and have a thick, sandy epipedon. The Maubila
soils are in lower positions than the Perdido soils and have a clayey
argillic horizon. The Notcher, Poarch, and Troup soils are in positions
similar to those of the Perdido soils. The Notcher soils are fine-loamy
and have brownish colors in the subsoil. The Poarch soils have brownish
colors in the subsoil. The Troup soils have a thick, sandy epipedon.

\<@32\>Typical pedon of Perdido sandy loam, 0 to 2 percent slopes; about
100 feet north and 100 feet west of the intersection of County Highway 4
and Raines Road; about 1,420 feet south and 50 feet east of the
northwest corner of sec. 10, T. 5 N., R. 31 W.

\<@23\>Ap---0 to 8 inches; dark yellowish brown (10YR 3/4) sandy loam;
moderate medium granular structure; friable; common medium, fine, and
very fine roots; strongly acid; clear smooth boundary.

\<@33\>Bt1---8 to 27 inches; strong brown (7.5YR 5/6) sandy loam; weak
medium subangular blocky structure; friable; common medium and fine
roots; few faint clay films on faces of peds; strongly acid; clear wavy
boundary.

\<@33\>Bt2---27 to 45 inches; yellowish red (5YR 5/6) sandy loam; weak
medium subangular blocky structure; friable; few fine roots; common
faint clay films on faces of peds; strongly acid; clear wavy boundary.

\<@33\>Btv---45 to 57 inches; strong brown (7.5YR 5/6) sandy loam; weak
medium subangular blocky structure; friable; few faint clay films on
faces of peds; about 10 percent, by volume, firm and brittle masses of
plinthite; common medium distinct red (2.5YR 4/6) masses of iron
accumulation; strongly acid; gradual wavy boundary.

\<@33\>B´t1---57 to 72 inches; red (2.5YR 4/6) sandy clay loam; weak
coarse subangular blocky structure; friable; few faint clay films on
faces of peds; strongly acid; gradual wavy boundary.

\<@33\>B´t2---72 to 80 inches; red (2.5YR 4/6) sandy loam; weak coarse
subangular blocky structure; friable; few faint clay films on faces of
peds; common medium distinct strong brown (7.5YR 5/6) masses of iron
accumulation; few fine distinct light gray (10YR 7/2) iron depletions;
strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction is very strongly
acid or strongly acid throughout the profile, except for the surface
layer in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 7.5YR or 10YR, value of 3 or 4,
and chroma of 2 to 4.

\<@32\>The E horizon, where present, has hue of 7.5YR or 10YR, value of
4 or 5, and chroma of 4 to 6. It is fine sandy loam or sandy loam.

\<@32\>The upper part of the Bt horizon has hue of 5YR or 7.5YR, value
of 4 or 5, and chroma of 4 to 6. It is sandy loam or fine sandy loam.
The lower part has hue of 2.5YR to 7.5YR, value of 4 or 5, and chroma of
6 to 8. It is sandy loam or sandy clay loam.

\<@32\>The Btv horizon has hue of 2.5YR to 7.5YR, value of 4 or 5, and
chroma of 6 to 8. It has few or common redoximorphic accumulations in
shades of yellow, olive, brown, and red and redoximorphic depletions in
shades of brown and gray. The content of nodular plinthite ranges from 5
to 15 percent, by volume. The texture is sandy loam or sandy clay loam.

\<@32\>The B´t horizon, where present, has hue of 2.5YR to 7.5YR, value
of 4 or 5, and chroma of 6 to 8. It has few or common redoximorphic
accumulations in shades of yellow, olive, brown, and red and
redoximorphic depletions in shades of brown and gray. It is sandy loam
or sandy clay loam.

\<@32\>The BC horizon, where present, has the same range in color as the
B´t horizon; or it has no dominant matrix color and is multicolored in
shades of red, brown, and gray. It is sandy loam or sandy clay loam.

\<@37\>Pickney Series

\<@32\>The Pickney series consists of very deep, very poorly drained
soils that formed in sandy marine sediments. These soils are on broad
flats and in shallow depressions. They are in the coastal lowlands. On
the flats, the seasonal high water table is within a depth of 1/2 foot
from December through April in most years. The depressional areas are
subject to ponding for long periods. Slopes are 0 to 1 percent. These
soils are sandy, siliceous, thermic Cumulic Humaquepts.

\<@32\>Pickney soils are geographically associated with Allanton,
Croatan, Hurricane, Leon, and Pottsburg soils. The very poorly drained
Allanton and Croatan soils are in positions similar to those of the
Pickney soils. The Allanton soils have a spodic horizon. The Croatan
soils have a thick, histic epipedon. The somewhat poorly drained
Hurricane soils are on knolls and do not have a thick, umbric epipedon.
The poorly drained Leon and Pottsburg soils are in slightly higher
positions than the Pickney soils on flats and in areas of flatwoods and
do not have a thick, umbric epipedon.

