PREPARED IN COOPERATION WITH - USGSOwens Valley ° 15' ° 15' ° ° ° ° ° ° ° ° ° ° ° ° °...
Transcript of PREPARED IN COOPERATION WITH - USGSOwens Valley ° 15' ° 15' ° ° ° ° ° ° ° ° ° ° ° ° °...
RiverOwens
Ow
ens
Riv
er
RiverOwenslower
Los AngelesAqueduct
Big
PineBishop
OwensRiver
CanalCr
Canal
Geiger Canal
Canal
CanalCollins
Cre
ek
Cre
ek
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
oodN
Lub
kin
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Cree
k
Oak
Sou
thNor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)
A-drain
C-drain
Freeman
Cr
Measured ground-water levels and simulated hydraulic heads for selected wells in the Owens Valley, California
ByWesley R. Danskin
1998
WHITE
SIERRA
NEVADA
SIERRA NEVADA
INY
O C
OU
NT
Y
FRESNOCOUNTY
TULARECOUNTY
MO
NO
CO
UN
TY
MOUNTAINS
INYO
MazourkaCanyon
MOUNTAINS
VALLEYOWENS
VALLEYOWENS
Alabama Hills
Volcanic
Tableland
Wauco
ba
Canyon
PovertyHills
Aqueductintake
Crater
Mountain
RedMtn
Tungsten
Hills
RoundValley
Valley
Chalfant
FRESNO COUNTYINYO COUNTY
NORTH
Mt Whitney
Owens River Go
rge
118°15'
118°15'
118°00'
118°30'
118°30'
118°45'
37°1
5'
37°0
0'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop
Laws
Big Pine
Independence
Lone Pine
EXPLANATION
395
136
395
Bedrock
Geologic contact
Boundary of theOwens Valleydrainage basin
Well field and name
Well and number
U.S. Geological Survey
Los Angeles Departmentof Water and Power
20 KILOMETERS0 5 10 15
20 MILES0 15105
Mono
Basin Sierra
Nevada
CaliforniaNevada
Area of map
North
Owens Valley
YEAR
HYDR
AULI
C HE
AD, I
N FE
ET A
BOVE
SEA
LEV
EL
For sale by the U.S. Geological SurveyBranch of Information ServicesBox 25286Denver, CO 80225-0286
For additional information write to:District ChiefU.S. Geological SurveyPlacer Hall6000 J StreetSacramento, CA 95819-6129
Laws
Bishop
Big Pine
Taboose-Aberdeen
Thibaut-Sawmill
Independence-Oak
Bairs-George
Symmes-Shepherd
LonePine
LonePine
Poleta
Canyon
Westgard P
ass
Black Canyon
Not simulated
Area simulatedwith ground-waterflow model
Valley fill
WATER-SUPPLY PAPER 2370–HMeasured ground-water levels and simulated hydraulic heads for selected wells–PLATE 1
Danskin, W.R., 1998, Evaluation of the hydrologic system and selectedwater-management alternatives in the Owens Valley, California
PREPARED IN COOPERATION WITHINYO COUNTY AND THE
LOS ANGELES DEPARTMENT OF WATER AND POWERU.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY
Hydrograph – Title of graph includes general location, well number, and model row, column, and layer. Model layer corresponding to the perforated interval of well is indicated by upper, lower, both, or unknown
348T
255
446T
13398T82
379T
363T
401T
72
USGS20A20C
USGS18A18CUSGS
14A 14C
USGS 16B 16A
USGS 17A 17C
USGS2
USGS3
USGS4 USGS
10
USGS10
252
425T
224
347
419T
160109
455T
367T
158454T 55
1T
403T
357
357
88 85
408T35
24T24AT175
327
421T362216
210
335T430T
237
501T
490T131107T
313AT
271
279
278
319T124
323AT
323T
172
3,830
3,810
3,790
3,770
3,750
3,730
1960 1970 1980 1990
3,970
3,950
3,930
3,910
3,890
3,870
1960 1970 1980 1990
3,900
3,800
3,700
3,600
3,950
3,850
3,750
3,650
1960 1970 1980 1990
3,950
3,930
3,910
3,890
3,870
3,850
1960 1970 1980 1990
3,840
3,820
3,800
3,780
3,760
3,740
1960 1970 1980 19901960 1970 1980 19901960 1970 1980 1990
3,850
3,830
3,810
3,790
3,770
3,870
1960 1970 1980 1990
3,850
3,830
3,810
3,790
3,770
3,750
1960 1970 1980 1990
3,880
3,860
3,840
3,820
3,800
3,780
1960 1970 1980 1990
3,850
3,830
3,810
3,790
3,770
3,750
1960 1970 1980 1990
3,860
3,840
3,820
3,800
3,780
3,760
1960 1970 1980 1990
3,850
3,830
3,810
3,790
3,770
3,750
1960 1970 1980 1990
3,870
3,850
3,830
3,810
3,790
3,770
