#1:/Tennessee Professional paper 108/sew00466

ID. Shaw, E.W. 466

Illustrating reddening and probable concentration of iron compounds near
surface; red sand with much iron oxide over impervious white clay, Grand
Junction, Hardeman County, Tennessee. 1913. Plate 57-C in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew00474

ID. Shaw, E.W. 474

Illustrating reddening and probable concentration of iron compounds near
surface;

One mile south-southeast of Oxford; upper part of white is impervious
clay and basal part of overlying red sand is more than half iron oxide.
Lafayette County, Mississippi. October 12, 1913. Plate 57-E in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew00478

ID. Shaw, E.W. 478

Stratification and general appearance of material formerly regarded as
"Lafayette Formation," at and near Oxford, the type locality, now
regarded as belonging to the Wilcox group. Uneven interfingering beds of
clay and sand three-fourths of mile north of Oxford. Lafayette County,
Mississippi. October 12, 1913. Plate 47-A in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew00481

ID. Shaw, E.W. 481

Illustrating occurrence and mode of development and the excellent
exposures afforded by old-field gullies; such gullies may have played an
important part in the Pliocene erosion of the region, though they were
no doubt much less numerous than today. The part played by the sod in
resisting erosion is well shown. Many of the gullies have rounded
instead of V-shaped head and evidently grow neither through erosion by
water flowing into their heads nor through softening of materials by
underground water issuing as a seepage, but only because of the fact
that the rain which falls in them finds erosion easier than that which
falls on sodded areas; at Oxford; shows filling after deep erosion.
Lafayette County, Mississippi. October 12, 1913. Plate 59-H in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew00483

ID. Shaw, E.W. 483

Stratification and general appearance of massive, cross-bedded, and
laminated material formerly included in the "Lafayette Formation," Now
interpreted as belonging with various formations underlying Mississippi.
Doubly cross-bedded sand of Wilcox group half mile north of Oxford.
Lafayette County, Mississippi. October 12, 1913. Plate 46-H in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew00485

ID. Shaw, E.W. 485

Residuum or material in place but modified somewhat by weathering,
though little if any part has been removed. The residuum seems to
contain material brought to it in solution and in form of minute
particles by the way of pores, from the strata removed in the Pliocene
and other epochs. Wilcox group at Oxford. Lafayette County, Mississippi.
October 13, 1913. Plate 56-C in U.S. Geological Survey. Professional
paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew00500

ID. Shaw, E.W. 500

Stratigraphic relations of Pliocene terrace deposits; terrace deposit
overlain by loess 1.5 miles south of Edwards; apparently gradation from
one to the other probably due to creep. Hinds County, Mississippi.
October 19, 1913. Plate 49-F in U.S. Geological Survey. Professional
paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew00517

ID. Shaw, E.W. 517

Illustrating reddening and probable concentration of iron compounds near
surface; gravel composed of hollow pebbles of iron oxide 1 mile north of
wharf at Natchez, Mississippi. 1913. Plate 57-B in U.S. Geological
Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01028

ID. Shaw, E.W. 1028

Typical exposures of colluvium, the colluvium shows little or
stratification and contains quartz pebbles and other elements commonly
lacking in underlying formations, also angular fragments of iron
cemented sandstone; distribution of pebbles in subsoil 1.5 miles east of
Iuka, Tishomingo County, Mississippi. September 16, 1914. Plate 52-E in
U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01032

ID. Shaw, E.W. 1032

Stratification and general appearance of massive, cross-bedded, and
laminated material formerly included in the "Lafayette Formation," Now
interpreted as belonging with various formations underlying Mississippi.
Indistinctly cross-bedded gravel 5 miles southeast of Iuka. Lafayette
County, Mississippi. September 16, 1914. Plate 46-B in U.S. Geological
Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01043

ID. Shaw, E.W. 1043

Stratification and general appearance of massive, cross-bedded, and
laminated material formerly included in the "Lafayette Formation," Now
interpreted as belonging with various formations underlying Mississippi.
Indistinctly cross-bedded sand of Eutaw formation(?), with clay pebbles
and streaks, 1 mile east of Iuka; altitude 600 feet Lafayette County,
Mississippi. September 19, 1914. Plate 46-D in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01060

