UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Analytical results and sample locality maps for stream-sediment, heavy-mineral-concentrate, and rock samples, Kings River, Rancheria, Agnew, and Oat Mountain Roadless Areas, Fresno County, California By David J. Grimes, Maurice A. Chaffee, Elmo F. Cooley, and Warren J. Nokleberg Open-File Report 84-022 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. 1984
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UNITED STATES DEPARTMENT OF THE INTERIOR
GEOLOGICAL SURVEY
Analytical results and sample locality maps
for stream-sediment, heavy-mineral-concentrate, and rock samples,
Kings River, Rancheria, Agnew, and Oat Mountain
Roadless Areas, Fresno County, California
By
David J. Grimes, Maurice A. Chaffee,
Elmo F. Cooley, and Warren J. Nokleberg
Open-File Report 84-022
This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS.
1984
-
CONTENTS
Page
Studies related to wilderness............................................. 1Introducti on.............................................................. 1Methods of study.......................................................... 1
Sample col 1ecti on.................................................... 1Stream-sediment samples......................................... 3Heavy-mineral-concentrate samples............................... 3Rock samp!es.................................................... 3
Sample preparation................................................... 3Sample analysi s...................................................... 4
Spectrographic method........................................... 4Chemi cal methods................................................ 6
RASS...................................................................... 6Description of Tables 3-5................................................. 6References cited.......................................................... 7
TABLES
TABLE 1. Limits of determination for Spectrographic analysis ofrock and stream-sediment samples......................... 5
TABLE 2. Chemical methods used...................................... 6TABLE 3. Data for stream-sediment samples........................... 8TABLE 4. Data for heavy-mineral-concentrate samples................. 17TABLE 5. Data for rock samples...................................... 23
ILLUSTRATIONS
FIGURE 1. Location map of the Kings River, Rancheria, Agnew, and Oat Mountain Roadless Areas, Fresno County, Cali forni a............................................... 2
PLATE 1. Map showing sample sites for stream-sediment and heavy-mineral-concentrate samples, Kings River, Rancheria, Agnew, and Oat Mountain Roadless Areas, Fresno County, California..........................in pocket
PLATE 2. Map showing sample sites for rock samples, KingsRiver, Rancheria, Agnew, and Oat Mountain RoadlessAreas, Fresno County, California...................in pocket
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STUDIES RELATED TO WILDERNESS
The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a yeochemical survey of the Kings River (B5198), Rancheria (C5198), Agnew (5199), and Oat Mountain (5197) Roadless Areas in the Sierra and Sequoia National Forests, Fresno County, California. The roadless areas were classified as further planning areas during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.
INTRODUCTION
In 1981 and 1982 we conducted a reconnaissance geochemical survey of the Kings River, Rancheria, Agnew, and Oat Mountain Roadless Areas, Fresno County, California. The Kings River, Rancheria, Agnew, and Oat Mountain Roadless Areas comprise about 145 mi 2 in eastern Fresno County, California, and lie about 28 to 56 mi east of Fresno, California (fig. 1). Access to the Kings River, Agnew, and Oat Mountain Roadless Areas is provided by State Highway 180 and a Fresno County road to the Pine Flat Reservoir. State Highway 168 and a Fresno County road to the Wishon Reservoir provide access to the Rancheria Roadless Area.
Three major rock units are present in the region encompassing the four study areas. These are (1) the oldest rocks, which occur as roof pendants in the Sierra Nevada batholith and consist mainly of Triassic and Jurassic sedimentary rocks and Jurassic volcanic rocks; (2) Cretaceous plutonic rocks, which vary in composition from quartz monzonite to granodiorite to quartz diorite and have intruded and generally metamorphosed the older rocks; and (3) scattered remnants of late Tertiary olivine basalt flows. Also present locally are alluvial, colluvial, and glacial deposits of Quaternary age (Nokleberg and others, 1983).
The region encompassing the study areas is extremely rugged, with elevations ranging from 800 ft in the bottom of the Kings River Canyon at the western edge of the Oat Mountain Roadless Area to 10,051 ft at the top of Spanish Mountain on the boundary between the Kings River and Rancheria Roadless Areas (fig. 1).
METHODS OF STUDY
Sample Collection
We collected stream-sediment samples at 127 sites (plate 1), heavy- mineral-concentrate samples at 56 sites (plate 1), and rock samples at 388 sites (plate 2) for a sampling density of about 1 sample per 1.1 mi 2 for the stream-sediment samples, about 1 sample per 2.6 mi 2 for the heavy-mineral- concentrate samples, and about 1 sample per 0.4 mi 2 for the rock samples.
-
Fig. 1. Location map of the Kings River, Rancheria, Agnew, and Oat Mountain Roadless Areas, Fresno County, California
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Stream-sediment samples
Analyses of the stream-sediment samples represent the chemistry of the rock material eroded from the drainage basin upstream from each sample site. Such information is useful in identifying those basins which contain concentrations of elements that may be related to mineral deposits.
The stream-sediment samples consisted of active alluvium collected primarily from first-order (unbranched) and second-order (below the junction of two first-order) streams as shown on USGS topographic maps (scale = 1:62,500). Each sample was composited from several localities within an area that may extend as much as 100 ft from the site plotted on the map (plate 1).
Heavy-mi neral-concentrate samples
We prepared heavy-mineral-concentrate samples from the same active alluvium used for the stream-sediment samples. Concentrate samples provide information about the chemistry of a limited number of minerals in rock material eroded from the drainage basin upstream from each sample site. The selective concentration of minerals, many of which are ore-related, permits determination of some elements that are not easily detected in stream-sediment samples.
Rock samples
We collected rock samples from outcrops in the vicinity of each plotted site location (plate 2). Most samples were of fresh rock. These samples provide background geochemical information on elements in rocks that have not been affected by alteration or mineralization. In addition, some altered and mineralized rocks were collected.
Sample Preparation
The stream-sediment samples were oven dried and sieved to minus 80 mesh (0.17 mm) using stainless-steel sieves. The portion of the sediment passing through the sieve was pulverized and saved for analysis.
The heavy-mineral-concentrate samples were processed from the same sediment. Each bulk sample was passed through a 10-mesh (2.0-mm) screen to remove the coarse material. The sediment passing through the screen was panned until most of the quartz, feldspar, organic material, and clay-sized material was removed. The sample was air dried. Bromoform was used to separate and remove the remaining quartz and feldspars from the heavy-mineral concentrate. The heavy minerals (specific gravity >2.8) were separated into three fractions using a large electromagnet (in this case a modified Frantz Isodynamic Separator). The most magnetic material (mostly magnetite) was discarded. The second fraction (mostly ferromagnesian silicates and iron oxides) was saved for archival storage. The third fraction (the least magnetic material, which includes nonmagnetic ore minerals, zircon, sphene, and so on) was divided into two splits using a Jones splitter. One split was hand ground for spectrographic analysis; the other split was saved for mineralogical analysis.
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The magnetic separates discussed are the same separates that would be produced by removing the magnetite with a hand magnet and then using a Frantz Isodynamic Separator set at a slope of 15° and a tilt of 10° with a current of 0.1 ampere to remove the ilmenite, and then a current of 0.6 ampere to split the remainder of the sample into magnetic and nonmagnetic fractions.
Rock samples were crushed and then pulverized between ceramic plates to at least minus 100 mesh (0.15 mm).
Sample Analysis
Spectrographic method
We analyzed the stream-sediment, heavy-mineral-concentrate, and rock samples for 31 elements using a semiquantitative, direct-current arc emission Spectrographic method (Grimes and Marranzino, 1968). Spectrographic results were obtained by visual comparison of spectra derived from the sample against spectra obtained from standards made from pure oxides and carbonates. Standard concentrations are geometrically spaced over any given order of magnitude of concentration as follows: 100, 50, 20, 10, and so forth. Samples whose concentrations are estimated to fall between those values are assigned values of 70, 30, 15, and so forth. The precision of the analytical method is approximately plus or minus one reporting value at the 83 percent confidence level and plus or minus two reporting values at the 96 percent confidence level (Motooka and Grimes, 1976). Values determined for the major elements (iron, magnesium, calcium, and titanium) are given in weight percent; all others are given in parts per million. The upper and lower limits of determination for each element are listed in Table 1.
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TABLE 1. Limits of determination for the spectrographic analysis of stream-sediment and rock samples, based on a 10-mg sample
[The spectrographic limits of determination for heavy-mineral-concentrate samples are two reporting values higher than the limits given for rock and stream-sediment samples]
Element Lower determination limit Upper determination limit
Percent
Iron (Fe)Magnesium (Mg)Calcium (Ca)Titanium (Ti)
0.05.02.05.002
201020
1
Parts per mill ion
Manganese (Mn)Silver (Ag)Arsenic (As)Gold (Au)Boron (B)Barium (Ba)Beryl liuffi (Be)Bismuth (Bi)Cadmium (Cd)Cobalt (Co)Chromium (Cr)Copper (Cu)Lanthanum (La)Molybdenum (Mo)Niobium (Mb)Nickel (Ni)Lead (Pb)Antimony (Sb)Scandium (Sc)Tin (Sn)Strontium (Sr)Vanadium (V)Tungsten (W)Yttrium (Y)Zinc (Zn)Zirconium (Zr)Thorium (Tn)
100.5
200101020
11020
510
520
520
510
1005.