1960 1970 1980 19901960 1970 1980 1990
3,850
3,830
3,810
3,790
3,770
3,770
3,850
3,830
3,810
3,790
3,770
3,870
1960 1970 1980 1990
3,890
3,870
3,850
3,830
3,810
3,790
1960 1970 1980 19901960 1970 1980 19901960 1970 1980 19901960 1970 1980 1990
3,920
3,900
3,880
3,860
3,840
3,820
1960 1970 1980 1990
3,910
3,890
3,870
3,850
3,830
3,810
1960 1970 1980 1990
3,900
3,880
3,860
3,840
3,820
3,800
1960 1970 1980 1990
3,940
3,920
3,900
3,880
3,860
3,840
1960 1970 1980 1990
3,970
3,950
3,930
3,910
3,890
3,870
1960 1970 1980 1990
3,900
3,920
3,940
3,960
3,980
4,000
1960 1970 1980 1990
4,050
4,030
4,010
3,990
3,970
3,950
4,060
4,040
4,020
4,000
3,980
3,960
1960 1970 1980 1990
4,100
4,080
4,060
4,040
4,020
4,000
1960 1970 1980 19901960 1970 1980 19901960 1970
HYDR
AULI
C HE
AD, I
N FE
ET A
BOVE
SEA
LEV
ELHY
DRAU
LIC
HEAD
, IN
FEET
ABO
VE S
EA L
EVEL
HYDR
AULI
C HE
AD, I
N FE
ET A
BOVE
SEA
LEV
ELHY
DRAU
LIC
HEAD
, IN
FEET
ABO
VE S
EA L
EVEL
HYDR
AULI
C HE
AD, I
N FE
ET A
BOVE
SEA
LEV
ELHY
DRAU
LIC
HEAD
, IN
FEET
ABO
VE S
EA L
EVEL
HYDR
AULI
C HE
AD, I
N FE
ET A
BOVE
SEA
LEV
EL
1980 1990
4,090
4,070
4,050
4,030
4,010
3,090
1960 1970 1980 19901960 1970 1980 19904,140
4,120
4,100
4,080
4,060
4,040
4,120
4,100
4,080
4,060
4,040
4,020
1960 1970 1980 19904,320
4,300
4,280
4,260
4,240
4,220
1960 1970 1980 19901960 1970 1980 19904,200
4,180
4,160
4,140
4,120
4,000
4,150
4,130
4,110
4,090
4,070
4,050
1960 1970 1980 19904,400
4,380
4,360
4,340
4,320
4,300
1960 1970 1980 19904,160
4,140
4,120
4,100
4,080
4,060
1960 1970 1980 19901960 1970 1980 19904,180
4,160
4,140
4,120
4,100
4,080
4,190
4,170
4,150
4,130
4,110
4,090
1960 1970 1980 1990
1960 1970 1980 1990
4,180
4,160
4,140
4,120
4,100
4,090
1960 1970 1980 19901960 1970 1980 19901960 1970 1980 19901960 1970 1980 19901960 1970 1980 1990
1960 1970 1980 19901960 1970 1980 19901960 1970 1980 19901960 1970 1980 19901960 1970 1980YEAR YEAR YEAR YEAR YEAR
YEAR YEAR YEAR YEAR YEAR
1990
3,850
3,830
3,810
3,790
3,770
3,750
1960 1970 1980 1990
3,850
3,830
3,810
3,790
3,770
3,750
1960 1970 1980 1990
3,730
3,830
3,810
3,790
3,770
3,750
1960 1970 1980 1990
3,850
3,830
3,810
3,790
3,770
3,750
1960 1970 1980 1990
3,770
3,750
3,730
3,710
3,690
3,670
1960 1970 1980 1990
3,750
3,730
3,710
3,690
3,670
3,650
3,750
3,730
3,710
3,690
3,670
3,650
1960 1970 1980 19901960 1970 1980 1990
3,820
3,800
3,780
3,760
3,740
3,720
1960 1970 1980 1990
4,120
4,100
4,080
4,060
4,040
4,020
1960 1970 1980 1990
3,750
3,730
3,710
3,690
3,670
3,650
1960 1970 1980 1990
3,680
3,660
3,640
3,620
3,600
3,580
1960 1970 1980 1990
3,720
3,700
3,680
3,660
3,640
3,620
1960 1970 1980 19901960 1970 1980 1990
3,700
3,680
3,660
3,640
3,620
3,600
1960 1970 1980 1990
3,730
3,710
3,690
3,670
3,650
3,630
1960 1970 1980 1990
4,150
4,130
4,110
4,090
4,070
4,050
3,900
3,880
3,860
3,840
3,820
3,800
3,900
3,880
3,860
3,840
3,820
3,800
3,900
3,880
3,860
3,840
3,820
3,800
3,900
3,880
3,860
3,840
3,820
3,800
3,910
3,890
3,870
3,850
3,830
3,810
3,770
3,750
3,730
3,710
3,690
3,670
Laws 107TRow Column Layer
7 31 upper Row Column Layer7 32 lower
Laws 252
Row Column Layer11 31 upper
Laws 313AT
Row Column Layer13 8 unknown
Bishop 278
Row Column Layer13 31 lower
Laws 271Row Column Layer16 20 both
Bishop 237Row Column Layer17 14 unknown
Bishop 279Row Column Layer21 25 upper
Bishop 501TRow Column Layer21 31 upper
Row Column Layer25 29 both
Bishop 490TRow Column Layer25 29 upper25
323T323AT 29 upper
Bishop 323T, 323AT
Bishop 131
Bishop 430TRow Column Layer26 20 upper
Row Column Layer30 29 upper30
319T124 29 lower
Bishop 319T, 124Row Column Layer32 21 upper
Bishop 335T
Row Column Layer37 24 upper
Bishop–USGS 2Row Column Layer49 26 upper
