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UNITED STATES DEPARTMENT OF THE INTERIOR
GEOLOGICAL SURVEY Water Resources Division
DATA ON WELLS, SPRINGS, AND THERMAL SPRINGS
IN LONG VALLEY, MONO COUNTY, CALIFORNIA
By
R. E. Lewis
7 y -
OPEN-FILE REPORT
Menlo Park, California January 16, 1974
CONTENTS
ILLUSTRATIONS
Page
os Q- 3.H.Q scop g- - - - - - - - - - - - jLocation and general features of the area 4Previous work and acknowledgments 4Conversion factors 5Well- and spring-numbering system 6
Shallow test-drilling program 7u J.ass il icat ion ot gp^ings /Temperature measurements in wells and test wells 8References cited 8
Figure 1. Index map 2. Index of quadrangle maps
3-13. Maps showing location of wells and springs3.4.5.6.7.8.9.
10.11.12.13.
T.T.T.T.T.T.T.T.T.T.T.
22233334444
S.,S.,S.,s.,S.,S.,S.,S.,S.,S.,S.,
R.R.R.R.R.R.R.R.R.R.R.
2728292728293027282930
T?
P
P
P
P
P
P
JD
PageQ
in: 11
1213
14151 A
171 R
19 20
21
TABLES
Page Table 1. Description of wells and springs 22
2. Chemical analyses of water 333. Temperature measurements in wells 39
DATA ON WELLS, SPRINGS, AND THERMAL SPRINGS IN LONG VALLEY, MONO COUNTY, CALIFORNIA
By R. E. Lewis
INTRODUCTION
Purpose and Scope
The U.S. Geological Survey started hydrologic, geologic, and geophysical investigations in Long Valley, Calif., in 1972 as part of a national program of geothermal research. As a result of this research, considerable basic data have been collected. The purpose of this report is to make these hydrologic data readily available. The scope of this report includes the tabulation of recent and historical data from wells, test wells, springs, and thermal springs. Included in these data are water-level measurements or flow rates and water temperatures shown in table 1 and chemical analyses shown in table 2. Temperature gradients (change in temperature with well depth) and bottom hole temperature measurements made in selected wells and test wells are shown in table 3.
Location and General Features of the Area
Long Valley is in southwestern Mono County, in east-central California about 35 mi (56 km) northwest of Bishop (fig. 1). The area included in this investigation encompasses about 270 mi2 (700 km2 ) and includes Long Valley and all its contributory drainage areas. The maximum relief of the area is 5,488 ft (1,673 m). The land-surface altitudes range from about 6,780 ft (2,067 m) above sea level at the surface of Lake Crowley to 12,268 ft (3,739 m) at Mount Morrison in the Sierra Nevada near the southern border of the area. The difference in altitudes within this relatively small area is 5,488 ft (1,673 m) and results in extremes of climate.
Precipitation at Long Valley Dam, altitude 6,800 ft (2,073 m), is about 10 in (25 cm) annually. Precipitation along the Sierra Nevada is considerably greater about 28.7 in (72.9 cm) annually at Mammoth Lakes, Calif., altitude 8,930 ft (2,722 m) and 56.5 in (144 cm) at Mammoth Mountain Pass, altitude 9,500 ft (2,896 m). Between 60 and 70 percent of the precipitation falls as snow during the winter months. Summer temperatures in the valley seldom exceed 90°F (32°C [Celsius]); winter temperatures are commonly below 0°F (-18°C).
The study area covers parts of six topographic quadrangles (fig. 2) The locations of wells and springs are shown in figures 3-13.
Previous Work and Acknowledgments
Most of the hydrologic data from Long Valley are from the prominent thermal springs in the area. The most spectacular area, Casa Diablo, was first mentioned in the literature by Whiting (1888) and Russell (1889), Several of the more prominent thermal springs in the Long Valley area were visited by Waring (1915) and briefly described in his paper on the springs of California. A later paper by Stearns, Stearns, and Waring (1937) repeated Waring f s data with minor additional information; the data from that paper were included in a recent report by Waring (1965) but were not updated. A report by the California Department of Water Resources (1967) proposed a water budget for the valley but was primarily concerned with water quality; numerous chemical and spectrographic analyses of surface water, ground water, and water from springs are included in the report. Kaysing (1970) summarized the general features of the major thermal springs in the area but did not include any chemical analyses of the spring waters in his compilation.
The writer acknowledges the assistance of Messrs. Richard Nakahara and Lindsay A. Swain of the U.S. Geological Survey, Hawaii District, in the field collection of well and spring data and test-well drilling in May-July 1972. The cooperation of the U.S. Forest Service, Bureau of Land Management, and the Los Angeles Department of Water and Power in granting drilling permission on lands owned or controlled by them is greatly appreciated.
Conversion Factors
In this report all water temperatures are reported in degrees Celsius (°C). Temperatures originally reported in degrees Fahrenheit (°F) were changed to °C. Degrees F are converted to °C by subtracting 32° and multiplying by 5/9.
In most reports published since 1900, concentrations of the various chemical constituents are reported in parts per thousand, per hundred thousand, or per million. In this report all concentrations are reported in milligrams per liter. Water containing less than about 7,000 ppm (parts per million) of dissolved solids has a density close to unity, and concentration values, for practical purposes, are the same whether expressed in parts per million or milligrams per liter. However, water containing more than about 7,000 ppm of dissolved solids has a density appreciably above unity, and the concentration values expressed in one unit cannot be equated to those expressed in the other (Waring, 1965, P. 4).
Factors for converting English units to the International System of Units (SI) are given below to four significant figures. However, in the text the metric equivalents are shown only to the number of significant figures consistent with the values for the English units.
English
acregal/min (gallon per minute)ft (foot)in (inch)mi (mile)
(square mile)
Multiply by
4.047 x 10"10.063090.30482.5401.6092.590
Metric (SI)
ha (hectare)1/s (liter per second)m (meter)cm (centimeter)km (kilometer)
(square kilometer)
Well- and Spring-Numbering System
Wells and springs are assigned numbers according to their location in the rectangular system for the subdivision of public land. For example, as shown in the accompanying diagram, in the well number 3S/29E-2A1 the part of the number preceding the slash indicates the township (T. 3 S.), the part between the slash and the hyphen indicates the range (R. 29 E.), the number between the hyphen and the letter indicates the section (sec. 2), and the letter indicates the 40-acre subdivision of the section.
MOUNT DIAilO BASE LINE
\V
T.I S.
T.2 S.
\ \
T.3 S.
\
\ T.4 S
R.I E. R.2 E. R.28 E. R.29E.
\
\
\
\
\
\\
6
7
18
19
30
31
5
8
17
20
29
32
4
9
16
21
28
33
3
10
15
22
27
34
2
11
14
23
26
35
/12
13
24
25
36
D
E
M
N
C
F,A
0
B
G'K
P
H
1
Q
2AI
/
Within the 40-acre (16-ha) tract wells and springs are numbered serially, as indicated by the final digit. Thus, well 3S/29E-^A1 is the first well to be listed in the NE%NE%, sec. 2, T. 3 S., R. 29 E., Mount Diablo base line and meridian. Springs are numbered similarly except that an S is placed between the 40-acre (16-ha) subdivision letter and the final digit, as shown in the following spring number: 3S/28E-35ES1.
The letter Z, substituted for the letter designating the 40-acre (16-ha) tract, indicates the well or spring was plotted from unverified descriptions; the described locations of such wells or springs were visited, but the data could not be correlated with existing wells or springs.
SHALLOW TEST-DRILLING PROGRAM
Forty-seven test wells were drilled in May, June, and October 1972 and May 1973 using the hollow-stem auger rig. The locations of the wells are shown in figures 3-13. Depth of the holes ranged from 6 to 107 ft (1.8 to 33 m), and the aggregate depth of the holes is 2,478 ft (755 m). The test wells were drilled to obtain (1) the depth to the ground-water surface, (2) geothermal-gradient measurements, and (3) geologic information about the water-bearing properties of the shallow sedimentary deposits.
Polyvinyl-chloride (PVC) pipe, 2 in (5 cm) in diameter, was set in 40 of the holes. Well points, 18 in (46 cm) in length, were placed at the bottom of the PVC pipe in 28 of the holes; slotted PVC pipe was used in 6 holes. In six test wells where drilling was terminated above the water table, closed-end PVC pipe was emplaced and filled with water in order to obtain subsequent measurements of the geothermal gradient.
CLASSIFICATION OF SPRINGS
Strictly defined, any spring (or well) water whose average temperature is noticeably above the mean annual temperature of the air at the same locality may be classed as thermal (Waring, 1965, p. 4). Among European springs that are developed commercially, only those whose temperature is higher than about 20°C are classified as thermal. In the United States, only those springs are called thermal whose temperature is 15 Fahrenheit degrees (8.4 Celsius degrees) above the mean annual temperature of the air at their localities. In areas where the mean annual air temperature is low, some springs that do not freeze in winter because of their natural protective conditions are considered to be thermal; in tropical areas some springs that are only a few degrees warmer than the temperature of the air may be considered thermal.
In the Long Valley area the average annual temperature is about 45°F (7.2°C). By United States standards, then, and for the purpose of this report, any spring having a temperature of 45° + 15°F or 60°F (15.6°C) may be classified as thermal.
TEMPERATURE MEASUREMENTS IN WELLS AND TEST WELLS
Temperature measurements were obtained from selected wells and test wells at various depth intervals using a measuring system borrowed from J. H. Sass of the U.S. Geological Survey in Menlo Park, Calif. The measuring system consisted of a multiconductor cable and hoist, a thermistor thermometer, and a resistance measuring system and is described in detail in Sass and others (1971). Temperatures converted from measured resistances and their depths are shown in table 3.
REFERENCES CITED
California Department of Water Resources, 1967, Investigation ofgeothermal waters in the Long Valley area, Mono County: California Dept. Water Resources rept., 141 p.
Kaysing, W. C., ed., 1970, Thermal springs of the western United States: Santa Barbara, Calif., Paradise Publishers, 36 p.
McNitt, J. R., 1963, Exploration and development of geothermal power in California: California Div. Mines and Geology, spec. rept. 75, 44 p.
Russell, I. C., 1889, Quaternary history of Mono Valley, California, in Eighth annual report of the United States Geological Survey, 1886-87, J. W. Powell, director: U.S. Geol. Survey annual repts., p. 261-394.
Sass, J. H., Lachenbruch, A. H., Monroe, R. J., Green, G. W., andMoses, T. H., Jr., 1971, Heat flow in the western United States: Jour. Geophys. Research, v. 76, no. 26, p. 6376-6413.
Stearns, N. D., Stearns, H. T., and Waring, G. A., 1937, Thermal springs in the United States: U.S. Geol. Survey Water-Supply Paper 679-B, p. 59-206.
Waring, G. A., 1915, Springs of California: U.S. Geol. Survey Water- Supply Paper 338, 410 p.
Waring, G. A., 1965, Thermal springs of the United States and othercountries of the world--a summary, as revised by R. R. Blankenship and Ray Bentall: U.S. Geol. Survey Prof. Paper 492, 383 p.
Whiting, H. A., 1888, Mono County: California Mining Bureau Eighth annual report, p. 352-401.
19°00'
REA OF V/INDEX MAP
37°30'
MAOERA COUNTY ? Mammoth X Lakes
10 20 30 KILOMETERS
FIGURE 1. Index map.
