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T 1042 8 <br /> 4 <br /> t <br /> and Odt%'lomArAte .:1n iectjoji q9 azici SeC� <br /> ., 4 <br /> . 72 „W, . . P I tss .... tapes <br /> l.at . .3 • <br /> bade .,are. <br /> not. <br /> r'e. any,:bode ".e�copt ".th" .rl y t ; <br /> nar a... . <br /> -o l.i.te• la" (p. :I4 <br /> 1S4)....seerf ta, reist this Atzciit. It ` s' us thin!. t 411y ".v,sry <br /> ' ronatel " S <br /> bedded. s���...is 'pp �.".'#`�et t '•s;,. , ; <br /> Al ugh mainly a''voicani..c zandstozia, .16cal "tom beds <br /> 'of vOlcOnic ngl*merAte and crossswiam ziated and -graded-bedded <br /> si•ltstone occur:. The ,color varies from shade"O f gray.to <br /> brown and pink, A typical sandstone is Unsorted and has <br /> angular to sutazaunded pheWclaSts of lithi.c and crystal grains. <br /> PheAoclasts of felsite are equal. in quantity with the grsainS . <br /> , <br /> of quartz, sar-i.di.ne, biotite, sericitex magnet a and per- <br /> tbite. The T.6trix is crowded, with smaller fz S <br /> . abmexss;;s of the <br /> phenoclassts3 and has, in addition, much hemvite 1adust.to <br /> Tha can:ti.tuents,,of'ihese,beds: are mainly rbyo li.ta; and• <br /> the strati,fica i,on indicates 'a fUtVial or," in the use of the <br /> graded $11tat6nes, a lacustrine origin wiith de�osi.ti.on of <br /> volcanic s.idi x-aent into a sm l 1. ca ldsrza L$tke or large pools <br /> of ,wat6r: <br /> lire ova ; icxa <br /> Thi;s� is,, the- nost widespread and best vkposed unit in the <br /> district. The best outcrops are gust north of, Si Ivor Cliff <br /> In r3fF N l+ *ec o- 16 ind. S19-:;4-,, sec. 7, T. 22 $o , R. 72 Y♦ The <br /> flew coVery an area of approxi.-tia.tely t�,vr - square wi les, anti is <br />