Big Pine–USGS 3Row Column Layer55 24 upper
Big Pine–USGS 4
Row Column Layer60 26 lower
Big Pine 210
Row Column Layer66 25 unknown
Big Pine 216 Big Pine–USGS 14C, 14A
Row Column Layer66 31 upper66
16B16A 31 lower
Row Column Layer66 28 upper66
14C14A 28 lower
Big Pine–USGS 16B, 16A
Big Pine 224
Row Column Layer72 26 lower
Row Column Layer72 27 upper
Big Pine 425T
Row Column Layer
Big Pine–USGS 17C, 17A
Row Column Layer90 24 upper90 24 lower
77 26 upper77
17C17A 26 lower
Taboose Creek 421T, 362 Row Column Layer91 20 both
Taboose Cr 347Row Column Layer96 20 unknown
Goodale Creek 160
Row Column Layer96 23 upper
Goodale Creek 419T
Row Column Layer100 18 unknown
Division Creek 109
Row Column Layer100 23 upper
Goodale Creek 455TRow Column Layer105 23 upper
Sawmill Creek 376T
Sawmill Creek 158
Row Column Layer106 15 lower
Row Column Layer109 17 upper
Sawmill Creek 454T
Row Column Layer114 17 lower
Thibaut Creek 55
Row Column Layer120 17 unknown
Oak Creek 88Row Column Layer123 17 both
Oak Creek 85
Row Column Layer127 19 unknown
Independence35
Row Column Layer127 21 upper
Independence 408T
Row Column Layer128 16 both
Independence 357
Row Column Layer129 12 upper
Independence 1T
Row Column Layer130 23 upper
Independence–USGS 10
Independence 327Row Column Layer130 28 lower
Row Column Layer133 20 unknown
Symmes Creek 175
Row Column Layer133 22 upper133
24AT24T 22 upper
Symmes Creek 24T, 24AT
Row Column Layer138 20 upper
Shepard Creek 403T Shepard Creek 401T, 72
Shepard Creek–USGS 18C, 18ARow Column Layer143 30 upper143
18C18A 30 lower
Row Column Layer147 17 upper
George Creek 363T
Row Column Layer148 22 upper148
398T82 22 lower
George Creek 398T, 82Row Column Layer148 30 upper
Lone Pine 379TRow Column Layer151 30 upper151
20C20A 30 lower
Row Column Layer141 20 upper141
401T72 20 both
Lone Pine–USGS 20C, 20A
Hogback Creek 13
Row Column Layer153 24 unknown
Row Column Layer159 25 upper
Lone Pine 446T
Row Column Layer168 23 unknown
Lone Pine 255
Row Column Layer168 26 upper
Lone Pine 172Row Column Layer180 27 unknown
Lone Pine 348T
Land surface datum
Measured
Upper model layerLower model layer
USGS 17C
USGS 17A
124
319T
421T
362
24T 24AT401T
398T
USGS 18AUSGS 18C
82
USGS 20CUSGS 20A
72
131
14C
14A
USGS16A
USGS16B
323T 323AT
Laws 107TRow Column Layer
7 31 upperLand-surface datum
Measuredground-water
level
Simulated hydraulichead for model layer:
UpperLower
RiverOwens
Ow
ens
Riv
er
RiverOwenslower
lower
Los Angeles
Aqueduct
Bishop
Owens
River
CanalCr
Canal
Geiger Canal
CanalCollins
Oak
Cre
ek
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
ood
N L
ubki
n
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Sou
th
Nor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)
RiverOwens
Ow
ens
Riv
er
RiverOwens
Los Angeles
Aqueduct
Bishop
Owens
River
CanalCr
Canal
Geiger Canal
CanalCollins
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle D
iaz
Cr
Car
roll
Cot
tonw
ood
N L
ubki
n
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Oak
Sou
th
Nor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
OwensLake(dry)
PleasantValley
Reservoir
Birch
Creek
Fulle
r
Goo
dale
Cr
Cr
BigPine
Canal
KlondikeLake
Warren
Lake
Rawson Canal
CanalSouth McNally
McNally
North
A-drain
DiazLake
Intake
Birch
Creek
Fulle
r
Goo
dale
Cr
Cr
BigPine
Canal
KlondikeLake
FishSprings
Fish Springs
Warren
Lake
Rawson Canal
CanalSouth McNally
McNally
North
A-drainDiazLake
Intake
FishSprings
FishSprings
C-drain
Freeman
Cr
C-drain
Freeman
Cr
FRESNO CO TULARE CO
Ground-water flowmodel grid – Rowand column numberindicated along edge
20 KILOMETERS0 5 10 15
20 MILES0 15105
Hydrogeologic model zones and hydraulic parameters for each layer of the ground-water flow modelin the Owens Valley, California