ID. Shaw, E.W. 1060

Exposures suggestive of origin of colluvium, showing particularly that
it commonly fills hollows and is in some places though rarely double,
colluvium with uneven base half mile west of Iuka. Tishomingo County,
Mississippi. September 21, 1914. Plate 53-F in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01061

ID. Shaw, E.W. 1061

Exposures suggestive of origin of colluvium, showing particularly that
it commonly fills hollows and is in some places though rarely double;
colluvium with very uneven base, 1 mile west of Iuka. Tishomingo County,
Mississippi. September 21, 1914. Plate 53-D in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew1063a

ID. Shaw, E.W. 1063a

Exposures suggestive of origin of colluvium, showing particularly that
it commonly fills hollows and is in some places though rarely double;
double (?) colluvium half mile west of Iuka, upper 8 or 10 feet is from
railway cut; below are two layers, each several feet thick, with quartz
pebbles at base. Tishomingo County, Mississippi. September 22, 1914.
Plate 53-H in U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01064

ID. Shaw, E.W. 1064

Stratification and general appearance of material formerly regarded as
"Lafayette Formation," at and near Oxford, the type locality, now
regarded as belonging to the Wilcox group. Intraformational unconformity
between stratified reddish sand and white clay half mile east of Oxford.
Lafayette County, Mississippi. September 23, 1914. Plate 47-C in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01067

ID. Shaw, E.W. 1067

Stratification and general appearance of massive, cross-bedded, and
laminated material formerly included in the "Lafayette Formation," Now
interpreted as belonging with various formations underlying Mississippi.
Cross-bedded silty sand of Wilcox group at Bailey's Spring, 1 mile
southeast of square at Oxford. Lafayette County, Mississippi. September
24, 1914. Plate 46-E in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi-Professional paper 108/sew01069

ID. Shaw, E.W. 1069

Exposures suggestive of origin of colluvium, showing particularly that
it commonly fills hollows and is in some places though rarely double;
colluvium with angular fragments of iron-cemented sandstone at base.
Fourmile Creek, 2 miles east of Oxford. Lafayette County, Mississippi.
September 24, 1914. Plate 53-E in U.S. Geological Survey. Professional
paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01070

ID. Shaw, E.W. 1070

Illustrating reddening and probable concentration of iron compounds near
surface, west side of Fourmile Creek, 2 miles east of Oxford. Lafayette
County, Mississippi. September 24, 1914. Plate 57-D in U.S. Geological
Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01071

ID. Shaw, E.W. 1071

Stratification and general appearance of material formerly regarded as
"Lafayette Formation," at and near Oxford, the type locality, now
regarded as belonging to the Wilcox group. Peculiar stratification of
silty sand on east side of Fourmile Creek, 2 miles east of Oxford.
Lafayette County, Mississippi. September 24, 1914. Plate 47-G in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01072

ID. Shaw, E.W. 1072

Typical exposures of colluvium, the colluvium shows little or
stratification and contains quartz pebbles and other elements commonly
lacking in underlying formations, also angular fragments of iron
cemented sandstone. Colluvium with fragments of iron cemented sandstone
at base, south edge of Oxford. Lafayette County, Mississippi. September
24, 1914. Plate 52-B in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi- Professional paper 108/sew01073

ID. Shaw, E.W. 1073

Stratification and general appearance of massive, cross-bedded, and
laminated material formerly included in the "Lafayette Formation," Now
interpreted as belonging with various formations underlying Mississippi.
Thin, hard evenly bedded white clay 6.5miles southeast of Oxford.
Lafayette County, Mississippi. September 26, 1914. Plate 46-G in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01074

ID. Shaw, E.W. 1074

Stratification and general appearance of Pliocene and early Pleistocene
terrace deposits, most of which have been classified as "Lafayette
Formation." The strata seems to range generally from 5 to 10 feet in
thickness and to be comparatively persistent and yet lenticular and
theses seem to be diagnostic features; 6.5 miles southeast of Oxford.
Lafayette County, Mississippi. September 26, 1914. Plate 48-C in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01077

