W
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BULLETIN No. 27. SAN FRANCISCO, JANUARY, 1908.
THE
QUICKSLVER RESOURCES
OF CALIFORNIA.
(SECOND EDITION.)
ISSUED BY
THE CALIFORNIA STATE MINING BUREAU,
FERRY BUILDING, SAN FRANCISCO.
UNDER THE DIRECTION OF
LEWIS E. AUBURY, - - State Mineralogist.
SACRAMENTO.
W. W. SHANNON. - - - SUPERINTENDENT OF STATE PRINTING.
1908.
LIBRARY
UNIVERSITY OF CAUFORNIA
DAVIS
LETTER OF TRANSMITTAL.
To Hon. George C. Pardee, Governor of the State of Cali-
fornia^ and the Honorable the Board of Trustees of the
State Mining Burea^i :
Gentlemen: I have the honor to transmit the results of
the recent work of the State Mining Bureau in investigating
the Quicksilver Resources of California, and which are embodied
in Bulletin Xo. 27.
This is the third of a series of bulletins, issued under my
direction, on special features of the mining industry in Cali-
fornia, and in which will be found a description of the geology
of all the deposits of economic importance in the State, together
with maps and such data as it was possible to obtain. The
geological field work for this bulletin was performed by Mr.
William Forstner, Assistant in the Field, of the State Mining
Bureau. No description of any mine or prospect, nor of the
geology of any part of the territory, has been given except after
personal investigation by Mr. Forstner.
In treating of the geology and the genesis of ore deposition,
subjects of which differences of opinion exist, endeavors have
been made to present as briefly and clearly as possible the
different opinions, and some suggestions have been added
which have resulted from Mr. Forstner's personal observation.
In the chapter on the metallurgy of quicksilver, it has been
the aim more to give the general principles upon which the
different methods of treatment are based than to make a mere
detailed description of the different installations.
The courtesy generally shown by the owners and superin-
91575
4 LETTER OF TRANSMITTAL.
tendents of the difierent mines deser\'es special mention. With
only one exception, at every mine all information which would
be of value from a technical and often from a commercial
standpoint was given with the greatest courtes}-. This is the
more appreciated, as quicksilver is a product for which the
demand is to a certain extent limited, and it is only natural
that operators do not feel inclined to disclose all the facts per-
taining to their business.
I wish to extend m}- thanks to Mr. J. W. C. Maxwell, who
assisted in the revision of the technical and descriptive portions
of the bulletin; to Mr. Charles G. Yale, for assistance in the
editorial part of the work; and to Mr. E. B. Preston, for the
classification of specimens of ores and formations submitted.
To the many owners and superintendents of quicksilver
mines and prospects who lent their assistance, I wish also to
extend my thanks, for without their valuable aid it would have
been impossible to present the full results of the work as herein
set forth.
Ver>- respect full}',
LEWIS E. AUBURY,
State Mineralogist.
San Francisco, June 30, 1903.
CONTENTS.
Page.
CONDITION OF THE INDUSTRY .-..(»
GEOLOGY OF THE QUICKSILVER BELT IN CALIFORNIA 12
ORE DEPOSITS ------- 23
GENESIS OF QUICKSILVER ORE DEPOSITS - - 26
COST OF MINING AND REDUCTION - - - - 34
DISTRICTS NORTH OF SAN FRANCISCO:
Mayacmas District ------ 35
Clear Lake District ----- 39
Sulphur Creek District - - - - - 40
Knoxville District . - - - . 42
QUICKSILVER MINES IN THE COUNTIES OF CALIFORNIA:
Colusa County ------ 43
Lake County ------- 46
Napa County - - - - - - 72
Solano County - - - - - - 93
Sonoma County ------ 97
Yolo County - - - - - - - 117
Fresno County ------ no
Kings County - - - - - - - 122
Monterey County ----- 123
San Benito County ------ 125
San Luis Obispo County ----- 144
Santa Clara County ------ Kjg
Stanislaus County ----- igg
El Dorado County ------ 190
Trinity County - - - - - - 190
Other Counties ------ 195
METALLURGY ------- 197
ELEVATIONS - - - - - ' . - - 254
LIST OF ILLUSTRATIONS.
SKETCHES.
Figure. Pagk
1. Section of northwest slope of Pine
Mountain, Sonoma County 38
2. Sulphur Creek District, section
over Abbott ridge 40
3. Abbott mine, Lake County, section
over the serpentine 46
4. Abbott mine, Lake County, plan
near intersection of Reardon
tunnel and first level 47
5. Plan and elevation of Abbott
mine . _ faces 48
6. Big Injun group, Lake County 50
7, 8. Sections of Chicago mine 52
9. Cross-section of Great Western
mine 54
10. Section over Great Western mine . 55
11. Cross-section of Helen mine. Lake
County -- -.- -- 56
12. Plan of Lucitta mine 59
13. Section of Bullion mine (Standard
Quicksilver Co.) _. 61
14. Sulphur Bank mine faces 62
15. Sulphur Bank mine, elevation of
Upper Wagon Spring Cut at X, . 63
16. Sulphur Bank mine, section and
plan of Herman shaft 67
17. Sulphur Bank mine, ore formation
in Herman shaft tj8
18. Sulphur Bank mine, section of
Diamond shaft 69
19. Front vievr of the Wall Street mine,
from opposite hill.side 71
20. ^Etna Consolidated mines 72
21. .Etna Consolidated mines, eleva-
tion at mouth of Tunnel No. 2.. 74
22. .Etna Consolidated mines, basalt
dike, Silver Bow claim 74
23. iEtna Consolidated mines, section
of Washington shaft... 75
24. Boston mine, section over the min-
eralizedzone 78
25. Corona mine .faces 78
26. Corona mine, section showing
formation. Dip S. W. 30' 79
27. Areal geology, Manhattan mine,
faces 80
28. Manhattan mine, section over the
works at (f,) 87
29. Napa Consolidated mines, general
trend of veins 89
Figure. Page.