WHITE
SIERRA
NEVADA
SIERRANEVADA
INY
O C
O
MO
NO
CO
UN
TY
MOUNTAINS INYOMOUNTAINS
VALLEYOWENS
VALLEYOWENS
Alabama Hills
Volcanic
Tableland
Wauco
ba
Canyon
PovertyHills
Crater Mtn
RedMtn
Tungsten
Hills
Round
Valley
Valley
Chalfant
INYO COUNTY
NORTH
Mount Whitney
OwensRive
r
Gorg
e
118°15'
118°15'
118°00'
118°30'
118°30'37°1
5'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop
Laws
Big Pine
Independence
Lone Pine
NORTH
WHITE
SIERRA
NEVADA
SIERRANEVADA
INY
O C
O
FRESNOCOUNTY
TULARECOUNTY
MO
NO
CO
UN
TY
MOUNTAINS INYOMOUNTAINS
VALLEYOWENS
VALLEYOWENS
Alabama Hills
Volcanic
Tableland
Wauco
ba
Canyon
PovertyHills
Tungsten
Hills
Round
Valley
Valley
Chalfant
FRESNO CO
INYO COUNTY
Mount Whitney
OwensRive
r
Gorg
e
118°15'
118°15'
118°00'
118°30'
118°30'37°1
5'
37°0
0'37
°00'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop
Laws
Big Pine
Independence
Lone Pine
395
395
136
395
136
395
Hydrogeologic modelzones and hydraulicparameters – Identifier indicates model zone andrelated hydraulicparameters (see table)
Crater Mtn
RedMtn
20
100
40
Rows
Co
lum
ns
10 20 30 40 50 60 70 80 90 100
110
120
130
140
150
160
1701
180
Rows
10 20 30 40 50 60 70 80 90 100
110
120
130
140
150
160
170
1 180
1
10
20
30
40
Co
lum
ns
1
10
20
30
Rows
Co
lum
ns
10 20 30 40 50 60 70 80 90 100
110
120
130
140
150
160
1701
180
Rows
10 20 30 40 50 60 70 80 90 100
110
120
130
140
150
160
170
1 180
1
10
20
30
40
Co
lum
ns
1
10
20
30
40
FL2A3
Valley fill
Bedrock
Geologic contact
EXPLANATION FOR MAP A AND B
Boundary of theOwens Valleydrainage basin
WATER-SUPPLY PAPER 2370–HHydrogeologic model zones and hydraulic parameters for each layer of the ground-water flow model–PLATE 2
Danskin, W.R., 1998, Evaluation of the hydrologic system and selectedwater-management alternatives in the Owens Valley, California
For sale by the U.S. Geological SurveyBranch of Information ServicesBox 25286Denver, CO 80225-0286
For additional information write to:District ChiefU.S. Geological SurveyPlacer Hall6000 J StreetSacramento, CA 95819-6129
A. Upper layer of the ground-water flow model
B. Lower layer of the ground-water flow model
ByWesley R. Danskin
1998
Mono
Basin Sierra
Nevada
CaliforniaNevada
Area of map
North
Owens Valley
PREPARED IN COOPERATION WITHINYO COUNTY AND THE
LOS ANGELES DEPARTMENT OF WATER AND POWERU.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY
FRESNO CO
FL1
FL1
FL2
FL2
A3A3
A3
A3
T1 T1
T1T1
T1
T1
T1T1
T1T1
T1
T1
T1
T1
T1
T1T1
T1
FL3
FL4FL4
A3 A3
A3
A3
A3T1
A3
A2A2
A2
A2
A2A2
A2A2
A2
A2
A2A2 A2
A1 A1 A1
A2
A2 A2
A2A3
A3A3
A3A3 A3
A3
A2A3A3 A3
V3
V6V6
V5
V5
T1
T1
T1
T1T1
T1
A3
A3
T1
T1 T1T1
T2T2
T2
T2
T2
T2
T1T1
T1T1
T2T2
T2
T2
T1 T1
V5
V5V6
V6
V3V1
V3
A2
V7
V5 V5
V5
V5
V5
V4
V4
V2
A2
A1
A1 A1A1
A1
A1
A1
A1A1
A1
A1A1
A1
A1A2
A1
A1
A1
A1
A1
A1
A1
A1A1
A1
A1 A1 A1
A1
A1
A1
A1
FL6
FL6FL6
F14F15
FL5
F1F1F1F1
F18
F18 F19F21F20
F18F18
F18
F18F18
F18
F8F7F9
F9
F9
F10F11
F16F17F13F12
F2F2
F3
A3
F22
FL3 FL3FL3
FL3
FL1
FL1
FL1
FL2
F5F4 F6
F5F4 F6
FL2
A3
A3
A3A3
A3
FL3
FL3
FL3FL3
A3
A3 A3
A3
A3
F3F3
A1
A1
A1
A1A1
A1
A1A1
A2
A2
A2A2
A2
A2
A2
A2A2
A2
A2
A3A3
A3V3
V6 V6
A3
A3
A3
A3
A3
A3
A3 A1
A1
A1
A1
A1
A2
A1
A3
A3
A2
A2A1
A1
A1A1
A3
A1
A1A1
A1
A3
A3
A3
A3A3
A3
A3A3A3
V3
V3V3V4
V3
V6
V3
A2
A2
A1A2
V7
V2
V1
A2
A1
A1
A1
A1A1
A1
A1
A1
A1
A1
A1
A1
A1
FL6
FL6
FL6
F6 F15
FL5
F1F1
F1
F18
F18 F19F21F20
F18F18
F18
F18
F8F9
F9
F9F7
F10F11
F16F17F13F12
F2F2
F22
FL3
FL3 FL3
FL14
FL1
A1
A3
V5
A1
Name (related zone numbersshown in parentheses for upper,lower model layers)
Hydrogeologic model zone Transmissivity[(gal/d)/ft2]
Hydraulic parameters for model zones
Zones with interbedded volcanic deposits
