NEVADA BUREAU OF MINES AND GEOLOGY
Tcs
Qai
Tlb
Tfha
25
Qay2
40 10
20
Qay2
Tfba
Qai
Qay2
35
Qai
Tfa
25 35
55
Qau
25
30
20
20
25
Thai
Kqd
35
Tva
30
Jm
Tva
20
Tva
Tfd
Tbhi
Thai
Thai
Tbhi 70
Tva
85
45
30
Thai
65
35
Tfa
50 40
Qay
Thai
30
30
15
Qay
80
Qay2
Qay2
Qay
Tva
Qay1
Qay1
Tfsa
Tva
Tod
85
15
Tva
Tvpa
Qai 80
40
20
25
Tbhi
45
Tvkb
Tfd
70 80
Qau
Qau
65
20
Tvba 20
Tfma
35
25
20
Tvbd
Tvba Tvkp 30 35
Qai
Tvba
Tvbd Qau
Tvba
Tvka 35 20
Tvkbd
20 30
45
Tvba
20
10
25
5
35
35
Qay
30
Tspa
Tspa
Qau
Tsdm
Tsdu
Tspa
Tsa
Qay
20
25
30
Qay1
Qay2
Qfl
Qfl
Qay2
Qay1 Qay1
Qay1
Qw
Qw
Qw
Qes
Qes
Qes
Qed
Qay
Qfl
Qay3
Qay3
Qay2
Qry4
Qry1
Older Carson River alluvial deposits (middle to early? Holocene)
Qc
Holocene and Pleistocene colluvium
Qls
Landslide deposits
Qtb
Basalt talus
Qry2
Qfl
Fluvio-lacustrine deposits (late to middle Pleistocene)
Lousetown Basalt
Tcs
Sedimentary rocks of the Chalk Hills
Tod
Dacite of Occidental Quarry
Qry1
Qry1
Piedmont Alluvium Qay
Qry2
Qry 1
Qfl
Qay3
Qry1
Qfl
Qfl Qay
Qry2 Qfl
Tspa
Pyroxene andesite flows
Tsa
Silver City andesite flows, undivided
Tsd
Undivided debris flows Middle debris flow unit
Undivided debris flows
Tsdl Tsha Tst
Andesites of Flowery Peak, undivided
Tfba
Andesites of Flowery Peak, undivided
Tfha
Hornblende andesite
Tfsa
Biotite-hornblende andesite of Sugarloaf
Tfra
Biotite-hornblende-pyroxene andesite of Rocky Peak
Tfma
Biotite-hornblende-pyroxene andesite of Mount Grosh
Hornblende andesite intrusive rocks
Ts
Hornblende andesite intrusive rocks
Tva
Virginia City andesites, undivided
Tvka
Andesites of the Kate Peak series
Tvkp
Olivine-pyroxene andesite
Hornblende andesite flow rock Santiago Canyon Tuff
OLIGOCENE ROCKS Tgm
Guild Mine Member, Mickey Pass Tuff(?)
PRE-TERTIARY ROCKS Klg
Leucogranitic rock
Kgd
Hornblende-biotite quartz diorite to granodiorite
Jm
Metamorphic rocks
References
Debris flows with biotite-hornblende andesite clasts
Thai
Qry3
Qay3 Qry
Castor, S.B., Garside, L.J., Henry, C.D., Hudson, D.M., and McIntosh, W,C., 2005, Epithermal mineralization and intermediate volcanism in the Virginia City area, Nevada, in Rhoden, H.N., Steininger, R.C., and Vikre, P.G. (editors), Symposium 2005, Window to the World: Geological Society of Nevada Symposium Proceedings, p. 125-134. Hudson, D.M., 2003, Epithermal alteration and mineralization in the Comstock District, Nevada: Economic Geology, v. 98, p. 367-385. Hudson, D.M., Castor, S.B., Garside, L.J., and Henry, C.D., 2003, Preliminary geologic map of the Virginia City Quadrangle, Nevada: Nevada Bureau of Mines and Geology Open-File Report 03-15. Morrison, R.B., 1964, Lake Lahontan: Geology of the southern Carson Desert, Nevada: U.S. Geological Survey Professional Paper 401, 156 p. Morrison, R.B., 1991, Quaternary stratigraphic, hydrologic, and climatic history of the Great Basin, with emphasis on Lakes Lahontan, Bonneville, and Tecopa, in Morrison, R.B., ed., Quaternary nonglacial geology: Conterminous U.S.: Geological Society of America, Geology of North America, v. K-2, p. 26-36.
