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"a <br /> 'Y layer near m1a Ar of sen:a. "n i i 3­ait wq.% at :'L­ <br /> _ cord <br /> mine. tin lorli&. -_Oaly' Iiiiorlitic sandy -)iltstorlp. <br /> SAWNTONE, buff, massive to mciderately bedded, tabular and trough sets or cross-bedding <br /> present but poorly Jrv­loT-4,d. Medium-grained, foldalAthic to lithic (local3y), locally <br /> 0 quartzitic; contains black chert in lathic Intervals. Upper 5 feet ama sewmal other in- <br /> teryaLes contain conlifl,,d plant twitaritil. OpnLo tutjs well­dovmloy-td whnrn prt3itnL <br /> 0 <br /> but not. corg,yon. Zor,tacts are sharp. Mirine. <br /> it <br /> 1 I = E I �Y -_r` -`---v- <br /> SXND5TON'F,, KID3MNIE, and 3HAI.F. marine. Sandstones buff to gray, nikNierately to <br /> well cross-bedl,o (unudlly in larqe, shallow trouth sets), fine, to OthNr <br /> units gray, shndy, e"nmmly Mile, Some ailtntonni show ripple laininhtiona. Ophlymor:15 <br /> present in a rew wwmonea, but not vonw)n. OIL- and mutistones show wv-ll-devolope, talbe.3", <br /> trails, burrows, etc. Contact with nowmarine section below Is gradational to ernalonal <br /> "nd varies now-who In vortical poAtion. Entire unit is moderately to strongly c0cwrewini) <br /> Bedding Is 9,2n(iraljy thin throughout. <br /> X. <br /> LU <br /> and SHALE, noninarin-. Sand'itone,l rilA silt'Aonell huff to <br /> 4p <br /> gray, snn-1--tone:, Kne-grniined; smnn oncillation ripple mirW ind minor c=3-bowing ets <br /> are prn.,.,nt in it,ot.h ro,,k t.,rpv:i. blank, cnrbonri�-eou.,i, cofrunonly _,tzn(iy. MrHlrijz, In <br /> --opt, Cur two -,hall lim,­itorw units near bottom. S(,av- burrow ol.ruct.uri-i hr, pre- <br /> :ient but n,t rorvi"n. nry,Lallina lim,otones near Lop probably algril In cirl&n. Whilng V, <br /> xenarall'y thin. oc <br /> cur in 5cmv- <br /> I anJ Corhiculn form the Well units an <br /> :;)me are wprikly calcareous. Contact with marine abovu gradational to <br /> unconfor-mable, with co.-il boam, below very sharp.6 Or)AL ;uld interlayerA, normarime. Coal clean at top, bottom seams bony; very <br /> --7� 11 to <br /> - rrinblf>; M'-e!ilx­volltilo bituminous, very strongly coking (Id ,cam). SlUstones grnj <br /> -3 -,ally very hAndy; massive, no beddtn4�. Coal mined at !latch Creek 3 <br /> Mark, conly, i <br /> 2 ( ..�. Wood) an­1 d4 (Bear Greek) mines and Anwinly at CM D"in mine. <br /> i � Y � m ( I � s ' � ,',�'�i k h-I <br /> huff to white,, missive to thin-bedded, locally poorly cross-bedded, usually in <br /> C Ftnw of larya Wulir 9tets. Five to nedium-griiined, feld'qQLliiC to quortLitic, contain_-, CI <br /> & ! I 0 mirior aux)unt3 or blrick Infer t. U, ­ 4 to 20 feet bleached whit#-, on outcrop, frti5h surfacer i <br /> 0 <br /> t"ray due to enrl0q,!A eod"­,led plant. Tiviterial. Qp1Lipjj)r-, n burrows preit-nt. in tleveral, <br /> di"tinct zonp-- I-veinpment varieu from poor to potxi. Si ile parting of varying <br /> rortion <br /> or(%iri n­i,r cect-r, of nj,�P�w)r; It 13 wray, gandy, nnd very iimilnr to i ­ <br />