Iden-tifieronplate
Uppermodellayer
Lowermodellayer
Relatedhydro-geologicsubunitforupper,lowermodellayers
Verticalconduct-ancebetweenmodellayers[(gal/d)/ft3]
Remarks and ratioof transmissivitycompared torelated zone forupper, lowermodel layers
Alluvial fan deposits, head A1 a, a 8,000 8,000 0.0100
Alluvial fan deposits, middle A2 a, a 16,000 24,000 0.0100
Alluvial fan deposits, toe A3 a, a 16,000 48,000 0.0080
Transition zone deposits
Transition zone deposits onsoutheast side of Owens Lake basin (--, T1)
T1 --, t -- 160,000 0.0010
T2 --, t -- 80,000 0.0010
Fluvial deposits FL1 c, c 40,000 110,000 0.0008
Fluvial deposits and terracegravels near Bishop (FL1, FL1)
FL2 c, c 20,000 110,000 0.0008
Fluvial and lacustrine deposits
Fluvial and lacustrine depositswith thick clay beds nearBig Pine (--, FL3)
Fluvial and lacustrine depositsnear Owens Lake, area 1 (FL3, FL3)
Fluvial and lacustrine depositsnear Owens Lake, area 2 (FL3, FL3)
FL3 c, c 20,000 80,000 0.0004 Upper zone is morepoorly sorted thanFL1
FL4 --, d -- 80,000 0.0002 Vertical conduct-ance is one-halfFL3 value
FL5 c, c 15,000 60,000 0.0004 (3:4, 3:4)
FL6 c, c 10,000 40,000 0.0003 (1:2, 1:2)
Alluvial fan fault zone nearAlabama Hills (A1-A3, A1-A3)
F1 a, a 800 1,200 0.0100 About (1:20, 1:20)
Alluvial fan fault nearRed Mountain (A2, A2)
F2 a, a 800 1,200 0.0100 About (1:20, 1:20)
Alluvial fan fault near Big Pine (A1-A3, A1-A3)
F3 a, a 800 2,400 0.0100 About (1:20, 1:20)
Fault west of Bishop (FL1, FL1) F4 c, c 4,000 11,000 0.0008 (1:10, 1:10)
Fault west of Bishop (FL2, FL2) F5 c, c 2,000 11,000 0.0008 (1:10, 1:10)
Fault west of Bishop (A3, FL1) F6 a, c 1,600 11,000 0.0008 (1:10, 1:10)
Owens Valley Fault (FL3, FL3) F7 c, c 20,000 80,000 0.0004 (1:1, 1:1)
Owens Valley Fault (FL3, FL3) F8 c, c 4,000 8,000 0.0004 (1:5, 1:10)
Owens Valley Fault (FL3 and FL5,FL3 and FL5)
F9 c, c 4,000 4,000 0.0004 About (1:5, 1:20)
Owens Valley Fault (FL5, FL5) F10 c, c 10,000 20,000
20,000
0.0004 (2:3, 1:3)
Owens Valley Fault (A3, FL5) F11 a, c 8,000
Owens Valley Fault (A1, T1) F12 a, t 1,600 16,000
0.0004 (1:2, 1:3)
Owens Valley Fault (FL5, T1) F13 c, t 2,000 8,000
0.0010 (1:5, 1:10)
Owens Valley Fault (FL6, FL6) F14 c, c 1,000 2,000
0.0010 (1:8, 1:20)
Owens Valley Fault (A3, FL6) F15 a, c 1,600 2,000
0.0003 (1:10, 1:20)
Owens Valley Fault (A3, FL6) F16 a, c 1,600 2,000
0.0003 (1:10, 1:20)
Owens Valley Fault (FL6, T1) F17 c, t 500 8,000
0.0003 (1:10, 1:20)
Springfield fault (A3, T1) F18 a, t 4,000 20,000
0.0010 (1:20, 1:20)
Springfield fault (A3, A3) F19 a, a 4,000 12,000
0.0010 (1:4, 1:8)
Springfield fault (A3, FL3) F20 a, c 4,000 20,000
0.0100 (1:4, 1:4)
Springfield fault (FL3, FL3) F21 c, c 10,000 40,000
0.0004 (1:4, 1:4)
0.0004 (1:2, 1:2)
Lone Pine sliver faults (FL6, FL6) F22 c, c 500 2,000 0.0003 (1:20, 1:20)
Alluvial fan deposits, head (A1, A1) V1 a, a 200,000 300,000 0.0100
Alluvial fan deposits, middle (A2, A2) V2 a, a 200,000 300,000 0.0100
Alluvial fan deposits, toe (A3, A3) V3 a, a 200,000 300,000 0.0080
Fluvial and lacustrine depositsnear Big Pine (FL3, FL4)
V4 c, d 200,000 300,000 0.0002
Transition-zone deposits (--, T1) V5 --, t -- 300,000 0.0010
Fluvial and lacustrinedeposits (FL3, FL3)
V6 c, c 200,000 300,000 0.0004
Fractured and highly transmissivevolcanic deposits nearCrater Mountain
Related hydrogeologic subunits are described in detail by Hollett and others, 1991 (U.S. Geological Survey Water-Supply Paper 2370-B, plate 2)
TABLE EXPLANATION
not applicableGallons per day per square foot
Gallons per day per cubic foot
--,
V7 v, v 1,500,000 1,500,000 0.0100
(--, 1:2)
Zones with faults
Major zones
(gal/d)/ft2
(gal/d)/ft3