ID. Shaw, E.W. 1077

Illustrating occurrence and mode of development and the excellent
exposures afforded by old-field gullies; such gullies may have played an
important part in the Pliocene erosion of the region, though they were
no doubt much less numerous than today. The part played by the sod in
resisting erosion is well shown. Many of the gullies have rounded
instead of V-shaped head and evidently grow neither through erosion by
water flowing into their heads nor through softening of materials by
underground water issuing as a seepage, but only because of the fact
that the rain which falls in them finds erosion easier than that which
falls on sodded areas; recent colluvium on border of flood plain 1.25
miles south of Delay. Lafayette County, Mississippi. September 26, 1914.
Plate 59-A in U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01080

ID. Shaw, E.W. 1080

Stratification and general appearance of material formerly regarded as
"Lafayette Formation," at and near Oxford, the type locality, now
regarded as belonging to the Wilcox group: somewhat indistinct, uneven
interfingering beds of clay and sand three-fourths of a mile north of
Oxford. Lafayette County, Mississippi. September 27, 1914. Plate 47-D in
U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew1080a

ID. Shaw, E.W. 1080a

Illustrating reddening and probable concentration of iron compounds near
surface, three-fourths mile north of Oxford. Lafayette County,
Mississippi. September 27, 1914. Plate 57-F in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01081

ID. Shaw, E.W. 1081

Illustrating reddening and probable concentration of iron compounds near
surface, 1 mile north of station at Oxford. Lafayette County,
Mississippi. September 27, 1914. Plate 57-A in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01082

ID. Shaw, E.W. 1082

Illustrating reddening and probable concentration of iron compounds near
surface, three-fourths mile south Oxford. Lafayette County, Mississippi.
September 27, 1914. Plate 57-G in U.S. Geological Survey. Professional
paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01086

ID. Shaw, E.W. 1086

Stratification and general appearance of massive, cross-bedded, and
laminated material formerly included in the "Lafayette Formation," Now
interpreted as belonging with various formations underlying Mississippi.
Massive purple clay of Wilcox group in bottom of Isom Ravine, Oxford
Lafayette County, Mississippi. September 26, 1914. Plate 46-F in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01089

ID. Shaw, E.W. 1089

Typical exposures of colluvium; the colluvium shows little or
stratification and contains quartz pebbles and other elements commonly
lacking in underlying formations, also angular fragments of iron
cemented sandstone. Colluvium about 2 feet thick, overlain by 2 feet of
loess and underlain by Wilcox group, with an old soil at top, half mile
north of station at Oxford. Lafayette County, Mississippi. September 26,
1914. Plate 52-A in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi- Professional paper 108/sew01092

ID. Shaw, E.W. 1092

Stratification and general appearance of material formerly regarded as
"Lafayette Formation," at and near Oxford, the type locality, now
regarded as belonging to the Wilcox group. Sharply defined
interfingering beds of white clay and red sands 1 mile north of Oxford.
Lafayette County, Mississippi. September 27, 1914. Plate 47-F in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01093

ID. Shaw, E.W. 1093

Remarkable pocket-like features, suggesting filled burrows or potholes,
and pebbles and boulders of quartz and quartzite from colluvium.
Quartzite in place in colluvium three-fourths of a mile north of Oxford.
Lafayette County, Mississippi. September 27, 1914. Plate 55-G in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01096

ID. Shaw, E.W. 1096

Stratification and general appearance of material formerly regarded as
"Lafayette Formation," at and near Oxford, the type locality, now
regarded as belonging to the Wilcox group. Heavy beds of sand and clay 3
miles west of Oxford. Lafayette County, Mississippi. September 27, 1914.
Plate 47-E in U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01097

ID. Shaw, E.W. 1097

Stratification and general appearance of material formerly regarded as
"Lafayette Formation," at and near Oxford, the type locality, now
regarded as belonging to the Wilcox group. "Jumbled" clay balls and
lenses 4 miles west of Oxford. Lafayette County, Mississippi. September
28, 1914. Plate 47-B in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi- Professional paper 108/sew01099

ID. Shaw, E.W. 1099

Illustrating occurrence and mode of development and the excellent
exposures afforded by old-field gullies; such gullies may have played an
important part in the Pliocene erosion of the region, though they were
no doubt much less numerous than today. The part played by the sod in
resisting erosion is well shown. Many of the gullies have rounded
instead of V-shaped head and evidently grow neither through erosion by
water flowing into their heads nor through softening of materials by
underground water issuing as a seepage, but only because of the fact
that the rain which falls in them finds erosion easier than that which
falls on sodded areas; 7 miles west of Oxford. Lafayette County,
Mississippi. September 28, 1914. Plate 59-E in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01100