\<@32\>Typical pedon of Pickney sand; about 1,500 feet south and 250
feet east of the northwest corner of sec. 14, T. 3 S., R. 31 W.

\<@23\>A1---0 to 10 inches; black (10YR 2/1) sand; weak medium granular
structure; very friable; common medium, fine, and very fine roots; very
strongly acid; gradual smooth boundary.

\<@33\>A2---10 to 35 inches; black (10YR 2/1) sand; single grained;
loose; common thin streaks of gray (10YR 6/1) uncoated sand; very
strongly acid; gradual smooth boundary.

\<@33\>Cg1---35 to 52 inches; very dark gray (10YR 3/1) coarse sand;
single grained; loose; very strongly acid; clear smooth boundary.

\<@33\>Cg2---52 to 80 inches; very dark grayish brown (10YR 3/2) sand;
single grained; loose; very strongly acid.

\<@8\>Reaction ranges from extremely acid to moderately acid throughout
the profile.

\<@32\>The A horizon has hue of 10YR or 2.5Y, value of 2 or 3, and
chroma of 1 or 2.

\<@32\>The Cg horizon has hue of 10YR or 2.5Y, value of 3 to 7, and
chroma of 1 or 2; or it is neutral in hue and has value of 3 to 7. It is
coarse sand or sand.

\<@37\>Poarch Series

\<@32\>The Poarch series consists of very deep, well drained soils that
formed in sandy and loamy sediments. These soils are on summits,
shoulder slopes, and side slopes in the uplands. The seasonal high water
table is at a depth of 2-1/2 to 4 feet from December through April in
most years. Slopes range from 0 to 8 percent. These soils are
coarse-loamy, siliceous, semiactive, thermic Plinthic Paleudults.

\<@32\>Poarch soils are geographically associated with Escambia, Grady,
Notcher, Perdido, and Red Bay soils. The somewhat poorly drained
Escambia soils are in slightly lower, less convex positions than those
of the Poarch soils. The poorly drained Grady soils are in depressions
and have a clayey argillic horizon. The Notcher, Perdido, and Red Bay
soils are in positions similar to those of the Poarch soils. The
moderately well drained Notcher soils are fine-loamy. The Perdido soils
have hue of 5YR or redder throughout the subsoil. The Red Bay soils have
a dark red argillic horizon.

\<@32\>Typical pedon of Poarch sandy loam, 0 to 2 percent slopes; about
250 feet north and 1,850 feet west of the southeast corner of sec. 1, T.
1 S., R. 31 W.

\<@23\>A---0 to 5 inches; very dark grayish brown (10YR 3/2) sandy loam;
weak fine granular structure; very friable; many fine and very fine
roots; strongly acid; clear smooth boundary.

\<@33\>Bt---5 to 31 inches; yellowish brown (10YR 5/6) sandy loam; weak
medium subangular blocky structure; very friable; common fine roots; few
faint clay films on faces of peds; strongly acid; clear wavy boundary.

\<@33\>Btv1---31 to 38 inches; yellowish brown (10YR 5/6) sandy loam;
weak medium subangular blocky structure; friable; few faint clay films
on faces of peds; about 7 percent, by volume, firm and brittle masses of
plinthite; common medium distinct strong brown (7.5YR 5/8) and common
medium prominent red (2.5YR 4/8) masses of iron accumulation; few fine
distinct light gray (10YR 7/2) iron depletions; very strongly acid;
gradual wavy boundary.

\<@33\>Btv2---38 to 45 inches; brownish yellow (10YR 6/6) sandy loam;
weak medium subangular blocky structure; friable; few faint clay films
on faces of peds; about 10 percent, by volume, firm and brittle masses
of plinthite; common medium distinct strong brown (7.5YR 5/8) and common
medium prominent red (2.5YR 4/8) masses of iron accumulation; few fine
distinct light gray (10YR 7/2) iron depletions; very strongly acid;
gradual wavy boundary.

\<@33\>Btv3---45 to 63 inches; brownish yellow (10YR 6/6) sandy loam;
weak medium subangular blocky structure; friable; few faint clay films
on faces of peds; about 10 percent, by volume, firm and brittle masses
of plinthite; common medium distinct strong brown (7.5YR 5/8) masses of
iron accumulation; common coarse distinct light gray (10YR 7/2) iron
depletions; very strongly acid; gradual wavy boundary.

\<@33\>Btv4---63 to 80 inches; 40 percent very pale brown (10YR 7/4), 30
percent brownish yellow (10YR 6/6), 20 percent light gray (10YR 7/2),
and 10 percent strong brown (7.5YR 5/8) sandy loam; weak coarse
subangular blocky structure; friable; few faint clay films on faces of
peds; about 5 percent, by volume, firm and brittle masses of plinthite;
areas of brownish yellow and strong brown are masses of iron
accumulation; areas of very pale brown and light gray are iron
depletions; very strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction is very strongly
acid or strongly acid throughout the profile, except for the surface
layer in areas where lime has been applied.