Tvkb
Biotite-hornblende andesite flows
Tvkd
Andesite debris flows
Schwartz, K.M., and Faulds, J.E., 2002, Preliminary geologic map of the Chalk Hills Quadrangle, Storey County, Nevada: Nevada Bureau of Mines and Geology Open-File Report 04-11.
Qay2 Qao
Qai
Qai
Qao
?
Qao Qao
Ql
Qfl
Qtb
Qc
?
?
Qls
Qnr
Qnb
Qnw
Qnt
Qns
QTs Contact Dashed where approximately located, short dashes indicate internal contact.
Tfa
? Fault Dashed where approximately located, queried where uncertain, dotted where concealed.
Intrusive Rocks
Tfra
Tfma
Lineament
Tfba
Tfha
Quartz vein or ledge, some showing dip.
Tfsa
Clay vein or clay along fault
Tfd
a
Thai
Alunite vein or ledge solid, dashed where approximately located. ? Lacustrine scarp/shoreline, queried where uncertain.
Tvkp Tvka Tva
Tvkbd
Strike and dip of beds
Tvkb
30
Tvkd Tvba
Tvbd
Tvpa
Qai
Qao
Tsa
Inclined
Tvs 30
Tsdm
Inclined
Vertical
Strike and plunge of columnar joints
Tsdu Tsd
Tst
Horizontal
Strike and dip of foliation in igneous rocks
Tspa
Tsha
Inclined
Strike and dip of joints
Tfsa
PRE TERTIARY
Qt
Rocks of the Naturalite Quarry
Tsbd
50
Tsdl
Tgm Kgd Jm
Field work 2002-2005 Geologic mapping was supported by the U.S. Geological Survey STATEMAP Program (Agreement No. 04-HQ-AG-0032 and 05-HQ-AG-0014)
Scale 1:24,000 Adjoining 7.5' quadrangle names 1
2
4
Stephen B. Castor, P. Kyle House, and Donald M. Hudson 2006
Qx
Ts
Qai
PRELIMINARY GEOLOGIC MAP OF THE FLOWERY PEAK QUADRANGLE, STOREY AND LYON COUNTIES, NEVADA
Qed
Anthropogenic Deposits
Tbhi
Qai
Qes
Qes
Other Deposits ? ?
Tod
Qfl
Qai
Qsp
QTa
Qed
Qay
Qry 1
Qry4
Qry2
Eolian Deposits
Lacustrine, Spring, and Related Deposits
Qry1
Tcs
Tsa
Qed
Qry1
Qay2
Tlb
Qai
Qry1
Qai
Qry1
Upper debris flow unit
Biotite-hornblende intrusive rocks
Carson River Alluvium
Qao
Qfl
Qes
Qry4
Tsdu
Tsdb
Tvkbd Biotite-bearing debris flows
Qay1
Qry1 Qry 1
Fine-grained andesite
Qw
Tsa
Qry 1
Tsfa
Tsdm
Tfa
Spring deposits (latest Holocene to late Pleistocene)
Qry1
Qry 1
Tlb
Rocks of the Virginia City Magmatic Suite
Undivided lacustrine deposits (latest to middle Pleistocene)
Qry1 Qfl Qfl
Qry3
Qfl
Spring deposits
Tfd
Ql
Qry3
Qry3
Qry3
Qay
Qry 1
Qry2
Intermediate-age mud, sand, and gravel deposits of the Carson River (late to middle? Holocene)
Qry3
Qry1
Qry 1
Qry2
Qry1
Qry3
Young mud, sand, and gravel deposits of the Carson River (latest to late Holocene)
Qry 3
Qry 1 Qry 1
QTs
Qai
Qry 3
Qay
Qry2
Qry2
Qry3
Pleistocene to Pliocene alluvium
Rocks of the Flowery Peak Magmatic Suite
Active channel and bars of the Carson River (latest Holocene)
Qry3
Qfl
Qry2
Qry
Qed
Qry
Qay2
Qay
Qes
Qfl
Qry1
Qfl
Qfl
Qes
Qfl
Qes
Qry1
Qry3
Qay Qay3
QTa
Tbhi
Carson River alluvial deposits, undivided (Holocene)
Qx
Qay2
Qay1
Qw
Qay
Qed
Qes
Qes
Qry 1
Qay
Qay2
Qes
Tsdm 25
Qes
Qay2
Qay1
Qay3
Qed
Qfl
Qry1
Qry1
Rocks of the Silver City Magmatic Suite
Qfl
Qes
Qfl
Qay1
Qai
Qry2
Qay
Qay2
Qay2
Qry1
Tuff ring deposits
Thompson, G.A., 1956, Geology of the Virginia City Quadrangle, Nevada: U.S. Geological Survey Bulletin 1042-C, 75 p., 1:52,500 map.