10100
105010
20010
100
5,0005,000
10,000500
2,0005,0001,0001,000
5002,0005,000
20,0001,0002,0002,0005,000
20,00010,000
1001,0005,000
10,00010,0002,000
10,0001,0002,000
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Chemical methods
Other methods of analysis used on samples from the Kings River, Rancheria, Agnew, and Oat Mountain Roadless Areas are summarized in table 2 Analytical results for stream-sediment, heavy-mineral-concentrate, and rock samples are given in tables 3, 4, and 5, respectively.
Table 2. Chemical methods used
Sample type
Constituent determined
Analytical method
Lower limit of determination
(ppm)
Analyst Reference
Stream sediment Zn .
Rock Au-P'
Au-'
AA J
AA J
AA J
5
0.05
0.002
R. W. Leinz Ward and others, 1969
R. W. Leinz Thompson, A. L. Gruzensky 1968
D. L. Fey Meier, 1980
" AA = atomic absorption spectrometryo
d P = partial digestion
^T = total digestion
ROCK ANALYSIS STORAGE SYSTEM
Upon completion of all analytical work, the analytical results were entered into a U.S. Geological Survey computer-based file called RASS (Rock Analysis Storage System). This RASS file contains both descriptive geological information and analytical data. Any or all of this information may be retrieved and converted to a binary form (STATPAC) for computerized statistical analysis or publication (VanTrump and Miesch, 1976).
DESCRIPTION OF TABLES 3-5
Tables 3-5 list the analyses for the samples of stream-sediment, concentrate, and rock, respectively. For the three tables the data are arranged so that column 1 contains the USGS-assigned sample numbers. These numbers correspond to the numbers shown on the site location maps (plates 1 and 2). Columns in which the element headings show the letter "s" below the element symbol are emission spectrographic analyses. In a similar manner, "aa" indicates atomic absorption analyses. A letter "N" in the tables indicates that a given element was looked for but not detected at the lower limit of determination shown for that element in table 1. If an element was
-
observed but was below the lowest reporting value, then a "less than" symbol () was entered in the tables in front of the upper limit of determination. If an element was not looked for in a sample, then two dashes (--) are entered in tables 3-5 in place of an analytical value. Because of the formatting used in the computer program that produced tables 3-5, some of the elements listed in these tables (Fe, Mg, Ca, Ti, Ag, and Be) carry one or more nonsignificant digits to the right of the significant digits. The analysts did not determine these elements to the accuracy suggested by the extra zeroes.
The spectrographic determinations for Ag, As, Au, Cd, Sb, and Zn in stream-sediment samples, for Au, Cd, and Zn in concentrate samples, and for Au in rock samples were all below the lower limits of determinations shown in table 1; consequently the columns for these elements have been deleted from tables 3, 4, and 5, respectively.
REFERENCES CITED
Grimes, D. J., and Marranzino, A. P., 1968, Direct-current arc andalternating-current spark emission spectrographic field methods for the semiquantitative analysis of geologic materials: U.S. Geological Survey Circular 591, 6 p.
Meier, A. L., 1980, Flameless atomic-absorption determination of gold ingeological materials: Journal of Geochemical Exploration, v. 13, no. 1, p. 77-85.
Motooka, J. M., and Grimes, D. J., 1976, Analytical precision of one-sixth order semiquantitative spectrographic analyses: U.S. Geological Survey Circular 738, 25 p.
Nokleberg, W. J., Moore, J. G., Chaffee, M. A., and Griscom, Andrew, 1983,Mineral resource potential map of the Kings River, Rancheria, Agnew, and Oat Mountain Roadless Areas, Fresno County, California: U.S. Geological Survey Miscellaneous Field Studies Map MF-1564-A, scale 1:62,500.
Thompson, C. E., Nakagawa, H. M., and VanSickle, G. H., 1968, Rapid analysis for gold in geologic materials, j_n_ Geological Survey research 1968: U.S. Geological Survey Professional Paper 600-B, p. B130-B132.
VanTrump, George, Jr., and Miesch, A. T., 1976, The U.S. Geological Survey RASS-STATPAC system for management and statistical reduction of geochemical data: Computers and Geosciences, v. 3, p. 475-488.
Ward, F. N., Nakagawa, H. M., Harms, T. F., and VanSickle, G. H., 1969, Atomic-absorption methods useful in geochemical exploration: U.S. Geological Survey Bulletin 1289, 45 p.
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Table 3.--Data fo
r s tr ear
n-se
d i ment samples/ Kings River/ Rancheria/ Agnew/ an
d Oat Mountain Roadless Areas/ California
Sample
Latitude
Longitude
81NK019A
81NK026C
81NK027A
81NKQ28A
81NK033A
81NK046A
81NK053A
81NK054A
81NK059A
81NK060A
81NK071A
81NK073A
81NK074A
81NK094A
81NK095A
81NK096A
81RM001A
81RMOQ3B
81RM006A
81RM007C
81RM015A
81RM017A
81RM018A
81RM019A
81RM027A
81RM028B
81RM030A
81RM031A
81RM032A
81RM041A
81RM051A
81RM052A
81RM077A
81RM078A
81 RM097A
81RM124A
81 Sti
004A
81SB012A
81S8018A
81SB019A
81SB023A
81SB029A
81SB030A
815B032A
H1SB033A
36 36 36 36 36 36 36 36 36 36 36
36 36 36 36 36 36
36 36
36 36 36 36
36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36
53 49 49 49 50 46 49 49 48 48 49
47 47 48 49 49 52 53 52
52 52 52 52 52 52 52 52 54 54 50 48
48 48 48 48 56 51 51 50 50 50 49 50
49 49
25 52 240 5
43 318
38 29 40 50 52 580 8
424
36 27
8 7 8224 2
458
25 18 20 1 5
12 32 43 27 25 38 27 37 58
476
1 1
57
1 1 9
1 19
1 19
119
119
119
119
1 19
118
118
118
118
118
118
118
118
119
119
11 9
1 19
119
119
11 9
1 19
1 19
119
11 9
11 9
119
119
11 9
119
118
118
1 18
1 18
1 19
119
119
119
1 1 9
1 19
11 9
1 19
119
7 8 8 8 9 0 0 058 58 52 53 53 53 53 539 9
10 10 14 13 1 2
118 8 7 6 5 9 3 3
51 51 49 555 2 5 5 5 3 3
1 2
13
12 48 30 26 41 32 49 540
22
532 45 20 23
8 820 38 59 101
42 49 29 223
59 336
41 30 57 22 57 30 417
16 11 45 25 18
40 31
Fe-pc t.
s
5 5 5 5 5 2 2 2 5 2 7 5 5 3 5 5 5 5 5 5 5 5 5 5 5 5 5 5 5 5 5 3 5 5 5 5 3 5 5 3 5 3 3 5 7
Mg-pc t.
s 1.5
1.5 ,7
1,0
1,0 ,5
.5
,5
.7
.5
1 .0
1,0 .7 ,7
1.0
1,0
1.0
1.5
1.0
1.0
1.0
1.0
1.5
1,0
1.0
1.5
1.5
1.5
1,5
1.5
1.5
.7
1.0
1,0
1,0
1,0 .7
1.0
1.0 .7
UO
,7
1.0
1.0
1.0
C a-pc t.
s 3.0
3.0
1.0
2.0
2.0
1 .0
1 .5
1 .5
2.0
1.5
2.0
2.0
2.0
1.5
2.0
2.0
2.0
2.0
2.0
2.0
2.0
2.0
2.0
3.0
1 .5
2.0
3.0
2.0
3.0
2.0
2.0
1.5
2.0
2.0
1 .5
1 .5
1 .5
1.5
2.0
2.0
2.0
Vi-pct.