38°00'
37°45'
37 U30
119°00' 118 0 45' 118°30
MONOCRATERS
1953R.r "
T.2S. F1
U -
DFVII <J
POSTPILE1953 T4S Fl
COWTRACK MTN
27 E.
JURE 3
1962
R.28 E. R.29 E.::::::::::. ::::::! ;; : :;::;;::::::::|
[filFiGURE.ii FIGURE|::i::::i4::::::l 5
JURE6
_
CURE10
FIGURE FIGURE7 8
i_ j.
FIGURE FIGURE11 12
LMT. MORRISON
1953
GLASSMOUNTAIN
1962
1
_.,. IL2JL.L.
FIGURE9
_j
FIGURE13
_LCASA DIABLO MTN.
1953
3B°00'
37 U45
37 U 30119°00 118°45' 118°30
6 MILES
02468 KILOMETERS
individual township maps are indicated by shaded areas and are shown in figures 3 through 13
FIGURE 2. Index of quadrangle maps.
10
Base from U.S. Geological Survey Mono Craters, 1953, Cowtrack Mtn., 1962, Devils Postpile, 1953, and Mt. Morrison, 1953
'FIGURE:!-:: i;3;;:i:i
FIGURE6
FIGURE10
FIGURE4
FIGURE7
FIGURE11
FIGURE5
FIGURE8
FIGURE12
FIGURE9
FIGURE13
EXPLANATION om WELL AND NUMBERJSl SPRING AND NUMBER
2 MILES
3 KILOMETERSCONTOUR INTERVAL 80 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 x 10" 1 )
FIGURE 3. Location of wells and springs in T. 2 S., R. 27 E.
11
118°55' R.28 E
Base from U.S. Geological Survey Cowtrack Mtn., 1962, and Mt. Morrison, 1953
FIGURE3
FIGURE6
FIGURE10
'.FIGURE;;!!!!!.4.!!l!l!
FIGURE7
FIGURE11
FIGURE5
FIGURE8
FIGURE12
FIGURE9
FIGURE13
. EXPLANATION oD1 WELL AND NUMBER Q?S1 SPRING AND NUMBER
2 MILES
3 KILOMETERSCONTOUR INTERVAL 80 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 x ID' 1 )
FIGURE 4. Location of wells and springs in T. 2 S., R. 28 E.
12
R.29 E. 118°45'
37°45'
Base from U.S. Geological Survey Cowtrack Mtn. , 1962, Glass Mountain 1962, Mt. Morrison, 1953, and Casa Diablo Mtn., 1953
FIGURE3
FIGURE6
FIGURE10
FIGURE4
FIGURE7
FIGURE11
iFiGUREiiiii! ; 5iiiii;
FIGURE8
FIGURE12
FIGURE9
FIGURE13
EXPLANATION
o pl WELL AND NUMBER<t>a SITE OF DESTROYED WELL
AND NUMBER
2 MILES
3 KILOMETERSCONTOUR INTERVAL 40 AND 80 FEET
DATUM IS MEAN SEA LEVEL-1(To convert feat to maters, multiply by 3.048 x 10 )
FIGURE 5. Location of wells in T. 2 S., R. 29 E.
13
ii9°oo' R.27 E.
37°40'
Base from U.S. Geological Survey Devils Postpile, 1953. and Mt. Morrison, 1953
FIGURE3
'FIGURE;!!!!!;; 6 I;;;::
FIGURE10
FIGURE4
FIGURE7
FIGURE11
FIGURE5
FIGURE8
FIGURE12
FIGURE9
FIGURE13
EXPLANATION oE1 WELL AND NUMBER
2 MILES
3 KILOMETERS
CONTOUR INTERVAL 80 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 x 10" 1 )
FIGURE 6. Location of wells in T. 3 S., R. 27 E.
14
37°40'
Base from U.S. Geological Survey Mt. Morrison, 1953
FIGURE 3
FIGURE6
FIGURE 10
FIGURE 4
FIGURE;;;;;;; 7 :;;;;!
FIGURE 11
FIGURE 5-
FIGURE8
FIGURE 12
FIGURE9
FIGURE 13
EXPLANATION oR1 WELL AND NUMBER *ES1 THERMAL SPRING AND
SPRING AND NUMBER NUMBER
2 MILES
3 KILOMETERSCONTOUR INTERVAL 80 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 x JO' 1 )
FIGURE 7. Location of wells and springs in T. 3 $., R. 28 £.
15
Base from U.S. Geological Survey Mt. Morrison, 1953, and Casa Diablo Mtn., 1953
FIGURE3
FIGURE6
FIGURE10
FIGURE4
FIGURE7
FIGURE11
FIGURE5
iFIGUREi;;;;H8;==:;;
FIGURE12
FIGURE9
FIGURE13
EXPLANATION WELL AND NUMBER of51 SPRING AND NUMBERSITE OF DESTROYED ^S1 THERMAL SPRING AND
WELL AND NUMBER NUMBER
2 MILES
3 KILOMETERS
CONTOUR INTERVAL 40 AND 80 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 * 10" 1 )
FIGURE 8. Location of wells and springs in T. 3 S., R. 29 E.
16
118°40' R.30 E.
37°40'
Base from U.S. Geological Survey Casa Diablo Mtn.,1953
FIGURE3
FIGURE6
FIGURE10
FIGURE4
FIGURE7
FIGURE11
FIGURE5
FIGURE8
FIGURE12
FIGURE;;;;;;;; 9 ;;;!;;;
FIGURE13
EXPLANATION 0M1 WELL AND NUMBER JDBS1 SPRING AND NUMBER+ K1 SITE OF DESTROYED
WELL AND NUMBER
2 MILES
3 KILOMETERS
CONTOUR INTERVAL 40 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 x 10~ l )
FIGURE 9. Location of wells and springs in T. 3 $., R. 30 E.
17
ii9°oo' R.27 E.
Base from U.S. Geological Survey DeviIs Postpi le, 1953, and Mt. Morrison, 1953
FIGURE3
FIGURE6
IFIGUREI;iiiiilOiiili
FIGURE4
FIGURE7
FIGURE11
FIGURE5
FIGURE8
FIGURE12
FIGURE9
FIGURE13
EXPLANATION
0B1 WELL AND NUMBER
2 MILES
3 KILOMETERSCONTOUR INTERVAL 80 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 x Id" 1 )
FIGURE 10. Location of wells in T. 4 $., R. 27 E.
18
R.28 E. 118°50'
37°35'
Base from U.S. Geological Survey Mt. Morrison, 1953
FIGURE3
FIGURE6
FIGURE10
FIGURE4
FIGURE7
iFIGURE:!:i:::l !:!:::
FIGURE5
FIGURE8
FIGURE12
FIGURE9
FIGURE13
EXPLANATION
0M WELL AND NUMBER <^ FSI SPRING AND NUMBER
<J> R1 SITE OF DESTROYEDWELL AND NUMBER
2 MILES
3 KILOMETERSCONTOUR INTERVAL 80 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 x 10" 1 )
fIGURE 11. Location of wells and springs in T. 4 S., R. 28 E.
19
37°35'
Base from U.S. Geological Survey . Mt. Morrison, 1953, and Casa Oiablo Mtn., 1953
FIGURE3
FIGURE6
FIGURE10
FIGURE4
FIGURE7
FIGURE11
FIGURE5
FIGURE8
JFIGUREi
mm
FIGURE9
FIGURE13
EXPLANATIOND1
0 WELL AND NUMBER
S1 SPR1NG AND NUMBER
nsiTHERMAL SPRING AND NUMBER
2 MILES
3 KILOMETERS
CONTOUR INTERVAL 40 AND 80 FEET DATUM IS MEAN SEA LEVEL
-1,(To convert feet to meters, multiply by 3.048 x 10" )
FIGURE 12. Location of wells and springs in T. 4 S ., R. 29 E.
20
118°40' R.30 E.XX
37°35'
Base from U.S. Geological Survey Casa Diablo Mtn., 1953
FIGURE3
FIGURE6
FIGURE10
FIGURE4
FIGURE7
FIGURE11
FIGURE5
FIGURE8
FIGURE.12
FIGURE9
'FIGURE;;!!!!!J.ai!J!JJ
EXPLANATION
SPRING AND NUMBER
2 MILES
3 KILOMETERSCONTOUR INTERVAL 40 FEET DATUM IS MEAN SEA LEVEL
(To convert feet to meters, multiply by 3.048 x 10~ l )
FIGURE 13. Location of springs in T. 4 S., R. 30 E.
21
TABLE 1. Description of wells and springs
LBoxhead explanations are abstracted from U.S. Geological Survey "Instructions for Using the Punch-Card System for the Storage and Retrieval ofGround-Water Data"]
State well number: The wells are identified according to their location in the rectangular system for the subdivision of public land. The identification consists of the township number, north or south; the range number, east or west; and the section number. The section is further subdivided into sixteen HO-acre tracts lettered consecutively (excepting I and 0), beginning with A in the northeast corner of the section and progressing in a sinusoidal manner to R in the southeast corner. Wells within the HO-acre tract are numbered sequentially. The base line and meridian are indicated by the final letter, as follows: H, Humboldt; M, Mount Diablo; S, San Bernardino.Spring number; Springs are numbered similarly. However the letter S is added after the UO-acre tract letter to differentiate the spring from a well.
Owner or user; The apparent owner or user on the date indicated. In some cases, the local name of the well or spring is given.
C CountyF Federal GovernmentM City, town, or unincorporated
village N Corporation or company,
churches, lodges, and othernonprofit, nongovernmentgroups
P Private S State agency W Water district.
Use of water:
A Air conditioningB BottlingC CommercialD DewateringE Power generationF Fire protectionH DomesticI IrrigationH MedicinalN Industrial, including
mining
P Public supplyR RecreationS Stock supplyT InstitutionalU UnusedV RepressurizationW RechargeX Desalination, public supplyY Desalination, other useZ Other.
X Waste disposal Z Destroyed.
Well data: In tabulation below, C, complete data; N, no data;P, partial data. Complete physical data include depth, diameter, and finish. Complete geologic data include lithology and aquifer thickness. Complete water-level data include altitude of land-surface datum, in feet above mean sea level; water level, in feet above(+) or below land-surface datum; and date of measurement. Complete yield data include rate of pumping and drawdown.
Code symbol 1 2 3 14 5 6 7 8 9 0
Physical Geologic Water level Yield
C C P C C N
C P N P
A Drilling-timeB Casing-collarC Caliper (diameter) surveyD Driller'sE ElectricF Fluid-conductivity or fluid-resistivityG Geologist or sampleH MagneticI InductionJ Gamma-ray
K Dipmeter or directional (inclinometer)survey
L Laterolog H Hicrolog N Neutron 0 Hicrolaterolog P Photographic Q Radioactive-tracer R Radiation (includes both neutron and
gamma-ray) S Sonic
Use of well:
A AnodeD DrainageG Seismic holeH Heat reservoir0 ObservationP Oil or gasR RechargeT Test holeU UnusedW Withdraw water
Chemical analyses:
C CompleteG Dissolved gasesJ Conductance and chlorideK ConductanceL ChlorideH Multiple (complete and one or more
partials) P Partial R Radiochemical (plus partial or complete
chemical) S Special (tritium, carbon-lu, and all
other special determinations) T Trace elements (spectrographic).