Los AngelesAqueduct
Big
PineBishop
OwensRiver
CanalCr
Canal
Geiger Canal
Canal
CanalCollins
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
oodN
Lub
kin
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Oak
Sou
thNor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)
Los AngelesAqueduct
Big
PineBishop
OwensRiver
CanalCr
Canal
Geiger Canal
Canal
CanalCollins
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
oodN
Lub
kin
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Oak
Sou
thNor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)
Los AngelesAqueduct
BigPineBishop
OwensRiver
CanalCr
Canal
Geiger Canal
Canal
CanalCollins
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
oodN
Lub
kin
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Oak
Sou
thNor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)
Los AngelesAqueduct
Big
PineBishop
OwensRiver
CanalCr
Canal
Geiger Canal
Canal
CanalCollins
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
oodN
Lub
kin
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Oak
Sou
thNor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)
RiverOwens
Los AngelesAqueduct
Big
PineBishop
OwensRiver
CanalCr
Canal
Geiger Canal
Canal
CanalCollins
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
oodN
Lub
kin
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Oak
Sou
thNor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)
Los AngelesAqueduct
Big
PineBishop
OwensRiver
CanalCr
Canal
Geiger Canal
Canal
CanalCollins
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
oodN
Lub
kin
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Oak
Sou
thNor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)River
Owens
Ow
ens
Riv
er
RiverOwens
Ow
ens
Riv
er
RiverOwenslower
RiverOwenslower
RiverOwens
Ow
ens
Riv
er
RiverOwens
Ow
ens
Riv
er
RiverOwens
Ow
ens
Riv
er
Ow
ens
Riv
er
RiverOwens
Ow
ens
Riv
er Los AngelesAqueduct
Big
PineBishop
OwensRiver
CanalCr
Canal
Geiger Canal
Canal
CanalCollins
Cr
Cr
Creek
Creek
Coyote
FishSlough
Baker B
ig P
ine
Cr
Bir
ch
Tabo
ose
Thib
aut
Sym
mes
She
pher
d
Lon
e
Tut
tle
Dia
z C
r
Car
roll
Cot
tonw
oodN
Lub
kin
Pin
eC
r
Hog
back
North Bairs C
rSouth B
airs Cr
Saw
mill
Div
isio
n
Cre
ek
Cre
ek
Cre
ek
Creek
Creek
Cr
Cr
George
Cre
ek
Cre
ek
Cre
ek
Cre
ekCre
ek
Cre
ek
Inde
pend
ence
Oak
Sou
thNor
th O
ak
Tin
emah
aC
reek
Cree
k
Cree
k
Creek
Creek
Cr
Cr
Horton
McGee
Creek
Raw
son
Red
Mtn
Cr
Shannon
Bishop
Cr
Pin
e
Silv
er C
anyo
n
Can
yon
Col
dwat
er
TinemahaReservoir
PleasantValley
Reservoir
OwensLake(dry)
RiverOwenslower
RiverOwenslower
RiverOwenslower
RiverOwenslower
RiverOwenslower
A-drain
C-drain
Freeman
Cr
WHITE
SIERRA
NEVADA
MO
NO
CO
UN
TY
MOUNTAINS INYO MOUNTAINS
VALLEYOWENS
VALLEYOWENS
Volcanic
Tableland
Wauco
biEmbaym
ent
Crater
Mtn
RedMtn
Tungsten
HillsRoundValley
Valley
Chalfant
FRESNO COUNTYINYO COUNTY NORTH
Owens River Go
rge
118°15'
118°15'
118°00'
118°30'
118°30'
118°45'
37°1
5'
37°0
0'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop
Laws
Big Pine
Independence
Lone Pine
395
136
395
Not simulated
Area simulated with ground-waterflow model
Valley fill EXPLANATION
Bedrock
Ground-water flow model grid – Row andcolumn number indicated along edge
Average value of simulated recharge to, or discharge from the ground-water system forwater years 1970-84 – All values in cubic feetper second
Geologic contact
Boundary of the Owens Valleydrainage basin
20 KILOMETERS0 5 10 15
20 MILES0 15105
Locations and average values of simulated ground-water recharge and discharge in theOwens Valley, California, for water years 1970-84
A. Precipitation and evapotranspiration