\<@32\>The A or Ap horizon has hue of 10YR or 2.5Y, value of 3 to 5, and
chroma of 1 to 3.

\<@32\>The E horizon, where present, has hue of 10YR or 7.5YR, value of
5 or 6, and chroma of 2 or 3. It is sandy loam, fine sandy loam, or
loam.

\<@32\>The Bt horizon has hue of 10YR or 2.5Y, value of 5 or 6, and
chroma of 4 to 8. It is fine sandy loam, sandy loam, or loam.

\<@32\>The Btv horizon has hue of 10YR or 2.5Y, value of 5 or 6, and
chroma of 4 to 8; or it does not have a dominant matrix color and is
multicolored in shades of brown, yellow, gray, and red. It has common or
many redoximorphic accumulations in shades of yellow, olive, brown, and
red and redoximorphic depletions in shades of brown and gray. It is
commonly fine sandy loam, sandy loam, or loam. In the lower part of some
pedons, however, it is sandy clay loam or clay loam. The content of
nodular plinthite ranges from 5 to about 25 percent, by volume.

\<@37\>Pottsburg Series

\<@32\>The Pottsburg series consists of very deep, poorly drained soils
that formed in sandy marine sediments. These soils are in areas of
flatwoods in the coastal lowlands. The seasonal high water table is at a
depth of 1/2 to 1 foot from December through April in most years. Slopes
range from 0 to 2 percent. These soils are sandy, siliceous, thermic
Grossarenic Alaquods.

\<@32\>Pottsburg soils are geographically associated with Allanton,
Hurricane, Leon, and Pickney soils. The very poorly drained Allanton
soils are in slightly lower positions than the Pottsburg soils. The
somewhat poorly drained Hurricane soils are on knolls at slightly higher
elevations than the Pottsburg soils. The Leon soils are in areas of
flatwoods adjacent to the Pottsburg soils and have a spodic horizon
within a depth of 30 inches. The very poorly drained Pickney soils are
in lower, more concave positions than those of the Pottsburg soils and
do not have a spodic horizon.

\<@32\>Typical pedon of Pottsburg sand, in an area of Allanton-Pottsburg
complex; about 450 feet north and 2,300 feet east of the southwest
corner of sec. 23, T. 2 S., R. 31 W.

\<@23\>A---0 to 7 inches; very dark grayish brown (10YR 3/2) sand; weak
fine granular structure; very friable; many medium and fine roots; very
strongly acid; clear wavy boundary.

\<@33\>E---7 to 21 inches; brown (10YR 5/3) sand; single grained; loose;
common medium and fine roots; common medium prominent strong brown
(7.5YR 5/6) masses of iron accumulation; common thin streaks and pockets
of light gray (10YR 7/2) uncoated sand; very strongly acid; clear wavy
boundary.

\<@33\>Eg1---21 to 38 inches; grayish brown (10YR 5/2) sand; single
grained; loose; common medium prominent strong brown (7.5YR 5/6) masses
of iron accumulation; very strongly acid; gradual wavy boundary.

\<@33\>Eg2---38 to 53 inches; grayish brown (10YR 5/2) sand; single
grained; loose; very strongly acid; clear wavy boundary.

\<@33\>Bh1---53 to 68 inches; dark reddish brown (5YR 3/2) sand;
massive; very friable; about 75 percent of the sand grains are coated
with organic matter; very strongly acid; gradual wavy boundary.

\<@33\>Bh2---68 to 80 inches; black (5YR 2/1) sand; massive; very
friable; about 90 percent of the sand grains are coated with organic
matter; very strongly acid.

\<@8\>The solum is more than 80 inches thick. Reaction ranges from
extremely acid to moderately acid throughout the profile, except in
areas where lime has been applied.

\<@32\>The A horizon has hue of 10YR, value of 2 to 5, and chroma of 1
or 2; or it is neutral in hue and has value of 2 to 5.

\<@32\>The E horizon has hue of 10YR or 2.5Y, value of 5 to 7, and
chroma of 3 or 4. It has few or common redoximorphic accumulations in
shades of yellow, olive, brown, and red and redoximorphic depletions in
shades of brown and gray. It is sand or fine sand.

\<@32\>The Eg horizon has hue of 10YR or 2.5Y, value of 5 to 8, and
chroma of 1 or 2. It has few or common redoximorphic accumulations in
shades of yellow, olive, brown, and red. It is sand or fine sand.

\<@32\>The Bh horizon has hue of 5YR to 10YR, value of 2 to 5, and
chroma of 1 to 4. It is sand, fine sand, loamy fine sand, or loamy sand.