s
1.0
1 .0 .5 .7 .7 .2
.2
.2
.3
.2 .5
.3
.3
.3
.3 .3
.5
.7
,7
.5 .7
.7
.7
1.0 .5 .5
.7
.7
.7
.7 .5
.5
.3
.5
,5 .5
.3
.3
.3
.3 .5
.5
.2
.5
.5
Mn-ppm
s
1/500
1 /500
1 /OOO
1/000
1 /OOO
500
500
300
1/500
1 /500
1 /OOO
1 /OOO
1 ,000
700
1 /OOO
1/000
1 /OOO
1 /500
1 /OOO
1 /500
1/000
1 /OOO
1/000
1/500
700
1 /500
1 /500
1/500
1 ,500
1 ,500
1 /500
700
1,000
1,000
1,000
1,000
500
700
1 ,000
1/000
1/000
1 ,000
1 ,500
1,500
1,500
B-ppm
S
20 20 50 20 50 10 10 10 10 10 10 10 10 10 10 50 30 20 50 20 20 20 20
100 20 20 10 20 20 30 70 10 10 10 20 20 20 20 10 70 30 10 20 20
Ba-ppm
s
700
500
1 ,500
1 ,500
1 ,000
300
300
500
1 ,500
700
300
500
500
300
300
500
500
1 ,000
700
1 ,000
500
500
700
1 ,000
1 ,000
1,000
1 ,000
200
1 ,500
300
700
1 ,000
500
300
300
300
500
1/000
500
500
300
700
500
500
500
-
Ta
ble
3.-
-Data
fo
r str
ea
m-s
ed
ime
nt
sa
mp
les/
Kin
gs
Riv
er,
R
ancheria,
Ag
ne
w,
and
Oat
Mo
un
tain
R
oa
dle
ss
Are
as,
Ca
lifo
rnia
Sa
mp
le
81NK019A
81NK026C
81NK027A
81NK028A
81NK033A
81 NKCK6A
81NK053A
81NK054A
81NK059A
81NK060A
81NK071A
81NK073A
81NK074A
81NK094A
81NK095A
81NK096A
81RM001A
81RM003B
81RM006A
81RMOU7C
)81RM015A
81RM017A
81RM018A
81RM019A
81RM027A
81RM028B
81RM030A
81RM031A
81RM032A
81 RMCK1 A
81RM051A
81RM052A
81RM077A
81RM078A
81 RM097A
81 RM1 24A
81SBOCKA
81SB012A
81SB018A
81SB019A
81SB023A
81SB029A
81SB030A
81SB032A
81SB033A
Be-ppm
s
1 .0
1 .0
1 .5
1 .0
1.0
2.0
2.0
2.0
2.0
2.0
1.0
1.5
1 .5
2.0
2.0
2.0
1 .0
1 .0
1 .0
1.0
1.0
1 .0
1 .0
1 .0
1.0
1.0
1.0
1.0
1 .0
1.0
1 .0
1 .0
2.0
2.0
2.0
2.0
2.0
2.0
1 .0
2.0
1.0
2.0
1 .0
1 .0
1 .0
Bi-ppm
s
N N N N N N N N N N N
N N N N N N N N
N N N N N N N N N N N N N N N N N N N N N N N N N N
Co-ppm
s
20 20 20 20 20 5 5 10 10 10 20 20 15 1 5
20 10 20 20 20 20 20 20 30 15 15 20 20
20 20 20 20 10 10
20 20 20 10 1 0
1 5
10 20 10 10 20 30
C r-ppm
s
100
100
150
100
100 N
<10
,1 50 20 70 30
20 10 10
100 20
100
1 50
100
1 50
100
100
100
200
150 50
100 50
1 50
200 50
1 00 10
100
100
100 30
1 50 20 10 70 20 20 70
200
C u-ppm
s
50 50 50 50 50
-
Table
3.-
-Data
fo
r str
ea
m-s
ed
ime
nt
sam
ple
s/
Kin
gs
Riv
er*
R
ancheria/
Agneu/
an
d
Oat
Mounta
in
Ro
ad
less
Are
as/
Ca
lifo
rnia
Sam
ple
81NK019A
81NK026C
81NK027A
81NK028A
81NK033A
81NK046A
81NK053A
81NK054A
81NK059A
81NK060A
81NK071 A
81NK073A
81NK074A
81NK094A
81NK095A
81NK096A
81RM001A
81RM003B
81RM006A
81RM007C
81RM015A
81RM017A
81 RM018A
81RM019A
81RM027A
81RM0288
81 RM030A
81 RM031A
81 RM032A
81 RMCK1 A
81 RM051 A
81RM052A
81RM077A
81RM078A
81RM097A
81RM124A
81SB004A
81SB012A
81SB018A
81SB019A
81SB023A
81SB029A
81SB030A
81SB032A
R1
Pb-ppm
s
20 50 30 30 30 30 30 30 50 30 20
20 30
20 20 20 20 30 20 30 20 30 30 20 30 30 20 20 30 20 20
30 30
20 20 20 20 50 10 20 10 30 10
20 20
Sc-ppm
s
30 50 20 30 30
7 5 7 107
20
30 20 15 20 30 20 50 20 30 30 30 30 30 20 30 30 30 50 30 30 10 30
30 30 30 15 20 20
10 20 20 20 20 30
Sn-ppm
s
N N N N N N N N N N N
20 N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
Sr-ppm
s
500
500
200
300
300
200
300
300
,500
300
300
200
300
200
200
300
300
500
200
200
500
500
500
500
200
500
500
300
500
.300
300
300
300
500
300
300
300
500
300
200
200
300
300
300
300
V-ppm
S 200
200
150
200
200 50 30 50 50 50
100
100
100 70
100
100
200
300
200
200
200
200
200
200
200
200
200
200
200
200
200
100
100
200
100
100
100
100
100
50
100 70
100
100
150
W-ppm
S
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
Y-ppm
S
50 70 50 70 50 20
20 20 50 30 30
70 50 50 50 50 50 70 70 50 30 30 30 50 30 50 50 50 70 50 50 50 70
50 50 70 30 50
30
30 30 70 50 50
50
Zr-ppm
s
150
700
300
500
300
200 70
100
700
500
500
1 /OOO
300
200
300
300
200
200
200
300
300
150
150
300
200
500
200 70
300
300
300
300
500
100
200
300
200
300
200
200
100
500
500
300
200
T h-ppm
s
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
I n-ppm
aa
-- tm *"
tm
-
Table
3
Sample
81 SB034A
81SB036A
81 SB042A
81SB058A
81ZN006A
81 ZN011 A
812N013A
81ZN014A
81ZN015A
81ZN016A
81ZN020A
81ZN021A
81ZN022A
82CB029A
82CB030A
82CB031A
82JM041A
82MC001 A
82MC002A
82MC003A
82MC004A
82MC005A
82MC006A
82MC007A
82MC008A
82MC009A
8 2 M C 01
0 A
82MC011A
82MC012A
82MC013A
82MCOUA
82MC015A
82MC016A
82MC017A
82MC018A
82MC019A
82MC020A
82MC021A
82MC022A
82MC023A
82MC024A
82MC025A
82MC026A
82MC027A
82MC028A
.--Data for
stream-sediment samples/ Kings River/ Rancheria/ Agnew/ and Oat Mountain Roadless Areas/ Ca
I ifornia--continued
La t
i t ude
Longitude
36 36
36 36
36 36 36 36 36 36 36
36 36 36 36
36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36
36 36 36 36 36 36 36
50 49 47 48 51 51 51 51 51 51 51 51 51 47 47 47 52 52 53 54 52 51 51 51 51 51 51 52 47 48 50 56 56 56 57 57 56 58 58 57 57 57 57 51 51
1 2 8
19 18
41 45 37 40 46 53 51 51 54 31 32 333
32 573
16 49 30 22 18
2123
42 41
11
11 2
33 28 21 53 32 29 21 25 22 1 1
36 33
119
119
119
1 1 9
119
1 19
1 19
1 19
119
119
11 8
118
118
1 18
118
118
118
119
119
119
1 19
119
119
1 19
118
118
118
1 18
1 19
119
11 9
118
1 18
1 18
118
1 1 8
118
118
1 18
118
118
1 18
118
1 19
1 19
135 5 4 6 2 3 4 3 1
58 58 57 44 44
44 58 5 4 4 1 0 0 0 59 58 57 564 2
12 54 54 55 54 54 51 55 55 57 57 56 56 10 10
48 13
133
10 45 38 41 11 29 55
230
21 1 7
11 29 50 20 18 37 49 59 1 1
55
012 39 58 39 21 47 40 32 10 9
29 13 11 25 316 7
30 38
Fe-pc t.
s
7 5 7 5 5 710 105 7 5
105 5 7 5 7 5 5 5 7 7 5
105 7 3 5 5 2 7 7 7 5 5 5 3 5 5 7 5 5 5 3 5
Mg-pct.
s 1.0
1.0
1.0
1.0
1.0
1.5
1.5
1.5
1.0
1.5
1.0
1.5
1.0
1.5
2,0
1.5
1,5
1,0
1.0
1,0
2,0
1,5
1,0
2.0
1,5
1,5 .7
1 .0
1.5 .5
1.5
2.0
1.0
1.5
2.0
1.5
1.0
1.0
1.5
3.0
1.0
5.0
1.5
.7
1.5
C a-pct,
s 2.0
2.0
3.0
1 .0
1.0
2.0
3.0
3.0
1 .0
2.0
2.0
3.0
2.0
5.0
5.0
3.0
5.0
1.5
1 .5
5.0
3.0
1 .5
1 .5
2.0
3.0
1.0
3.0
5.0
1 .5
3.0
3.0
1 .5
1 .5
5.0
1 .5
1 .0
Ti-pct.