ID. Shaw, E.W. 1100

Illustrating occurrence and mode of development and the excellent
exposures afforded by old-field gullies; such gullies may have played an
important part in the Pliocene erosion of the region, though they were
no doubt much less numerous than today. The part played by the sod in
resisting erosion is well shown. Many of the gullies have rounded
instead of V-shaped head and evidently grow neither through erosion by
water flowing into their heads nor through softening of materials by
underground water issuing as a seepage, but only because of the fact
that the rain which falls in them finds erosion easier than that which
falls on sodded areas; 12 east of Batesville. Panola County,
Mississippi. September 28, 1914. Plate 59-D in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01101

ID. Shaw, E.W. 1101

Illustrating occurrence and mode of development and the excellent
exposures afforded by old-field gullies; such gullies may have played an
important part in the Pliocene erosion of the region, though they were
no doubt much less numerous than today. The part played by the sod in
resisting erosion is well shown. Many of the gullies have rounded
instead of V-shaped head and evidently grow neither through erosion by
water flowing into their heads nor through softening of materials by
underground water issuing as a seepage, but only because of the fact
that the rain which falls in them finds erosion easier than that which
falls on sodded areas; 12 miles west of Oxford. Lafayette County,
Mississippi. October 1, 1914. Plate 59-F in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01105

ID. Shaw, E.W. 1105

Illustrating occurrence and mode of development and the excellent
exposures afforded by old-field gullies; such gullies may have played an
important part in the Pliocene erosion of the region, though they were
no doubt much less numerous than today. The part played by the sod in
resisting erosion is well shown. Many of the gullies have rounded
instead of V-shaped head and evidently grow neither through erosion by
water flowing into their heads nor through softening of materials by
underground water issuing as a seepage, but only because of the fact
that the rain which falls in them finds erosion easier than that which
falls on sodded areas; 15 miles east of Batesville. Panola County,
Mississippi. September 28, 1914. Plate 59-G in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01107

ID. Shaw, E.W. 1107

Stratification and general appearance of massive, cross-bedded, and
laminated material formerly included in the "Lafayette Formation," Now
interpreted as belonging with various formations underlying Mississippi.
Thin wavy-bedded silty sand with embedded fragments of iron cemented
sandstone 5 miles east of Batesville. Panola County, Mississippi.
September 28, 1914. Plate 46-A in U.S. Geological Survey. Professional
paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew1113a

ID. Shaw, E.W. 1113a

Stratigraphic relations of Pliocene terrace deposits; terrace deposits
resting on strata of Wilcox group and overlain by 2 feet of loess 4.5
miles east of Batesville. Panola County, Mississippi. September 29,
1914. Plate 49-A in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi-Professional paper 108/sew01116

ID. Shaw, E.W. 1116

Stratification and general appearance of Pliocene and early Pleistocene
terrace deposits, most of which have been classified as "Lafayette
Formation." The strata seems to range generally from 5 to 10 feet in
thickness and to be comparatively persistent and yet lenticular and
theses seem to be diagnostic features; 3.5 miles east of Batesville.
Panola County, Mississippi. September 29, 1914. Plate 48-A in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01117

ID. Shaw, E.W. 1117

Stratification and general appearance of Pliocene and early Pleistocene
terrace deposits, most of which have been classified as "Lafayette
Formation." The strata seems to range generally from 5 to 10 feet in
thickness and to be comparatively persistent and yet lenticular and
theses seem to be diagnostic features; 3.5 miles east of Batesville.
Panola County, Mississippi. September 29, 1914. Plate 48-A in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01118

ID. Shaw, E.W. 1118

Stratification and general appearance of Pliocene and early Pleistocene
terrace deposits, most of which have been classified as "Lafayette
Formation." The strata seems to range generally from 5 to 10 feet in
thickness and to be comparatively persistent and yet lenticular and
theses seem to be diagnostic features; 3 miles east of Batesville.
Panola County, Mississippi. September 29, 1914. Plate 48-B in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01120

ID. Shaw, E.W. 1120

Uneven bedding and gravelly portions of Pliocene terrace deposits,
undulating bedding plane with old soil 3 miles east of Batesville.
Panola County, Mississippi. September 29, 1914. Plate 51-D in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01124