\<@37\>Red Bay Series

\<@32\>The Red Bay series consists of very deep, well drained soils that
formed in loamy sediments. These soils are on summits, shoulder slopes,
and side slopes in the uplands. The seasonal high water table is below a
depth of 6 feet throughout the year. Slopes range from 0 to 8 percent.
These soils are fine-loamy, kaolinitic, thermic Rhodic Kandiudults.

\<@32\>Red Bay soils are geographically associated with Bama, Emory,
Grady, Malbis, and Perdido soils. The Bama, Malbis, and Perdido soils
are in positions similar to those of the Red Bay soils. The Bama soils
do not have dark red colors throughout the subsoil. The Malbis soils
have brownish colors and have a significant accumulation of plinthite in
the subsoil. The Perdido soils are coarse-loamy and have a significant
accumulation of plinthite in the subsoil. The Emory soils are in shallow
depressions and are subject to ponding. The poorly drained Grady soils
are in depressions and have a clayey argillic horizon.

\<@32\>Typical pedon of Red Bay fine sandy loam, 0 to 2 percent slopes;
2,050 feet east and 1,835 feet north of the southwest corner of sec. 13,
T. 1 N., R. 30 W.

\<@23\>Ap---0 to 6 inches; brown (10YR 4/3) fine sandy loam; moderate
fine granular structure; very friable; common medium roots and many fine
and very fine roots; strongly acid; clear wavy boundary.

\<@33\>BA---6 to 12 inches; yellowish red (5YR 4/6) sandy loam; moderate
medium granular structure; friable; common medium roots and many fine
and very fine roots; strongly acid; clear wavy boundary.

\<@33\>Bt1---12 to 72 inches; dark red (2.5YR 3/6) sandy clay loam;
moderate medium subangular blocky structure; friable; few fine roots;
few faint clay films on faces of peds; strongly acid; gradual wavy
boundary.

\<@33\>Bt2---72 to 80 inches; dark red (2.5YR 3/6) sandy loam; moderate
medium subangular blocky structure; friable; few faint clay films on
faces of peds; strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction ranges from very
strongly acid to moderately acid in the Ap and BA horizons, except in
areas where lime has been applied, and is very strongly acid or strongly
acid in the Bt horizon.

\<@32\>The Ap horizon has hue of 5YR to 10YR, value of 3 or 4, and
chroma of 2 to 4.

\<@32\>The BA horizon, where present, has hue of 2.5YR or 5YR, value of
3 or 4, and chroma of 4 to 6. It is sandy loam or fine sandy loam.

\<@32\>The Bt horizon has hue of 10R or 2.5YR, value of 3, and chroma of
4 to 6. It is sandy loam or sandy clay loam.

\<@37\>Resota Series

\<@32\>The Resota series consists of very deep, moderately well drained
soils that formed in sandy marine sediments. These soils are on low
ridges and knolls in the coastal lowlands. The seasonal high water table
is at a depth of 3-1/2 to 6 feet from December through April in most
years. Slopes range from 0 to 5 percent. These soils are thermic,
uncoated Spodic Quartzipsamments.

\<@32\>Resota soils are geographically associated with Corolla,
Duckston, Kureb, Lakeland, and Newhan soils. The somewhat poorly drained
Corolla and poorly drained Duckston soils are on the lower parts of
dunes and in swales. The excessively drained Kureb and Lakeland soils
are in slightly higher positions than the Resota soils and do not have a
seasonal high water within a depth of 6 feet. The Newhan soils are on
dunes that receive salt spray from the Gulf and do not have spodic
materials within the profile.

\<@32\>Typical pedon of Resota sand, 0 to 5 percent slopes; about 380
feet east and 1,900 feet south of the northwest corner of sec. 23, T. 3
S., R. 31 W.

\<@23\>A---0 to 3 inches; gray (10YR 5/1) sand; single grained; loose;
many medium and fine roots; strongly acid; clear smooth boundary.

\<@33\>E---3 to 19 inches; white (10YR 8/1) sand; single grained; loose;
common medium and fine roots; strongly acid; clear irregular boundary.

\<@33\>B/E---19 to 25 inches; 75 percent brownish yellow (10YR 6/8) sand
(B); single grained; loose; 25 percent streaks or tongues of white (10YR
8/1) sand (E); single grained; loose; a thin, discontinuous band of dark
reddish brown (5YR 3/2) spodic material borders the E material; strongly
acid; clear irregular boundary.

\<@33\>Bw1---25 to 44 inches; yellow (10YR 7/6) sand; single grained;
loose; few streaks of brownish yellow (10YR 6/8) sand bordered by a
thin, discontinuous band of dark reddish brown (5YR 3/3) sand; strongly
acid; gradual wavy boundary.