s
1 .0
.3
.5
.5
.3 .5
1.0 .5
.5
.7 .7
.7
.5
.5
.1 .7
.1
.7
.7
1.0
1.0
1.0 .5
1.0
.7 .7 .5
.5
.5
.5
>1 .0 .1
.7
.5
.5 .5
.5
.5 .51.0 .5
.7
.7
.3
.7
Mn-pp m
S
2/000
1 /500
1 /500
1/500
1 /OOO
1 /500
2/000
2/000
1 /OOO
1 /500
1 /500
1/500
1/000
700
1 /500
700
1 /500
1 /OOO
1 /OOO
1/000
1 /500
3/000
1/000
1 /500
1 /OOO
1 /500
700
1 /OOO
1 /500
700
2/000
1 /500
1 /OOO
700
700
1 /OOO
700
700
700
1/000
1 /OOO
1 /OOO
1 /OOO
500
1 /OOO
8- ppm
S8a-ppm
s
20 20 50300
100
100 20 20
100 20 10 10 15 20 15 15 15
100
100 10
<10 10 10 15 15 10 70 10 50 15
-
Table
3
Sample
81SB034A
81S6036A
81SD058A
81ZN006A
81ZN011A
81ZN013A
81 ZNOUA
81ZN015A
81ZN016A
81ZN020A
81ZN021A
81ZN022A
82CB029A
82C8030A
82CB031A
82JMQA1A
82MC001A
82MC002A
82MC003A
82HC004A
82MC005A
82MC006A
82HC007A
82MC008A
82MC009A
82MC010A
82MC011A
82MC012A
82MC013A
82MCOUA
82MC015A
82MC016A
82MC017A
82HC018A
82MC019A
82MC020A
82MC021A
82MC022A
82MC023A
82MC024A
82MC025A
82MC026A
82MC027A
82NC028A
.--Data fo
r stream-sediment samples/ Kings River/ Rancheria/ Agnew/ and Oat Mountain Roadless Areas/ California--
8e-ppm
s
1.0
1.0
1 .0
1 .5
1.5
1 .5
1.0
1.0
1.5
1,0
1,0
1.0
1.5
1,5
1,5
1,5
1.5
1 .0
1.5
1.5
:i .0
1 .5
2.0
1 .0
1.5
1 .0
1.5
2.0
1.0
2.0
:1 .0
1 .5
1.0
1.5
1.5
1 .5
2.0
1 .5
2.0
1 .5
1 .5
1 .5
1.5
B i-ppm
s
N N N N N N
N N N N
20 N N N N N N N N N N
N N N N N N N N N N N N N N N N N N N N N N N N
Co-ppm
S
20 15 20 1 5
15 20 20 20 20 20 10 20 10
15 20 30 30 20 20 10 30 20 15 30 15 20 20 10 155
20 30
20 20 20 30 10 15 15 30 20 30 20 15 30
Cr-ppm
s
70 50 50
150 50
1 50
1 50
200
200
100 30
100 30 15
30
300 50 70
150 50 30 20 30 70 30 20 70
20 20 15 15
200
10070
500
200
100
150
200
500
150
700
1 50 50
150
Cu-ppm
s
50 50 1 5
70 50 70 70 70
100 50 10 15 107
20 50 15 70 507
-
Table
3
Sample
81SB034A
81SB036A
81S0042A
81SB058A
81ZN006A
81ZN011 A
81ZN013A
81ZN014A
81ZN015A
81ZN016A
81ZN020A
81ZN021A
81ZN022A
82C8029A
82C8030A
82CB031A
82JM041A
82MC001A
82MC002A
82MC003A
t> 82MC004A
82MC005A
82MC006A
82MC007A
82MC008A
82MC009A
82MC010A
82MC011A
82MC012A
82MC013A
82MC014A
82MC015A
82MC016A
82MC017A
82MC018A
82MC019A
82MC020A
82MC021A
82MC022A
82MC023A
82MC024A
82MC025A
82MC026A
82MC027A
82MC028A
.--Data for
stream-sediment samples* Kings River* Rancheria* Agnew* and Oat Mountain Roadless Areas* California--
Pb-ppm
s
20
20 20 30 15 30 20 20
30
20 20 20
100
20 15 20 15 15
20 15 10 15 15 15 20 20
10 20 10
20 10 15 20 15 20 2020 20
20 15 20 30 20 20
20
Sc-ppm
s
30 30 30 20 20
30 50 30 20
30 20
30 20 20 20 20 30 15 20 20 30 20 15 30
10 20 15 10
20 5 30 20 20 20 15 15 10 107
20 20 20 20 10
20
Sn-p
pra
s
N N N N N N N N N N N N N N N N N N N N N
15N N N N N N N N N N N N N N N N N N N N N N N
Sr-ppm
sV-ppm
S
300
300
300
200
200
300
500
500
,200
300
200
500
300
500
500
500
200
200
150
200
150
200
200
200
200
200
150
200
200
200
200
200
200
200
200
200
300
200
300
300
200
300
200
100
100
100
150
150
200
150
200
200
300
200
200
100
200
100
100
150
100
150
100
150
100
150
100 70
200
100
100
100
150
100 50
100
150
100
100 70
100 70
100 70
150
100
100
100
100
150
W-ppm
s
N N N N N N
N N N N N N N N N N N N N N N
50
N N N N
N N N N N N N N N N N N N N N N N N N
Y-ppm
S
Z r-ppm
s
50 50
50 5020
50
50
50
30 50
70
70
303050
30
303030
70 3050
20
50
30 50
30 50
3030 50
50
5070 20
2020
20 20
50
30 3050
20
20
300
200
500
200 70
200
200
500
150
300
300
500
500
300
500
200
300
200
200
300
150
700
500
500
200
300
200
500
100
200
>1*000
500
500
500
300
500
300
300
200
500
500
300
300
100
150
T h-ppm
s
N N N N N N N N N N N N N N N N N N
N N N N N N N N N N N N N N N N
100 N N N N N N N N N N
cont i
nued
Zn-ppm
aa
30
20 45 40 75
80 15 20 30 45 30 30
45 65 35 1530 25 25 30 35 30 40 25 35 20 30 40
35
3Q
110 65
-
Table
3
Sample
82MC029A
82MC030A
82MC031A
82MC032A
82MC033A
82MC034A
82MC035A
82MC036A
82MC037A
82MC038A
82MC039A
82MC040A
82MC041A
82MC042A
82MC043A
82MC044A
82MC045A
82MC046A
82MC047A
82MC048A
k. 82MC049A
82MC050A
82MC051A
82MC052A
82MC053A
82MC054A
82MC055A
82MC056A
82MC057A
82MC058A
82MC059A
82NK033A
82NK034A
82NK051A
82NK052A
82RM047A
82SB061C
, Data for stream-sediment samples/ Kings River* Rancheria/ Agnew/ and Oat Mountain Roadless Areas/ Ca Iifornia--continued
Lati tude
Long i
tude
36
3636 36
36 36 3636
36 36
36 36
363636 36
36 36
3636
36
36
36 36
36
36 36 36
36 36
3636
36
36 36 36
36
50
50 47 47
48 48
48 48
47 50
50 50 51 50
50 51 52 52
53 53 52 52 52 52
52 51 51 49
49 48
48 47
47
47
47 51 46
56
58
40 47 13 21 19 1
1 3
14 33
317
58
57 12 57 59
38 36
41 59 58 38
38 31 28
36 0
48
49 38
4243
48 21 52
119
1 19
118
1 18
118
1 18
1 18
118
11 8
1 18
118
118
1 18
1 18
118
1 19
1 18
1 18
118
1 18
11 8
11 8 1818
18 18 18
18
118
1 18
.118
1 19
119
119
119
1 1 9
1 18
7 743 43
45
464848
47 52 52 52 53 55 55 1 4
59 58
57 57
55 55 55 53 53 52 52 58
50 49 482 2 1 1
1 2
47
28
32 129 2
51 39 8
27 47 117
55 13
48 593
58 21 13 59
24 20 21 13
22 26 59 22 59 57 38 33 52 51 59
52
Fe-pc t.
s
7 5107 3 5 5 5 3 5 5 7 7 5 5 5 5 5 5 7 3 7 5 3 3 3 3 5 3 5 3 5 3 2 5 3 5
Mg-pc t .
s 2.0
US
1.5.7
.7
1 .5
1.0
, 1.0
.7
1.5 .5
1.5
.7 .7
1.5
1.5
1.5
1.5
1.5
1 .0
1.0
1.5
1-5 .5
.7
.7
.5
1 .5
1.0
1.0
1.5
1.5
.7
-5
1.0
1.0
1.0
Ca-pct.
s 5.0
2.0
1.5
2.0
1.5
2.0
1 .0
5.0
1 .5
1.5
5.0
2.0
1 .5
3.0
3.0
3.0
2.0
2.0
5.0
1.0
1.5
1.5
1.5
2.0
2.0
1 .5
5.0
3.0
1.5
2.0
3.0
2.0
2.0
Ti-pct.