ID. Shaw, E.W. 1124

Uneven bedding and gravelly portions of Pliocene terrace deposits;
evenly stratified red gravel 2 miles north of Batesville. Panola County,
Mississippi. September 29, 1914. Plate 51-A in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01125

ID. Shaw, E.W. 1125

Stratigraphic relations of Pliocene terrace deposits; eastern edge of
terrace deposit resting on Wilcox group and overlain by loess 2.5 miles
north of Batesville. Panola County, Mississippi. September 29, 1914.
Plate 49-D in U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01129

ID. Shaw, E.W. 1129

Stratigraphic relations of Pliocene terrace deposits; terrace deposit
resting on strata of Wilcox group and overlain by 2 feet of loess 5
miles northeast of Sardis. Panola County, Mississippi. September 29,
1914. Plate 49-B in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi- Professional paper 108/sew01133

ID. Shaw, E.W. 1133

Recently formed deposits of known origin and history, somewhat
resembling the older colluvium but still differing rather markedly.
Product of creep half mile south of Oxford. Lafayette County,
Mississippi. October 1, 1914. Plate 54-B in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01137

ID. Shaw, E.W. 1137

Stratification and general appearance of material formerly regarded as
"Lafayette Formation," at and near Oxford, the type locality, now
regarded as belonging to the Wilcox group. Irregular stratification of
sand 1 mile south of Oxford. Lafayette County, Mississippi. October 1,
1914. Plate 47-H in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi- Professional paper 108/sew01139

ID. Shaw, E.W. 1139

Illustrating peneplain and monadnocks: Thackers Mountain, a monadock,
from point 5.5 miles south of Oxford. Lafayette County, Mississippi.
October 1, 1914. Plate 60-C in U.S. Geological Survey. Professional
paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01140

ID. Shaw, E.W. 1140

Illustrating reddening and probable concentration of iron compounds near
the surface, 4.5 miles south of Oxford; sand is white under clay lens
showing in upper part of view but reddened to each side. Lafayette
County, Mississippi. October 2, 1914. Plate 57-H in U.S. Geological
Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01141

ID. Shaw, E.W. 1141

Residuum or material in place but modified somewhat by weathering,
though little if any part as been removed. Wilcox group 6.5 miles east
of Sardis. Panola County, Mississippi. October 3, 1914. Plate 56-E in
U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01147

ID. Shaw, E.W. 1147

Remarkable pocket-like features, suggesting filled burrows or potholes,
and pebbles and boulders of quartz and quartzite from colluvium.
Botryoidal quartzite from colluvium 5.5 miles south of Oxford. Lafayette
County, Mississippi. October 4, 1914. Plate 55-F in U.S. Geological
Survey. Professional paper 108. 1918

#1:/Mississippi- Professional paper 108/sew01148

ID. Shaw, E.W. 1148

Remarkable pocket-like features, suggesting filled burrows or potholes,
and pebbles and boulders of quartz and quartzite from colluvium.
Botryoidal quartzite from colluvium 5.5 miles south of Oxford. Lafayette
County, Mississippi. October 4, 1914. Plate 55-B in U.S. Geological
Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01154

ID. Shaw, E.W. 1154

Remarkable pocket-like features, suggesting filled burrows or potholes,
and pebbles and boulders of quartz and quartzite from colluvium; pebbles
and blocks of quartz and quartzite from colluvium 1 mile northeast of
Buford Mills. Lafayette County, Mississippi. October 3, 1914. Plate 55-D
in U.S. Geological Survey. Professional paper 108. 1918

#1:/Mississippi- Professional paper 108/sew01157

ID. Shaw, E.W. 1157

Illustrating occurrence and mode of development and the excellent
exposures afforded by old-field gullies; such gullies may have played an
important part in the Pliocene erosion of the region, though they were
no doubt much less numerous than today. The part played by the sod in
resisting erosion is well shown. Many of the gullies have rounded
instead of V-shaped head and evidently grow neither through erosion by
water flowing into their heads nor through softening of materials by
underground water issuing as a seepage, but only because of the fact
that the rain which falls in them finds erosion easier than that which
falls on sodded areas; 5 miles west of Grenada. Grenada County
Mississippi. October 5, 1914. Plate 59-C in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01163

