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E <br />T , <br />Tcr <br />01 \1 r o <br />/ <br />Tse <br />O <br />r - / !'' QI <br />Ths r - 10 r <br />EXPLANATION <br />C�t'.,locflc < ally, ' , c1tv,ll+•cl wllc`l f approxiirlc-lte <br />Qal \i \ \QI I '� <br />Z -Tvs I <br />Tfc <br />PLATE 1 <br />Fault ; dashed where approximate, queried <br />where uncertain ; dotted where concealed <br />1-°A Strike and dip of compaction foliation or flow layering <br />/ \\ �\ �, -QI Ths <br />/Qc 1 - - -/ 20 <br />i Ths Tha Strike and dip of beds <br />✓ QI <br />r <br />Tse 1`I+ \I \�\ r .'/ 1000 0 2000 Feet <br />15 \\•. 1 ( QM of 500 0 500 Meters <br />Ths ' <br />_Tur -. _ Base from Lake City and Lake San <br />\\ \� `\ r Of //1 Tcr r/ Cristobal 7.5 - Minute Quadrangles, Colorado <br />Tse <br />\� \ Contour Interval -�0 feet <br />\ Thq \\ ` � / , ! <br />Tua <br />%I _ -- I` /-.-- ; ° i Ths �.• ; (��'? lQm <br />Tfc ' r o ; _ Tfc (5 50 Tur <br />\ i \ 2O `•�,Tia , <br />,Thq \\ �j�� =70 <br />\\ 5 `\ �� \ 15 <br />\ / QC ` o ©' ��� i .Ths \\ , \\ .�3T -'�.� T <br />r( I \ \\ o <br />\� \ \1° Tse `� ii a., ,o Tfc \ \\ i ,,_�`� -/ L talk Tia <br />/ • Qal \ ° dog° / <br />„x` -/• +•`!\ `, Thq 5 r-'' `°6rks!>�oNOEa / Tua J/ <br />Tm /• , 20 c <br />, / ••.`� ' ^ \moo -- - --- /� ,' ' r r/ <br />• _� \_ _ Tql sew t �A ; <br />,' II r \\\� 11 1 / /.. w o O O�� '`� ��Q� `\ �� 1'�T CGO1p QuAiCfl' I // <br />35 I�Th5r/ �' Oyes `i -Y // Tur <br />I IN Of <br />QI <br />Trn <br />Tur <br />Ths <br />`\ '\ 15' \ `may - <br />LL Tcr.. , <br />Vse `, r '�\ Tcr <br />/ Tqg <br />Tfc <br />\I Tfc t ,, �,. ,; I : - _F ---- - - - - -- <br />1 ,I 204 , <br />r \ \i Thq <br />TqI ` I. !i� Q <br />I \: <br />Q) <br />Of Qm <br />Tvs �/ f ; am <br />25 1 <br />r ! Tm Tfc <br />do f. i I\ Tcr <br />Cic <br />1 I \ \\ - f. <br />25 . �. �, QC +' i' Tur \{ I <br />_.. t . . <br />+ <br />Ths r <br />T99 Thq <br />. � •/ ' \ 1, I \ \ / I r <br />Thq <br />I\ QI I \ ,{ �. i I " Qm Tua <br />� <br />125 it 25 <br />I Tcr I . <br />Tvs , <br />\•r; ! I / ac <br />Tcr i \ <br />Thq \ i Tfc r' �,' \\ _ \j �\ <br />Thq r!, i Qm <br />Thq _ - - -- Ths <br />Feet A 1 <br />12,000 <br />11,000 <br />Tqg <br />10,000 <br />g000 <br />IIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIII <br />00015765 <br />Topographic Walll of L <br />Lake City Caldlera o <br />oc <br />L- 0 <br />Tfc TVs <br />% Ths C <br />Tql Tlhq 20 Of Tfc Tcr <br />Tse hs <br />Vertical Exaggeration 1 r 2 x <br />GEOLOGIC MAP AND SECTION <br />Tur <br />OF THE <br />See Plate 3 for map location <br />O WnTFrl WFL L , <br />$H ENR <br />I <br />Intrusive aRocks <br />Tla Al clesite dikes <br />L <br />ro <br />P <br />L <br />L <br />ris <br />L <br />H <br />0 <br />� <br />Tlq Quartz latite dikes <br />Sedimentary and Volcanic <br />L <br />Cu <br />C <br />L <br />v <br />ro <br />7 <br />N <br />u <br />I <br />N <br />C <br />I a� <br />u <br />O <br />I <br />I <br />Ya <br />I � <br />li <br />o <br />10 <br />A' Met,•rs <br />3400 <br />Tua 3200 <br />_ 3000 <br />2800 <br />LAKE <br />Qal Alluvium <br />Qc Colluvium <br />QI Landslide material <br />Rocks <br />Qf <br />Debris and earth flows <br />Qm <br />Glacial moraine <br />Tqg <br />Quartz latite lavas <br />of Grassy Mountain <br />Tqr <br />Quartz latite lavas <br />of Red Mountain <br />Tql <br />Local quartz latite <br />lava,, <br />Tua <br />I <br />Andesite lavas of <br />Uncompahgre Peak <br />Tur j <br />Rhyolite lavas of <br />Uncompahgre Peak <br />Tcr Carpenter Ridge Tuff <br />Tvs Local volcaniclastic sediments <br />L Tfc Fish Canyon Tuff <br />, Iw2 <br />Tha Local andesite lavas of Henson Formation <br />Ths Volcaniclastic sediments of Henson Formation <br />Thq Quartz latite lava,, of Henson Formation <br />T'm Volcanic mudflows <br />Tse Eureka Member of Sapinero Mesa Tuff <br />Geology by John F. Slack <br />1973 -1975 <br />DISTRICT <br />("ra(b.t - Wot� jkl, <br />�L) <br />