\<@33\>Bw2---44 to 65 inches; very pale brown (10YR 7/4) sand; single
grained; loose; common medium distinct yellowish brown (10YR 5/6) masses
of iron accumulation; common medium faint light gray (10YR 7/2) iron
depletions; strongly acid; gradual wavy boundary.

\<@33\>Cg---65 to 80 inches; white (10YR 8/1) sand; single grained;
loose; strongly acid.

\<@8\>The solum is more than 50 inches thick. Reaction ranges from
extremely acid to slightly acid throughout the profile.

\<@32\>The A horizon has hue of 10YR, value of 4 to 6, and chroma of 1
or 2.

\<@32\>The E horizon and the E part of the B/E horizon have hue of 10YR,
value of 6 to 8, and chroma of 1 or 2. They are sand or fine sand.

\<@32\>In most pedons, the B/E horizon, where present, has thin,
discontinuous bands, streaks, or spots of spodic materials.

\<@32\>The Bw horizon and B part of the B/E horizon have hue of 10YR or
7.5YR, value of 5 to 7, and chroma of 4 to 8. They are sand or fine
sand. In most pedons, the upper part of the Bw horizon has thin,
discontinuous bands, streaks, or spots of spodic materials. The lower
part of the Bw horizon has common or many redoximorphic accumulations in
shades of yellow, olive, brown, and red.

\<@32\>The Cg horizon has hue of 10YR, value of 6 to 8, and chroma of 1
or 2. It has few or common redoximorphic accumulations in shades of
yellow, olive, brown, and red. It is sand or fine sand.

\<@37\>Robertsdale Series

\<@32\>The Robertsdale series consists of very deep, somewhat poorly
drained soils that formed in loamy sediments. These soils are in flat
and slightly concave positions on nearly level summits in the uplands.
The seasonal high water table is at a depth of 1 to 2 feet from December
through April in most years. Slopes range from 0 to 2 percent. These
soils are fine-loamy, siliceous, semiactive, thermic Plinthaquic
Paleudults.

\<@32\>Robertsdale soils are geographically associated with Escambia,
Grady, Malbis, and Notcher soils. The Escambia soils are in positions
similar to those of the Robertsdale soils and are coarse-loamy. The
poorly drained Grady soils are in depressions and have a clayey argillic
horizon. The well drained Malbis and moderately well drained Notcher
soils are in slightly higher, more convex positions than those of the
Robertsdale soils.

\<@32\>Typical pedon of Robertsdale sandy loam, 0 to 2 percent slopes;
about 335 feet north and 2,335 feet east of the southwest corner of sec.
1, T. 5 N., R. 33 W.

\<@23\>Ap---0 to 5 inches; very dark gray (10YR 3/1) sandy loam;
moderate fine granular structure; very friable; many medium, fine, and
very fine roots; about 4 percent, by volume, fine nodules of ironstone;
strongly acid; abrupt smooth boundary.

\<@33\>EB---5 to 12 inches; brownish yellow (10YR 6/6) fine sandy loam;
weak coarse subangular blocky structure; very friable; many medium and
fine roots; about 4 percent, by volume, fine nodules of ironstone;
strongly acid; clear wavy boundary.

\<@33\>Btc---12 to 24 inches; light yellowish brown (2.5Y 6/4) loam;
moderate medium subangular blocky structure; friable; few fine roots;
few faint clay films on faces of peds; about 5 percent, by volume, fine
and medium nodules of ironstone; common fine distinct light gray (10YR
7/1) iron depletions throughout the matrix; common medium distinct
brownish yellow (10YR 6/6) and common medium prominent reddish yellow
(7.5YR 6/8) masses of iron accumulation with sharp boundaries throughout
the matrix; very strongly acid; clear wavy boundary.

\<@33\>Btvg1---24 to 48 inches; 50 percent light gray (10YR 7/1), 30
percent brownish yellow (10YR 6/8), and 20 percent strong brown (7.5YR
5/8) sandy clay loam; moderate medium subangular blocky structure; firm;
few faint clay films on faces of peds; about 5 percent, by volume, fine
and medium nodules of ironstone; about 5 percent, by volume, firm and
brittle masses of plinthite; areas of light gray are iron depletions;
areas of brownish yellow and strong brown are masses of iron
accumulation; strongly acid; gradual wavy boundary.

\<@33\>Btvg2---48 to 80 inches; 50 percent gray (10YR 5/1), 20 percent
brownish yellow (10YR 6/8), 15 percent strong brown (7.5YR 5/8), and 15
percent red (10R 4/6) sandy clay loam; moderate medium subangular blocky
structure; firm; few faint clay films on faces of peds; about 5 percent,
by volume, fine nodules of ironstone; about 7 percent, by volume, firm
and brittle masses of plinthite; areas of gray are iron depletions;
areas of brownish yellow, strong brown, and red are masses of iron
accumulation; strongly acid.