30. Napa Consolidated mines, crossing
of two veins . . . 91
31. St. John mine, section east and
west over main tunnel shaft 93
32. St. John mine, plan showing main
tunnel west of shaft ... 96
33. St. John mine, plan of works in
main tunnel shaft 96
34. Cloverdale mine, section over
works. Mount Vernon claim 99
35. Cloverdale mine 100
36. Cloverdale mine, plan and section
of Murphy tunnel . 101
37. Plan of Crown Point and Pacific
mines _ . 103
38. Section of Culver-Baer mine... ... 104
39. Eureka mine 107
40. Great Eastern mine, general plan,
faces 108
41. Section over the Great Eastern
mine 108
42. Great Eastern mine, plan showing
the form of the ore bodies 111
43. Socrates mine 116
44. Plan of Mexican mine, Fresno
County 120
45. Workings, Bradford mine 132
Cerro Bonito mine . 134
46. Elevations open cut (6), Cerro Bo-
nito mine 136
47. New Idria mine 140
48. Plan of New Idria mine 141
49 Section west end of fifth level. New
Idria mine 142
50. Open cut, San Carlos mine 144
51. Section at Gray buck shaft, Stayton
mine 148
52. Plan of .\lice and Modoc mine 1-55
53. Libertad tunnel No. 2 160
54. Lower Ocean View tunnel. Pine
Mountain Mine 164
55. Section near R R. B. shafl, New
Almaden property. 170
56. Section on road above Randol shaft,
New Almaden mine ... 170
57. Ore bodies in the New jVlmaden
mine .faces 174
58. Section of Mine Hill, New Alma-
den 178
LIST OF ILLUSTRATIONS.
Figure Page.
59. Section over Santa Rita West,
Giant Powder stopes, New Al-
maden 178
60. Plan of the clay walls, New Alma-
den mine (from Atlas, Mono-
graph XIII, V. S. G. S.) ./aces 184
61. Section in Enriquita mine, New
Almaden -._ 185
62. Sketch of works in the Santa
Teresa mine _ 186
Trinity County quicksilver districts 191
6.1a . U nderg^ound workin gs of In tegral
„- mine 194
63y Plan and elevations of concentrat-
@ing system, Manzanita mine 199
Pipe retort furnace, by G. V.
Northey 201
65. Condensing plant, soot retort, Bos-
ton mine 202
66. Johnson & McKay furnace 203
67. Continuous retort, quicksilver fur-
nace 204
68. Exeli furnace - _ 209
69. Knox & Osborne coarse-ore fur-
nace.. ._ 211
70. Coarse-ore furnace, John Neat's
patent 212
71. New Idria coarse-ore furnace 213
"i*. Longitudinal section, modified
Livermore quicksilver furnace.. 215
73. Knox & Osborne fine-ore furnace. 216
GURE. Page.
Plan of Hiittner & Scott 8-tile fur-
nace 220
Tilings of Furnace No. 3, New Al-
maden 221
Tiling of Cermak-Spirek furnace.. 221
Ore-drier, utilizing exhaust steam . 225
Ore-drier, special furnace at Abbott
mine 227
New Idria fine-ore furnace — meth-
od of conveying fumes from top. 228
Top of the modified Scott furnace. 229
Top of Hiittner & Scott furnace ... 230
Discharge Scott furnace. 2.32
New Idria fine-ore furnace, details
of drawing door 234
General plan of reduction works
(from Mineral Industry, Vol. 7),
between 234-235
Sketch showing method of hand-
ling ore at Abbott mine. Lake
County 236
. Plan of works 237
Details of condensers 237
, Installation to save flour mercury.
New Almaden 240
Scott's brick condenser plant 248
Knox ironclad condenser _. 249
Watertank condenser.. 250
The Baker flue 251
Wooden condenser box, Corona
mine.. 252
Soot-cleaning machine 253
PHOTOGRAPHS.
No. Page.
1. Chicago plant 51
2. Great Western quicksilver mine .. 53
3 Western cut. Sulphur Banks 62
4. .^itna quicksilver mine 73
5. Boston quicksilver mine 77
6. Manhattan quicksilver mine 81
7. Oathill quicksilver mine . 90
8. St. John mine and furnace 94
9. St. John quicksilver 'mine 94
10. Great Eastern quicksilver mine. . 109
11. Thin section of sandstone and ser-
pentine from New Idria district. 127
12. View of New Idria 1:59
1:'.. Los Picachos mine (Ramirez Con-
solidated) 146
14. La Libertad mine 159
15. General view of New Almaden
mine 175
ir>. Dump of New Almaden mine
works 179
17. Durapof Grey shaft and Mine Hill,
New Almaden 180
18. Victoria shafl, New .\lmaden 181
P.4.GE.
Santa Isabel shaft. New .\lraaden . 182
Randol shaft. New Almaden. 183
Entrance Castella development
tunnel. Integral mine 193
Pipe-retort furnace. Manzanita ^
mine, Colusa County ^200
Corona furnace 207"
Tufa furnace in course of construc-
tion. Corona quicksilver mine. . . 207
New Idria quicksilver mine, show-
ing new SO-ton coarse-ore furnace 214
Cloverdale reduction plant 217
Great Western Quicksilver Mining
Company's reduction plant 217
Manhattan furnace 218
Altoona quicksilver mine 219
Furnace plant, Integral mine,
Trinity County 222
Karl furnace, San Luis Obispo 224
Great Eastern mine, drying ore in
sun "226
Reduction works at New Almaden,
Hacienda 231
8
LIST OF ILLUSTRATIONS.
No. Page.
34. General view of reduction works
at New Almaden, Hacienda 233
35. Furnace Nos. 1 and 2, New Alma-
den, Hacienda 233
36. Reduction plant in cour.se of con-
struction, Silver Creek Quick-
silver Mining Company, Santa
Clara County 235
37. Reduction plant, Silver Creek
Quicksilver Mining Company,
Santa Clara County 238
38. Great Eastern furnaces 239
39. New Idria mine, showing Scott fur-
nace _ _. 241
40. Boston quicksilver mine, quicksil-
ver furnace 242
41. Flues connecting furnace with con-
denser plant. New Almaden,
Hacienda - 242
No. Page.
42 Oceanic quicksilver reduction
plant, San l,uis Obispo County. 243
43. Interior view of reduction works.
New Almaden. Hacienda 245
44. New Idria, showing round wooden
flue and wooden tanks used for
condensers 245
45. Retorting soot, Great Eastern 246
Ferry building, San Francisco, one
half of which is occupied by the
State Mining Bureau 261
Mineral Museum, California State
Mining Bureau __. 263
Library and free reading-room, Cali-
fornia State Mining Bureau 265
Laboratory, California State Mining
Bureau 267
Draughting department, California
State Mining Bureau 269
MAPS— (Folders).
P.\GE.