ID. Shaw, E.W. 1163

Stratification and general appearance of Pliocene and early Pleistocene
terrace deposits, most of which have been classified as "Lafayette
Formation." The strata seems to range generally from 5 to 10 feet in
thickness and to be comparatively persistent and yet lenticular and
theses seem to be diagnostic features; 8.5 miles west of Grenada,
Grenada County, Mississippi. October 5, 1914. Plate 48-H in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01170

ID. Shaw, E.W. 1170

Recently formed deposits of known origin and history, somewhat
resembling the older colluvium but still differing rather markedly.
Small filled gully 5.5 miles east of Grenada. Grenada County,
Mississippi. October 7, 1914. Plate 54-E in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01182

ID. Shaw, E.W. 1182

Stratification and general appearance of Pliocene and early Pleistocene
terrace deposits, most of which have been classified as "Lafayette
Formation." The strata seems to range generally from 5 to 10 feet in
thickness and to be comparatively persistent and yet lenticular and
theses seem to be diagnostic features; west end of main part of
petrified forest 3 miles southwest of Flora. Madison County,
Mississippi. October 9, 1914. Plate 48-F in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01187

ID. Shaw, E.W. 1187

Recently formed deposits of known origin and history, somewhat
resembling the older colluvium but still differing rather markedly.
Exposure 7 miles northeast of Canton showing coarse material left behind
in a wash; perhaps the old colluvium was formed in part by the burial of
residual accumulation of this kind. Madison County, Mississippi. October
13, 1914. Plate 54-A in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Alabama-Professional paper 108/sew01207

ID. Shaw, E.W. 1207

Stratigraphic relations of Pliocene terrace deposits; terrace deposits,
perhaps somewhat shifted and reworked, resting on Tuscaloosa formation.
Tuscaloosa, Tuscaloosa County, Alabama. May 23, 1915. Plate 49-G in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Alabama- Professional paper 108/sew01215

ID. Shaw, E.W. 1215

Residuum or material in place but modified somewhat by weathering,
though little if any part as been removed. Dr. E.A. Smith believes that
much of the iron cementation shown in railway cuts has occurred since
the cuts were made, but some is apparently much older, perhaps Pliocene.
The residuum seems to contain material brought to it in solution and in
form of minute particles by the way of pores, from the strata removed in
the Pliocene and other epochs. Tuscaloosa formation 5 miles east of
Tuscaloosa. Tuscaloosa County, Alabama. May 27, 1915. Plate 56-A in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Alabama- Professional paper 108/sew01218

ID. Shaw, E.W. 1218

Stratigraphic relations of Pliocene terrace deposits; reworked terrace
gravel on deformed and eroded edges of Tuscaloosa formation, Cottondale,
Tuscaloosa County, Alabama. May 27, 1915. Plate 49-C in U.S. Geological
Survey. Professional paper 108. 1918.

#1:/Alabama-Professional paper 108/sew01220

ID. Shaw, E.W. 1220

Uneven bedding and gravelly portions of Pliocene terrace deposits;
gravel in pit on campus at University, Tuscaloosa County, Alabama. May
27, 1915. Plate 51-C in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi- Professional paper 108/sew01237

ID. Shaw, E.W. 1237

Residuum or material in place but modified somewhat by weathering,
though little if any part has been removed, Eutaw formation about 1.75
miles northwest of Leedy, Tishomingo County, Mississippi. May 29, 1915.
Plate 56-D in U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01239

ID. Shaw, E.W. 1239

Typical exposures of colluvium, the colluvium shows little or
stratification and contains quartz pebbles and other elements commonly
lacking in underlying formations, also angular fragments of iron
cemented sandstone; colluvium, from 5 to 15 feet thick, resting on Eutaw
formation about 2 miles northwest of Leedy. Tishomingo County,
Mississippi. May 29, 1915. Plate 52-C in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01240

ID. Shaw, E.W. 1240

Exposures suggestive of origin of colluvium, showing particularly that
it commonly fills hollows and is in some places though rarely double.
Panorama of colluvium 10 miles southeast of Corinth; the concretionary
mass beneath the collecting bag throws light on the origin of the
surficial deposit, for it contains many Eutaw fossils, is very fragile
and has evidently been let down from the concretionary layer seen in the
distance at a stratigraphic position about 10 feet higher. The
concretion is of a kind characteristic of this layer. The associated
pebbles, however, are not common, if indeed such pebbles occur at all in
the underlying Eutaw formation, and hence the conclusion seems
unavoidable that the coarser parts of overlying strata have been
concentrated downward in the development of the surficial formation and
the none of the material has been transported very far. Alcorn County,
Mississippi. May 29, 1915. Plate 53-B in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01241