\<@8\>The solum is more than 60 inches thick. Reaction is very strongly
acid or strongly acid throughout the profile, except for surface layer
in areas where lime has been applied. The content of ironstone nodules
ranges from 4 to 12 percent, by volume, in the Ap and EB horizons and
from 5 to 25 percent, by volume, in the Bt horizons.

\<@32\>The Ap or A horizon has hue of 10YR, value of 2 to 4, and chroma
of 1 or 2.

\<@32\>The EB or BE horizon, where present, has hue of 10YR or 2.5Y,
value of 5 or 6, and chroma of 3 to 6. It is loam, fine sandy loam, or
sandy loam.

\<@32\>The Btc horizon has hue of 10YR or 2.5Y, value of 5 or 6, and
chroma of 4 to 8. It has few or common redoximorphic accumulations in
shades of yellow, olive, brown, and red and redoximorphic depletions in
shades of brown and gray. It is loam, sandy clay loam, or clay loam.

\<@32\>The Btvg horizon commonly does not have a dominant matrix color
and is multicolored in shades of brown, yellow, gray, and red. In some
pedons, however, it has hue of 10YR or 2.5Y, value of 5 to 7, and chroma
of 1 or 2. It has common or many redoximorphic accumulations in shades
of yellow, olive, brown, and red and redoximorphic depletions in shades
of brown and gray. The content of nodular plinthite ranges from 5 to 20
percent, by volume.

\<@37\>Troup Series

\<@32\>The Troup series consists of very deep, somewhat excessively
drained soils that formed in sandy and loamy marine sediments. These
soils are on summits, shoulder slopes, and side slopes in the uplands.
The seasonal high water table is below a depth of 6 feet throughout the
year. Slopes range from 0 to 35 percent. These soils are loamy,
kaolinitic, thermic Grossarenic Kandiudults.

\<@32\>Troup soils are geographically associated with Bonifay, Cowarts,
Lakeland, Lucy, and Perdido soils. The Bonifay soils are in positions
similar to those of the Troup soils and have a significant accumulation
of plinthite in the subsoil. The Cowarts and Perdido soils are on side
slopes and do not have a thick, sandy epipedon. The Lakeland soils are
in positions similar to those of the Troup soils and do not have loamy
subhorizons within a depth of 80 inches. The Lucy soils are in slightly
higher positions than the Troup soils and have a sandy epipedon that is
20 to 40 inches thick.

\<@32\>Typical pedon of Troup sand, 0 to 5 percent slopes; about 50 feet
north and 1,500 feet east of the southwest corner of Spanish Land Grant
42, T. 1 S., R. 30 W.

\<@23\>A---0 to 5 inches; dark grayish brown (10YR 4/2) sand; weak fine
granular structure; very friable; common medium and fine roots; very
strongly acid; clear smooth boundary.

\<@33\>E1---5 to 21 inches; yellowish brown (10YR 5/6) sand; single
grained; loose; few medium and fine roots; very strongly acid; clear
wavy boundary.

\<@33\>E2---21 to 42 inches; strong brown (7.5YR 5/6) sand; single
grained; loose; very friable; very strongly acid; gradual wavy boundary.

\<@33\>E3---42 to 58 inches; yellowish red (5YR 5/6) loamy sand; weak
coarse subangular blocky structure; very friable; very strongly acid;
gradual wavy boundary.

\<@33\>Bt1---58 to 68 inches; red (2.5YR 4/6) sandy loam; weak medium
subangular blocky structure; friable; few faint clay films on faces of
peds; very strongly acid; gradual wavy boundary.

\<@33\>Bt2---68 to 80 inches; red (2.5YR 4/6) sandy clay loam; moderate
medium subangular blocky structure; friable; few faint clay films on
faces of peds; very strongly acid.

\<@8\>The solum is more than 80 inches thick. Reaction ranges from very
strongly acid to moderately acid in the A and E horizons, except in
areas where lime has been applied, and is very strongly acid or strongly
acid in the Bt horizon.

\<@32\>The A or Ap horizon has hue of 7.5YR or 10YR, value of 3 to 5,
and chroma of 2 to 4.

\<@32\>The E horizon has hue of 5YR to 10YR, value of 5 or 6, and chroma
of 3 to 6. It is sand, loamy sand, or loamy fine sand.

\<@32\>The Bt horizon has hue of 10R to 5YR, value of 4 or 5, and chroma
of 4 to 8. It is sandy loam, fine sandy loam, or sandy clay loam.

\<@37\>Weston Series

\<@32\>The Weston series consists of very deep, poorly drained soils
that formed in loamy sediments. These soils are in flat and slightly
concave positions on stream terraces. The seasonal high water table is
within a depth of 1 foot from December through April in most years.
Slopes range from 0 to 2 percent. These soils are coarse-loamy,
siliceous, semiactive, thermic Typic Endoaquults.

