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<br />LIMITS OF,,GROUND SURVEY o
<br />PROVIDED BY
<br />FORESIGHT WEST SURVEYING. TIBX
<br />F TEIX1L
<br />- DIATREME
<br />3 / BOU DARY
<br />PHASE 1
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<br />TPH
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<br />EXISTI G STATE 4.
<br />%Nb HIGH AY 67 , d
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<br />N 55,00
<br />EXPLANATION
<br />THBX - HYDROTHERMAL BRECCIA - LATE STAGE BRECCIA PIPES CONSISTING OF ANGULAR TO
<br />THBX ROUNDED, HETEROLITHIC CLASTS IN A ROCK FLOUR MATRIX. TYPICALLY ASSOCIATED WITH PERVASIVE
<br />LL ARGILLIC ALTERATION.
<br />rn TLB - BIOTITE BEARING - LAMPROPHYRE DIKE DARK - GREEN, FINE -TO MEDIUM - GRAINED PORPHYRY
<br />TLB WITH BIOTITE PHENOCRYSTS IN A FINE - GRAINED GROUNDMASS CONSISTING OF ANALCIME, ALKALI
<br />a L FELDSPAR, BIOTITE, HORNBLENDE AND MINOR MAGNETITE.
<br />0
<br />of - -
<br />TLBX LAMPROPHYRE BRECCIA LATE -STAGE LAMPROPHYRIC BRECCIA PIPE CONSISTING OF BOTH
<br />MATRIX AND CLAST SUPPORTED HETEROLITHIC BRECCIA WITH ABUNDANT DARK -GREEN LAMPROPHYRE
<br />g CLASTS AND VARIABLE LATE CARBONATE ALTERATION.
<br />TSY - TEPHRIPHONOLITE - GREY, MEDIUM -TO FINE - GRAINED INTRUSIVE COMPOSED OF ORTHOCLASE,
<br />PLAGIOCLASE, PYROXENE AND MINOR HORNBLENDE AND ANALCIME, COMMONLY OCCURING AS SMALL TO
<br />J MEDIUM SIZED STOCKS.
<br />TPHD TPHD - PHONOLITE DIKE (SAME AS TPH)
<br />a TPH TPH - PHONOLITE - GRAY, BROWN OR PINK, APHANITIC PHONOLITE COMPOSED OF FINE- GRAINED
<br />� ORTHOCLASE, NEPHELINE, MINOR AEGIRINE - AUGITE, AND ANALCIME.
<br />o rn
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<br />~ TPHK - FELDSPAR BEARING - PLAGIOCLASE PHONOLITE LIGHT -TO MEDIUM -GRAY, PORPHYRY WITH
<br />0 TPH SUBHEDRAL TO EUHEDRAL, MEDIUM -TO COARSE - GRAINED PHENOCRYSTS OF ALKALI FELDSPAR WITH
<br />0 F j MINOR AMOUNTS OF FELDSPATHOIDS, GLASSY APATITE AND PYROXENES.
<br />TPHH - HORNBLENDE YROXENE BEARING - PLAGIOCLASE PHONOLITE GREY, MEDIUM - GRAINED
<br />TPHH PORPHYRY WITH EUHEDRAL TO SUBHEDRAL HORNBLENDE, AEGIRINE - AUGITE, AND ALKALI FELDSPAR
<br />PHENOCRYSTS.
<br />E TPHEI TPHB - BIOTITE BEARING - PLAGIOCLASE PHONOLITE GRAY, FINE - GRAINED PORPHYRY WITH EUHEDRAL
<br />J BIOTITE AND ALKALI FELDSPAR PHENOCRYSTS.
<br />a TBX7 L - CRIPPLE CREEK LAPILLI BRECCIA - GENERALLY MASSIVE, STRUCTURELESS, MATRIX
<br />SUPPORTED BRECCIA THAT IS POORLY SORTED, TYPICAL OF DIATREMAL CRATER FILL BRECCIA. CLASTS
<br />Y� TBX1L ARE SUB - ANGULAR TO SUB - ROUNDED AND PRIMARILY COMPOSED OF VARIOUS PHONOLITE UNITS WITH
<br />OCCASIONAL PRECAMBRIAN FRAGMENTS. COMMONLY SHOWS VARYING DEGREES OF HYDROTHERMAL
<br />ALTERATION.
<br />Z XGD - GRANODIORITE - MASSIVE TO FOLIATED, MEDIUM -TO COARSE - GRAINED, HORNBLENDE- BIOTITE
<br />a XGD GRANODIORITE. LOCALLY OCCURS AS AN AUGEN GNEISS. INCLUDES DIABASE DIKES AND SCHISTOSE
<br />m ( LENSES.
<br />1
<br />XGNB XGNB — BIOTITE GNEISS STRONGLY FOLIATED, BIOTITE— QUARTZ — PLAGIOCLASE GNEISS TO SCHIST, WHICH
<br />a IS LOCALLY MIGMATITIC.
<br />NOTE:
<br />1. GEOLOGY MAP WAS PROVIDED BY CC &V TO AMEC ON JULY 20, 2007 IN A DRAWING
<br />CALLED INTERPRETIVE GEOLOGICAL MAP OF THE CRIPPLE CREEK MINING DISTRICT.
<br />LEGEND:
<br />EXISTING GROUND SURFACE CONTOUR EL, FEET
<br />STATE HIGHWAY 67
<br />EXISTING ROADS
<br />— EXISTING DRAINAGES
<br />EXISTING RAILROAD
<br />- -/ SQUAW GULCH VLF BOUNDARY
<br />— — DIATREME BOUNDARY
<br />/— PSSA LIMITS
<br />APPROXIMATE ' ��� _s F _ , PEFFRENCE:
<br />-=AND OF RAILROAD
<br />N 55003 / \ #1� a' ' - -� f' X,ISfING GRCUIII, ILI iJG'r n, E'il NIBi III G YIE h:'L,(LvIIJG 1L-S
<br />� 1
<br />RECV FROM SIGHT NEST SURVEYING, INC.: E 33724 ' SO AN GULCH
<br />BASF- TOFO - PHASE Eh VL:ED.DWG
<br />g,- - E_ - - -Ef�, SQUAWCGULCHI BASE TOPO �- PHASE 7 DIN';
<br />-I 2010
<br />"BF' E- _ SCUAW GULCH BAS Oi -0 PHASE 3 DV'1G
<br />F, �- , (RECV MAY 4 ?.010
<br />C.V IC�O EX'ANSiO,•: 12-29-10 NOf <,H AREADVJG
<br />RECV JAN'1AeY 13, 2011)
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<br />V TOP O EXPANSION 01 -
<br />28
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<br />RE V JANUARY 28 20 11
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<br />-S / l ®3 -�_.? _ ch ! I.:. (RECV AUGUST 9, 2011
<br />N 54,000 )
<br />�.; 019028- CCMOSITF TORO MLE LIMITS.DWG
<br />(RECV MAY 28, 2010 FROM CC &V) PROJECT
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