ID. Shaw, E.W. 1241

Exposures suggestive of origin of colluvium, showing particularly that
it commonly fills hollows and is in some places though rarely double.
Panorama of colluvium 10 miles southeast of Corinth; the concretionary
mass beneath the collecting bag throws light on the origin of the
surficial deposit, for it contains many Eutaw fossils, is very fragile
and has evidently been let down from the concretionary layer seen in the
distance at a stratigraphic position about 10 feet higher. The
concretion is of a kind characteristic of this layer. The associated
pebbles, however, are not common, if indeed such pebbles occur at all in
the underlying Eutaw formation, and hence the conclusion seems
unavoidable that the coarser parts of overlying strata have been
concentrated downward in the development of the surficial formation and
the none of the material has been transported very far. Alcorn County,
Mississippi. May 29, 1915. . Plate 53-A in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01244

ID. Shaw, E.W. 1244

Exposures suggestive of origin of colluvium, showing particularly that
it commonly fills hollows and is in some places though rarely double.
Small valley filled with colluvium 8 miles southeast of Corinth. Alcorn
County, Mississippi. May 29, 1915. Plate 53-C in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01251

ID. Shaw, E.W. 1251

Typical exposures of colluvium, the colluvium shows little or
stratification and contains quartz pebbles and other elements commonly
lacking in underlying formations, also angular fragments of iron
cemented sandstone; colluvium, largely red sand with layer of
iron-cemented sandstone fragments at base, 4 miles northeast of Holly
Springs. Marshall County, Mississippi. May 31, 1915. Plate 52-H in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01255

ID. Shaw, E.W. 1255

Typical exposures of colluvium, the colluvium shows little or
stratification and contains quartz pebbles and other elements commonly
lacking in underlying formations, also angular fragments of iron
cemented sandstone; layer of iron-cemented sandstone fragments and
concretions at of colluvium 10 miles northwest of Holly Springs.
Marshall County, Mississippi. June 1, 1915. 1914. Plate 52-D in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01257

ID. Shaw, E.W. 1257

Uneven bedding and gravelly portions of Pliocene terrace deposits;
uneven bedding planes 9 miles west of Holly Springs; red (dark) material
Wilcox group. Marshall County, Mississippi. June 1, 1915. Plate 51-B in
U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01262

ID. Shaw, E.W. 1262

Recently formed deposits of known origin and history, somewhat
resembling the older colluvium but still differing rather markedly;
colluvium in bank of small stream 7.25 southeast of Byhalia. Marshall
County, Mississippi. June 1, 1915. Plate 54-C in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01264

ID. Shaw, E.W. 1264

Recently formed deposits of known origin and history, somewhat
resembling the older colluvium but still differing rather markedly;
colluvium in bank of small stream 7.25 miles southeast of Byhalia.
Marshall County, Mississippi. June 1, 1915. Plate 54-F in U.S.
Geological Survey. Professional paper 108. 1918

#1:/Mississippi-Professional paper 108/sew01265

ID. Shaw, E.W. 1265

Recently formed deposits of known origin and history, somewhat
resembling the older colluvium but still differing rather markedly;
colluvium in bank of small stream 7.25 miles southeast of Byhalia,
somewhat similar to the old colluvium. Marshall County, Mississippi.
June 1, 1915. Plate 54-D in U.S. Geological Survey. Professional paper
108. 1918.

#1:/Mississippi-Professional paper 108/sew01266

ID. Shaw, E.W. 1266

Uneven bedding and gravelly portions of Pliocene terrace deposits:
gravel resting upon Wilcox group 7.5 miles southeast of Byhalia.
Marshall County, Mississippi. June 1, 1915. Plate 51-F in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01270

ID. Shaw, E.W. 1270

Residuum or material in place but modified somewhat by weathering,
though little if any part as been removed, Wilcox group 2 miles east of
Holly Springs. Marshall County, Mississippi. June 2, 1915. Plate 56-B in
U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01271