T TemperatureU Temperature and fluid-conductivity
(resistivity)V Fluid-velocityW Electric and radiationX Electric, radiation, caliper, and fluid-
velocityY Electric, radiation, and sample (or driller's)Z Electric, radiation, temperature, and fluid-
conductivity.
Depth of well; Depth, in feet below land-surface datum, as reported by owner, driller, or others, or as measured by the Geological Survey.
Depth cased: Length of casing, in feet below land-surface datum, to the top of the first perforations.
Diameter: Inside diameter of the well, in inches; nominal inside diameter, in inches, of the innermost casing at the surface for drilled cased wells
Well finish:
C Porous concreteF Gravel wall, perforated or
slotted casingG Gravel wall, commercial screenH Horizontal gallery or collector0 Open endP Perforated or slotted casingS screeni Sand pointW Walled or shoredX Open hole in aquifer (generally
cased to aquifer)Z Other.
Power:
1 Hand 2 Natural gas engine
A 0-20 hpB >20-60C >50-100D>100-200E >200
Altitude of Isd: Altitude of land-suland surface at the time of the fir
"later level: Depth to water, in feet
Date measured: Month and year of the
Method drilled:
ABCDHJPRTV
WZ
.
RotaryBored or augeredCable-toolDugHydraul ic -rotaryJettedAir percussionReverse-rotaryTrenchingDrivenDrive-washOther.
3 Gasoline engine + L/j.ese.L en£j.ne F 0-5 hp H 0-50 hpG >5-20H >20-50J >50-100K >100-200L >200
rface datum, in
N >50-150P>150--400Q>400-750R >750
feet, above mean sea level. Land-surfacest measurement and used as the plane of reference for all
, above ( * ) or be
water-level mea
low land-surface datuir. .
surement; other data given generally apply
Lift type:
A AirB BucketC CentrifugalJ JetL Multiple (centrifugal)M Multiple (turbine)N NoneP PistonR RotaryS SubmergibleT TurbineZ Other.
5 Electric motor 7 LP gas engineS 0-1 hp (propane or butane)T >l-5 A 0-20 hpU >5-15 B >20-5CV>15-100 C >50-100W >100 D>100-200
6 Wind L >2008 Other.
datum is an arbitrary plane closely approximatingsubsequent measurements.
for this date.
Yieiq ot well (or spring): Yield, in gallons per minute; drawdown, in feet.
22
WELLS
St.ite wo 11 number
2S/27E-35D1
2S/28E-27R1
2S/28E-28R1
2S/28E-29D1
2S/29E-30N1
2S/29E-30N2
2S/29E-31P1
2S/29E-32C1
2S/29E-35N1
2S/29E-36P1
3S/27E-31C1
3S/27E-35E1
3S/28E-14J1
3S/28E-15P1
3S/28E-30R1
3S/28E-30R2
3S/28E-32C1
3S/28E-32E4
3S/28E-32E5
3S/28E-32E6
3S/28E-32E7
3S/28E-32E8
3S/28E-32E9
3S/28E-32E10
3S/28E-32G1
3S/28E-33P4
3S/28E-34R1
3S/28E-35E2
0) T3 T3a) wo)U) i-l i-l>,l-l ,-t 3 3
^ CO rH O O H) iH C cy i-l 'O r-l
Owner or user u rH co 3D <y 01D. CO <U <fl ,J3 U) ^O
H 3 3 J-> rH CO <H CO.^ oj nj *J O u O" tn >j-t m 'O o co 4* 0)w. o o -r-i-a j3« ji a cy ^H (3 u m u M-i rt <i> a) , i a: or. cx^ ex*-' 3 w M <u .c o a> a)0 U y 5: O i-J Q Q
USGS 1 LV-27 F U T G,T 60 60
U U 43
U U C
Arcularius Ranch P H W c T 42
Arcularius Ranch P H W
Arcularius Ranch P U U T 35
P U U C 9
USGS 1 LV-14 F U Z GO
P S W
P U U
Mammoth Mtn. Inn P C W C 110
P U U 14
USGS 1 LV-46 F U T G,T 103 103
U.S. Forest Svc F U U C 14
USGS 1 LV-15 F U T C G,T 57 55
USGS1 LV-44 F U T G,T 79 77
Magma Power Co. PUT.
Magma Power Co. P U U C T 22
Magma Power Co. PUT M 630 400
Magma Power Co. PUT M 810 4o6
Magma Power Co. PUT C 570 352
Magma Power Co. PUT P 513 224
Magma Power Co. PUT C 40? 235
Magma Power Co. PUT 756 192
Magma Power Co. PUT C 670
Mono Co. Sheriff C H W C D 80 51
Mammoth School C T W C 47
Magma Power Co. PUT 805 237
-0 La* -- -
-a ,-i <3 a>0) rH 3 'OrH -0 O 41
C3l-Hcy 'H i-l r-l rJ V-^0>-HrH O 4141 3 QJ Uj.rliw.-icy >J3 «! C
ViHJC-O-^CX U *~^. 41 fl 0) ,C -rl ^ >, T3 U rH W 41 <1 4J o <4J 'O T3 U 341 41 E Ca) c o _ 4-1 a) v-i <u cg -rH i-l JS JwiJO) -rlU-1 O) 1" O r-. CO^-^rHU CO*->3 U^-^ U*-' U t-
rH 111 IV 11 -H O rH fl CO ClQ 3; X! >< J * < 3 Q c
2 Z B 1972 II 7,505 dry 6-12-72
36 P C P 6 7,040 36 6-25-6030.4 5-11-72
PC P 6 7,125 5-11-72
8 P C 1960 P 6 7,100 12.8 6-13-66 11.14 5-11-72
P 6 6,940 5-11-72
8 P C B 6,913 8.90 5-11-72
36 P C P 6 6,915 6 6-13-663.93 5-10-723.60 8- 9-73
B 1972 6,890 8 5-31-72
6 P c P 6 6,914 2.30 5-10-72
6 P C P 6 6,995 69.61 5-10-72
-
6 P C T U 7,880 13.5 5-30-72
2 Z B 1973 N 7,160 dry 5-18-73
30 P 6 7,200 1.01 5- 8-72
2 T B 1972 N 7,340 4,73 5-31-72 5.42 10-4-725.39 5-15-73 4.95 8- 7-73
2 T B 1973 N 7,340 7.53 8- 7-73
12 0 N 7,340
6 P C N 7,340 21.3 6-22-72
8^ 0 H 1959 N 7,360
8^ 0 H I960 N 7,360
&| 0 H I960 N 7,360
12 0 1961 N 7,350
12 0 1962 N 7,350
12 0 1962 N 7,350
12 0 1962 N 7,025 '
8 P C 1961 T T 7,183 23.80 5-12-72
8 P C 1949 7,070 5-23-72
18 o 1961 N 7,025 n . 7 8. ^ 73
minute i-". !£ O i
Drawdown r- '
(feet) i
See footnotes at end of table.
23
WELLS
Statewell number
3S/29E- 2A1
3S/29E-4J1
3S/29E- 4J2
3S/29E-5D1
3S/29E- 7A1
3S/29E-13C1
3S/29E-13C2
3S/29E-16J1
3S/29E-17K2
3S/29E-18B1
3S/29E-18J1
3S/29E-19P1
3S/29E-19R1
3S/29E-21F3
3S/29E-23F2
3S/29E-23F3
3S/29E-23F1*
3S/29E-27L1
3S/29E-27L2
' 3S/29E-27L3
3S/29E-27TA
(a -o 130) U) U)<J) r~t r-t>,.H rH 3 3
>J tO rH O O01 . H Cl 01 rH '<3 rH
Owner or user u ,H « 3 <u <u <uC. CTJ 01 cfl ,O U) ,Q H l< 3 IJ rH qj U-l qj
.rt mmtJ o u otJw 'n U-, 'o o m m a)>-< O O -H T3 ,C <U ,C 0)01 rH g 4J UJ IJ t-lri a) oi rH u; or ex*-' c.^-'Swuioi^o a) a)o u> ;j ;= o J Q n
P S W
USGS 1 LV-7 F U T C G,T 99 69
USGS 1 LV-8 F U T G,T 12 10
USGS 1 LV-1+0 F U T G,T 39 37
USGS 1 LV-25 F U T G,T 1? 15
P S W C 80
USGS 1 LV-21 F U T G,T 22 20
USGS 1 LV-10 F U T C G,T 15 13
USGS 1 LV-Ul F U T C G,T ill 39
USGS 1 LV-31 F U T C G 6 U
USGS 1 LV-30 F U T G 8 6
USGS 1 LV-^7 F U T G,T 102 102
USGS 1 LV-^2 F U T C G,T 22 20
USGS 1 FUG C
USGS 1 LV-9 F U Z G 0
USGS 1 LV-12 F U T G,T 12 10
USGS 1 LV-13 F U Z G 0
USGS 1 LV-6 F U T C G,T 58 56
USGS 1 LV-37 F U T C T 39 36
USGS 1 LV-38 F U T T ly ID
USGS 1 LV-39 F U T 52
Yield^J of well
U) ._-- ---
0 .H 13 U)a) rH 3 'O
1-1 -o o a)C ,H 0) 'n r-l ,H >y >J
^-K ui -H 1-4 o aim 3 <uUJ'HUrHO) >J3 U) O-
i-i OP G -a -H tx u^-v m m QJC: -01,^-H HX T3»J iHlJ 0) (0 i-l 3 UuouH'O'd*-1 3*u a) ts c^oo)QJC! o i-iuoi >jij ocoa)6 -H iH ^3 H U 0) 'H >W 0) '*-! 0) rH -H 3 '4-1nj^i-HiJ n!4-i3 u*-' u*-' u rH f= «J ^^
H (u a) oi r-i o rH <D nl <o V"as>:>^j!ai<: 3 Q u ra
10 P C P 6 6,922 5-10-72
2 P B 1972 N 6,870 +0.6 6-1^-72+0.6 10- i|-72+0.k 5-11-73+0.8 8- 9-73
2 T B 1972 N 6,870 8.15 5-2^-728.99 10- ^-72ii.37 5-11-735.27 8- 9-73
2 T B 1973 N 6,930 18.83 5-17-7318.31 8- U-73
2 T B 1972 N 6,910 10. kk 6- 9-725.57 5-17-736.^2 8- U-73
6 P C N 6,860 flow 5- 9-72 1.8flow 10-9-72 l.U
2 T B 1972 N 6,855 - 8.2 6- 6-728.57 10- 9-728.115 8- 9-73
2 T B 1972 N 6,835 2.81 5-21*- 723.50 10- 9-723.66 8- 9-73
2 T B 1973 N 6,905 0.62 5-17-730.1*7 8- 9-73
2 T B 1972 N 6,930 1*.26 10-20-72+0.01* 5-17-731.85 8- l*-73
2 T B 1972 N 6,915 I*.o8 10-20-721.17 8- i*-73
2 Z B 1973 N 7,025 dry 5-21-73
2 T B 1973 N 6,960 6.01 5-17-736.29 8- 2-736.27 10- 1-73
5 x H 1973 N 6,880 flow 5-8-73 l.i*
B 1972 6,820 5-2U-72
2 T B 1972 N 6,810 ir.24 5-31-72U.92 10- 9-722.78 5-11-73U.29 &. 9.73
B 1972 6,820 5.2 5-31-72
2 T B 1972 N 6,870 1.93 5-22-721.71 5- 3-732.73 >-ls-731.76 8- 2-73
2 P B 1973 N 6,870 0.38 5-16-731.21 b- 2-73
2 P B 1973 K 6,870 0.90 5-16-733.28 8- 2-73
2 p B 1973 N 6,870 2.58 5-16-733.61 8- 2-73
See footnotes at end of table.