Geological map of portions of Napa, Sonoma, and Lake County quicksilver districts,
California _ ._ _ 35
Geological map of Napa, Sonoma, Lake, and Yolo County quicksilver deposits 39
Map of Sulphur Creek District _ _ . 40
Map of Little Panoche Mining District _ 118
Geol ogical map of quicksilver districts in southern portion of San Benito County . . _ 126
Geologfical map of Stay ton Mining District. ._. 129
Geological map of quicksilver districts northwestern portion of San Luis Obispo
County ... 149
Map of the New Almaden Mining District 168
THE QUICKSILVER RESOURCES
OF CALIFORNIA.
By WM. FORSTNER, E.M.
Assistant in the Field.
CONDITION OF THE INDUSTRY.
Quicksilver has been produced in California since 1850. The
table published in the report of the Eleventh Census (1890),
page 188, compiled bj' Mr. J. B. Randol, giving the annual pro-
duction of the various mines from 1850 to 1889, indicates that
in the decade 1850 to i860 the Xew Almaden mine was about
the onl}- producer. In the latter part of the 6o's, the New
Idria, Redington, and i^tna mines began to produce. The
greatest number of mines were in operation between the years
1874 and 1880. This activity was due to the high price of
quicksilver obtained in 1874, when the prices per flask in San
Francisco were: highest, $126.22; lowest, $84. 15. In 1875 the
price dropped to $49.75, and until 1883 the average price was
about $30. The lowest price was in this period for awhile,
$25. For years the price remained rather low, but in the last
few 3-ears it has maintained a figure which gives the operators
a fair remuneration. These low prices in 1879 and 1880 caused
the closing of a number of quicksilver mines, and for some
years quicksilver mining was carried on only at a few of the
large mines. In later years the price of quicksilver has risen,
although by no means to that of the prosperous times, and
graduall}- the old mines, closed for years, are being reopened.
In the meanwhile the older mines, which have been steady
producers for many years, appear to have worked out their
bodies of high-grade ores, and are all now working what in
(9)
10
QUICKSILVER RESOURCES OF CALIFORNIA.
years past would have been classed as poor ores. In the well-
managed properties, however, where they have availed them-
selves of the more economical methods of mining and especially
of reducing the ores, a fair interest on the investment is earned
from these low-grade ores. The yearly production of quick-
silver in California has been as follows:
TABLE GIVING YEARLY PRODUCTION OF CALIFORNIA MINES AND
AVERAGE PRICE PER FLASK IN SAN FRANCISCO.
Flasks
Year. Produced.
1850 [a) 7,723
1851 27,779
1852 20,000
1853 22.284
1854 3O1OO4
1855 33,000
1856 30,000
1857 W 28,204
1858 31,000
1859 13,000
i860 10,000
1861 35,000
1862 42,000
1863 40,531
1864 47,489
1865 53.000
1866 46,550
1867 47,000
1868 47,728
1869 33,8x1
1870 30,077
1S71 31,686
1872 31,621
1873 27,642
1874 27,756
1875 50,250
1876 75,074
1877 79,396
1878 63,880
Average
Price per
Flask.
V
$99 45
I
66 93
I
58 33
1
55 45
I
55 45
I
53 55
I
51 65
I
48 73
I
47 83
I
63 13
I
53 55
I
42 05
I
36 35
I
42 08
1
45 90
I
45 90
I
53 13
I
45 90
I
45 90
I
45 90
Ic
57 38
II
63 10
K
65 93
IC
80 33
I(
105 18
I(
84 15
K
44 00
K
37 30
It
32 90
Flasks
Produced.
1879 73,684
1880 59,926
il 60,851
£882 52,732
1883 46,725
t884 31,913
[885 . 32,073
[886 29.981
1887 (<r) 33,760
1888 33,250
1889 26 464
22 926
[891 22,904
1892 . 27,993
i893(d?) 30,164
30,416
C895 36,104
1896 30,765
1897 26,648
[898 3^,092
1899 29,454
[900 26,317
[901 26,720
1902 29,552
1903 32,094
[904 28,876
[905......... 24,655
[906 19,516
Average
Price per
Flask.
$29
85
31
00
29
83
28
23
28
75
30 50
30
75
35
50
42
37>^
42
50
45
00
52
50
45
25
40 71
36
75
30
70
37 04
34
96
37
28
38
23
47
70
44 94
48 46
43
20
42
25
37
62
35
94
36
50
(<7) Report nth Census. 1850 to 1865, great bulk of quicksilver produced by the
New .\ltQaden mine.
16) The New Idria mine begins to produce 1857.
(c) From 1887 to 1893, Dr. Day's Report, U. S Geol. Survey.
(rf) 1893 to date. Annual Statistical Bulletins, California State Mining Bureau.
Quicksilver furnaces are great consumers of wood, and even
those mines which are located in well-timbered regions find
the cost of their fuel steadil}' increasing. Only in exceptional
cases can mines get their cordwood delivered for $3.50 per
cord; generally the price is higher, in some cases double that
figure. Hence most of the quicksilver mine managers are
eagerly looking for a substitute for cordwood as fuel in
CONDITION OF THE INDUSTRY. 11
their furnaces. Up to the present time, however, this has not
been found.
As mentioned above, many of the quicksilver mines have
been idle for some years, and of these it is very difficult to
obtain either reliable historical data, or details of the old work-
ings or of the output of mercury. Even in the mines which
have been in continuous operation, large portions have been
worked out and abandoned, and it is nearly impossible to get
the desired information regarding these portions of the mines.
In regard to several of the principal mines of the State, belong-
ing to the Napa Consolidated and affiliated companies, these
data were to a great extent destroyed in 1898, in which year
the main office in Oathill was burned and most of the mine
maps, etc., were destroyed.
Whatever information of this character it was possible to
collect, is inserted in the descriptions of the respective mines.
It may here be stated that in accordance with the general
scheme of this Bulletin, its contents are confined strictly to
the occurrence of quicksilver in the State of California, for
which reason all reference to mines and works in other locali-
ties is omitted.
GEOLOGY OF THE QUICKSILVER BELT
IN CALIFORNL\.
The quicksilver deposits in California are, with a few scat-
tered exceptions, located in the Coast Ranges. There is a ver>'
marked difierence of opinion among the geologists who have
made a special study of this territory, regarding two points:
First, as to the age of the metamorphic series which form such a
prominent part of the rocks in this territory; and secondly, as
to the origin of the serpentine. Thej^ all agree that violent
geological disturbances took place in this region at some period
within the Mesozoic age. These disturbances were sudden and
sharp, resulting in the crushing and fracturing of the strata
rather than their uplifting and folding [Whitnej', Auriferous
Gravels, page 15], and gave this series a characteristic struc-
ture, which serves to its identification. The epoch of this
revolution is placed by Becker at the end of the Xeocomian or
Lower Cretaceous, while Fairbanks and others place it at the
close of the Jurassic epoch, hence as pre-Cretaceous.
