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MINEBK00263
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Last modified
1/9/2009 3:34:56 PM
Creation date
11/18/2007 12:00:09 PM
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Mine Books
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San Miguel
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v.,, <br /> a~ <br /> <br /> ;; ;, <br /> <br /> ~s, <br /> s <br /> ;~ <br /> ;~ <br /> ~~ <br />~; <br /> <br /> <br />_~._, <br />4 -t . <br />,,, <br />~ ~ <br />,..._ <br />...: _. <br />... ~ <br /> <br />' <br /> <br />. a. <br />~ 'i. ~. <br /> <br /> <br />C.I. <br />.. ~:. <br /> <br />FbTraatioa Nema. Thickness Character of rocks. <br />i~ <br /> !n feet. <br /> >k <br /> Cray or rusty-brown quartzosa sandatones~ ~ E <br /> with a variable conglomerate containing i -~ <br /> email ohert pebbles at or near the base. ~r;; <br />Dakota Forc:7ation. 126-1?5 Car~naceous shale paetin~s occur at <br /> several horizons. ,Coal iR locally de- ~ ;! <br /> veloped in these shales. Poorly pre- ' ' <br /> earned plant reaaains are the Daly fossils. ~ <br />i. <br /> <br /> <br /> lacy aiternmting beds of friable? fins- <br />w LicElar~o foricatimn. SGO-900 grained gray aaadstone and var4e~,~ted <br />~ <br /> ahales~ often sandy. Fossils have.a~ot j <br />p <br /> been Poland. <br />' <br /> <br /> (( <br />'y l <br /> Rlso vhite~ even- arad fine-grained sand- i <br />_..~ .. _. <br />is Plata saaaPatolie. <br />100.175 <br />stones separated by a th4n black lime- <br />~`~ <br /> stone or calcareous shale. i7o determin- ~i' <br /> able toasfla have been found. ~'', <br />~! <br />A aeries of reddish quartzose saaadatonea, +, <br />grits albd ooaglomerates~ the latter us- ;i?j <br />wally coaltalnilag granitic debris and i'i''. <br />fragmeata of Aigonkian achiats and quartz- ?, <br />I~. <br />itea. Several thin limestone oonglomsr- ~( <br />~,lt.-.. :° -.ts~w~ 751:(1 ataa.,ai~th small namhl es. nharar_teri zethe ~`~~. <br />upper pert. These contain Posails, among ~~ <br />zal7ioh era teeth. of a crocodile (Belodon) `'jj'; ~i <br />and of a megaloaauroid Diaoaaur, remains 'I', <br />of a ~noid fish, s gastropod like Vivi- ! <br />parusl A Union and some andeterminad ,~°„ <br />,: <br />species of'plaata. <br />Ifs! <br />~. <br />it should be borne mind that the above section is as marked a ~ e~neral- i~f'' <br />u <br />!~ <br />ed section of the Teliulide Quadrangle.a To flluetrate: The 1lancoa shales i <br />li4 ' <br />I ~~2 <br />ked 2000 feet thick sway be fovald a taw miles went of the City of Toiluride. "`' <br />,? <br />11e_near Paaetora this stasis; fay misaing~ or ia.othsr wards has- been eroded <br />g, i <br />' ': <br />aY. <br />"~ ''s' <br />,. ~ i <br /># j',i <br />_., ~ i <br />... __ _..__.. ~,~ q. <br />I4 9 <br />
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