s
1.0
.71.0
.5
.5 .7
.5
.5
.5 .5 .3
1.0
.5
.5
.7 .7
.51 .0
.7
.7 .5
.5
1 .0
.5
.3 .3
.5
.5
.7
.5 .5
.7
.5
.3
.7 .5
.5
Mn-ppm
s
2/000
1 /OOO
1/000
700
700
1/000
700
1/000
500
1/000
700
1 /500
1/000
1 /OOO
1/000
1/000
700
1/000
1/000
1 /OOO
1/000
700
1/000
700
700
700
500
2/000
1/000
1 /OOO
1/500
700
1/000
500
1/000
1/000
1 /OOO
B-ppm
s
20100 20 10
70 30 15 50
200 10 10
50
15
<10
10 20
<10
15
10
10 20 20 15 10 15 15
20 50
100 30 15
10 15 20 15
Ba-ppm
s
300
700
500
300
700
500
700
700
1/000
500
500
700
500
500
500
500
300
500
500
300
700
300
500
300
500
500
500
700
2/000
300
500
500
700
1 /OOO
700
1 /OOO
700
-
Table
3
S a mp
I e
82MC029A
82MC030A
82MC031 A
82MC032A
82MC033A
82MC034A
82MC035A
82MC036A
82MC037A
82MC038A
82MC039A
82MC040A
82MC041A
82MC042A
82MC043A
82MC044A
82MCCK5A
82MC046A
82MC047A
82MC048A
82MC049A
82MC050A
82MC051A
82MC052A
82HC053A
82MC054A
82MC055A
82MC056A
82MC057A
82MC058A
82MC059A
82NK033A
82NK034A
82NK051A
82NK052A
82RM047A
82SB061C
,--Oata fo
r stream-sediment samples* Kings River* Rancheria* Agneu* an
d Oat Mountain Roadless Areas* Ca
I ifornia--continued
Be-ppm
s
-
Table 3.--Data fo
r stream-sediment samples/ Kings River/ Rancheria/ Agnew/ and Oat Mountain Roadless Areas/ California--continued
Sample
82MC029A
82MC030A
82MC031A
82MC032A
82MC033A
82MC034A
82MC035A
82MC036A
82MC037A
82MC038A
82MC039A
82MC040A
82MC041A
82MC042A
82MC043A
82MC044A
82MC045A
82MC046A
82MC047A
82MC048A
82MC049A
82MC050A
82MC051A
82MC052A
82MC053A
82MC054A
82MC055A
82MC056A
82MC057A
82MC058A
82MC059A
82NK033A
82NK034A
82NK051A
82NKOS2A
82RM047A
82SB061C
Pb-ppm
s
15 20 20 10 15 15 20 30 15 15 20 15 20 20 15 10 20 20 20 15 20 10 20 20 20 20 20 50 15 15 15 15 20 20 15 15 20
Sc-ppm
s
30 20 15 107
20 15 10
10 30
720 10 10 30 20 20 20 15 10 7
15 155 5
107
15 15 15
7207 7
10 10 15
Sn-ppm
s
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
Sr-ppm
S
200
1 50
300
200
200
200
200
200
150
200
200
200
200
200
200
200
150
200
300
200
200
200
300
200
200
200
200
200
200
200
150
300
200
200
300
200
200
V-ppm
s 200
100
200
150
' 50
100
100
100
150
100
100
150
100
100
100
100
100
100
150
100
70
100
100 70 50
50 50
100
100
100
701 50
50 50 70
100
100
W-ppm
S
N N N N N N N N N N N N<50 N N N N N N N N N N N N
<50 N N N N N N N N N N N
Y-ppm
S
20 50 50 20 30 20 30 30 20 50 50 50
100 50 70 30 50 70 50
30
50
20 50
70 30 50 50 20
20 30 30 30
30 1 5
50
20 20
2 r-ppm
s
100
300
500
300
200
300
300
300
500
500
300
300
500
500
700
500
200
500
300
300
500
300
300
200
200
200
300
200
300
300
150
300
200
200
200
150
700
Th-ppm
S
N N100 N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
<100 N N
Zn-ppm
aa
30 65 20 40 50 25 30 35 60 25 30 25 40 45 1 5
25 25 35 40 40 40 40 30
40 35 45 35 60 45 50 80 40 45 30 35 50 30
-
Table 4.--Data for
concentrate samples* Kings River/ Rancheria/ Agneu/ and Oa
t Mountain Roadless Areas/ California
Sample
Lat
i tude
Long i
t ude
82MC001B
82MC002B
82MC003B
82MC004B
82MC005B
82MC006B
82MC007B
82MC008B
82MC009B
82MC011B
82MC012B
82MC013B
82MC014B
82MC015B
82MC016B
82MC017B
82MC018B
82MC019B
82MC020B
82MC021B
82MC022B
82MC023B
82MC024B
82MC025B
82MC026B
82MC027B
82MC028B
82MC029B
82MC030B
82MC032B
82MC033B
82MC034B
82MC035B
82MC036B
82MC037B
82MC038B
82MC039B
82MC040B
82MC041B
82MC042B
82MC043B
82MC044B
82MC045B
82MC046B
82MC047B
36 36 36 36 36
36 36
36 36
36 36 36 36
36 36
36 36 36 36
36 36 36 36 36 36 36 36
36 36 36 36 36 36
36 36 36 36 36 36 36 36 36 36 36 36
52 53 54 52 51 51 51 51 51 52 47 48 50 56 56 56 57 57 56
58 58
57 57 57 57
51 51 50 50
47 48
48 48
48 47 50 50 50 51 50 50 51 52 52 53
32 573
16 49 30 22 182 3
42 411
11 12 33 28 21 53 32 29 21 25 22 1 1
36 33 56 58 47 13
21 19 1 13 14 33 317
58 57 12 57 59 38
1 19
119
119
119
1 19
1 19
1 19
1 18
1 18
1 18
1 19
1 19
119
118
118
118
118
118
1 18
1 18
118
118
1 18
1 18
118
1 19
1 19
119
119
118
1 18
118
118
118
1 18
118
118
1 18
118
1 18
118
1 19
118
1 18
118
5 4 4 1 0 0 059 58 56
4 212 54 54 55 54 54 51 55 53 57 57 56 56 10 107 7
43 45
46 48
48 47 52 52 52 53 55 55 14 59 58 57
50 20 18 37 49 59 1 1
55 0 39 58
39 21 47
40 32 109
29 13 55 25 316 7
30 38 28 329 2
51 39 8
27 47 1 1 7
55 13 48 593
58 21
Fe-pct .
s
.51.
01.
51.0 .7
1.0
1.0
1.5
2.0
1.0
1.0 .7 .3
1.5 .7 .7 .7
1.0 .7 .7 .7
1.5 .7
1.0
1.5
2.0
1.0
2.0
2.0
1.0 .7 .7
1.5
1.0 .5 .7
1.0
1.0
2,0 .7
1 .0 .7 .7 .7 .5
Mg-pc t .
S
.30
.20
.70
.20
.70
.15
.70
1.50
.,.50
.50
.10
.10
.07
1.00
.20
.50
.10
1 .00
.10
.15
1.00
3.00
.15
3.00
1 .0
0
1.00
.70
1.00
.70
.15
.10
1.00
.50
3.00
.70
.30
.30
.30
.10
.30
.20
.70
.15
.20
.10
Ca-pc t
.s 15.0
1.5
10.0
10.0
15.0
7.0
10.0
10.0
5.0
15.0
2.0
3.0
10.0
15.0
20.0
15.0
15.0
1 5.0
15.0
10.0
15.0
20.0
15.0
15.0
20.0
5.0
7.0
10.0
10.0
20.0
20.0
10.0
15.0
10.0
15.0
5.0
7.0
10.0
10.0
10.0
10.0
7.0
3.0
1 5.0
15.0
Ti-pct .
s >2.0
>2.0
>2.0
>2.0
2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
>2.0
Mn-ppm
S
500
150
700
300
500
500
300
500
300
300
150
200
150
700
500
300
1/000
1/000
700
700
700
1/000
700
1 /OOO
1/000
200
1/500
500
700
1/000
700
700
700
500
700
200
500
1/000
500
1/000
500
300
150
500
500
A s-ppm
S
N N N N N
2/000 N
500 N N N N N N N N N N N N N N N N N N N N N N N N
2/000 N N N
700
5/000 N N N N N N N
B-ppm
s
700
150 30 20
-
Table A.
Data fo
r concentrate samples* Kings River/ Rancheria/ Agnew/ and Oat
Mountain Roadless Areas* California
Sample
82MC001B
82MC002B
82MC003B
82MC004B
82MC005B
82MC006B
82MC007B
82MC008B
82MC009B
82MC011B
82MC012B
82MC013B
82MCOUB
82HC015B
82MC016B
82MC017B
82MC018B
82MC019B
82MC020B
82MC021B
82MC022B
82MC023B
82MC02AB
82MC025B
82MC026B
82MC027B
82MC028B
82MC029B
82MC030B
82MC032B
82MC033B
82MC034B
82MC035B
82MC036B
82MC037B
82MC038B
82MC039B
82MC040B
82MCOUB
82MC042B
82MC043B
82MCCK4B
82MC045B
82MC046B
82MC047B
Be-ppm
s
N N N
-
Table
4.--Data fo
r concentrate samples/ Kings River/ Rancheria/ Agnew/ and
Oat
Mountain Roadless Areas/ California
Sample
82MC001B
82MC002B
82MC003B
82MC004B
82MC005B
82MC006B
82MC007B
82MC008B
82MC009B
82MC011B
82MC012B
82MC013B
82MCOUB
82MC015B
82MC016B
82MC017B
82MC018B
82MC019B
82MC020B
82MC021B
82MC022B
82MC023B
82MC024B
82MC025B
82MC026B
82MC027B
82MC028B
82MC029B
82MC030B
82MC032B
82MC033B
82MC034B
82MC035B
82MC036B
82MC037B
82MC038B
82MC039B
82MC040B
82MC041B
82MC042B
82MC04.3B
82MCO^^B
82MC045B
82MC046B
82MC047B
S b-ppm
s
N N N N N N N
1/000 N N N N N N N N N N N N N N N N N N N N N N N
N N N N N N N N N N N N N N
Sc-ppm
s
20 30 15 20 30 30 20 50 70 30 70 30 70 1 5
15 30 20 20 15 15 30
20 15 30 20 15 30 50 1 5
10 10 15 20 15 20 50 30 20 50 30 30 20 50 20 20
Sn-ppm
s
100
-
Table
4. D
ata
fo
r concentr
ate
sam
ple
s/
Kin
gs
Riv
er/
R
an
ch
eria
/ A
gn
ew
/ and
Oa
t M
ou
nta
in
Ro
ad
less
Are
as/
Ca
Iifo
rnia
--co
ntin
ue
d
S a
mp
le
82
HC
05
98
La
t i tu
de
36
48
49
Long i t
ude
82MC0488
82MC0498
82MC050B
82MC0518
82MC0528
82MC053B
82MC054B
82MC056B
82MC057B
82MCOS88
36 36 36 36
36 36
36 36 36 36
53 52 52 52 52 52 51 49 49 48
36 41 59 58
38 38 31 360
48
118
1 18
118
1 18
118
118
1 18
118
1 18
1 18
57 55 55 55
53 53 52 58 50 49
13 59 24 20
21 13
22 59 22 59
11
8
48
57
Fe-pct.
s 1.0
1.5
1.5
1.0
2.0
1.0
1.5
1.0
1 .5
2.0
Mg-pc t .