The rock series metamorphosed b}- the revolution is called
by Becker the Xeocomian, and also occasionally the Metamorphic
series; by Fairbanks, the Pre-Cretaceous or the Metamorphic
series; by Lawson, the Franciscan series. These rocks rest
upon a basement complex consisting of crystalline limestones
and schists and granites. The granite does not appear at the
surface north of the bay of San Francisco, except on the coast
twenty miles north of San Francisco at Point Tomales; but
south of San Francisco there are two ages of granitic uplifts.
The granite is intrusive in the older strata. The crystalline
rocks of the basement complex are only found at a few points;
the granitic uplifts brought them within a zone of such
efiective erosion that the granite was almost entirely denuded
before the next period of subsidence and deposition of the
Franciscan series set in. The age of the crystalline rocks of
the basement complex is either Carboniferous or older. [See
Bulletin Geological Society of America, vol. VI, pages 79-81.]
(12)
GEOLOGY OF THE QUICKSILVER BELT. 13
Intimately mingled with the rocks of the Franciscan series
are large masses of serpentine. Becker holds that these are
prominently altered sedimentaries [see Mineral Resources, 1892,
U. S. G. S., page 144]; while Fairbanks holds these serpen-
tines to be exclusivel}^ derived from eruptives. A. C. L,awson
is of the same opinion, so far as the serpentines in the penin-
sula of San Francisco are concerned. Apparenth' the latter
views as to the origin of the serpentine in the Coast Ranges
are entertained by all the geologists on the Pacific Coast. The
serpentine bodies occur in different forms and the rocks them-
selves vary very sensibly in structure in different regions and
in the various bodies of serpentine. In places the serpentine
occurs in bodies indicating an original dike formation and
showing intrusive phenomena; while in other places large
areas of serpentine occur which can hardly be conceived to be
derived from eruptive masses, and wherein are found small
areas of sandstone and occasionally shales, indurated but
slightly altered, in places even unaltered. In other places the
serpentine overlies or underlies the sandstone and shales with-
out any intrusive phenomena. During the investigation in
the preparation of this Bulletin, in the neighborhood of New
Idria [see general description of the New Idria district, page
125] and near Cambria, San Luis Obispo County, sandstone and
serpentine were found intimately associated. Samples of these
occurrences are in the museum of the State Mining Bureau,
and a slide of the first mentioned has been prepared and
photographed.
Both views of the origin of the serpentine can be sustained
by microscopical examination. [See, for instance, Becker,
Mon. XIII, U. S. G. S., page 275, and following; A. C. Law-
son, 15th Ann. Report, U. S. G. S., pages 417, 433, and 447;
etc.] It may be argued that both views are correct and that
probably the serpentine is an alteration product of both sedi-
mentaries and eruptives in this region, as is the case elsewhere.
This view is that of the majority of geologists. In 1888 this
question was submitted to the American Committee of the
International Congress of Geologists [.see American Geologist,
vol. II, page 180], in the following form:
Question N — Is serpentine (i) sometimes, (2) always an
alteration product, (3) of eruptives, (4) of sedimentaries, (5) of
either?
14 QUICKSILVER RESOURCES OF CALIFORNIA.
Thirteen answers were received, which can be summarized
as follows: Twelve declared serpentine to be an alteration
product, and one characterized it as an original aqueous rock.
Three of the first twelve took the view that it is exclusively an
alteration product of igneous rocks; one exclusively of sedi-
mentar\' rocks; two, generalh' of igneous rocks, but could also
be such of sedimentarN' rocks; and five that it is an alteration
product of both eruptive and sedimentary rocks, while one
leaves this part of the question unanswered.
Professor van Hise remarks, in his Principles of North
American Pre-Cambrian Geology [i6th Ann. Report, U. S.
G. S., Part I, page 68g] : "Actinolite, serpentine, and magnetite
"have been observed to replace quartz. In the case of the two
"former minerals their relation to the quartz suggests that the
"other constituents, with the exception of silica, were at hand
"or were furnished b}" the percolating water out of which the
"serpentine and actinolite formed; and that the quartz itself
"ma}' have furnished the necessary silica to produce these
"minerals." [On page 691:] "Among basic sedimentan,- rock
"serpentine very often develops."
E. S. Dana [Mineralogy, 1898, page 477] states: "Microscopic
"examination has established the fact that serpentine is largely
"produced by the alteration of chrysolite; in other cases it has
"resulted from the alteration of pyroxene or amphibolite."
[See also Williams, Lithology, page 254.]
A. C. Lawson, in describing the deformations of the earth-
crust which have influenced the geology of the San Francisco
peninsula [15th Ann. Report, U. S. G. S., page 466], mentions
"an invasion of the upper portion of the Franciscan series by
"peridotite magma, which solidified in the form of dikes or
"laccolitic lenses."
The granites of that part of the Coast Range which contains
the quicksilver belt appear only at the surface south of San
Francisco. Lawson has carefully studied granite in two
places: the Montara granite in the San Francisco peninsula
[above cited, page 411], which he describes as a coarse gray
hornblende, biotite granite, which originally was a hornblende
granite; and at Carmel Bay [Bulletin Geological Department,
University of California, vol. I], which he describes as a coarse
porphyritic granite. Similar granite rocks are found in the
Santa Lucia Peak, and in the San Jose range.
GEOLOGY OF THE QUICKSILVER BELT. 15
Fairbanks has studied extensively the granites in the Coast
Range south of San Francisco, and considers them as true
mica feldspar quartz granites, difiering from the granites in the
Sierra Nevada, which are usually hornblendic. [Bulletin Geo-
logical Society of America, vol. VI, page 79.]
H. W. Turner [Am. Geol., vol. XI, page 324] supposes these
granites to be of Carboniferous age. Fairbanks thinks this
may be true or they may be older.
Accepting the suggestion of Becker that the entire Coast
Range is underlaid by granite [Mon. XIII, page 140], a source
of ferro-magnesian silicates other than the suggested post-
Franciscan peridotite intrusions is present in this region. Law-
son [above cited, page 434] calls attention to the fact that the
entire period of accumulation of the Franciscan series was
a period of volcanic activity, and that the lower portions of
this series were traversed by igneous rocks, which arriving at
the surface, became constituents of the upper portion of the
series.
