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UNITED STATES DEPARTMENT OF THE INTERIOR
GEOLOGICAL SURVEY

BULLETIN 1060 PLATE 4

& ae
e S8s|o0 Construction g 32|
i | oa EE/BS| Formation Member Description a $18] section ER) rein — eset Construction
e s3ele maneeele Bs See materials
<2 (5 21
8 Hollenberg limestone] Ten-gray celular coarsely crystalline limestone with doloritic zones | Road metal and
_— Darkgray to darcbrown clayey sit containing tenses of sand and rgate and
loviom a i atenat
g
E Pwe | *Welington ght tan gay to faintly varicolored thinbedded calerecus
a 40 Peer! shale a ny canetelons and some thi tangray cystine
olomtie limestone ae
5
Fa iparatn ta Darcey to brown rm eayey st contain lenses of sand anc Mineral fies and ae
2 |_| =
3 ‘Structural stone,
Tan to gry fay hard massive thick bedded fossiliferous dolomi I
0 Herington umestone| "Ynneone wth geodes Iocaly stander Ne | aegegate ana
Pn | Nolans limestone
Poddock shale | Tanto gray thinbedded to blocky calcareous shale with fossils locally
Reddish-brown to light-ray sit and clay containing lenses of butt to | Minera! ie, aggre Gael
Sanborn “srange, fine to medium wellsorted quartz sand and thin lenses of eee Krier limestone _| Tan to gray soft clayey limestone
Pt ed il tnd fil mater
Fill materi
bealtes|l! wom apm ey aan een lt sity endive shale with hin iy zones
fed town tn, oto hard and ine to medium gained sandstone, | Aggregate, road
ees anty of quar ana imeeaies wih-cnyey | Nets nnd fi
She ait shale ranging mm light ery through Gor pray 2nd
Pc ipo ht aa mate
ert aes
LECT 1d dolomitic fossiliferous limestone with | Structural stone,
28 Ceesswall limestone andiin beds in upper par. sone | Sadat”
Pa | Wiaflate limestone Band,
Grant shale | Gray to tan silty calcareous fosiferous shale
3 Stovolt limestone ‘Hard gray massive cherty fossiliferous limestone
re
<
& Shae with ayy Thinbecided to massive fossferous shale; greenish gayto ton ang | "eral
ene layers of bentonite ihe Par it mm Gage shaie alates in uper ar and geen arn, and ayey in wer
lionte and hematite
z Doyle shate
= /‘structral stone,
Fa rosd metal
a ‘Towanda limestone | Hard tan to gray platy to blocky limestone Saareeste,
— ira
Imesvile arty calcareous shale with» thin
Hotmeavite shale | Oe Bat and ioc! enses of imestone Fil nti
Aton shote ‘ale con-
Structural stone,
Crayton ay hard foniterous stone with hin see paring Tosd meta
Fort ieytmentorn) i Bede's aaave bes m mand near bese ower | Satay,
shed armock fon
‘trent
‘State Creek shole Dark-gray thin-bedded clayey shale
Bomeston limestone] _Okato shale | Gray calcareous fssilifeous sity shale Fil material
Highiond le | Grayigreen, maroon, and red thinbedded clayey shale
to tan thick bedded fossiliferous limestone with many beds and L
Florence limestone | tnddij ct cen ad atin shale parting si, eres
‘ftrterst
limestone that splits int thin plates; five Springs abate | Banded maroon, gay and green, massive toblocty clayey sity poorly
imestone in Wiebus | Road metal and ng en
Corton ti TS aaa Til matenal sie
Mafia shale | Kinney limestone an
Al
Ae *Welington
E vinore stale | Tagen and mtn, teas to ak sity and cares
Light-green, maroon, and red soft clayey thin-bedded shale
Wreford limestone | Schroyer limestone | Gray massive limestone containing nodules and lenses of chet

Aroaty aroun | Sgn pink masse cated ad const enstaine si:
Two bes of white chy inestone separated by hale; Pra Creek
‘bed limestone ss i
aude, Springs
hole

with ght buf sft thin-bed

* Subdivisions of Wellington formation modified from Ver Wiebe (1937, p 4 and5)

STRATIGRAPHIC UNITS THAT CROP OUT IN MARION COUNTY, KANSAS,
AND THE CONSTRUCTION MATERIALS OF EACH