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XGNB
<br /><1I
<br />LI IIT; CF GROUND SURVEY
<br />ILPROVIDED BY
<br />FCFE SIFT WEST SURVEYING
<br />I
<br />APPROXIMATE
<br />-SEND OF RAILROAD
<br />N - 55003
<br />E - 33724
<br />I
<br />a 0 0 0
<br />TPII�
<br />V I e
<br />1 _
<br />❑ O o n \\., I
<br />PHASE 2
<br />� o SQUAW GULCH VLF �
<br />� TPHIC
<br />I \
<br />REFERENCE:
<br />EXISTING GROUND TOPOGRAPHY WAS CREATED BY COMBINING THE FOLLOWING FILES
<br />RECV FROM FORESIGHT WEST SURVEYING, INC.:
<br />SQUAW GULCH BASE TORO - PHASE 1 - REVISED.DWG
<br />(RECV MARCH 14, 2010)
<br />SQUAW GULCH BASE TOPO - PHASE 2.DWG
<br />(RECV APRIL 24, 2010)
<br />SQUAW GULCH BASE TORO - PHASE 3.DWG
<br />(RECV MAY 4, 2010)
<br />CCV TORO EXPANSION 12-29-10 NORTH ARE4.DWG
<br />(RECV JANUARY 13, 2011)
<br />CCV TORO EXPANSION 01-28-11 SOUTH AREA.DWG
<br />(RECV JANUARY 28, 2011)
<br />SH67 TOP O 7-07-11.DWG
<br />(RECV JULY 11, 2011)
<br />VLF2 TOP O EXPANSION 8-05-11.DWG
<br />(RECV AUGUST 9, 2011)
<br />09028-COMOSITE-TOPO MILE LIMITS.DWG
<br />(RECV MAY 28, 2010 FROM CC&V)
<br />EXISTING IT
<br />HIGHWAY S
<br />V X
<br />V ---- -- TLBX
<br />\' TBXIL
<br />PHASE 1
<br />SQUAW GULCH VLF /
<br />-� NNW,
<br />300 .. 300 600 FEET
<br />EXPLANATION
<br />THBX - HYDROTHERMAL BRECCIA - LATE STAGE BRECCIA PIPES CONSISTING OF ANGULAR TO
<br />ROUNDED, HETEROLITHIC CLASTS IN A ROCK FLOUR MATRIX. TYPICALLY ASSOCIATED WITH PERVASIVE
<br />ARGILLIC ALTERATION.
<br />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 />= FELDSPAR, BIOTITE, HORNBLENDE AND MINOR MAGNETITE.
<br />a
<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 />MEDIUM SIZED STOCKS.
<br />XGD
<br />TPHD - PHONOLITE DIKE (SAME AS TPH)
<br />XGD - GRANODIORITE - MASSIVE TO FOLIATED, MEDIUM -TO COARSE-GRAINED, HORNBLENDE- BIOTITE
<br />a
<br />GRANODIORITE. LOCALLY OCCURS AS AN AUGEN GNEISS. INCLUDES DIABASE DIKES AND SCHISTOSE
<br />I
<br />APPROXIMATE
<br />-SEND OF RAILROAD
<br />N - 55003
<br />E - 33724
<br />I
<br />a 0 0 0
<br />TPII�
<br />V I e
<br />1 _
<br />❑ O o n \\., I
<br />PHASE 2
<br />� o SQUAW GULCH VLF �
<br />� TPHIC
<br />I \
<br />REFERENCE:
<br />EXISTING GROUND TOPOGRAPHY WAS CREATED BY COMBINING THE FOLLOWING FILES
<br />RECV FROM FORESIGHT WEST SURVEYING, INC.:
<br />SQUAW GULCH BASE TORO - PHASE 1 - REVISED.DWG
<br />(RECV MARCH 14, 2010)
<br />SQUAW GULCH BASE TOPO - PHASE 2.DWG
<br />(RECV APRIL 24, 2010)
<br />SQUAW GULCH BASE TORO - PHASE 3.DWG
<br />(RECV MAY 4, 2010)
<br />CCV TORO EXPANSION 12-29-10 NORTH ARE4.DWG
<br />(RECV JANUARY 13, 2011)
<br />CCV TORO EXPANSION 01-28-11 SOUTH AREA.DWG
<br />(RECV JANUARY 28, 2011)
<br />SH67 TOP O 7-07-11.DWG
<br />(RECV JULY 11, 2011)
<br />VLF2 TOP O EXPANSION 8-05-11.DWG
<br />(RECV AUGUST 9, 2011)
<br />09028-COMOSITE-TOPO MILE LIMITS.DWG
<br />(RECV MAY 28, 2010 FROM CC&V)
<br />EXISTING IT
<br />HIGHWAY S
<br />V X
<br />V ---- -- TLBX
<br />\' TBXIL
<br />PHASE 1
<br />SQUAW GULCH VLF /
<br />-� NNW,
<br />300 .. 300 600 FEET
<br />EXPLANATION
<br />THBX - HYDROTHERMAL BRECCIA - LATE STAGE BRECCIA PIPES CONSISTING OF ANGULAR TO
<br />ROUNDED, HETEROLITHIC CLASTS IN A ROCK FLOUR MATRIX. TYPICALLY ASSOCIATED WITH PERVASIVE
<br />ARGILLIC ALTERATION.