It appears most probable that all of these materials have
contributed to the formation of the bodies of serpentine found
in this region. As van Hise remarks [above cited, page 691],
" Material for the serpentines maybe furnished in part or in
"whole by minerals present, or the material of the serpentine
''may come from an extraneous source. Also, widespread for-
"mations may be extensively serpentinized, so as to give for
"considerable areas almost solid masses of serpentine."
The pressures which caused these deformations produced
great heat from dynamic action, which was increased by that
obtained from the intruding magmas; consequently both
pressure and temperature were raised during the deformations,
causing an increased chemical activity of the circulating
waters, and it appears only reasonable to assume that all
available sources for the formation of serpentine masses were
called upon.
The later intrusions, forming the dike and laccolitic lenses,
can be generally defined by the phenomena of contact meta-
morphism accompanying them; while the large, widely-dis-
tributed ma.sses of serpentine were probably formed by
magnesian solutions acting upon the rock material. [Mon.
XIII, pages 1 21-127, ^^^d 273-278.] The ferro-magnesian
silicates are probably derived from the basal granite, and per-
16
QUICKSILVER RESOURCES OF CALIFORNIA.
haps from intrusives, which would explain the entire lack of
contact metamorphism phenomena at the contact of many ser-
pentine bodies with the other rocks. This lack of contact
metamorphism and intricate mixture of serpentine with the
sandstones and shales of the Franciscan series, and even
probabl3' with the schists of the basal complex, can be exten-
sively studied in the New Idria district.
As already stated above, there is a great diversit}' of opinion
as to the historical geology of the Coast Ranges. The accom-
panying table of comparison will set this forth. [See American
Geologist, vol. XL]
AGE. Period.
Gabb —
CALI-
FORNIA.
WHITE AND ' °STAVTOn''°
C^Li'f'oRnTa NORTHCrLIPOR- I'^-^^-'
CALIFORNIA. ^.j^ ^^^ OREGON.
Cenozoic.
Miocene.
Eocene.
Chico Tejon.
Probable place of
the Wallalla.
Tejon.
Monterey
Series.
Light color'd
Sandstone?
Upper
Cretaceous.
Tejon.
Martinez.
Chico.
V,
.a
'C
V
m
o
■I
(J
5
7.
Hiatus
and
nconformity. ^ r.
: '*-
'Chico. j «
o
N
O
Ol
Lower
Cretaceous.
Shasta.
Hiatus of White.
Unconformity of
Becker.
. fHorsetown.
i i Knoxville,
j: including
'"^ L Mariposa.
Horsetown.
t Knoxville.
a
a
u
•s
a
1
Jurassic.
Mariposa.
Mariposa.
This difference of classification is closely related to the above-
mentioned difference of opinion as to the period wherein took
place the disturbances which caused the metamorphism of the
rocks deposited after the first-recorded intrusions. J. S. Diller
says [Bulletin Geological Society of America, vol. IV, page
2o6] : " The Cretaceous of north California, embracing the
" Chico, Horsetown, and Knoxville beds, are essentiall}^ con-
" formable, hence the upheaval must have been pre-Neocomian."
Becker places the upheaval after the Horsetown series, refer-
ring to it as post-Xeocomian. Fairbanks indorses Diller's
opinion, and names the Metamorphic series the Pre- Cretaceous
series.
GEOLOGY OF THE QUICKSILVER BELT. l7
Whatever may be its age, this Franciscan series presents some
distinguishing characteristics which facilitate its identification
from the underlying crystalline limestones and schists of the
basement complex, and from the overlying younger rocks.
This series consists mainly of sandstones, associated with some
shales, cherts, and occasionally limestone. The sandstones are
rather massive; the bedding planes have often intercalated
beds of shale. They are very generally altered through a
process of recrystallization and cementation by silicification.
All grades of alteration can be observed, from nearly unaltered
arkose sandstone to compact jasper, or jaspilite (a term sug-
gested by Wadsworth). [See i6th Ann. Rep. U. S. G. S.,
Pt. I, page 702.] Interbedded with the sandstones are lime-
stones, cherts, and volcanic rocks.
The chert beds form a very characteristic member of this
series, but are much more prominent in the districts north of
San Francisco than in those south. They have been exten-
sively discussed by Becker, Fairbanks, and Lawson. The
first named refers to them as schistose rocks which have been
subjected to a process of silicification, and classes them as
phthanites. Blake supposed that they had resulted from the
metamorphism of shales and sandstones by igneous action.
J. J. Newberry [General Geology of California, page 66] says:
" Whether the material of which they are composed is thrown
" up from below, or, as is more probable, it is a metamorphosed
" form of the associated rocks, it is evident that the material
" has been subject to great heat." Fairbanks [Bulletin Geo-
logical Society of America, vol. VI, page 71] classifies this
formation as jasper. Lawson [above cited, page 420] as
Radiolarian cherts, which designation appears the most correct.
The following is a concise statement of Mr. Lawson's study
of this formation :
"These beds consist of alternate thin sheets of chert, rang-
"ing generally from one to four inches in thickness, only
" exceptionally having a much greater thickness, with part-
"ings of shale from one eighth to one half inch thick. Some-
" times the regularity is much less marked, and in the less
''ferruginous varieties of the chert beds the sheets of chert
"assume occasionally a lenticular form. The difference of
"opinion as to the proper classification of this formation is
2— QR
18 QUICKSILVER RESOURCES OF CALIFORNIA.
"due to the fact that petrographically these cherts are not
"uniform. In many cases they are true jaspers; in others
"the silica is chiefly amorphous, and the rocks have a flinty
"character; in still other cases the proportion of iron oxide
"is so great that the cherty character disappears and the
"beds become locally very soft. All gradations between
"cherts composed almost wholly of amorphous silica, to those
"which are a holocrystalline aggregate of quartz granules,
"are found. The amorphous silica differs, however, from opal,
"in that it has a much higher specific gravity and contains
"much less combined water. The cherts are, then, minutely
"granular aggregates of cr^^stalline silica, tending more toward
"the chalcedonic than to the quartz variety, with varying pro-
" portions of amorphous silica, mixed with ferric oxide and
"ferric hydrate, sometimes uniformly distributed, or again in
"patches or streaks. The mass is intersected bj' numerous
"small, often microscopical veins, the smaller filled with chal-
"cedonic, the larger with quartzose silica, and occurring in two
"sets of fissures crossing at high angle. Zoisiteis often found
"in the vein filling. These chert beds contain round or oval
"spaces, occupied by chalcedony, which are the residual casts
"of Radiolaria. The intervening shale consists of silica, iron,
"considerable magnesia, and a small amount of alumina with-
"out any clastic material. The association of chert beds with
"the sandstone precludes the possibility of their formation
"under deep-sea conditions, which would be indicated by the
"absence of fragmental material."