24
WELLS
State well number
3S/29E-29K2
3S/29E-29N1
3S/29E-29R1
3S/29E-31G2
3S/29E-31G3
3S/29E-31R1
3S/29E-32A1
3S/29E-33K1
3S/29E-36K1
3S/30E-18K1
3S/30E-19M1
1*S/27E-4B12
1*S/28E- 1F1
1*S/28E- 1L1
1*S/28E- 3J1
1*S/28E- 3J2
1*S/28E- 3R1
1*S/28E- 4P1
1*S/28E- 4P2
1*S/28E- 6R1
1*S/28E-12K1
l*S/28E-ll*Rl
1*S/29E- 3B1
01 -O T3 a) 01 atOl rH r-l
rH rH 3 3r-i <s rH o o
_ OJrHC 0) rH 'O rH
Owner or user *-> -H <a 3 <u <u o>
05 '4H '4J rO O CO (U (UH O O -H T3 .G !U ,C (1)
3 u> U) 0. .£3 O <U (U O 3 P 2: U hJ O ("3
USGSl LV-17 F U Z G 0
USGS 1 LV-18 PUT C G,T 69 67
USGS1 LV-1*5 F U T G,T 96 96
P U U 2
P U U 2
USGS1 LV-16 F U T C G,T 97 95
USGS 1 LV-21* F U T G,T 13 13
USGS1 LV-29 PUT C G,T 35 33
USGS1 LV-11 PUT G,T 75 73
USGS 1 LV-20 F U Z G 0
USGS1 LV-28 PUT C G,T 87 85
YieldT? of wellw - - ~
T3 rH a 01
<U rH 3 'O rH T3 O tU
,C rH UJ 14-! ,_| rH >-l )-> /-x CO -rl rH O Or 0, 3 O
(0 -H 14 rH 0) >JO 10 O.r-l(l)CT3'Hft d)r-^ <U <fl <UCr-s tUr-^'H r-«rN TJ4J rH4-r QJ L04J 34-14JUm'OT34J 3QJ U S C3OQJDC o >-i u aj s-i ai o a -o D6 -H rH J3 (j u (U -H iw !U H-l !U rH -H 3 '4-1
H U 01 01 H O rH CS cd nj'lJO3>:r"ji,<; 3 o o o
B 1972 6,970 6- 2-72
2 T B 1972 N 6,990 19.3 6- 2-72 19.03 10- 9-72 17.32 5-2U-73 17.9!* 8-10-73 18. Ol* 9- 7-73
2 Z B 1973 N 6,970 5-25-73
36 0 D N 7,000 1.02 5- 9-72
36 0 D N 7,000 0.93 5- 9-72
2 T B 1972 N 6,990 1*1.1 6- 1-7261.16 10- 9-72 60.91 5-22-73 60.1*6 8-10-73
2 Z B 1972JJ 6,97!* dry 6- 8-72
2 T B 1972 N 6,975 6.75 5-H-73 6.77 8- 2-73
2 T B 1972 N 6,820 51.5 6-1U-72 51.09 7-25-72 51:11 10-9-72 50.98 5-11-73 51.02 8- 9-73
B 1972 7,005 dry 6-6-72
2 T B 1972 N 6,950 69.35 10-19-72 68.50 8- 9-73
Mammoth County W P W D 1*20 356 2 P H 1969 N 8,260 flow 10-10-69 75 Water District
USGS 1 LV-19 PUT G,T 98 96 2 T B 1972 N 7,090 39.2 6- 7-72 36.78 10- l*-72 36.25 5-2U-73
Mammoth County C C W C 70 Airport
Sierra Materials P C W C
10 P C S T 7,108 5-11-72
6 P C J T 7,100 3i8.i7 5-15-72
Sierra Materials 'P C W 28 15 8 P H 1962 T T 7,100 15 5-15-72
USGS 1 LV-22 F U Z G 0
USGS 1 LV-1 F U Z G 0
B 1972 7,ll*5 6- 6-72
B 1972 7,195 5-16-72
USGS 1 LV-2 PUT G,T 1*3 1*1 2 T B 1972 N 7,195 1*2.65 5-17-72 38.2 8- l*-73
USGS l LV-26 PUT G,T 30 30 2 Z B 1972 N 7,1*10 dry 6- 9-72
Bureau of Sport F T W C D 75 3!* Fisheries
Convict Cr. Resort P C W C D 1*0 25
USGS 1 LV- 5 PUT G,T 97 95
6 P H 1959 S T 7,095 30.8 9-16-59
6 P c 1957 7,580 7 l*-10-57 70 6
2 T B 1972 N 6,81*0 23.1* 5-23-72 23.33 10-1* .73 22.55 5- 3-73 23.27 8- 2-73
See footnotes at end of table.
25
WELLS
State well number
Owner or userD
H
43<n
0)CS0
1S
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a) a)Ul 43<oO 4-1
0)43 n)p, *-sa)Q
U)V-t Q)Q) .'SU OQ). C
(T3 "^
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{3 rltM
rH
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a a)
rH
rH rl
^1 a
jj<oa)
a)(X
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3 0)U Q) rl <H
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rH
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rH rH
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rH 4J
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aa)3 Ula<aeQ)U<0Q
Yieldof well
a)(X
a)'Jl UG 30 C
rH -rH
rH g
O
(3 '"^2 *JO (UO (UU <Mco ^
Q
4S/29E-3C1
4S/29E-4J1
4S/29E-4J2
4S/29E-5B1
4S/29E-5B2
US/29E-5B3
US/29E-7D1
4S/29E-8C1
US/29E-17D1
US/29E-2111
US/29E-2UN1
USGS x LV-23
USGS 1 LV-33
USGS l LV-34
USGS A LV- 3
USGS J LV-35
USGS J LV-36
USGS J LV-4
USGS1 LV-32
F U T G,T 57 23 2 P B 1972 N 6,850 23.84 8- 2-73
F U Z G 0 B 1973 6,855 5- 1-73
FUTCT 96 942TB 1973 N 6,855
F U T C G,T 97 95 2 T B 1972 N 6,918
F U T 75
F U T 5U
F U T G,T 60
73 2 T B 1973 N 6,918
52 2 T B 1973 N 6,918
58 2 T B 1972 N 7,038
FUTCG 23 212TB 1972 6,915
USGS1 LV-U3 F U T G 52
McGee Cr. Lodge P H W 51
Los Angeles Dept. MEW D 90 Water & Power
50 2 T B 1973 N 6,900
6 P C S T 7,000
U4 8 P C 1959 S T 6,8UO
9 5- 1-738.55 5-17-738.46 8- 2-73
44.69 5-17-72 44.49 10- 5-7245.30 5-11-7345.31 5-17-73 44.79 8- 2-73
46.09 5-17-73 46.52 8- 2-73
44.89 5-17-73 44.69 8- 2-73
7.27 5-10-72 3.49 10- 4-72 6.19 5-15-73 2.34 8-19-73
17.85 10-21-72 8.51 5-24-73 8.51 8-10-73
lkL.21 5-18-72
38.9 8-28-59
See footnotes at end of table.
26
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o
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r
Use
o
f sp
rin
g
Ch
em
ica
l a
na
lyse
s
Tem
pera
ture
°C
Fie
ld C
onductivity
(mm
hos/
cm)
Altitude o
f Is
d(f
ee
t)
Da
te
me
asu
red
Yie
ld o
f spring
(gal/m
in)
TABLE 2, Chemical a
nalyses of water
Dissolved so
lids
: Values indicate the
residue on
evaporation at 18
0°C,
except those preceded by
the
letter "a
," which have bs
en calculated (s
ura
of determined constituents).
Labo
ratory
; mK> California Department of
Water Resources; LA
EWP,
Los
Angeles Department of
Water and Po
wer;
Ci
3 SLC, a.
S. Geological Su
rvey
, Salt Lake City La
b.;
GS MP,
'J.S.
Geological Survey, Menlo Park La
b.;
'JSA
C, U.S. Agricultural Consultants, Lein La
b.
WELLS
Wel
l nu
mbe
r
B
O V 8 o V Q
^ I "o D.
Q
? 3 V D.
1 u « ^
U.S
. P
ubli
c H
ealt
h Se
rvic
e dr
inki
ng-w
ater
sta
ndar
ds (
1962
)
2S/2
8E-2
8R1
2S/2
8E-2
9D1
2S/2
9E-3
1P1
3S/2
7E-3
1C1
3S
/28
E-1
5P
1
3S/2
8E-3
0R1
3S/2
8E-3
2E4
3S/2
8E-3
2E5
3S/2
8E-3
2E6
3S/2
8E-3
2E7
3S/2
8E-3
2E8
6-2
5-6
0
6-1
3-6
6
6-2
5-6
06-1
3-6
6
6-2
2-6
6
6-2
0-6
6
9-1
0-7
3
6-2
0-6
6
3-1
4-6
33-2
6-6
310
-21
-63
11-2
6-6
3
10
-20
-60
8-3
1-6
09
-27
-60
42 __ 110 14 57 22 630
630
630
630
630
810
810
570
570
513
12.8
3.9
13.3
15.0
53.3
54.4
Resu
lts
in m
illi
gra
ms
per
li
ter,
ex
cept
for
iron,
boro
n,
and
ars
en
ic w
hic
h are
in
mic
rogra
ms
per
li
ter
0 52 a i/5 47 - 64 " - 63 250
256 48 __ 223
200
~ t B 0 -
300
22
,00
0
'a U
S 3 jj "a U
28 10 10 11 3 3
26 51 11 6 12 6 3 0 1.6
4
OD 5 S 3 B a S 5 4 3 3 2 0 10 0 2 1 1 1 0 1 0
Z B 3 "5 OT 13 22 26 25
8 9 9
360
380
420
420
410
405
375
408
415
400
308
^ B 3 efl 01 as O a. 2 5 5.5
5 4 5 3.5
38 47 34 35 32 30 459
44 36 32
^^ 0
U X B o JO S U £
137 95 92 95 46 34
154
549
527
476
458
459
166
423
232
~ O U 1 JO c3 U 0 0 0 0 - 0 0 0 0 0 0 0 90 37 120
x~v O OT u i2 3 OT 250 1 4 12 14 0 5 8.4
120 61 140
139
132
134 62 147
128
130 96
j-^ O 3 JD !c U 250 2 6 5 3 0 1
17 258
276
266
274
288
291
276
301
293
293
227
£ o 'i 3 Z 1.5
0.3 .5
1.2 .6 .1 .3
1.0
11.0
11.0
10.0
20.0
5.0
14.0
13.0
13.0
20
0 Z 0 5 .ti Z 45 4.3 .3
4.3 1.3 .0
0
.33
.8
1.0
1.0
0 0 0 0 6.2
S B O O 09
30 310
120 80 0 0
610
11
,00
0
14
,00
01
2,0
00
13
,40
012,9
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5,0
00
__ 13,0
00
11
,00
0
8 o .> S Q 500 18
1
150
157
165 55 47
a238
1,3
80
1,3
90
1,3
70
1,4
50
1,4
00
1,4
90
1,4
10
1,5
00
O
U o a S B (0 X 91 42 38 40 16 8
110
127 36 19 34 19 4 4 8
fO O
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Si
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O £
Z
a H c 0) 01 *
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0 0 0
190
1,8
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1,0
60
820
200
gu
B J
la
<s3
a !i E.u
O
u '
c
D.^
(A
233
186
194
206 79 696
273
1,8
90
1,9
70
1,9
40
1,7
40
1,8
00
2,0
10
1,9
40
X D.