C a-pc t
.s
.10
.30
1 .50
.70
.20
.70
50
.20
,.50
1.00
s 15.0
1 5,0
10,0
10.0
1.0
3.0
3.0
15.0
20.0
3.0
T i-pc t .
s >2.0
>2.0
>2.0
>2.0
2.0
2.0
2.0
>2.0
>2.0
1 .5
Mn-ppm
s
500
700
300
300
1/500
300
500
300
300
300
Ag-ppm
s
N N N N N N N100 N N
As-ppm
s
N N N N N N N N N1 /OOO
B-ppm
s
N N
-
Table 4. Data
for
concentrate samples* Kings River, Rancheria/ Agnew/ and
Oat
Mountain Roadless Areas/ California continued
Sample
82MCOA8B
82MCOA9B
82MC050B
82MC051B
82MC052B
82MC053B
82MC05AB
82MC056B
82MC057B
82MC058B
82MC059B
8e-ppm
s
N N N N 2 N N N N N N
Bi-ppm
s 2/000
500 70
1/50
0 N 50>2/000 30
500 N
100
Co-ppm
s
70 15 70 30
30 15
15 10 70
100 20
C r-ppm
s
20 50 20 20
30 70 50 30
.,20 30
150
Cu-ppm
s
N 1010
010
0 10 10
2/000
>2/000
>2/000
>2/000
700
.50
150
Mo-ppm
s
200 N
100 50 N N 70 10 N 30
N
Nb-ppm
s
70200
<50 50
-
Table A.--Data for
concentrate samples/ Kings River/ Rancheria/ Agnew/ an
d Oat
Mountain Roadless Areas/ CaIifornia--continued
Sample
82MC048B
82MC049B
82MC050B
82MC0518
82MC0528
82MC053B
82MC0548
82MC0568
82MC057B
82MC058B
Sb-ppm
s
N N N N N N N2/000 N N
Sc-ppm
s
20 20 50 30 70 30
20 30
30 10
Sn-ppm
s
70100 N 20 20
N N>2/000 N N
S r-ppm
s
N N N<200 N N N
, N
300
<200
V-ppm
S 200
300
150
150 50 70 50
100
150 70
W-ppm
S
500
150
500
700
500
700
1/500
500
300
500
Y-ppm
s
700
1/000
700
500
>5/000
2/000
2/000
1/000
700
200
Z r-ppm
s
>2/000
>2/000
>2/000
>2/000
>2/000
>2/000
>2/000
>2/000
>2/000
>2/000
Th-ppm
S 1/000
2/000
1/500
1/500
>5/000
5/000
3/000
1/000
300
200
82MC0598
200
100
200
150
>2/000
200
-
v Ni
Tabl
e 5
Sample
81 NK003A
81 NK003B
81NK008A
81 NK010A
81 NK016A
81 NK0
1 7A
81NK018A
81 NK024A
81NK025A
81 NK026A
81 NK026B
81 NK029A
81 NK030B
81NK031 A
81 NK031B
81 NK032A
81 NK034A
81NK035A
81NK054B
81NK055A
81NK057A
81 NK058A
81 NK0
61 A
81NK062A
81 NK065A
81 NK068A
81NK069A
81 NK070A
81NK072A
81NK075A
81 NK076A
81 NK078A
81 NK080A
81NK081A
81NK082A
81 NK083D
81 NK085A
81NK086A
81NK088A
81 NK090A
81NK090B
81NK091 A
81 NK092A
81 NK097B
81 NK098C
. Data
for
Lat
i t ude
Lo
ng i tud
36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36 36
53 53 52 52 54 54 54 49 48 49 49 48 50 51 51 49 46 46 49 49 49 49 49 48 49 48 49 49 49 47 47 46 47 47 47 47 47 47 47 47 47 48 48 49 49
10 10 42 19 20 122 19 31 52 52 22 42 39 39 10
36 308
30 17 47 24 50 0 46 49 25 52 39 7 581 2
10
8 5 13 30 39 39 27 48 43 36
119
119
119
119
119
119
119
1 19
119
119
119
1 19
119
119
119
119
119
119
119
119
118
118
118
1 18
118
118
118 18 18 18 18 18 19 118
118
118
118
118
118
118
118
118
118
1 18
118
9 9 8 7 7 7 7 7 7 8 8 8 14 15 15 12 21 0 0 57 57 55 56 54 59 54 53 52 50 50 48 48 47 47 47 49 49
49 48 48 51 51 51 51
8 842 56 32 10 11 49 26 48 483
28 33 33 40 22 15 54 48 37 22 472
37 441
22 25 53 36 252 55 55 49 21 19 3
40 405
12 55 50
ta
for
rock
sa
mp
les/
Kin
gs
Riv
er/
R
ancheria/
Agnew
/ a
nd
O
at
Mo
un
tain
R
oa
dle
ss
Are
as/
Ca
lifo
rnia
Fe
-pct.
s 2.0
07.0
07.0
07.0
07.0
0
1.0
0
5.0
0
7.0
0
<.0
5
5.0
0
10
.00
5.0
01
0.0
01
0.0
01
0.0
0
10
.00
1.5
01.5
01.5
03.0
0
2.0
01.0
03.0
03.0
0.5
0
2.0
03.0
01
.50
3.0
03.0
0
5.0
01.5
0.0
51
.50
3.0
0
5.0
05
.00
20.0
07.0
0.1
0
.10
5.0
0.5
05
.00
5.0
0
Mg
-pc t.
s .20
1.0
02.0
0.7
01.0
0
.15
.70
1 .0
0<
.02
1 .0
0
1.5
01.0
02.0
07.0
03.0
0
2.0
0.3
0.2
0.5
03.0
0
.50
.20
1.0
03.0
0.0
7
.70
1 .0
0.5
01.0
0.7
0
1 .0
0.5
0.5
01.5
02.0
0
2.0
01
.00
.20
1 .5
0.7
0
1 .0
01
.00
.10
.70
.70
Ca
-pc t.
s
.70
1.5
05,0
01 .5
01
.50
.50
-50
,,1
.00
<,0
51.5
0
2.0
01
-50
10
.00
.07
5.0
0
2.0
0.5
0.5
01.0
03
.00
1-5
0
1.0
0
3.0
0
2.0
0
.20
1.5
02.0
01.5
02.0
01
.50
2.0
01
.50
1 5
.00 00
00
3.0
02.0
05.0
01 .0
01.5
0
2.0
0
.20
.0
5
.20
.20
T i-p
c t.
s
.100
.300
.300
1 .0
00
.300
.05
0-3
00
-70
0N .3
00
.500
.300
.700
.020
.700
.50
0.1
00
.100
.200
1.0
00
.200
.100
.500
.300
.050
.300
.500
.100
,300
.300
.500
.200
,002
.300
.500
.500
.500
-15
01 .0
00
.010
.010
.500
.200
4300
.500
Mn-p
pm
A
g-p
pm
s
s
200
1 /O
OO
1/500
1/000
1 /O
OO 300
500
500 70
700
1/000
1 /O
OO
1/500
1 /OOO
1 /5
00
1/000
300
300
500
700
300
300
1/500
1 /O
OO 50
1/000
1/000
300
500
700
1/000
700 70
700
500
700
1/000
>5/000
2/000
200
200
700 70
200
700
N N N N N
3.0
N N N N N N N N
N N N N N N N N N
N N N N N N N N
N 5/0
00
1/0
00
1/0
00
1/0
00
1/5
00
30
0
1 /5
00
50
07
00
500
2/0
00
1/0
00
1/0
00
<2
0500
30
0
500
1/0
00
30
01/0
00
50
0
10
07
00
10
0500
50
0
Be-p
pm
s 1 .0
-
Ta
ble
5. D
ata
fo
r ro
ck
s a
Sa
mp
le
81N
K003A
8
1N
K0
03
B
81N
K008A
8
1N
K0
10
A
81N
K016A
81N
K017A
81N
K018A
8
1N
K0
24
A
81
NK
02
5A
8
1N
K0
26
A
81N
K026B
8
1N
K0
29
A
81
NK
03
08
81N
K031A
8
1N
K0
31
8
81N
K032A
81N
K03A
A
81 N
K0
35
A
81 N
K0
54
B
81 N
K0
55
A
81 N
K057A
81
NK
05
8A
81
NK
06
1A
81
NK
06
2A
81
NK
06
5A
81 N
K068A
81
NK
06
9A
81N
K070A
81
NK
07
2A
8
1N
K0
75
A
81N
K076A
81
NK
07
8A
81N
K080A
81
NK
081 A
81N
K082A
81N
K0830
81
NK
08
5A
81
NK
086A
81N
K088A
81N
K090A
81
NK
09
0B
81N
K091A
81N
K092A
81N
K0978
81N
K098C
mp
les*
Kin
gs
Riv
er*
R
an
ch
eria
/ A
gn
ew
, a
nd
O
at
Mounta
in
Ro
ad
less
Are
as/
Ca
lifo
rnia
ppm
C
u-p
pm
La-p
pm
M
o-p
pm
N
b-p
pm
N
i-ppm
P
b-p
pm
S
b-p
pm
S
c-p
pm
S
n-p
pm
8 i -p
pm
s
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
C d
- pp
ms
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
Co-p
pm
s
<5
20
20
10
15 N
15
20 N
15
30 15 50
70
50
20 N N
<5
30 5 N 10
50 N
<5
15 N
10 5
10 N N
<5
10
10 5
15
1 5 N N
20
<5 15 15
Cr-
pp
m
Cu-p
pm
s
N<
10
100
150 N N
70
30
0 N20
20
20
20
03
,00
07
00
100 N N N
70
0 N N20
70
0 N N2
0 N2
01
0
10
<10 N 50
10
0
150
10
15
02
00 N N
200
20
100
10
0
.