The most probable hypothesis of their formation is, as sug-
gested by lyawson, that the silica was derived from siliceous
springs and precipitated in the bed of the ocean in local accu-
mulations, in which Radiolarian remains were imbedded. The
alteration of the beds of chert with partings of shale may
perhaps be ascribed to an intermittent action of the springs.
These chert beds occur throughout the Coast Range in a spo-
radic manner, and are especially of interest, as in some mines
they form the ore-bearing zones. Associated with these rocks
of the Franciscan series are metamorphic schists which appear
to represent stages of alteration of rocks of very diverse origin,
and may be principally the result of contact metamorphism,
which, as H. W. Turner remarks, "is, however, yet to be fully
demonstrated." As already stated above, the rocks of this
GEOLOGY OF THE OUICKSIL\^R BELT. 19
series are further associated with many and various igneous
intrusives, entirely separate from the later Tertiary and post-
Tertiary igneous ejections.
There must have been a considerable difference in the geo-
logical history of the northern and southern part of the quick-
silver belt. South of San Francisco the Franciscan series were
elevated and eroded to such an extent that the Tejon is found
resting directly on the granite and a second elevation, and
post-Miocene erosion must have followed, as the Pliocene is
also found resting direct on the granite. North of the bay of
San Francisco, the erosion of the Franciscan series has been
much less, so that between the bay and Clear Lake the granite
does not appear at the surface and the younger formations all
rest on this series.
The metamorphism of the Franciscan series was eminently
a process of recrystallization of the clastic sediments into holo-
cr^'stalline feldspathic rocks, carrj'ing ferro-magnesian silicates,
and in the formation of vast quantities of serpentine. [See
Becker, above cited, page 57.] The serpentinization was pos-
terior to the former process, which included a silicification which
altered part of the shales to jaspery masses and formed in these
and in other rocks innumerable minute veins of quartz. \_Ibid.,
page 393-]
There are reasons to believe that the metamorphism of this
series took place at no great depth. The rocks were often
crushed into a confused mass of rubble by dynamic action [see
above, page 12], which is often recemented bj- metamorphic
process. The readjustment of the strata under pressure hence
took place largely through fracturing, rather than through
flowage and flexure of the rocks, consequently they can not
have been buried at great depths.
A much later silicification process took place attendant upon
or just prior to the ore deposition and of a distinct character
from that above mentioned, in many cases resulting in the
formation of a black opal rock. This opal replaces constitu-
ents of the rock masses, particularly but not exclusively serpen-
tine. The opal is often deep black, resembling some varieties
of obsidian, and is accompanied by small amounts of crystal-
line silica, quartz, and chalcedonite — the name suggested by
Dr. Becker [above cited, page 390] for a mixture of opal and
cr>'stalline silica ; sometimes it contains a small amount of
20 QUICKSILVER RESOURCES OF CALIFORNIA.
calcite. A perfect network of minute bands of quartz often
traverses the opal, resulting from infiltration into fissured opal.
This material is seldom, if ever, free from sulphides of iron,
occasionally of nickel, and at least traces of cinnabar are inva-
riably found close to it (hence its local name of "quicksilver
rock"), showing its close relation to metalliferous solutions.
While some of this opaline rock has certainl}- been deposited
in pre-existing openings, a large part is a substitution product.
The silica solutions seem to have permeated more or less frac-
tured rocks, principally serpentine, dissolving the bases and
depositing the opal.
This silicification process is closeh' related to the deposition
of cinnabar ores and to the later igneous phenomena. As
above stated, cinnabar is often found in the filling of minute
cracks in the opaline rock, accompanied bj' quartz and chal-
cedonite, but seldom if ever imbedded in the opal. Hence this
silicification process must have preceded the ore deposition;
but the effects of the two processes are so closeh' related that
the former must have been an earlier stage of the latter. The
fact that mercuric ores are hardly ever found in direct contact
with the opal is hard to explain, as it would suggest that the
siliceous solutions during that period of the process were
entirely barren of mercuric sulphide. The solutions during the
ore deposition were, however, also certainl}- siliceous, and
hence it is hard to understand wh}' the former should have
been entirelj' barren. Dr. Becker ofiers as explanation the
hypothesis that the cinnabar was separated from the solutions
in the fissures when the siliceous fluids permeated the rocks,
through a mechanical process more or less analogous to dialysis.
The difficulty is, however, that metallic salts are cr3'stalloid
bodies and pass readilj' through membranes, while silica is
colloid. In the Manhattan mine, Xapa Count}^ sulphide of
mercury- is, besides, found intimately mixed with the chalce-
donite. This silicification process was directly connected with
the later igneous eruptions and intrusions. Perhaps the greater
heat during the first part of the period covered by this process
may ofier an explanation for the absence of mercuric sulphide
in the opal then formed. [See, on this point. Genesis of the
Quicksilver Deposits, page 26.]
Calcite and dolomite form besides the silica the gangue min-
erals accompanying the cinnabar. Sometimes these carbonates
GEOLOGY OF THE QUICKSILVER BELT. 21
are in direct contact with the cinnabar. The associated
metallic minerals are in nearly all cases pyrite and marcasite;
very often arsenious and antimonious minerals, and sometimes
copper minerals. Cinnabar ores are nearly exclusively depos-
ited in pre-existing openings. Ore bodies precipitated b}'
substitution are very rare. Where cinnabar deposition can
now be observed the same rule holds good. The later igneous
eruptions, to which the ore deposition is related, are of Tertiary
or later date. Becker [above cited, page 152 and following]
cites three different periods: The first, pre- Pliocene, during
which large masses of andesite were ejected — a bluish-gray
rock, containing pyroxene and feldspar crystals imbedded in a
ground mass of feldspar and magnetite. A later andesitic
eruption, very late Pliocene or at the close thereof; the ande-
sites belonging to a special group having a trachytic character,
for which Becker proposes the name Asperites. Rhyolite,
probably younger than the andesites, is found near New Alma-
den and in the northwestern part of San Luis Obispo County.