\<@32\>Weston soils are geographically associated with Eunola, Izagora,
Mantachie, Pelham, and Yemassee soils. The moderately well drained
Eunola and Izagora and somewhat poorly drained Yemassee soils are in the
slightly higher, more convex positions on the terraces and are
fine-loamy. The somewhat poorly drained Mantachie soils are on flood
plains in areas adjacent to the Weston soils. The Pelham soils are in
positions similar to those of the Weston soils on terraces and have a
thick, sandy epipedon.

\<@32\>Typical pedon of Weston fine sandy loam, 0 to 2 percent slopes;
about 1,170 feet south and 500 feet west of the northeast corner of sec.
34, T. 3 N., R. 32 W.

\<@23\>A---0 to 4 inches; dark grayish brown (10YR 4/2) fine sandy loam;
weak medium granular structure; very friable; many medium and fine
roots; very strongly acid; clear wavy boundary.

\<@33\>Btg1---4 to 15 inches; grayish brown (10YR 5/2) fine sandy loam;
weak medium subangular blocky structure; friable; common medium and fine
roots; few faint clay films on faces of peds; common medium prominent
yellowish red (5YR 5/8) irregularly shaped masses of iron accumulation
with diffuse boundaries throughout; very strongly acid; gradual wavy
boundary.

\<@33\>Btg2---15 to 40 inches; gray (10YR 5/1) fine sandy loam; weak
medium subangular blocky structure; friable; few faint clay films on
faces of peds; common fine faint light gray (10YR 7/1) irregularly
shaped iron depletions with clear boundaries in the matrix; common
medium prominent yellowish red (5YR 5/8) masses of iron accumulation
with sharp boundaries throughout the matrix; very strongly acid; gradual
wavy boundary.

\<@33\>Btg3---40 to 68 inches; gray (10YR 5/1) sandy loam; weak coarse
subangular blocky structure; friable; few faint clay films on faces of
peds; common fine faint light gray (10YR 7/2) irregularly shaped iron
depletions with clear boundaries in the matrix; common medium prominent
yellowish red (5YR 5/8) masses of iron accumulation with sharp
boundaries throughout the matrix; very strongly acid; gradual wavy
boundary.

\<@33\>Cg---68 to 80 inches; 35 percent gray (10YR 6/1), 25 percent
olive yellow (2.5Y 6/6), 20 percent yellowish red (5YR 5/8), and 20
percent very pale brown (10YR 8/2) sandy loam; massive, thinly bedded;
very friable; areas of gray and very pale brown are iron depletions;
areas of yellowish red and olive yellow are masses of iron accumulation;
very strongly acid.

\<@8\>The solum is more than 40 inches thick. Reaction ranges from very
strongly acid to moderately acid in the A and E horizons, except in
areas where lime has been applied, and is very strongly acid or strongly
acid in the Btg and Cg horizons.

\<@32\>The A horizon has hue of 10YR, value of 3 or 4, and chroma of 1
or 2.

\<@32\>The E horizon, where present, has hue of 10YR or 2.5Y, value of 5
or 6, and chroma of 2 to 4. It has few or common redoximorphic
accumulations in shades of yellow, olive, brown, and red and
redoximorphic depletions in shades of brown and gray. It is fine sandy
loam, sandy loam, or loamy fine sand.

\<@32\>The Btg horizon has hue of 10YR or 2.5Y, value of 5 or 6, and
chroma of 1 or 2. It has common or many redoximorphic accumulations in
shades of yellow, olive, brown, and red. It is sandy loam, fine sandy
loam, or loam.

\<@32\>The Cg horizon commonly is stratified. It does not have a
dominant matrix color and is multicolored in shades of gray, brown,
yellow, and red. The texture is variable, but the range in texture
includes sandy clay loam, loam, sandy loam, and loamy sand.

\<@37\>Yemassee Series

\<@32\>The Yemassee series consists of very deep, somewhat poorly
drained soils that formed in sandy and loamy fluvial sediments. These
soils are in flat or slightly concave positions on stream terraces. The
seasonal high water table is at a depth of 1 to 1-1/2 feet from December
through April in most years. These soils are subject to occasional
flooding. Slopes range from 0 to 2 percent. These soils are fine-loamy,
siliceous, semiactive, thermic Aeric Endoaquults.

\<@32\>Yemassee soils are geographically associated with Bigbee, Eunola,
Garcon, Izagora, Pelham, and Weston soils. The Bigbee soils are on flood
plains adjacent to the Yemassee soils and are sandy throughout. The
moderately well drained Eunola and Izagora soils are in the slightly
higher, more convex positions on the terraces. The Garcon, Pelham, and
Weston soils are in the slightly lower positions on the stream terraces.
The Garcon and Pelham soils have a thick, sandy epipedon. The Weston
soils are poorly drained and are coarse-loamy.