7.6
7.7
7.7
7.0
5.9
7.2
6.7 6.8
8.8
67
.17
.67.3
7.8
8.6
19
.2
8.9
9.2
6.5
o u to o to
DWR
DWR
DWR
DWR
DWR
DWR
GS
SLC
DWR
McN
itt
(196
3)U
nkno
wn
DWR
USA
CU
SAC
McN
itt
(196
3)U
nkno
wn
Unk
now
nGS
M
P
McN
itt
(196
3)
WEL
LS
Wel
l nu
mbe
r
3S/2
8E-3
2E9
3S/2
8E-3
2G1
3S
/28
E-3
3P
4
3S/2
8E-3
4R1
3S
/29
E-4
J1
3S/2
9E-1
3C1
Dat
e
10-2
0-6
07
-24
-63
5-1
9-7
2
7-2
3-6
3
9-1
0-6
3
3-2
6-6
3
4-
2-6
35
-21
-63
6-2
5-6
38
- 8
-63
9-1
5-6
310-2
1-6
311-
4-6
312-1
0-6
31-1
3-6
42-
3-6
43
-29
-64
4-2
5-6
45-1
1-6
45-1
3-6
4
3-2
6-6
34-
2-6
35-2
1-6
36-2
5-6
39
-16
-63
10-2
1-6
311-1
9-6
31
2-1
0-6
31-1
3-6
42
- 3
-64
3-2
9-6
45-1
1-6
46
-20
-66
10
- 3
-73
6-2
1-6
65-2
3-7
2
Dep
th
405
405
405
670
670 71 __ _ __ __ __ __ __ __ __ __ __ __ "
47 99 80
°C
32.8
31.7
31.7
25 17.8
16.7
16.1
15.6
10.0
9.4
10
Si0
2
96 98 170 13
19
6
100 9
98 75 68 54 60 61 65 71 72 63 62 60 45 60 60 48 46 45 47 47 43 "
54
__ 64
FeC
a 4 1.9
1 0 13
15 9 8 9 13 20 15 17 16 16 14 31 27 13 10 11 13 8 12 13 10 11 12 20 12 13 10 17 4 5.3
Mg
0 2.1
0 1 9 8 12 5 5 5 4 8 8 7 6 7 9 8 9 9 9 8 10 5 5 8 7 5 4 7 7 8 8 0.2
Na
420
475
390
165
430 42
43 43 32 26 33 40 41 44 45 46 40 40 41 58 25 25 28 26 23 23 23 23 23 24 23 24 22 230 39 38
K 38 30 45 50
48
8 7 7 6 6 6 7 7 8 7 7 6 8 7 7 5 5 4 5 5 5 5 5 5 5 4 5 5 10 2 1.3
HC
O3
241
340
450
328
330
117
116
122 90 92 105
117
120
124
128
121
117
175
153
173
120
122
122
115
111
110
117
118
116
129
126
111
110
188 90 111
CO
3
108
139 30 55
128 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 " 0 7 2
.8
SO
4
140 96 130
180
170 16
17 18 12 12 8 17 16 19 16 23 18 19 19 17 5 13 10 12 10 10 9 7 6 8 7 12 7 73 11 3.7
Cl
283
310
280 26
33
0 37
38 38 21 28 25 33 36 37 40 37 34 36 39 33 6 5 10 12 4 5 4 4 4 5 5 11 7
260 3 3
.0
F
14.0
21.0
12 2.1
11.0 .4
.4 .4 .4 .1 .2 .2 .2 .2 .2 .2 .1 .1 .2 .4 .4 .4 .3 .3 .2 .2 .2 .2 .4 .2 .1 .2 .3 .9 .6 .5
7
NO
3
0 1.2
<.0
5
1.2
3.8 .5
0
.51.2
3.8
0 0 0 0 0 0 0 0 0 0 1.0
0.5
1.9
0 0 0 0 0 0 0 0.7 .5
5
0.0
5
B
5,0
00
13,0
00
15,0
00
13
,00
0
1,5
00
1,2
80
1,3
80
1,4
00
960
700
1,0
60
1,6
60
1,4
30
1,4
80
1,5
30
1,4
50
1,4
40
1,4
40
1,2
80
1,4
60
320
280
400
460
340
' 31
0
260
270
330
330
330
280
740
240
Dis
solv
ed
soli
ds
1,4
20
1,5
50
1,4
20
1,2
80
1
,57
0
265
284
280
190
224
228
262
256
276
278
258
236
300
256
310
160
184
180
165
166
166
166
170
140
162
138
144
155
a749 15
516
6
Har
d
ness 10 11 3 3 4 70
71 72 41 43 53 67 71 76 69 65 64 11
510
1 70 62 65 66 61 51 53 58 57 51 67 59 62 58 75 10 14
Non
- ca
r -
bon-
at
e
Ar
se
nic
1,6
00
2,2
00
3,0
00 50 10 20
10 10 30
10 0 0 40 80 60 40 40 50 30 30
30 50 95 70 20
Spec
, co
nd.
1,9
70
1,9
20
350
330
357
235
135
262
320
350
360
330
348
315
400
350
409
227
230
247
240
234
205
220
215
22
422
521
6
1,3
20
194
191
PH 9.1
9.3
9.2
5
8.8
9.3
6.7
6
.56.7
6.6
7.1
7.8
6.5
7.3
7.3
7.3
6.8
7.0
7.1
8.0
7.5 7.6
7.3
7.5
7.1
7.0
7.7
7.8
7.2
7.2
7.6
7.9
7.7 7.2
7.5
8.6
8.8
2
Lab
.
Unk
now
nU
nkno
wn
GS
MP
Unk
now
n U
nkno
wn
DWR
USA
CDW
RDW
RU
nkno
wn
USA
CU
SAC
Unk
now
nU
nkno
wn
Unk
now
nU
nkno
wn
USA
CU
SAC
USA
CDW
R
DWR
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now
nDW
RDW
RU
SAC
USA
CU
nkno
wn
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now
nU
nkno
wn
Unk
now
nU
SAC
USA
CDW
R
GS
SLC
DWR
GS
MP
WEL
LS
Wel
l nu
mbe
r
3S
/29E
-16
J1
3S/2
9E-1
7K2
3S/2
9E-1
8B1
3S/2
9E-1
9R1
3S/2
9E-2
1F3
3S/2
9E-2
7L1
3S/2
9E-2
7L2
3S/2
9E-2
9N1
3S/2
9E-3
1R1
3S/2
9E-3
3K1
3S/3
0E-1
9M1
4S/2
8E-1
L1
4S
/28
E-3
J1
4S/2
8E-1
2K1
4S/2
8E-1
4R1
4S
/29E
-4J2
4S/2
9E-5
B1
4S/2
9E-8
C1
Dat
e
6-1
1-7
3
10
- 4-7
3
10
- 2-7
3
10
- 1-7
3
5-1
5-7
3
6-1
1-7
3
6-1
1-7
3
9-
9-7
3
9-1
2-7
3
10-
1-7
3
9-1
2-7
3
6-1
5-6
6
6-2
0-6
6
6-2
1-6
6
6-2
4-6
6
9-1
2-7
3
9-1
1-7
3
6-1
2-7
3
Dep
th
15 41 6 22 58 39 28.5
97 35 87 70 75 40 96 97 23
°C
11 13.2
16.3
39.0
36 49 46 69 32.5
31.0
14.2
14.4
- 9.4
38 43.2
11
Si0
2
62 42 43 90 150
180
170
67 58 67 35 - - 100
140 11
Fe 70
0
2,5
00
1,8
00
480 10
"410
3,4
00
3,3
00
310
19
,00
0
2,9
00
1,1
00
3,1
00
120
Ca
28 34
8
17 34 24 24 15 6.9
20 23 23 11 24 38 45 27 25
Mg
13 2.9 2.5 .7 1.2 .9 .8 .7 .6
2.2
3.6 4 6 1 1 2.6 1.1
1.1
Na
140
130
360
430
430
380
380
260
160
250 26 11 21
1 3
230
370 1
.5
K 10 14 16 26 32 36 36 16 13 24
6.1
2 5 1 2 6.4 4.3 1.4
HC
Oj
441
387
524
850
830
774
771
412
276
510
154
104
110 69 106
547
689 73
CO
3 0 0
144 0 0 0 0 0 0 0 0 ~ 0 - " 0 0 0
SO
4
27 26 16 46 65 67 67 58 38
4.7
12 9 9 8 13 31 66 11
Cl
47 35 79
180
150
170
170
150 85 150 6
.0
3 4 1 2
100
170 1
.0
F 2.4
2.4 5.5
5.8
5.3
5.5
5.7
7.4
3.0
3.8 .7 .3 .4 .1 .1
3.3
4.8 .1
N0
3
0
.06
.03 .02
.10
.04
.16
.24
.01
.18
1.0 .5 .0
2.2 .0
6
.03
0
B
3,1
00
1,8
00
5,3
00
8,9
00
6,7
00
3,4
00
3,4
00
7,0
00
3,8
00
6,2
00
110 60
160 0 0
5,0
00
8,1
00 0
Din
olv
ed
loli
ds
a551
a482
a940
al,
220
al,
900
al,
250
al,
240
a788
a506
a795
a!9
2
135
150 70 140
a794
al,
130
a88
Har
d
ness
120
97 30 45 90 64 63 40 20 59 72 74 52 64 99 120 72 67
Non
- ca
r-
bon-
at
e
Ar
se
nic
220 52 79 34
260
410
270
130
270 17 29
0 90 0 0
130
430 1
Spec
, co
nd.
849
722
1,3
60
1,8
20
2,9
40
1,7
90
1,7
80
1,2
00
759
1,2
80
254
194
204
134
206
1,1
90
1,6
70
124
PH 8.2
7.6
8.9 7.7
7.4
8.2
8.1
7.5 7.6
6.9
7.5 8.1
7.4
7.3
7.6
7.3
7.1 7.9
Lab.