Basalt eruptions, belonging to the Quaternary and more recent
periods. These eruptions are closely related to the fissure
system of the former upheavals, which had established lines of
weakness, along which the strata adjusted themselves to the
posterior deformations. The ore depositions were most prob-
ably formed by mineral springs connected with the volcanic
activity of the post- Andesitic period; hence the3' belong to the
post-Pliocene period. According to Becker, this is indicated
by the usual association of cinnabar with basalt, or as in New
Almaden with rhyolite, and also by the unimportance of cin-
nabar deposits in andesite. It is a striking fact that most of
the prominent mines north of San Francisco are in close prox-
imity to basaltic or relatively recent eruptions, as for instance:
The .^tna mines, a basalt dike on the Silver Bow claim, and
basalt in the Star claim; the Oathill mine, a large basalt body
in close vicinity to the mine; the Corona and Twin Peaks
mines, between the basalt of Oathill and that of the Howell
Mountains; the Great Western, a body of basalt south and in
close proximity to the mine; the Sulphur Bank, basalt all
around the mine; the Manhattan, surrounded by basalt to the
east and north; the Boston, within half a mile of the basalt in
the Manhattan ground.
In the southern field the geological conditions vary very
22 QUICKSILVER RESOURCES OF CALIFORNIA.
much. In the New Idria district no definitive!}^ post-Tertiarj'
igneous rocks can be found, and those rocks which show indi-
cations of igneous origin are so altered that it requires micro-
scopic stud}' of the rocks to determine whether they are altered
eruptives or sedimentaries. In the Stayton district, the
country rock near the ore deposition is prominently basaltic,
sometimes closely related to Becker's asperites. In San Luis
Obispo County, in the Pine Mountain, Adelaide, and Oceanic
districts, the scattered exposures of igneous rock are of rhyo-
lite. In Santa Clara County the only eruptive rock in the
neighborhood of the ore deposits is rhyolite.
ORE DEPOSITS,
The peculiar characteristics of quicksilver, so different from
those of all other metals, render the study of the conditions
governing the genesis of quicksilver deposits an intricate
problem; in fact, some of the phenomena occurring in those
deposits have as yet not been fully explained.
Quicksilver occurs in nature principally as a sulphide,
occasionally to a small extent associated with the native metal.
The compounds of mercury with chlorine, selenium, tellurium
antimony, etc., are all rare minerals, and probably the result of
secondar}' concentration.
Quicksilver differs in many characteristics from gold, which
occurs in nature principally as native metal, though occasion-
ally as a telluride. Gold is soluble in solutions of alkaline
sulphides and iodides, ferric sulphate, and carbonate of sodium
above 200° C. Chlorine is a prominent solvent of gold,
especially in desert regions. In whatever form gold may be
transported, it is precipitated either as a telluride, or as metallic
gold associated with tellurides and sulphides; whether gold is
precipitated in nature as a sulphide is, as yet, uncertain,
because the existence of a sulphide of gold in nature has not
been definitely established. At all events, this sulphide of gold
would be an unstable compound, while sulphide of mercury is
a very stable compound. These differences are here presented,
because the fact that gold is present in cinnabar deposits has
been used as a strong argument in the discussion of the genesis
of those deposits.
Quicksilver also differs greatly from silver in its chemical
behavior toward other elements. The original forms of silver
deposits are, besides sulphides, sulphantimonious and sulph-
arsenious salts. In the zone of oxidation, silver occurs to some
extent in the native state, but much more commonly as a
chloride, cerargyrite.
Mercuric sulphide is not found intimately associated with
the sulphides of lead, zinc, and iron, as is the sulphide of silver.
Sulphide of iron is often found in contact with mercuric
(23)
24 QUICKSILVER RESOURCES OF CALIFORNIA.
sulphide, but no mixtures of the sulphides, like argentiferous
galena, etc., have been found. Oxidation products of mercuric
sulphide, similar to those of the sulphides of lead, zinc, copper,
and iron, are also unknown.
Quicksilver dififers further materially from all other metals
in its behavior toward heat. Nearly all metals have high
melting and boiling points, but mercury becomes a solid at
— 39-5° C., and boils at 357" C, even vaporizing to a certain
extent at ordinar}- temperatures.
Following is a list of the known quicksilver ores:
Amalgam. — A compound of silver and mercury, AgHg or
Ag,Hg3.
Arguerite, from Coquimbo, Chili. AgioHg.
Kongsbergite, from Norway. AgisHg.
Color silver white, in isometric crystals and massive.
Ammiolite. — A compound of mercury containing antimony
and copper, also a little sulphur and iron. An earthy powder;
color deep red or scarlet. Possibly antimonate of copper mixed
with mercuric sulphide. Rare.
Arguerite. — See Amalgam.
Barcenite. — Related to Ammiolite, but contains no copper.
Possibly antimonate of mercury. Rare.
Calomel, or Horn Quicksilver. — Mercurous chloride,
Hg2Cl2. Color light yellowish or gray; luster adamantine,
translucent or subtranslucent. Tough and sectile. Not
abundant.
Cinnabar. — Mercuric sulphide, RgSorHgiSi- Color bright
red to brownish-red and brownish-black. Streak,. scarlet-red.
Subtransparent to nearly opaque. Cr^^stals often tabular,
sometimes acicular; also massive and in earthy coatings.
Cinnabar is the principal mercurial ore.
Hepatic Cinnabar^ or Liver Ore, contains some carbon
and clay; color and streak brownish.
Metacinnabarite^ or black sulphide of mercury, HgS or
HgsSs. Amorphous, color black, resembling graphite,
streak same color. Fracture like tetrahedrite. Recrys-
tallizes on slow cooling into cinnabar.
CocciNiTE. — Iodide of mercury. Color red to yellow, some-
times green and greenish-gray. In acicular crystals or mas-
sive. Rare.
ORE DEPOSITS. 25
CoLORADOiTE. — Telluride of mercury, HgTe. Color gray-
ish-black. Rare.
GuADALCAZARiTE. — Sulphide of mercury; closely allied to
metacinnabarite. Part of the sulphur is replaced by selenium,
some zinc is also present, although these latter two metals are
probably no essential portions of the mineral. Rare.
KoNGSBERGiTE. — See Amalgam.
Lehrbachite. — A combination of selenide of mercury and
of lead. Rare.
Leviglianite. — A ferriferous guadalcazarite. Rare.
LiviNGSTONiTE. — A Combination of sulphides of mercury
and antimonium, HgS, aSbiS;;. Color grayish-black, generally
fibrous, also massive, resembling stibnite. Rare.
AIagnolite. — Mercurous tellurate, HgTe-;04. Rare.