Qfl
Qay1
Qay1
Qed Qay3
Qnt
Qed
Qay2
Qay1
Qry1
Qes
Qay1
Tva
Qes
Qay3
Qry3
Qfl
Tsdl
Ql
30
Qay1
Qes
Qay
Qc
Tsbd
Qx
Qry1
Qes
Qay2
Qai
Qw
Qw
Qes
Qes
Qau
QTa
Tsdm
Qx
Qw
Qes
Old alluvium (middle to early Pleistocene)
Oligocene
Qay3
35
Tsbd
Tsha
Qay
Qay
Qay
Qay1
Qay
Qay
QTa
30
Tsdm
Qao
Qay
QTa
35
Qx
Pyroxene andesite flows
Silberman, M.L., White, D.E., and Keith, T.E.C., 1979, Duration of hydrothermal activity as Steamboat Springs, Nevada, from ages of spatially associated volcanic rocks. U.S. Geological Survey Professional Paper 458-D, 14 p.
Qfl
Qry2
Qay3
30
QTa
Qx
Tvs
Intrusive Rocks
Qao
Qsp
Qay
Qay1
Qay2
Qes
Qes
Qay3
Tsdu
Qay Tspa
Qay1
Qai
Qao
QTa
Tspa
Qai
Qai
Tsdu
QTa
Qay1
Tspa
Tvka
Thai
Qc
Qay1
Qay1
Qai
QTa
QTa
Qay
Qay
Qai
Tvbd
12
18
Tsha Qc Tsdu Qay
Qay3
Rhyolite breccia
Other Late Cenozoic Units
Qay2
Qx
Qx
Qt
QTa
Qay
Qay1
Qai
Tsha
Qc
Tsdu Tspa Tvba
Tspa
Qay
Qay Tvkd
Qai
Qau
Tvbd Tvkd
Tvba Tspa
Tsdu
QTa
Tsdu
Qai
Tsha
Qau
QTa Qau
30 30
Tspa
Qay
20
Tvba
17
40
Qay
Tvbd
35 12
Qai
Tvba
Qai
10
Qc
Qay1
Qay2
Qay
Qai
Qx Qt
Qay1
Tbhi Tsdu
Qau QTa
Qai
Qai
60
70
Qai
Tvba
Qai
40
Qau
Tvbd
Thai
Qau
QTs
Ql
Qnb
Qay3
Qay2
Qes
Qay
Qay
Tvba
10
30
Tvba
QTs
Tbhi
20
Qao
QTa
Qay
Thai
Qay1
Qw
QTa
45
Pyroxene andesite flows
Qay2
Qay3
Thai
Thai
Thai
40
QTls
QTa
Qay1
Qay1
Qao
Qay3
25
Qay3
Tbhi
Qay
Tvba
20 40
30
Young inactive alluvium (middle? Holocene to latest Pleistocene)
Fluvial and Lacustrine Deposits of Lake Lahontan
Qay2
Qao Tva
Qau
Tvpa
Qai
Qao
Qay2
Tva
30
Qai Qai
Tvbd
30
20
Thai
Qay
Qay1
Tva
Tvpa
Tvba
20
QTa
Qay1
Hillslope and Mass-Wasting Deposits
Qai
Qao
Qao
70
50
QTls
40
Tvka
Qai
Tbhi
Tvbd
40
60
Tvba
70
Qao
Qay2
Qay1
Glassy rhyolite
QTa
25
Tvba
Qai
Tvba
Tvba
45
5
Tvka
Tvpa 30
25
35
Qay
Tvba
Tbhi
35
Qay2
QTa
Qao
30
Qai
Qao
Young active alluvium, (latest to middle Holocene)
Intermediate-age alluvium (late to middle? Pleistocene)
55
Tfba
Qai
Qai
Qai
Qay2
Qai
Qay
Qay1 Qay1
Youngest active alluvium (latest Holocene)
Qry4
Qai
20
Tva
15
30
70 25
30
Tvkb
Tfd
30
Qao
Qay3
Qry
Qai
Qay1
Qai
Qnr
Undivided young piedmont alluvium
Qw
Qai Tfba 5
Tfba
Qay1
Qay2
Undivided piedmont alluvium