GS
SLC
GS
SLC
GS
SLC
GS
SLC
GS
SLC
GS
SLC
G6
SLC
GS
SLC
GS
SLC
GS
SLC
GS
SLC
DWR
DWR
DWR
DWR
GS
SLC
GS
SLC
GS
SLC
SPR
ING
S
Spri
ng
nu
mbe
r
2S/2
7E-2
5AS
1
2S/2
8E-2
0RS
1
3S/2
8E-1
3ES
1
3S/2
8E-1
3ES
3
3S/2
8E-2
5AS
1
3S/2
8E-2
5HS
5
3S/2
8E-3
2ES
3
3S/2
8E-3
3PS
1
3S/2
8E-3
4RS
33S
/28E
-35E
S1
3S
/28
E-3
5JS
1
3S/2
8E-3
5KS
1
Dat
e
6-2
5-6
010
-10
-61
9-2
1-6
65
-21
-72
8-
7-7
3
6-1
3-6
6
6-1
6-6
61-1
2-7
3
5-1
8-7
2
5-1
7-5
75-1
2-6
6
7-2
6-7
3
8-
6-7
3
3-1
2-6
33
-26
-63
4-
2-6
35
-21
-63
7-
2-6
38-
8-6
31-1
3-6
42-1
8-6
43-2
9-6
44-2
5-6
45-1
1-6
45-1
3-6
4
7-2
6-7
39
- 5
-54
12-2
9-6
06
-14
-66
5-2
4-7
2
7-2
6-7
3
4-2
4-5
55-1
4-6
37-
8
-63
11
-26
-63
5-1
1-6
46-1
4-6
61
-13
-73
Dep
th°C
__ 11.1
11 10 11.1
82 79 93 88 93 93 __ 17 17 18 -- 14 14.5
-- 74 60 10.5
12 12 13 12
SiO
2
46 46 __ 58 54 -- __ 79 110
131
-- 130
160 90 54 42 57 43 49 38 39 40 39
5612
617
0 30
0 38 44 27 25 35 32
Fe 40 30
150 40
7,4
00 20
<30 30
<10
Ca 6 8 5 5.1
5.1
11 25 22 50
4 3 1.6
19 15 23 28 16 10 10 29 25 25 25 24 18 10 8.0 7 7 3.3
15 12 13 13 25 14 12 13
Mg
5 5 6 5.9
5.8
5 0.5 .6
0 1
.1
41
9 7 4 10 4 3 3 10 10 9 7 7 8.4
0 1 2.1
4.4
5 4 4 4 3 5 3.9
Na
23 23 24 23 23 25
400
437
410
350
325
360 27 48 50 52 51 18 22 38 43 48 48 51 33 21
376
361
372
380 11 14 16 16 15 16 16 11
K 4 3 4 4.0
4.0
5 30 27 30 20 22 23 17 7 8 7 8 5 5 6 7 7 7 8 6 4.8
23.2
22 23 25
3.1
3 3 3 4 3 4 2.5
HC
03
76 85 95 90 95 102
727
735
497
481
453 0
142
117
115
124 83 86 111
124
132
131
115
105
111
475
409
451
466 84 88 90 90 123 86 91
C0
3
0 0 0 0 0 0 8 0 30 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 1 0 0 0 0 0 0 0
SO 4 3 5 5 8.1
6.7
7 90 103 96 90 84 91
1,50
0 16 28 29 27 18 13 19 31 28 35 31 21 12
116
134
107
120 12 11 8 8 9 10 8 14
Cl
11 11 8 5.7 7.0
8
204
197
200
200
190
210 20 39 55 53 46 10 18 45 52 60 54 62 31 6
.525
824
526
425
0 2.4
2 2 3 3 3 3 1.8
F 0.5 .1 .5 .5 .5 .5
8.6
7.2
8.4
10.0
8.6
8.3 .4 .4 .4 .2 .3 .5 .1 .2 .1 .1 .1 .2 .3 .3
5.0
10.0
11.0
11
.2 .1 .2 .3 .2 .2 .3 .2
N0
3
3.7
1.4
0.1 .1
0
.5 .8 .9 .05
0 1.2 .0
4
.06
.31.5
0.5
2 4.0
0 0 0 0 0.5 .2
8.8
01.9 .5 .0
5
.13
.21.0
1.5
1.5
0.6
3.1
B 150'
590
320
400
340
9,4
00
9,1
00
10
,60
0
10
,00
09
,20
0
9,4
00 50
1,4
00
1,8
50
1,8
40
1,7
00
580
500
1,6
00
1,9
70
2,1
20
1,8
60
2,3
00
1,4
60
270
.11
,10
01
0,4
00
11
,00
013
,00
0 80 100
100
100
170
130 80 100
Dis
solv
ed
soli
ds
112
134
139
156
a!5
4
150
1,2
40
1,6
50
1,2
60
1,1
10
1,0
40
al,
090
al,
820
300
255
282
270
228
254
224
278
262
266
298
300
a!7
5
1,2
16
1,2
25
1,3
00
a!2
8
131
130
130
156
142
120
161
Har
d
ness 36 41 37 37 37 48 63 58 130 10 12 4
220 75 87 87 81 42 38 85 104
104
100 89 74 60 22 269 56 51 49 49 79 48 51 49
Non
- ca
r -
bon-
at
e
Ar
se
nic 20 20 20 50
1,1
00
600
740
1,0
00
1,1
00
1,0
00 5
60 120
140 30 70 30 80 50 10 50 60 50
__ 2,0
00
340 20
40 40 40 30 20 20
Spec
, co
nd.
151
179
187
182
185
211
1,9
08
2,0
00
1,9
50
1,6
20
1,5
42
1,6
30
398
420
410
407
160
110
350
390
430
410
400
313
218
1,8
20
1,7
10
1,7
40
1,8
00
164
166
168
174
240
165
173
160
pH 7.3
7.4
7.5
6.8
37
.4
7.2
7.1
8.2
7
6.5
1
8.3
8.2
8.7 3.7
7.0
7.4
7.0
7.1
7.3
7.2
7.6
7.6
8.0
7.1
8.1
7.5
7.3
7.3
57
.48
.27.1
5
7.4
7.5
7.3
7.3
7.4
7.5
7.3
7.6
6
Lab DW
RU
nkno
wn
DWR
GS
MP
GS
SLC
DWR
DWR
LADW
P
GS
MP
Unk
now
nDW
R
GS
SLC
GS
SLC
DWR
DWR
USA
CDW
RDW
RDW
RU
SAC
USA
CU
SAC
USA
CU
SAC
DWR
GS
SLC
GS
MP
Unk
now
nDW
RG
S M
P
GS
SLC
Unk
now
nU
nkno
wn
Unk
now
nU
nkno
wn
Unk
now
nDW
RLA
DWP
SPR
ING
S
Spri
ng
num
ber
3S/2
8E-3
5NS
1
3S/2
8E-3
5NS
2
3S/2
8E-3
5PS
1
3S/2
8E-3
5QS
1
3S/2
8E-3
6MS
1
3S/2
9E-1
7RS
1
3S/2
9E-1
7RS
4
3S/2
9E-2
0NS
1
Dat
e
4-2
4-5
59-2
2-6
012
-29
-60
5-1
4-6
37
- 8
-63
7-1
1-6
39
-16
-63
10
-21
-63
11-2
6-6
312-3
1-6
31-1
3-6
42
-18
-64
3-2
9-6
44-2
5-6
46-1
4-6
6
4-2
4-5
59-2
2-6
05-1
4-6
37-
8-6
37-1
1-6
39-1
6-6
310
-21
-63
11-
4-6
311-1
9-6
312
-31
-63
2-
3-6
43
-10
-64
4-1
3-6
45-1
1-6
46-1
4-6
6
12
-29
-60
5-1
4-6
37-
8-6
311-2
6-6
35-1
1-6
46-1
4-6
6
1-1
2-7
31-1
3-7
3
8-
9-7
3
8-
9-7
3
7-2
6-7
3
Dep
th°C
17 16 16 16 16 _ __ ._ __ __ _.
.. .. 17 17 16 16 16 -- -- ._ 16 13 16 12 __ 37 17.5
66
SiO
2
67 56 56 12 13 13 45 46 46 46 44 44 44 45 63 61 11 11 13 44 45 43 47 43 44 44 45 52 17 16 40 ..
33 39 210
120
130
Fe
<10 30 50 20 30
Ca
12 15 15 9 9 11 14 18 18 12 12 12 14 14 10 11 14 8 8 11 15 16 12 12 12 12 12 12 12 9 10 9 9 13 11 11 16 16 21 23 24
Mg
10 7 10 9 8 9 5 5 6 7 5 7 6 7 7 9 7 10 8 8 4 3 6 7 6 6 6 7 7 7 7 7 8 5 6 6 4.4
4.7 .5
1.4 .1
Na
23 27 28 25 24 25 22 24 24 24 23 24 25 27 24 23 27 24 22 24 21 22 22 22 23 24 23 23 23 22 19 20 20 20 21 19 11 11 470
420
440
K 5 6 5 5 5 4 5 7 5 5 5 5 6 5 5--
5 5 5 6 4 5 5 5 5 5 5 5 5 4.7
4 4 4 4 5 2.6
3.4
35 28 19
HC
O3
130
128
128
120
112
122
106
125
126
121
116
119
124
126
115
128
126
122
107
117
105
108
114
113
115
113
121
123
120
108
104
105
107
108
106
101
__87 97
4
876
836
C0
3
0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 __ 0 0 0 0
SO
4
11 11 5 9 10 9 12 10 12 6 4 9 8 8 8 12 11 8 9 8 12 10 8 10 10 6 10 9 11 7 6 7 8 8 9 7 13 13 66 65 81
Cl 7 8 18 6 6 8 4 7 5 5 2 7 9 9 9 5 6 5 5 7 3 4 3 4 3 8 4 4 5 5 4 3 4 2 6 4 1
.82
.6
190
160
200
F 0.3
_. .3 .3 .3 .3 .2 .2 .4 .2 .2 .1 .1 .1 .3 .3
--.3 .3 .4 .2 .2 .2 .2 .2 .2 .1 .1 .2 .3 .6 .3 .3 .2 .2 .3 .2 .5 5.2
4.4
5.4
N0
3
0.3 .3
2.5
1.0
1.0
1.5
0 0 4.1
0 0 0 0 0.7 .2 .3
1.0
1.0
1.0
3.6
0 0 1.0
1.0
0 0 0 0.7
1.9 1.0
1.0 .9
0 0 1.3 .1
6
.06
.35
.04
B 320
350
240
280
420
290
400
300
330
230
420
440
420
340
200
280
240
240
230
230
210
380
240
250
330
260
240
170
140
140
140
170
170
130 90
100
7,60
0
6,4
00
8,8
00
Dis
solv
ed
soli
ds
188
193
202
170
175
185
158
180
200
172
152
168
168
176
170
181
194
185
175
170
198
150
162
166
138
166
152
150
180
150
146
150
155
146
150
135
169
a!3
4
al,
490
al,
260
al,
320
Har
d
ness 71 67 79 60 56 65 56 66 70 59 51 59 60 64 54 65 64 61 53 61 54 53 55 59 55 55 55 59 59 52 55 52 56 53 52 52 57 59 55 63 60
Non
- ca
r-
bon-
at
e
Ar
se
nic
40 50 80 50 50 70 30 40 50 50 50 50 __ _ 60 __ 40 60 40 30 40 30 _ 10 40 _ 50 ~ 50 50 60 80 30 10 16 350
300
460
Spe
c,
cond
.
243
238
291
227
219
241
375
226
267
237
207
222
220
245
214
231
225
223
209
222
360
230
210
243
215
220
212
225
210
201
192
194
200
197
195
187
172
170
2,0
40
1,8
40
1,9
40
pH 7.4
7.7
7.3
7.3
7.3
7.2
7.3
7.0
7.1
7.1
7'.l
8.0
8.0
7.3
7.2
7.5
7.9
7.3
7.3
7.9
7.1
7.1
7.8
7.9
7.2
7.4
7.6
7.7
7.7
7.2
7.5
7.4
7.3
7.4
7.6
7.5
7.9
47.3 7.7
7.7
7.5
Lab
.
