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 />
|