s
N
20
20 30 10
N5
01
00 N 20
20 10
70
50
15
0 50 N N N
100 N N N 50
<5 N 5
<5 5 N
<5 15
<5 10
10
0
50
50
10
50
<5
20
70
<5
<5 50
La-p
pm
s
70
20
20
10
02
0
20
10
020>
20
20
20
50
20
20
20
50
20
30
30
70 70
70
70
70
50
50
50
70 50
70
50
50 N
50
50
50
70
50
100
20
20
70
20
30
70
Mo-p
pm
s
N N N N N
20 N N N N N N N N N N N N N N N N N N
10 N
<5 N N N N 5 N N N N N
<5 N N N
<5 N N N
Nb
-pp
mS <20
<20
<2
0<
20
<20
<2
0<
20
<20
<20
<20
<20
<20
<2
0<
20
<20
<20
<20
<20
<20
<20
<20
<2
0<
20
<20
<2
0
<20
<20
<20
<20
<20
<2
0<
20 N
<20
<20
<2
0<
20
<20
<20
<20
<20
<2
0 N N N
N i-p
pm
S
<5
<5 5
<5
<5
<5 50
10
0<
5 10 5 5
70
1/5
00
1 5
0
15
<5
<5
<5
300
<5
<5
<5
300 <5
<5
<5
<5
<5
<5
<5
<5 N
20
50
50
<5
20
50
<5
<5 50
<5 50
50
Pb-p
pm
s
10 10 15 30
10
300 20
20 N
10
10
15 10 N
20 20
30
30
20
70 10 50
30
30 20 50 20
50 20 50
50 50
<10 20 30
30 30
10 50N
00 30
N15 30
Sc-p
pm
s
520
30
30 10 5
10
50 N
20
30
20 50
20
50 305 5 5
30
5 520
20
<5
10
15 5
10
10
20 5 N
10
30 30
30
10
30 N N
305
10
10
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
N N N N20 N N N N N N N
-
Sample
Table 5. Data for
rock samples/ Kings River/ Rancheria/ Agnew/ an
d Oat
Mountain Roadless Areas/ California
Roc
k na
mes
Sr-
pp
m
V-p
pm
W
-pp
m
Y-p
pm
s
s s
sZ
n-p
pm
Z
r-p
pm
s
s
KJ
81 NK003A
81 NK0038
81NK008A
81NK010A
81 NK016A
81NK01 7A
81 NK018A
81NK024A
81NK025A
81NK026A
81 NK0268
81NK029A
81 NK0308
81NK031A
81 NK031B
81NK032A
81NK034A
81 NK035A
81 NK0548
81NK055A
81 NK057A
81 NK058A
81NK061 A
81 NK062A
81 NK065A
81NK068A
81 NK069A
81NK070A
81NK072A
81NK075A
81 NK076A
81NK078A
81NK080A
81NK081 A
81NK082A
81NK083D
81NK085A
81NK086A
81 NK088A
81NK09QA
81 NK0908
81NK091 A
81 NK092A
81NK097B
81 NK098C
300
300
500
700
500
100
200
100 N
300
500
300
500 N
200
500
200
200
200
5/000
700
150
700
1/000
100
500
500
500
500
500
500
500
300
100
500
1/000
300
200
200 N N
<100 N
100
100
10200
200
200 70 10
70200 N
100
200
100
300 30
300
200 20 20
20
100 20
< 10
100
100
<10 50
100 20
100 50 70 30 20
100
200
200
100
300
200 20 20
1 50 20 70 70
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N1/000 N N N N N N N
<10 30
30 50
<10 10 30 50N
20 50 20 50N
70 50N
00 20 30 20
1 00 50 20 20 20 20 30 20 50 50 20N
20 30 30 50 50 70N N
50
-
Table 5.--Data for
rock samples/ Kings River/ Rancheria/ Agnew/ and Oa
t Mountain Roadless Areas/ Ca Iifornia--continued
Sam
ple
81N
K102C
81N
K104A
81N
K106A
81
NK
10
7B
81
NK
10
8B
81N
K108C
81
NK
10
9B
81 N
K1
09
C81N
K1 1
1A81
NK
1 11
E
81
NK
11
4A
81N
K1148
81
NK
11
5A
81 N
K1
16A
81N
K1 1
7A
81 N
K1
18B
81 N
K1
18C
81N
K1 1
9A81N
K1 1
9A
81N
K121A
Ki
XT* 8
1N
K123A
81N
K124B
81N
K125A
81N
K1 2
8A
81 N
K130A
81 N
K1
34A
81 N
K136A
81
NK
13
8A
81
NK
14
2A
81N
K143A
81 N
K144A
81 N
K1
44
C81
NK
144E
81 N
K1
44
I81
NK
145A
81 N
K147A
81 N
K1
49
A81N
K157B
81N
K1 5
8A
81
RM
00
2A
81 R
M003D
81 R
M0
03
F81
RM
009A
81
RM
01
QA
81 R
M0
12
B
La
t i tu
de
36
49
36
49
36
49
36
4
836
48
36
4
836
49
36
49
36
49
36
49
36
48
36
48
36
48
36
4
83
6
48
36
4
836
48
36
4
83
6
48
36
48
36
48
36
48
36
48
36
48
36
48
36
4
836
5736
5736
59
36
55
36
55
36
553
6
5536
553
6
55
36
543
6
5536
47
36
4736
52
36
53
36
5
336
513
6
5136
50
25 185
57 50
50 16
16 22
22 58
58 59 57
44
41 41 40
40 50 28
29 35
22 28 4
37
42 19
47 13 13 13
13 9 58 13
16 14 57 4 4 31 48 53
Lo
ng
i tu
de
1 18
11
8118
11
8118
118
11
8118
11
81
18
118
118
11
81
18
11
8
11
81
18
11
81
18
11
8
11
81
18
11
81
18
1 1
8
11
8118
11
81
18
118
118
118
11
8118
11
8
11
81
18
11
81
18
119
11
91
19
1 19
11
9119
50
50 50
50 50 50
49
49 49
49 49
49 49
48
48
48
48
48
48
48 47
47 47
48
46 50
57 54 54 53
52 52 52 52 52 52 52
47 47 9 9 9 7 7 8
51 40
26
18 9 9
59
59 50 50 13
13 1
58 49
38 38 30
30
16
47
33
20
29 51 410
57
214
49 49 49
49 52
94
929
12 19 20
20
47 54 20
Fe-p
c t
.s 5 3 1 3 5 7 7 1 3 2 3 3 3 7 2 3 5 3 3 5 2 5 3 2 5 2 3
20 2 1 5 1 3 5 2 5
.00
.00
.00
.00
.00
.00
.00
.00
.70
.00
.50
.20
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.20
.20
.00
.00
.10
.00
.50
.00
.00
.00
.15
.00
.50
Mg
-pc t.
s
2.0
01
.00
.30
1.5
01
.00
1.5
01
.00
.50
5.0
01.0
0
5.0
01
0.0
03
.00
1.5
01
.00
1.5
02.0
01
.00
1.0
01
.50
1.0
0.7
01
.00
1 .0
02
.00
5.0
0.7
05
.00
.50
1.0
0
3.0
0.5
05.0
0.5
0.2
0
7.0
02.0
01.0
0.3
01
.00
.70
.70
.05
1 .0
0.0
2
Ca
-pc t .
s 7.0
02
.00
1.0
0.7
02
0.0
0
5.0
0.1
0,.05
7,0
0.0
5
10
.00
10,0
05.0
02
.00
1 .5
0
1.0
05
.00
2.0
02
.00
5.0
0
2.0
0.7
0.5
02
.00
5.0
0
3.0
01
.50
3.0
01
.50
2.0
0
3.0
01
.50
7.0
0,5
01
.50
3.0
01
0.0
03.0
0.2
01
.50
1 .0
02
.00
.10
<.0
5<
.05
Ti-p
ct.
s
.500
.30
0.1
00
.30
0.2
00
.20
0.5
00
.300
.020
.500
.02
0.0
05
.070
.300
.30
0
.30
0.7
00
.300
.200
.500
.500
.300
.300
.300
.500
.30
0.2
00
.500
.15
0.3
00
.010
.500
.01
0.0
70
.070
.500
.02
0.2
00
.100
.300
.500
.200
.01
0.5
00
.010
Mn-p
pm
s
1 /O
OO
70
0300
20
03
00
1/5
00
20
0 70
1/0
00
30
0
15
0100
30
0300
10
0
1 5
01
/00
03
00
1 5
01
/00
0
20
05
00
50
0500
1/0
00
1/0
00
300
70
03
00
500
5/0
00
1/0
00
1 5
050
30
0
1 /O
OO 50
20
0200
50
0
50
05
00
10
05
00
< 1
0
Ag-p
pm
s
N N N N N .5 N N N N N N .5 .5 .5 N N1
.0<
.5 N
< .
5N .5 N N N N N N N
300.0 N
<.
5.5
2.0
2.0 N .5
< .5 N N N N N N
A s-p
pm
s
N N N N N N N N N N N N
200 N N N N N N N N N N N N N N N N N
1/0
00 N N
.