DWR
Unk
now
nU
nkno
wn
DWR
DWR
DWR
USA
CU
SAC
USA
CU
SAC
USA
CU
SAC
USA
CU
SAC
DWR
Unk
now
nU
nkno
wn
DWR
DWR
DWR
USA
CU
SAC
USA
CU
SAC
USA
CU
SAC
USA
CU
SAC
USA
CDW
R
DWR
DWR
DWR
USA
CU
SAC
DWR
LADW
PGS
SL
C
GS
SLC
GS
SLC
GS
SLC
SPR
ING
S
Sp
rin
g
num
ber
3S/2
9E-2
1LS
1
3S/2
9E-2
1PS
1
3S/2
9E-2
8HS
1
3S/2
9E-2
9CS
1
3S/2
9E-2
9CS
2
3S/2
9E-2
9DS
1
3S/2
9E-2
9FS
1
3S/2
9E-3
1AS
1
3S/2
9E-3
4KS
1
3S/2
9E-3
6QS
1
3S/3
0E-2
2BS
1
4S
/28E
-9F
S1
4S/2
9E-1
BS
1
4S/2
9E-6
HS
1
4S/2
9E-6
QS
1
4S/2
9E-1
8AS
1
4S/2
9E-3
6LS
1
Dat
e
6-1
1-6
61
-12
-73
6-2
2-6
61-1
2-7
3
5-2
2-7
2
7-2
8-7
3
7-2
8-7
3
8-
4-7
3
7-2
7-7
3
5-
7-57
6-2
5-6
05-1
3-6
65-2
0-7
2
5-2
3-7
2
6-1
1-6
6
1-1
5-7
3
6-1
9-6
6
1-1
5-7
3
8-2
0-4
11-
8-4
610-
3-52
2
-28
-56
12
-12
-61
5-1
2-6
6
2-2
8-5
612-1
2-6
15-1
2-6
6
3-2
0-5
61
2-1
2-6
1
6-1
6-6
6
Dep
th°C
53 56 49 75 52.5
55 29 56 58 41 28 12.0
12 20.6
__ __ 37 __ __ ~ 10
Si0
2
« 167
__ 165
240
170
210
130
110
118
110
120
205
" 63 - 5.8
60 15 32 94 ~ 27 35 -- 23 24 -
Fe 20 20
<30
140 50 80 30
<30
450
<1
0
Ca
28 25 26 25 22 35 35 25 21 18 15 16 15 23
5 11 16 11 16 22 22 20 21 32 31 30 38 37 10
Mg
0.5
0.5 .6 .7
1.2 .4
1.1 .5
1 1.4
1.2
0 3.2
0
.2
9 2 2 2 3 2 2 2 2 2 1
Na
380
385
380
376
400
390
430
460
310
317
306
315
310
320 83 14 5 60 192
132
131
132
130
140 5 5 5 6 6 6
K 37 32 35 32 43 23 26 20 18 19 20 21 22 28 6 3.8 1 3.9
_ 7 10 9 9 1 1 1 3 2 1
HC
03
790
781
845
784
853
859
544
497
482
498
516
695
173 63 46 " __ __ 0
0
110
107 46
C0
3
0 -- 0 0 0 0 0 0 0 0 0 1.9
0 5 0 0 ~ 320
263
263
250
276 97 99 98 __ -- 0
SO
,
60 68 60 69 69 73 81 83 70 80 77 78 81 59 16 5.1
13 19 46 36 48 39 41 24 11 12 20 21
3
Cl
160
145
158
145
170
190
200
200
150
172
181
180
170
150 22 3
.5 1 14
200 71 72 78 Ik 1 6 2 5 5 1
F 4.9
5.0
4.8
5.2
4.8
6.0
4.2 3.1
3.8
._7.0
6.0
7.5
4.6 1.9 .1 .2
1.5
4.0 1.4
1.6
2.9
3.2 .2
0.2 .1
0
.2
N0
3
0.3
2.6
0 1.3 .0
5
.03
.01
.04
.27
_
4.3
0.0
5
<.0
5
.5
2.0
0 4.9
__ 0 0 2 0
.81.2
0
.6 .8 .5
B
31
,00
06
,50
0
31
,00
06
,20
0
8,8
00
8,9
00
8,6
00
8,6
00
6,8
00
8,2
00
8,0
00
8,0
00
8,1
00
580
_20 0
300
4,6
00
3,5
00
2,4
50
3,6
00
3,7
00 30 100 0 30 100 0
Dis
solv
ed
soli
ds
1,2
70
1,6
40
1,2
40
1,6
30
1,3
40
al,
280
al,
420
al,
350
a961
1,1
90
964
960
1,0
00
1,1
30
270
a 14
4 65 269
_ a419
49
2a4
51a5
03 510
a!4
1a!
41
130
a!5
2a!
51 55
Har
d
ness 70 64 65 64 57 90 92 64 57 42 44 39 62 13 41 40 28 77 63 63 58 65 88 86 83 103
101 29
Non
- ca
r -
bon-
at
e
Ar
se
nic
520
370
400
360
340
490
510
530
680
__ 1,1
80
840
360
130 1 10 70 460
0 0
Spe
c,
cond
.
1,7
80
1,8
00
1,7
50
1,8
00
1,9
00
1,8
40
1,9
40
1,9
40
1,4
00
1,9
60
1,4
40
1,4
90
1,5
00
1,6
30
403
138
118
340
948
715
774
733
772
759
212
221
191
227
250 86
PH 7.3
8.0
3
7.0
7.9
0
6.6
0
7.0
7.6
7.8
7.3
8.0
7.3
8.2 7.5
3
6.6
4
8.4
8.1 7.6
8.3
2
7.7
8.2 8.1
8.0
8.2
7.6
7.8
7.8
Lab
.
DWR
LADW
P
DWR
LA
DWP
GS
MP
GS
SLC
GS
SLC
GS
SLC
GS
SLC
GS
MP
DW
RDW
RGS
M
P
GS
MP
DWR
GS
SLC
DWR
LADW
P
Unk
now
nU
nkno
wn
Unk
now
n U
nkno
wn
Unk
now
nDW
R
Unk
now
nU
nkno
wn
DWR
Unk
now
nU
nkno
wn
DWR
TABLE 3. Temperature measurements in wells
Depth below^ land surface Date
datum(feet)
Temper ature( C)
Depth belowland surface
Date , . datum(feet)
Temper ature^
State Well No. 2S/27E-35D1, Project Well No. LV-27
June 19, 1972 5.010.014.016.018.020.022.024.026.028.030.032.034.0
7.968.138.148.418.638.728.748.758.758.758.758.768.79
June 19, 1972 36.038.040.042.044.046.048.050.052.054.056.058.2
Aug. 7, 1973 10.020.0
8.848.878.898.908.918.948.989.019.059.099.129.168.27.6
State Well No. 2S/28E-29D1
June 19, 1972 9.011.013.015.017.019.021.0
9.499.199.189.189.199.219.23
June 19, 1972 23.025.027.029.031.033.034.8
9.249.259.269.259.269.269.31
State Well No. 2S/29E-30N2
June 20, 1972 12.017.022.027.0
7.747.958.248.43
June 20, 1972 29.031.033.035.5
8.679.039.049.13
39
Depth below^ fc land surface Date
datum(feet)
State Well No
May 22, 1973 1.02.03.04.05.0
10.020.030.0
State Well No
June 16, 1972 5.07.09.0
--,.' 11.013.015.017.019.021.023.025.027.029.031.0
State Well No.
May 18, 1973 1.02.03.04.05.06.07.08.09.0
10.0
Temper ature
( C)
Depth belowland surface
Date , . datum(feet)
. 3S/28E-14J1, Project Well No. LV-46
9.669.368.878.598.558.88
10.4913.10
May 22, 1973 40.050.060.070.080.090.0
100.0102.7
. 3S/28E-30R1, Project Well No. LV-15
9.419.098.959.109.289.479.69
10.0310.4210.7711.0211.3611.6711.98
June 16, 1972 33.035.037.039.041.043.045.047.049.051.053.055.057.1
Aug. 7, 1973 10.020.0
3S/28E-30R2, Project Well No. LV-44
12.609.027.916.727.367.397.467.567.808.10
May 18, 1973 15.020.025.030.040.050.060.070.075.7
Aug. 7, 1973 10.020.0
Temper ature,( '
15.2118.1520.2822.9824.9026.7928.8229.13
12.1512.3312.6812.9113.0313.2513.4513.6613.9314.1314.3114.4715.279.85
10.10
8.8910.2510.9612.0512.6813.5314.4115.3915.8010.3510.30
40
Depth below^ land surface Date , datum
(feet)
Temper ature
( C)
Depth belowland surface
Date , . datum(feet)
Temper ature
^ '
State Well No. 3S/28E-32E4
June 22, 1972 6.08.0
10.012.0
State Well
May 25, 1972 10.015.020.025.030.035.040.045.050.055.060.065.070.075.080.085.090.092.7
May 2, 1973 1.02.03.04.05.0
17.8619.5019.4419.59
June 22, 1972 14.016.018.020.022.0
No. 3S/29E-4J1, Project Well No. LV-7
8.218.308.528.628.668.678.688.688.698.718.728.738.758.768.788.798.818.814.442.132.584.282.31
May 2, 1973 6.07.08.09.0
10.015.020.025.030.035.040.045.050.055.060.065.070.075.080.085.090.092.0
Aug. 9, 1973 10.020.0
19.6619.7619.8220.0324.13
2.222.252.322.332.362.502.512.883.093.164.494.614.684.734.784.814.794.784.454.384.404.308.377.87
41
Date
May 25, 1972
Aug. 6, 1973
June 16, 1972
June 14, 1972
June 8, 1972
Depth below land surface
datum(feet)
State Well No
11.9
State Well No.
1.02.03.04.05.0 '6.07.08.0
State Well No.
11.013.0
State Well No.
9.011.013.015.0
State Well No.
4.06.0
Temper ature
( C)
Depth belowland surface
Date . . datum(teet)
. 3S/29E-4J2, Project Well No. LV-8
7.95 Aug. 9, 1973 10.0
3S/29E-5D1, Project Well No. LV-40
17.3816.9616.0414.9213.7412.6711.5810.65
Aug. 6, 1973 9.010.015.020.025.030.035.037.7
3S/29E-7A1, Project Well No. LV-25
7.577.75
June 16, 1972 15.016.9
Aug. 7, 1973 10.0
3S/29E-13C2, Project Well No. LV-21
8.548.408.378.38
June 14, 1972 19.021.2
Aug. 9, 1973 10.020.0
3S/29E-16J1, Project Well No. LV-10
9.097.79
June 8, 1972 8.010.013.3
Temper ature
( c '
8.50
9.969.398.128.688.969.229.299.29
7.967.667.38
8.548.619.308.20
7,557.527.43
42
Depth below land surface Date , 4
datum(feet)
State Well No.
May 2, 1973 2.03.04.05.06.07.0
State Well No.
May 25, 1973 1.02.03.04.05.0
10.015.0
State Well No.