B. Tributary streams, ungaged mountain-front runoff between tributary streams, and local runoff from bedrock outcrops within the valley fill
C. Owens River-Los Angeles Aqueduct, Lower Owens River, lakes, and reservoirs
E. Irrigation and watering of livestock
F. Springs, seeps, and pumped and flowing wells
G. Spillgate releases and underflow
D. Canals, ditches, ponds, and miscellaneous water operations
Mono
Basin SierraNevada
CaliforniaNevada
Area of map
North
Owens Valley
EXPLANATION
0 to 0.005
0.005 to 0.010
0 to 0.05
0.05 to 0.10
0.10 to 0.20
Greater than 0.20
EXPLANATION
0 to 0.10
0.10 to 0.20
0.20 to 0.40
Greater than 0.40
EXPLANATION
0 to 0.05
0.05 to 0.10
0.10 to 0.20
Greater than 0.20 0 to 0.10
0.10 to 0.20
0.20 to 0.40
Greater than 0.40
0 to 0.05 (recharge)
0 to 0.05 (discharge)
EXPLANATION
Average recharge from irrigation and stock watering – In cubic feet per second
0 to 0.05
0.05 to 0.10
0.10 to 0.20
Greater than 0.20
0 to 0.05
0.05 to 0.10
0.10 to 0.20
Greater than 0.20
EXPLANATION
0 to 0.5
0.5 to 1.0
1.0 to 2.0
Greater than 2.0
0 to 0.05
0.05 to 0.10
0.10 to 0.20
Greater than 0.20
0 to 0.05
Average recharge – In cubic feet per second
EXPLANATION
0 to 0.10
0.10 to 0.20
0.20 to 0.40
Greater than 0.40
0 to 0.10
0.10 to 0.20
0.20 to 0.40
Greater than 0.40
0 to 0.10
0.10 to 0.20
0.20 to 0.40
Greater than 0.40
Average underflow – In cubic feet per second
EXPLANATION
Average discharge – In cubic feet per second
0 to 1.0
1.0 to 2.0
2.0 to 4.0
Greater than 4.0
0 to 0.20NV
No values in this rangeNV
NV
NV
0.20 to 0.40
0.40 to 0.60
Greater than 0.60
WHITE
SIERRA
NEVADA
MO
NO
CO
UN
TY
MOUNTAINS INYO MOUNTAINS
VALLEYOWENS
VALLEYOWENS
Volcanic
Tableland
Wauco
biEmbaym
ent
Crater
Mtn
RedMtn
Tungsten
HillsRoundValley
Valley
Chalfant
FRESNO COUNTYINYO COUNTY NORTH
Owens River Go
rge
118°15'
118°15'
118°00'
118°30'
118°30'
118°45'
37°1
5'
37°0
0'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop Big Pine
Independence
Lone Pine395
136
395
WHITE
SIERRA
NEVADA
MO
NO
CO
UN
TY
MOUNTAINS INYO MOUNTAINS
VALLEYOWENS
VALLEYOWENS
Volcanic
Tableland
Wauco
biEmbaym
ent
Crater
Mtn
RedMtn
Tungsten
HillsRoundValley
Valley
Chalfant
FRESNO COUNTYINYO COUNTY NORTH
Owens River Go
rge
118°15'
118°15'
118°00'
118°30'
118°30'
118°45'
37°1
5'
37°0
0'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop
Big Pine
Independence
Lone Pine
395
136
395
WHITE
SIERRA
NEVADA
MO
NO
CO
UN
TY
MOUNTAINS INYO MOUNTAINS
VALLEYOWENS
VALLEYOWENS
Volcanic
Tableland
Wauco
biEmbaym
ent
Crater
Mtn
RedMtn
Tungsten
HillsRoundValley
Valley
Chalfant
FRESNO COUNTYINYO COUNTY NORTH
Owens River Go
rge
118°15'
118°15'
118°00'
118°30'
118°30'
118°45'
37°1
5'
37°0
0'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop
Big Pine
Independence
Lone Pine395
136
395
WHITE
SIERRA
NEVADA
MO
NO
CO
UN
TY
MOUNTAINS INYO MOUNTAINS
VALLEYOWENS
VALLEYOWENS
Volcanic
Tableland
Wauco
biEmbaym
ent
Crater
Mtn
RedMtn
Tungsten
HillsRoundValley
Valley
Chalfant
FRESNO COUNTYINYO COUNTY NORTH
Owens River Go
rge
118°15'
118°15'
118°00'
118°30'
118°30'
118°45'
37°1
5'
37°0
0'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop
Big Pine
Independence
Lone Pine395
136
395
WHITE
SIERRA
NEVADA
MO
NO
CO
UN
TY
MOUNTAINS INYO MOUNTAINS
VALLEYOWENS
VALLEYOWENS
Volcanic
Tableland
Wauco
biEmbaym
ent
Crater
Mtn
RedMtn
Tungsten
HillsRoundValley
Valley
Chalfant
FRESNO COUNTYINYO COUNTY NORTH
Owens River Go
rge
118°15'
118°15'
118°00'
118°30'
118°30'
118°45'
37°1
5'
37°0
0'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
Bishop
Big Pine
Independence
Lone Pine395
136
395
WHITE
SIERRA
NEVADA
MO
NO
CO
UN
TY
MOUNTAINS INYO MOUNTAINS
VALLEYOWENS
VALLEYOWENS
Volcanic
Tableland
Wauco
biEmbaym
ent
Crater