\<@32\>Typical pedon of Yemassee fine sandy loam, 0 to 2 percent slopes,
occasionally flooded; about 2,085 feet north and 1,335 feet west of the
southeast corner of sec. 13, T. 1 N., R. 32 W.

\<@23\>A---0 to 5 inches; very dark grayish brown (10YR 3/2) fine sandy
loam; moderate medium granular structure; very friable; common medium
and fine roots; very strongly acid; clear smooth boundary.

\<@33\>E---5 to 12 inches; grayish brown (2.5Y 5/2) fine sandy loam;
weak medium granular structure; very friable; common medium and fine
roots; very strongly acid; clear wavy boundary.

\<@33\>Bt1---12 to 26 inches; olive yellow (2.5Y 6/4) sandy clay loam;
moderate medium subangular blocky structure; friable; few fine roots;
few faint clay films on faces of peds; common medium prominent strong
brown (7.5YR 5/8) masses of iron accumulation; common fine distinct
light gray (2.5Y 7/2) irregularly shaped iron depletions; very strongly
acid; gradual wavy boundary.

\<@33\>Bt2---26 to 42 inches; olive yellow (2.5Y 6/4) fine sandy loam;
weak medium subangular blocky structure; friable; few faint clay films
on faces of peds; common fine distinct light gray (2.5Y 7/2) irregularly
shaped iron depletions; few fine distinct brownish yellow (10YR 6/6)
masses of iron accumulation; very strongly acid; gradual wavy boundary.

\<@33\>Bt3---42 to 48 inches; olive yellow (2.5Y 6/4) sandy clay loam;
moderate medium subangular blocky structure; friable; few faint clay
films on faces of peds; common medium prominent strong brown (7.5YR 5/8)
masses of iron accumulation; common medium distinct light gray (2.5Y
7/2) irregularly shaped iron depletions; very strongly acid; gradual
wavy boundary.

\<@33\>Bt4---48 to 62 inches; 25 percent brownish yellow (10YR 6/6), 20
percent yellowish brown (10YR 5/6), 20 percent light gray (10YR 7/2), 20
percent strong brown (7.5YR 5/8), and 15 percent red (2.5YR 5/6) fine
sandy loam; moderate medium subangular blocky structure; friable; very
strongly acid; few faint clay films on faces of peds; areas of brownish
yellow, yellowish brown, strong brown, and red are masses of iron
accumulation; areas of light gray are iron depletions; very strongly
acid; gradual wavy boundary.

\<@33\>Btg---62 to 74 inches; light gray (10YR 7/1) fine sandy loam;
weak coarse subangular blocky structure; friable; few faint clay films
on faces of peds; common medium prominent strong brown (7.5YR 5/6),
reddish brown (2.5YR 5/4), and light yellowish brown (2.5Y 6/4) masses
of iron accumulation; very strongly acid; clear wavy boundary.

\<@33\>Cg---74 to 80 inches; light gray (10YR 7/1) sand; single grained;
loose; common coarse distinct light yellowish brown (10YR 6/4) masses of
iron accumulation; very strongly acid.

\<@8\>The solum is more than 40 inches thick. Reaction ranges from
extremely acid to moderately acid in the A and E horizons, except in
areas where lime has been applied, and ranges from extremely acid to
strongly acid in the Bt, Btg, and Cg horizons.

\<@32\>The A or Ap horizon has hue of 10YR or 2.5Y, value of 2 to 5, and
chroma of 1 or 2.

\<@32\>The E horizon, where present, has hue of 10YR or 2.5Y, value of 5
or 6, and chroma of 2 to 4. It is fine sandy loam or loamy fine sand.

\<@32\>The upper part of the Bt horizon has hue of 10YR or 2.5Y, value
of 5 or 6, and chroma of 3 to 8. It has few or common redoximorphic
accumulations in shades of yellow, olive, brown, and red and
redoximorphic depletions in shades of brown and gray. The lower part of
the horizon does not have a dominant matrix color and is multicolored in
shades of brown, yellow, red, and gray. The Bt horizon is fine sandy
loam, sandy clay loam, or clay loam.

\<@32\>The Btg horizon has hue of 10YR or 2.5Y, value of 5 to 7, and
chroma of 1 or 2. It has common or many redoximorphic accumulations in
shades of yellow, olive, brown, and red. It is fine sandy loam, sandy
clay loam, or clay loam.

\<@32\>The Cg horizon has hue of 10YR to 5Y, value of 5 to 8, and chroma
of 1 or 2. It has common or many redoximorphic accumulations in shades
of brown, yellow, or red. The texture is variable, but the range in
texture includes fine sandy loam, sandy loam, sandy clay loam, clay
loam, loamy sand, and sand. In some pedons, the Cg horizon is stratified
with contrasting textures.