May 28, 1973 1.02.03.04.05.0
10.020.030.0
Temper ature
C c)
Depth belowland surface
Date , . datum(feet)
Temper ature
^ '
3S/29E-16J1, Project Well No. LV-10 Continued
0.222.292.492.582.592.74
May 2, 1973 8.09.0
10.011.012.0
Aug. 9, 1973 10.0
3S/29E-17K2, Project Well No. LV-41
13.499.958.948.187.597.088.90
May 25, 1973 20.025.030.035.039.0
Aug. 9, 1973 10.020.0
3S/29E-19P1, Project Well No. LV-47
13.0611.5710.429.659.098.39
10.2712.25
May 28, 1973 40.050.060.070.080.090.0
100.0101.5
3.043.023.033.063.537.65
9.8710.7011.2411.6612.2211.4910.26
13.8214.9716.0917.2718.5019.6720.4820.82
43
Date
Aug. 6, 1973
June 14, 1972
May 25, 1972
May 3, 1973
Depth below land surface
datum(feet)
State Well No.
2.03.04.05.06.07.0
State Well No.
6.08.0
State Well No.
5.010.015.020.025.030.035.040.045.050.052.054.056.52.03.04.05.0
Temper ature
( C)
Depth below^ ^ land surface Date , . datum
(feet)
3S/29E-19R1, Project Well No. LV-42
29.9830.2430.9731.8033.1734.62
Aug. 6, 1973 8.09.0
10.015.020.020.6
3S/29E-23F3, Project Well No. LV-12
10.178.92
June 14, 1972 10.011.6
Aug. 9, 1973 10.0
3S/29E-27L1, Project Well No. LV-6
17.3819.0323.1428.6033.4138.0742.0945.3247.4848.6848.9449.1649.267.157.247.397.67
May 3, 1973 6.07.08.09.0
10.015.020.025.030.035.040.045.050.055.057.0
Aug. 10, 1973 10.020.0
Temper ature
( C;
35.4335.7637.4941.4745.0245.79
8.287.809.57
7.878.368.829.59
10.5615.0319.1122.2123.9540.7543.1745.9046.8546.9746.6022.3730.00
44
Depth below land surface
Date , ^ datum(feet)
State Well No.
June 11, 1973 2.03.04.05.06.07.08.09.0
State Well No.
June 11, 1973 3.04.05.06.07.08.0
State Well No.
June 21, 1972 21.023.025.027.029.031.033.035.037.039.041.043.0
Temperature
( C)
Depth below land surface
Date datum(feet)
3S/29E-27L2, Project Well No. LV-37
17.7317.3117.2617.3017.3417.7018.2218.65
June 11, 1973 10.015.020.025.030.034.6
Aug. 10, 1973 10.020.0
3S/29E-27L3, Project Well No. LV-38
17.0616.9516.9417.1917.44
June 11, 1973 9.010.015.018.3
Aug. 10, 1973 10.020.0
3S/29E-29N1, Project Well No. LV-18
26.2827.1727.2027.6628.0728.5628.8729.1729.4929.7229.8629.98
June 21, 1972 45.047.049.051.053.055.057.059.061.063.065.067.0
Temperature
( C;
19.2623.8929.1234.2438.3943.2722.9429.93
17.5218.7221.3027.2822.1427.09
30.1130.2130.3630.5030.6330.8030.9031.0731.1831.3431.4931.58
45
Depth below^ land surface Date datum
(feet)
Temper ature
( C)
Depth belowland surface
Date , ^ datum(feet)
Temper ature
( C)
State Well No. 3S/29E-29N1, Project Well No. LV-18- -Continued
June 21, 1972 69.1May 3, 1973 1.0
2.03.04.05.06.07.08.09.0
10.015.0
State Well No.
May 25, 1973 1.02.03.04.05.0
10.015.020.0
State Well No.
June 8, 1972 45.060.065.070.075.080.090.092.0
31.964.964.945.595.996.186.947.037.388.048.51
12.59
May 3, 1973 20.025.030.035.040.045.050.055.060.065.066.6
Aug. 10, 1973 10.020.0
3S/29E-29R1, Project Well No. LV-45
11.7611.4610.7110.1810.0810.2411.1012.35
May 25, 1973 25.030.040.050.060.070.080.090.096.0
3S/29E-31R1, Project Well No. LV-16
31.0436.4938.1039.4441.1042.5644.9445.26
June 8, 1972 94.0May 5, 1973 1.0
2.03.04.05.06.07.0
16.0117.5918.2819.0719.1419.3019.2519.4320.5721.1724.6420.3325.72
13.8815.1616.7117.7918.6819.5220.8421.9522.78
45.889.838.118.488.798.839.56
10.34
46
Depth below^ land surface Date , datum
(feet)
Temper ature
( C)
Depth below^ ^ land surface Date datum
(feet)
Temper ature
( C)
State Well No. 3S/29E-31R1, Project Well No. LV-16 Continued
May 5, 1973 8.09.0
10.015.020.025.030.035.040.0
State Well No.
June 15, 1972 2.54.06.0
State Well No.
Aug. 6, 1973 1.02.03.04.05.06.07.0
10.8711.3811.4314.4918.9821.6323.6225.8028.23
May 5, 1973 45.050.055.060.065.070.073.9
Aug. 10, 1973 10.020.0
3S/29E-32A1, Project Well No. LV-24
15.0614.1713.32
June 15, 1972 8.010.012.0
3S/29E-33K1, Project Well No. LV-29
20.9320.9620.9921.0021.0121.0821.15
Aug. 6, 1973 8.09.0
10.015.020.025.030.035.0
30.3232.2234.1636.1038.2239.3240.2915.6018.14
12.7712.6311.90
21.1721.8021.9424.3127.8531.8335.4438.93
47
Depth belowland surface
Date , . datum(feet)
State Well No.
June 14, 1972 56.058.060.063.065.9
May 3, 1973 1.02.03.04.05.06.07.08.09.0
State Well No.
May 3, 1973 1.02.03.04.05.06.07.08.09.0
10.015.020.025.030.0
Temper ature
( c;
Depth below land surface
Date datum(feet)
3S/29E-36K1, Project Well No. LV-11
15.6615.7115.7615.8216.124.283.453.292.532.092.052.422.993.41
May 3, 1973 10.015.020.025.030.035.040.045.050.055.060.065.0
Aug. 9, 1973 10.020.0
3S/30E-19M1, Project Well No. LV-28
3.983.512.802.191.511.181.241.541.671.884.205.216.096.12
May 3, 1973 35.040.045.050.055.060.065.070.075.080.085.085.9
Aug. 9, 1973 10.020.0
Temper ature
3.865.636.797.617.978.308.748.999.679.99
10.2210.6213.1612.32
6.396.045.725.685.535.435.345.155.225.175.305.30
11.129.08
48
Depth below^ land surface Date
datum(feet)
State Well No.
June 16, 1972 40.042.044.046.048.050.052.054.056.058.060.062.064.066.068.070.072.074.076.078.080.082.084.086.088.090.092.094.096.0
Temper ature(°c)
Depth belowland surface
Date , . datum(feet)
4S/28E-1F1, Project Well No. LV-19
10.7310.7410.7510.7710.7810.7810.7710.7710.7510.7510.7510.7310.7310.7310.7210.7210.7210.7210.7210.7310.7310.7410.7410.7510.7610.7710.7810.7910.80
June 16, 1972 98.0May 3, 1973 1.0
2.03.04.05.06.07.08.09.0
10.015.020.025.030.035.040.045.050.055.060.065.070.075.080.085.090.095.0
Aug. 8, 1973 10.020.0
Temper ature(°c)
10.7910.017.656.805.775.214.844.594.564.754.977.268.379.22
10.2310.6410.7710.8010.8010.7610.7310.7010.7010.6910.6910.6910.7110.7211.9110.85
49
Depth below^ land surface Date , . datum
(feet)
State Well No.
June 21, 1972 41.043.0
Aug. 6, 1973 2.03.04.05.06.07.0
State Well No.
June 19, 1972 3.05.07.09.0
11.013.015.0
State Well No.
May 2, 1973 1.02.03.04.05.06.07.08.09.0
10.015.020.025.030.0
Temper ature
( C)
Depth below land surface
Date datum(feet)
4S/28E-4P2, Project Well No. LV-2
15.6615.4217.4315.2416.3115.6214.9814.29
Aug. 6, 1973 8.09.0
10.015.020.025.030.035.042.4
4S/28E-6R1, Project Well No. LV-26
12.8711.128.118.117.417.117.13
June 19, 1972 17.019.021.023.025.026.9
Aug. 10, 1973 10.020.0
4S/29E-3B1, Project Well No. LV-5
14.7110.148.387.486.646.196.607.668.229.03
10.3912.8714.5015.40
May 2, 1973 35.040.045.050.055.060.065.070.075.080.085.090.0
Aug. 10, 1973 10.020.0
Temper ature
^ '
13.6413.0612.6011.0210.5911.6313.2014.4514.90
7.207.287.407.467.537.57
13.048.17
15.8116.0216.4917.0517.5818.1618.5619.0219.6020.0720.7321.0315.3112.98
50
Depth belowland surface
Date , . datum(feet)
State Well No.
June 15, 1972 26.028.030.032.034.036.038.040.042.0
State Well No.
Aug. 6, 1973 1.02.03.04.05.06.07.08.09.0
10.015.0
State Well No.
May 22, 1972 60.065.070.075.080.085.088.090.092.094.0
Temper ature
( c)
Depth belowland surface
Date , . datum(feet)
4S/29E-3C1, Project Well No. LV-23
19.4619.5019.5219.5719.6319.7419.8319.9120.22
June 15, 1972 44.046.048.050.052.054.056.057.7
Aug. 10, 1973 10.020.0
4S/29E-4J2, Project Well No. LV-34
23.5123.8024.3224.8024.9725.0525.2225.4125.6326.2527.17
Aug. 6, 1973 20.025.030.035.040,050.060.070.076.5
Aug. 10, 1973 10.020.0
4S/29E-5B1, Project Well No. LV-3
40.0141.0742.7244.2445.4146.8146.8947.2047.3848.16
May 22, 1972 95.095.9
Aug. 6, 1973 1.02.03.04.05.06.07.08.0
Temper ature
( C;
20.8421.7922.4222.7623.4224.8425.2825.6716.9715.03
29.0031.8235.4737.7639.0640.8841.9242.7543.3926.5328.72
48.2748.4718.6318.8718.9519.0219.0818.9518.4017.75
51
Depth below ^ land surface Date datum
(feet)
Temper ature
( C)
Depth below_ land surface Date , . datum
(feet)
Temper ature
( C)
State Well No. 4S/29E-5B1, Project Well No. LV- 3 Continued
Aug. 6, 1973 9.010.015.020.025.030.0
State Well No.
May 28, 1972 10.015.020.025.030.035.040.045.050.052.054.056.057.9
May 3, 1973 l.o2.03.04.0
17.5317.6718.7521.95
-28.49
Aug. 6, 1973 40.050.060.070.080.090.093.9
4S/29E-7D1, Project Well No. LV-4
7.357.317.548.018.579.249.65
10.01-
10.3010.4010.4310.463.602.772.231.63
May 3, 1973 5.06.07.08.09.0
10.015.020.025.030.035.040.045.050.055.059.1
Aug. 9, 1973 10.020.0
34.0838.5039.4742.6846.1048.0148.42
1.501.321.201.181.461.592.243.003.984.635.435.956.216.476.556.66
10.668.62
52