Mtn
RedMtn
Tungsten
HillsRoundValley
Valley
Chalfant
FRESNO COUNTYINYO COUNTY NORTH
Owens River Go
rge
118°15'
118°15'
118°00'
118°30'
118°30'
118°45'
37°1
5'
37°0
0'
37°0
0'
36°4
5'
36°3
0'
37°1
5'
37°3
0'
BishopBig Pine
Independence
Lone Pine395
136
395
0 to 0.20
0.20 to 0.40
0.40 to 0.60
Greater than 0.60
For sale by the U.S. Geological SurveyBranch of Information ServicesBox 25286Denver, CO 80225-0286
For additional information write to:District ChiefU.S. Geological SurveyPlacer Hall6000 J StreetSacramento, CA 95819-6129
Average discharge to river, aqueduct, lakes,and reservoirs – In cubic feet per second
Average recharge from river, aqueduct, lakes,and reservoirs – In cubic feet per second
Local runoff from bedrockoutcrops within the valley fill
Ungaged mountain-front runoff between tributary streams
Tributary streams
Average recharge from precipitation –In cubic feet per second
Average discharge from evapotranspiration –In cubic feet per second
Average recharge from canals and ditches –In cubic feet per second
Average recharge from miscellaneouswater operations – In cubic feet per second.Includes operational diversions of surface water,artificial ground-water recharge, and watersupplied for recreation and wildlife and forenhancement and mitigation projects
Average recharge or discharge for sewageponds – In cubic feet per second
Non-Indian lands Indian lands
Pumped and flowing wellsSprings and seeps
Average recharge from spillgate releases – In cubicfeet per second. Recharge from additional releases inwet years are included as "miscellaneous water operations" on plate 3D
DischargeRecharge
ByWesley R. Danskin
1998
20
100
Laws
Laws
Laws
Laws
Laws
Laws
WATER-SUPPLY PAPER 2370–HLocations and average values of simulated ground-water recharge and discharge–PLATE 3
Danskin, W.R., 1998, Evaluation of the hydrologic system and selectedwater-management alternatives in the Owens Valley, California
PREPARED IN COOPERATION WITHINYO COUNTY AND THE
LOS ANGELES DEPARTMENT OF WATER AND POWERU.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY
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10 20 30 40 50 60 70 80 90 100
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10 20 30 40 50 60 70 80 90 100
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10 20 30 40 50 60 70 80 90 100
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10 20 30 40 50 60 70 80 90 100
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10
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30
0 to 0.20
0.20 to 0.40
0.20 to 0.40
0.05 to 0.10
0.10 to 0.20
0 to 0.5
0.40 to 0.60
Greater than 0.60
Greater than 0.20Greater than 2.0
0 to 0.100.10 to 0.20
0.20 to 0.40
0.5 to 1.0
1.0 to 2.0
0 to 0.05
0 to 0.5
Greater than 0.40
0.05 to 0.10
0 to 0.05
0.10 to 0.20
Greater than 0.20
0 to 0.005
0.005 to 0.010
0.10 to 0.20
0 to 0.10
0 to 0.05 (recharge)
0 to 0.05 (discharge)
0.20 to 0.40Greater than 0.40
0.05 to 0.100.10 to 0.20
0 to 0.05
Greater than 0.20
0.05 to 0.10Piute-Shoshone
Indian Reservation
0.05 to 0.10
0.10 to 0.20
0 to 0.05
Greater than 0.20
1.0 to 2.0
0 to 1.0
2.0 to 4.0
Greater than 4.0
0.40 to 0.60
0 to 0.20
Greater than 0.60
0.10 to 0.20
Greater than 0.400.10 to 0.20
0.20 to 0.40
0 to 0.10
Greater than 0.40 0.10 to 0.200 to 0.10
0.20 to 0.40
Greater than 0.40
Alabama Hills
PovertyHills
Alabama Hills
PovertyHills
Alabama Hills
PovertyHills
Alabama Hills
PovertyHills
Alabama Hills
PovertyHills
Alabama Hills
PovertyHills
Alabama Hills
PovertyHills
0 to 0.05
0.10 to 0.20
Big PineIndian Rancheria
0.05 to 0.10
Fort IndependenceIndian Reservation
Greater than 0.20
Lone PineIndian Reservation
0 to 0.05