<br />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 />= FELDSPAR, BIOTITE, HORNBLENDE AND MINOR MAGNETITE.
<br />a
<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 />MEDIUM SIZED STOCKS.
<br />¢� TBX1L - CRIPPLE CREEK LAPILLI BRECCIA - GENERALLY MASSIVE, STRUCTURELESS, MATRIX
<br />SUPPORTED BRECCIA THATIS POORLY SORTED, TYPICAL OF DIATREMAL CRATER FILL BRECCIA. CLASTS
<br />0 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 />m ALTERATION.
<br />TPHD
<br />TPHD - PHONOLITE DIKE (SAME AS TPH)
<br />XGD - GRANODIORITE - MASSIVE TO FOLIATED, MEDIUM -TO COARSE-GRAINED, HORNBLENDE- BIOTITE
<br />a
<br />GRANODIORITE. LOCALLY OCCURS AS AN AUGEN GNEISS. INCLUDES DIABASE DIKES AND SCHISTOSE
<br />a
<br />LENSES
<br />TER - PHONOLITE - GRAY, BROWN OR PINK, APHANITIC PHONOLITE COMPOSED OF FINE-GRAINED
<br />w N
<br />d
<br />ORTHOCLASE, NEPHELINE, MINOR AEGIRINE-AUGITE, AND ANALCIME.
<br />~
<br />TPHK - FELDSPAR BEARING - PLAGIOCLASE PHONOLITE LIGHT -TO MEDIUM -GRAY, PORPHYRY WITH
<br />o
<br />®
<br />SUBHEDRAL TO EUHEDRAL, MEDIUM -TO COARSE-GRAINED PHENOCRYSTS OF ALKALI FELDSPAR WITH
<br />zo
<br />x
<br />MINOR AMOUNTS OF FELDSPATHOIDS, GLASSY APATITE AND PYROXENES.
<br />a
<br />TPHH - HORNBLENDE YROXENE BEARING - PLAGIOCLASE PHONOLITE GREY, MEDIUM -GRAINED
<br />TPHH
<br />PORPHYRY WITH EUHEDRAL TO SUBHEDRAL HORNBLENDE, AEGIRINE-AUGITE, AND ALKALI FELDSPAR
<br />PHENOCRYSTS.
<br />TPHB - BIOTITE BEARING - PLAGIOCLASE PHONOLITE GRAY, FINE-GRAINED PORPHYRY WITH EUHEDRAL
<br />BIOTITE AND ALKALI FELDSPAR PHENOCRYSTS.
<br />¢� TBX1L - CRIPPLE CREEK LAPILLI BRECCIA - GENERALLY MASSIVE, STRUCTURELESS, MATRIX
<br />SUPPORTED BRECCIA THATIS POORLY SORTED, TYPICAL OF DIATREMAL CRATER FILL BRECCIA. CLASTS
<br />0 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 />m ALTERATION.
<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 />2. REMOVED EXISTING UTILITIES FROM DRAWING.
<br />3. UPDATED EXITING GROUND TO INCLUDE MILL PLATFORM.
<br />LEGEND:
<br />EXISTING GROUND SURFACE CONTOUR EL, FEET (AERIAL SURVEY)
<br />EXISTING GROUND SURFACE CONTOUR EL, FEET (LAND SURVEY)
<br />MILL PLATFORM GROUND SURFACE CONTOUR EL, FEET
<br />STATE HIGHWAY 67
<br />EXISTING ROADS
<br />--.� EXISTING DRAINAGES
<br />EXISTING RAILROAD
<br />/— — —� SQUAW GULCH VLF BOUNDARY (LIMITS OF LINER)
<br />-- DIATREME BOUNDARY
<br />PSSA LIMITS
<br />EXISTING BUILDING
<br />I
<br />XGD - GRANODIORITE - MASSIVE TO FOLIATED, MEDIUM -TO COARSE-GRAINED, HORNBLENDE- BIOTITE
<br />a
<br />GRANODIORITE. LOCALLY OCCURS AS AN AUGEN GNEISS. INCLUDES DIABASE DIKES AND SCHISTOSE
<br />m
<br />LENSES
<br />w
<br />XGNB BIOTITE GNEISS STRONGLY FOLIATED, BIOTITE-QUARTZ-PLAGIOCLASE GNEISS TO SCHIST, WHICH
<br />d
<br />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 />2. REMOVED EXISTING UTILITIES FROM DRAWING.
<br />3. UPDATED EXITING GROUND TO INCLUDE MILL PLATFORM.
<br />LEGEND:
<br />EXISTING GROUND SURFACE CONTOUR EL, FEET (AERIAL SURVEY)
<br />EXISTING GROUND SURFACE CONTOUR EL, FEET (LAND SURVEY)
<br />MILL PLATFORM GROUND SURFACE CONTOUR EL, FEET
<br />STATE HIGHWAY 67
<br />EXISTING ROADS
<br />--.� EXISTING DRAINAGES
<br />EXISTING RAILROAD
<br />/— — —� SQUAW GULCH VLF BOUNDARY (LIMITS OF LINER)
<br />-- DIATREME BOUNDARY
<br />PSSA LIMITS
<br />EXISTING BUILDING
<br />
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