ID. Shaw, E.W. 1271 and 1273

Illustrating peneplain and monadnocks; both of these, peneplain with
monadnock in distance 6 miles east of Holly Springs; the road (see
sew01273) on the right follows an even-crested divide, whose top was
once a part of the peneplain. Marshall County, Mississippi. June 2,
1915. Plate 60-A and B, respectively in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01273

ID. Shaw, E.W. 1271 and 1273

Illustrating peneplain and monadnocks; both of these, peneplain with
monadnock in distance 6 miles east of Holly Springs; the road (see
sew01273) on the right follows an even-crested divide, whose top was
once a part of the peneplain. Marshall County, Mississippi. June 2,
1915. Plate 60-A and B, respectively in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01275

ID. Shaw, E.W. 1275

Illustrating peneplain and monadnocks; flat plain at altitude of 600
feet (barometric) on Ripley Road 11 miles east of Holly Springs.
Marshall County, Mississippi. June 2, 1915. Plate 60-D in U.S.
Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01276

ID. Shaw, E.W. 1276

Residuum or material in place but modified somewhat by weathering,
though little if any part as been removed, Wilcox group 13 miles east of
Holly Springs. Marshall County, Mississippi. June 2, 1915. Plate 56-F in
U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01292

ID. Shaw, E.W. 1292

Uneven bedding and gravelly portions of Pliocene terrace deposits:
gravel and clay at Rocky Springs. Claiborne County, Mississippi. June 2,
1915. Plate 51-E in U.S. Geological Survey. Professional paper 108.
1918.

#1:/Mississippi- Professional paper 108/sew01320

ID. Shaw, E.W. 1320

Stratification and general appearance of Pliocene and early Pleistocene
terrace deposits, most of which have been classified as "Lafayette
Formation." The strata seems to range generally from 5 to 10 feet in
thickness and to be comparatively persistent and yet lenticular and
theses seem to be diagnostic features; detail from sew01324; type
exposure of Port Hudson formation at Port Hickey, probably early
Pleistocene but shows same general form of stratification as Pliocene
terrace deposits. Louisiana. June 9, 1915. Plate 48-G in U.S. Geological
Survey. Professional paper 108. 1918.

#1:/Louisana-Professional paper 108/sew01324

ID. Shaw, E.W. 1324

Stratification and general appearance of Pliocene and early Pleistocene
terrace deposits, most of which have been classified as "Lafayette
Formation." The strata seems to range generally from 5 to 10 feet in
thickness and to be comparatively persistent and yet lenticular and
theses seem to be diagnostic features; part of type exposure of Port
Hudson formation at Port Hickey, probably early Pleistocene but shows
same general form of stratification as Pliocene terrace deposits.
Louisiana. June 9, 1915. Plate 48-E in U.S. Geological Survey.
Professional paper 108. 1918.

#1:/Mississippi-Professional paper 108/sew01353

ID. Shaw, E.W. 1353

Stratigraphic relations of Pliocene terrace deposits; terrace deposit
overlain by loess, with well-preserved old soil between, 15 miles east
of Yazoo City, Yazoo County, Mississippi. June 17, 1915. Plate 49-E in
U.S. Geological Survey. Professional paper 108. 1918.

#1:/Mississippi- Professional paper 108/sew01355

ID. Shaw, E.W. 1355

Illustrating occurrence and mode of development and the excellent
exposures afforded by old-field gullies; such gullies may have played an
important part in the Pliocene erosion of the region, though they were
no doubt much less numerous than today. The part played by the sod in
resisting erosion is well shown. Many of the gullies have rounded
instead of V-shaped head and evidently grow neither through erosion by
water flowing into their heads nor through softening of materials by
underground water issuing as a seepage, but only because of the fact
that the rain which falls in them finds erosion easier than that which
falls on sodded areas; 8 miles south-southwest of Yazoo City, Yazoo
County, Mississippi. June 17, 1915. Plate 59-B in U.S. Geological
Survey. Professional paper 108. 1918.

#1:/Alabama- Professional paper 108/sew01498

ID. Shaw, E.W. 1498

Typical exposures of colluvium, the colluvium shows little or
stratification and contains quartz pebbles and other elements commonly
lacking in underlying formations, also angular fragments of iron
cemented sandstone; colluvium resting on Citronelle formation 1 mile
south of Lamberts. Mobile County, Alabama. September 15, 1915. Plate
52-G in U.S. Geological Survey. Professional paper 108. 1918