Alluvial and eolian deposits of the Wyemaha Alloformation (Morrison, 1964, 1991) (late Pleistocene)
Qay3
45
Qao
Qai
Biotite-hornblende andesite debris flows
MIOCENE ROCKS
Carson River Alluvial Deposits
Qai
QTa
Qay1
Qc
Qay3
Tvba
Tvpa
Tbhi
Tod
80
Qt
30
35
35
Tsa
Qai
Qai
70
Tva
15
20
40
Qai
Tst
30
Tbhi
Tva
Tst Qay
Tva
Qau
20
Qt
Tbhi
10
80
45
QTa
Tbhi
50
Tfsa
40
Tsd
Tfd
Qai
Tva
QTa
Qay
Tvpa
Qay3
Qt
Qau
Tsa
Tbhi
Tvba
30
80
30
40
30
Qay
Tfsa
Tva
Tvkb
70
Tsa
25
Tfd
Qns
Qns
Qay1
25
75
80
QTa
Qay
25
20
Tsfa
Qao
40
QTa
15
Qay2
Tvs
Tfra
Tfra
Qao
Qay
Qay
25 35
20
Qns
Qao
Tva
Qay3
25
50
QlsKg
30
Qt
Qay
Tbhi
Qau
40
50
Qau
Qay3
Qay
Tva
Qt Qay1
Tbhi
20
Tbhi
60
Qay Tbhi
Qt
50
60
Qt
Tva
Tbhi
Tva
Qai
Tfba
Qt
Qai
Tgm
Kgd
75
Qnb
10
Qao
Qay2
Thai
Qay 15
75
40
Qns
35
60
Qai
Qai
45
75
Tva
50
Qnt
Tfba
Qai
QTa
Qt
55
Qau
60
Kg
70
85
Tbhi
Tbhi
Qay
Tva
Tbhi
Tfra
Tfra
75
70
60
Tvs
Tbhi
65 70
40
Tfa Qay3
60
80
45
70
Tfra
55
85
25
Qau
55
30
Tvs
45
65
Tbhi
80
35
Tbhi
Thai Tbhi
15
80
15
Tva
Tbhi
Thai
Qns Tfd
10
50
Tfra
80
Thai
30 60
Qay
Jms
80 55
Tfd
Qao
50
Qnr
Qao
Tsa
Qay3 Qns
Tvbd
Eolian sand sheet
Qau
Biotite-hornblende andesite flows
Welded rhyolite airfall
35
Tsa
Qay
Tsa
30
Qsp
30
Tbhi
Jm
70
Qao
Qai
80
75
Qns
Eolian Dunes
Tvba
Qnw
QUATERNARY AND TERTIARY DEPOSITS
Piedmont Alluvial Deposits
40
50
Qed Qes
Qai
Tsd
Tsa
Qao
Qay3
Qay1
Qnt
15
70
70
Qns Tsa
80
Qns
35
Qai
5
Qai
25
Ts
Qao
Qao Qai
10
10
Qnw
20
Tsa
Tbhi
Klg
80
Tsd
Tsa
Qai
Qay2
Klg
20
40
25
Qc
Qay
35
Qai
Qay1
Tsa 60
45
Qns
Kqd
Tbhi
35
50
Klg
Qnr
50
Qt
Qai
Qc
Thai
45
25
Qau
Tsd
Tsa
Qns
Klg
Klg
45
20
35
Qai Tsa
50
Tsa
Tfba
Qay3
Tsd
Qay
Tfd
Ts
32
50
Tss Qay
Tsa
Tsfa
Qao
QTa
Tfba
QTa
Qai
35
Qay
Klg
Klg
20
Tva
Thai
Qau
Klg
35
10
15
QTa
50
Qau
Tsa
30
Thai
Tfd Tfd
40
15
Tfd
30
Qsp
Qay
55
40
10
Qns
Tfba
Qai
Tva
Qsp
Qsp
30 20
Tsa
Qai
35
Tfha
Tfd
20
10
Kgd
Kgd 20
Tsa
Qai Tsa
Tsa
Tfha
Tfd
25
50
Qsp
Tva
Tfha
50
Tfba
Tfd
Tfd
75
60
20
Tfba
Tfa
Tfa
25
Tfa
25
35
45
Qay Kgd
Qai
Tfa
20
60
25
25
35
20
45
25
30
30
Tfra
20
25
Tfd
Qai
Tsd
Jm
30
Tfba
Qay
Tfba
Tsd
Eolian Deposits
70
35
Qai
60
65
55
Extensively disturbed areas (e.g., gravel pits and borrow pits)
Qx
Qau
Qai
Qao
Qay
Qao Qay
QTa Tsfa
Qao
Tfba
Tfba