200 N N N N N N N N N N N
B-p
pm
s
20
50
10
50
20
20
10
01
5<
1 0
30 N N
20
50
20
10
20
100
15
01
0
100
50
20
50
20
<1
0
-
Sam
ple
Ta
ble
5.
B i-p
pm
s
--D
ata
fo
r ro
ck
sa
mp
les*
Kin
gs
Riv
er*
R
an
ch
eria
* A
gnew
* a
nd
O
at
Mo
un
tain
R
oa
dle
ss
Are
as*
Ca
lifo
rnia
--co
ntin
ue
d
Cd-p
pm
C
o-p
pm
C
r-ppm
C
u-p
ptn
L
a-p
pm
M
o-p
pm
N
b-p
pm
N
i-p
pm
ecee
ecec
Pb
-pp
m
Sb-p
pm
S
c-p
pm
S
n-p
pm
s
s s
s
81N
K102C
81
NK
1C
KA
81N
K106A
81
NK
10
7B
81
NK
10
8B
81
NK
10
8C
81
NK
10
9B
81
NK
10
9C
81N
K1 1
1A
81N
K111E
81
NK
1U
A81N
K1 U
B8
1N
K1
15
A81N
K1 1
6A
81
NK
1 1
7A
81
NK
11
8B
81N
K118C
81N
K1 1
9A
81
NK
11
9A
81N
K121 A
81
NK
12
3A
81
NK
12
AB
81
NK
12
5A
81
NK
12
8A
81 N
K130A
81
NK
13
4A
81
NK
13
6A
81N
K138A
81
NK
1A
2A
81N
KU
3A
81N
KU
4A
81
NK
U4
C8
1 N
K144E
81 N
K1
44
I81N
KU
5A
81
NK
14
7A
81 N
K149A
81N
K157B
81N
K158A
81
RM
00
2A
81
RM
00
3D
81 R
M003F
81
RM
00
9A
81
RM
01
0A
81 R
M0
12
B
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
50 N N N N N N N N N N N N N N
N N N N N N N N N N N N<
20 N N N N N N N N N N N N N N N N N
>500 N N
20 N N N
<2
0 N N N N N N N
20 10 N
15
20
50
30
10 7
10 N N 7
10 7 10
20
10
10
15
15
-
Tab
le
5. D
ata
fo
r ro
ck
sam
ple
s,
Kin
gs
Riv
er,
R
an
ch
eri
a,
Ag
new
* an
d
Oat
Mo
un
tain
R
oad
less
Are
as*
Ca
lifo
rnia
co
nti
nu
ed
Roc
k na
mes
Sa
mp
le
81N
K102C
81N
K104A
81N
K106A
81
NK
10
7B
81 N
K1
08
B
81N
K108C
81
NK
10
98
81N
K109C
81
NK
1 1
1 A
81
NK
1 1
1E
81N
K1 H
A8
1N
K1
UB
81
NK
1 1
5A
81
NK
11
6A
81N
K117A
81N
K1188
81 N
K1
18
C8
1N
K1
19
A81N
K119A
81 N
K1
21 A
N)
06
81N
K123A
81
NK
12
4B
81
NK
1 2
5A
81
NK
12
8A
81N
K130A
81N
K134A
81
NK
1 3
6A
81N
K138A
81 N
KU
2A
81N
KU
3A
81 N
K144A
81N
K144C
81 N
K 1
44
E8
1N
K1
4U
81N
K145A
81
NK
14
7A
81 N
K149A
81
NK
15
7B
81N
K1 5
8A
81R
M002A
81 R
H003D
81
RM
00
3F
81
RM
009A
81
RM
01
0A
81R
M012B
Sr-
pp
ms
1,0
00
30
0200
150
2,0
00
700
200 N
300 N
300
10
0<
10
01
00
10
0
<100
700
500
200
1,0
00
300
200
200
200
500
1,0
00
50
01
,50
03
00
300
10
0200
200
10
0500
1,0
00
500
200
30
0500
200
200 N N N
V-p
pm
s 200
70
20
70
50
50
150 20
20
50
10
10
30
07
070
100
200
200
150
15
0
300 30
50
200
200
200 50
1 50
20
10
0
<10 50
10
3,0
00 10
200 15
200 20
30
1 0
050
<1 0 70
< 1
0
W-p
pm
s
N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N
Y-p
pm
s 50
30
20
30
30
30
50
20 N
30 N N
20
50
30
30
30
30
30
50
50
50
70
50
70
20
10
20
10
20 N
70 N
30
70
20 N
20
<1
01
0
70
10 N
30 N
Z n
-pp
ms
N N N N<
20
0
<2
00 N N N
<2
00 N N
30
0 N N
<2
00 N
50
0<
20
0 N
20
0 N N<
20
0 N N N N N N
>1
0,0
00 N N
500
<2
00
500 N
20
0 N N N N<
20
0<
20
0 N
Zr-
pp
ms
700
15
05
0150
10
0
100
100
200
,15
100
15
<1
050
150
100
100
100
15
0100
20
0
200
20
0500
200
300
15
05
0300
100
50 N
>1
,00
0 15
50
100
150
<1 0
15
07
0100
300
10
0 N1
00 N
Th-p
pm
s
N N N N N N N N N N N N N N N N N N N N N N N N N N N * N N N N N
<1
00 N N N N N N N N N N N N
Au
-P-
aa
--
- --
--
--
--
" "
N N N --
N --
--
--
--
^ ̂ --
--
--
- *
--
- N N
--
N N -- -
-
Au-T-ppm
aa 026
004
002
380
018
003
Horn
ble
nde-
bio
tite
met
adio
rite
Q
uart
z-bi
otit
e-ho
rnbl
ende
-cor
undu
m s
chis
t P
orp
hyri
tic
bio
tite
-qu
artz
mon
zoni
te
Qua
rtz-
biot
ite-
horn
blen
de-c
orun
dum
sc
his
t '
Sca
poli
te-c
linopyro
xen
e sc
his
t an
d sk
arn
Pla
gio
clas
e-cl
inopyro
xen
e sc
his
tW
hite
m
ica-
chlo
rite
-an
dal
usi
te sc
his
tQ
uart
z-w
hite
m
ica-
bio
tite
sc
his
tM
arbl
eBi
otit
e-wh
ite
mica
-and
alus
ite-
quar
tz schist
Marb
le
Marb
leGr
aphi
te-e
pido
te-q
uart
z sc
hist
Quartz-biotite m
ylon
ite
Quar
tz-b
ioti
te m
ylon
ite
Quar
tz-b
ioti
te-h
ornb
lend
e sc
hist
Bi
otit
e-ho
rnbl
ende
metadiorite
Quartz-biotite schist
Quar
tz-b
ioti
te schist
Gale-silicate
mylo
nite
Meta
daci
te
Meta
rhyo
lite
tuff
Quar
tz-w
hite
mica schist
Quartz-biotite m
ylonite
Horn
blen
de-b
ioti
te granodiorite
Metadacite p
orphyry
Oliv
ine-
clin
opyr
oxen
e-bi
otit
e al
kali
basalt
Oliv
ine-
clin
opyr
oxen
e basalt
Biotite-quartz m
onzonite
Hornblende-biotite g
ranodiorite
Calc
ite-
oliv
ine-
phlo
gopi
te-s
ulfi
de skarn
Quartz-plagioclase-hornblende
schi
st
Oliv
ine
marble
Quar
tz-w
hite
mi
ca-g
raph
ite
schi
st
Porh
yrit
ic b
ioti
te-q
uart
z mo
nzon
ite
Oliv
ine-
clin
opyr
oxen
e-bi
otit
e al
kali
basalt
Marb
leGa
le-s
ilic
ate
phyl
loni
teMe
tarh
yoda
cite
porphyry
Biot
ite-
quar
tz d
iorite
Quartz-biotite-white mi
ca-s
illi
mani
te schist
Quar
tz-c
lino
zois
ite-
woll
asto
nite
schist
Quartz ve
inQu
artz
-bio
tite
-whi
te mica-andalusite
schist
Quartzits
-
Table 5.--Data for
rock samples/ Kings River/ Rancheria/ Agnew/ and Oat Mountain Roadless Areas/ California--continued
Sam
ple
81R
M013A
81R
M014A
81 R
M014B
81 R
M0
1 5
88
1R
M0
15
C
81 R
M016A
81 R
M0188
81 R
M0
18
C81
RM
021B
81 R
M0
21
C
81 R
M022A
81 R
M023A
81 R
M0238
81 R
M024B
81 R
M0
32
B
81 R
M034A
81 R
M034B
81 R
M035A
81 R
M040D
81 R
M040F
81R
M042A
81 R
M0
43
A81
RM
04
3B
81 R
M043C
81 R
M0
44
A
81 R
M0
47
B81
RM
047C
81 R
M0
48
A81
R
M048C
81 R
M0
68
A
81
RM
070D
81 R
M071 A
81
RM
07
3A
81 R
M0
75
A81
RM
07
9A
81R
M082A
81 R
M083A
81
RM
0858
81
RM
08
8A
81
RM
08
9A
81R
M091A
81
RM
091B
81 R
M092C
81
RM
09
5A
81R
M109B
La
titu
de
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
36
50
3
75
3
053
052
852
8
51
5952
8
52
851
18
51
18
51
350
42
50
42
50
254
2
5
50
5950
59
50
5250
55
50
55
51
251
31
51
3151
31
51
46
50
58
50
5850
58
50
534
8
9
46
43
46
94
7
52
-48
2448
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