30
30
40
40
30
Tfba
45
35
45
Tfa
40
Qau
Qau
Tsa
20
Qau
Tfba
Qay2
Qay
Qau
35
35
Tfa
Qau
25
Tfba
30
Tfa
Tfra
Tfa 30
30
Tfba
40
70
40
30
25
15
75
35
Tsa
25
Mine waste and mill tailings (latest Holocene)
Qt 80
45
Tsa
30
15
Qay2
20
Tfba
Qai
Qai
Deposits of the Naturalite Dome Area
Anthropogenic Deposits
40
15
25
Tfd
Jmv
40 20
20
Tfd
35
25
20
Qau
15
Qau
Tgm
Jmv
40
Qay3 60
45
10
40
Tsa
Tgm
Tgm
Tfra
Tfd
Qai
15
Qau
45
70
50
25
Tfd
Tfa
30
45
30
45
30
20
25
Tfba
30
Tfa
30
55
Qai
20 25
Tcs
Tfra
Tfa
Qau
20
Qay2
40
20
20
Tcs
Tlb
Tcs
QUATERNARY DEPOSITS
Tfba
Flowery Peak Suite
25
Tcs
55
Virginia City Suite
20
15
15
35
30
Silver City Suite
Tcs
25
30
25
Holocene
30
Qay3
Qai
30
Qay3
Pleistocene
Tcs
Qtb
Qai
Tcs
Pliocene
10
Miocene
20
QUATERNARY
Tcs
Tlb
Qtb
Qau
Tlb
TERTIARY
Tlb
Tfba
Tfba
OPEN-FILE REPORT 06-16 PRELIMINARY GEOLOGIC MAP OF THE FLOWERY PEAK QUADRANGLE, STOREY AND LYON COUNTIES, NEVADA
Prepared as part of the STATEMAP component of the National Cooperative Geologic Mapping Program in cooperation with the U.S. Geological Survey
6
3 5
7
8
1 Steamboat 2 Chalk Hills 3 Martin Canyon 4 Virginia City 5 Misfits Flat 6 New Empire 7 Dayton 8 Como
0
0.5
0 0
0.5 1000
DRAFT
1 kilometer
2000
1 mile 3000
4000
5000 feet
CONTOUR INTERVAL 40 FEET Base map: U.S. Geological Survey Flowery Peak 7.5' Quadrangle, 1985 Universal Transverse Mercator projection, 1927 North American Datum
Preliminary geologic map. Has not undergone office or field review. Will be revised before publication.
First Edition. Printed by Nevada Bureau of Mines and Geology Digital geologic compilation by P. Kyle House, Stephen B. Castor, and Jennifer Mauldin Cartography by Jennifer Mauldin Nevada Bureau of Mines and Geology University of Nevada, Mail Stop 178 Reno, Nevada 89557-0088 (775)784-6691, ext. 2 www.nbmg.unr.edu,
[email protected] This map was printed on an electronic plotter directly from digital files. Dimensional calibration may vary between electronic plotters and X and Y directions on the same plotter, and paper may change size due to atmospheric conditions; therefore, scale and proportions may not be exact on plots of this map.