Mercury, Native. — Occurs to some extent in many quick-
silver mines, exceptionally in large quantities, generally in dis-
seminated fine globules.
Metacinnabarite. — See Cinnabar.
OnofriTE. — A sulphide of mercury, wherein the sulphur is
partly replaced by selenium, Hg (S, Se), often associated with
tiemanite. Rare.
TiEMANiTE. — Selenide of mercury, HgSe. Color dark steel
gray, resembling galena. Rare.
TerlinguaiTE. — Oxychloride of mercury. Rare.
TocORNALiTE. — Iodide of silver and mercurj'. Color pale
yellow; granulaf and massive. Rare.
The hydrocarbons Idrialite and Aragotite in places carry
cinnabar. Rare.
In Hungary a copper ore, consisting of sulphides of copper,
iron, zinc, mercury, antimony, and arsenic, is found, often rich
enough in mercury to warrant the special extraction of that
metal as a by-product.
This list shows that mercury combines in nature almost
exclusively with sulphur, which in rare instances is partially
or totally replaced by its closely related elements, selenium
and tellurium; and that mercury also, but rarely, combines
with the halogens chlorine and iodine.
From a practical point of view, sulphide of mercury and
native mercury are the only products requiring consideration,
the others being of no commercial importance.
GENESIS OF QUICKSILVER ORE DEPOSITS^
The majority of the geologists who have treated the subject
of ore deposits consider them, as they exist to-day in situ, as
principall)^ the result of precipitation from aqueous solution.
[See Genesis of Ore Deposits, pages 57 and 73, F. Posepny;
ibid., page 284, C. R. van Hise; ibid., page 658, Prof. J. H. L.
Vogt, etc.] More especially in reference to quicksilver deposits.
[Monograph XIII, U. S. Geological Sur\'ey, page 416, G. F.
Becker; x\merican Journal of Science, vol. XVII, 3d series,
S. B. Christ}-; Genesis of Ore Deposits, page 596, W. Lindgren.]
A concise exposition of the modern views of the genesis of ore
deposits is required to explain the special phenomena obser^-ed
in quicksilver ore deposits, and the deductions to be derived
therefrom.
There is no reason for supposing that the heavj- metals of
ore deposits come from the enormously compressed centro-
sphere; hence the conclusion that the ore deposits are derived
from the crust of the earth. Indeed, a notable number of ore
deposits may be referred to eruptive processes connected, not
with the heavj- interior, but with the crust of the earth, which
must be regarded as being at least 50 kilometers in thickness.
This crust can be divided into zones from two different
standpoints:
{a) The zone of fracture.
The intermediate zone of combined fracture and flowage.
The zone oi flowage.
These zones are delimited b}- the manner in which the rocks
j'ield to deformation. In the upper zone of fracture, the strata
yield to deformation by fracturing; in the deepest zone, onh*
spaces of microscopic size can exist, and the deformation
process is similar to that of mashing or kneading.
The maximum depth (assuming no lateral pressures occur)
be3''ond which the strongest rock material will yield to defor-
mation by flowage can be placed at 12,000 meters. In regions
of orogenic and eruptive actions, the lateral stresses may
(26)
GENESIS OF QUICKSILVER ORE DEPOSITS. 27
materially reduce this depth, which probably may have to be
further reduced, because of the greatly increased plasticity of
the rocks saturated with superheated water. It therefore
follows that all fissures must disappear at a certain depth.
As rocks are of varying strength, and as lateral pressures
materially influence the conditions under which the rocks
exist, there must be a zone of combined fracture and flowage
below the zone of fracture. This belt has a considerable
thickness, possibly over 5000 meters.
The earth crust may also be subdivided from a physico-
chemical standpoint, controlled by the relations between chem-
ical action and heat and pressure, into:
(d) The Upper Physico-cJiemical zone, resubdivided into:
. Upper Belt — Belt of weathering.
LrOwer Belt — Belt of cementation.
The Lower Physico-chemical zone.
Near the surface, where temperature and pressure are low,
the preponderating reactions are heat-developing. In the
lower zone the heat-absorbing reactions preponderate, accord-
ing to van Hoff's law. [W. Nernst, Theoretical Chemistry,
page 583.]
Two important reactions separate these zones: First, tne
reactions between oxygen and sulphur. In the upper zone
oxygen replaces sulphur, resulting in great liberation of heat
and expansion of the volume of the solid compound. In the
lower zone sulphur replaces oxygen with condensation and
great absorption of heat. This reaction is the more important
when considering that oxide of iron, in the form of magnetite,
is one of the constituents of eruptive rocks (rocks of deep-
seated origin). Secondly, the reaction between carbon dioxide
and silica. In the upper zone, especially in the belt of weather-
ing, carbon dioxide replaces silica, acting specially upon sili-
cates; the liberated silica passing into solution in a colloidal
form and not ionized [Kahlenberg and Lincoln, Journal of
Physical Chemistry, 1898, page 88], and carried downward into
the belt of cementation. In the lower zone silica replaces car-
bon dioxide, with great absorption of heat and with condensa-
tion; the carbon dioxide entering into the solution.
The depths at which these reactions reverse for different
compounds, and for the same compound under different con-
28 QUICKSILVER RESOURCES OF CALIFORNIA.
ditions, are very variable, and are greatly affected b\- the fact
whether the latter are mass-static or mass-dynamic.
The water circulation through the earth crust represents a
cycle, caused chiefly by gravitation stress, and is due to the
fact that the water entering the ground at a certain level, after
a short or long underground journey, issues at a lower level.
From the point of view of the genesis of ore deposits, only
the water that enters that part of the earth crust situate below
ground-water level is of importance. Its temperature increases
with depth, and below 3000 meters, in the zone of fracture, it
is in the form of superheated water, having consequently great
chemical activity.
There is a strong tendency for water entering through an
indefinite number of small openings to converge into larger
openings which are located on the lines of weakness in the
formations. These waters reach, in the lowest part of their
course, where they possess their highest chemical activity, the
zone wherein sulphur is the more active agent, so that they
dissolve prominently sulpho-compounds out of the rocks,
through which they percolate in capillary and supercapillary
openings, until saturated, and hold them in solutions in ion-
ized form. The precipitation out of these solutions is the
result of supersaturation due to several causes, among which
the most prominent are dilution and loss in temperature and
pressure.
It is more than probable, from the intimate association of
igneous rocks with a large majority of ore deposits, that they
are the main source of the metallic ores; and that there is
a direct genetic relation between ore deposits and eruptive
processes. A number are, in fact, intimately connected with
eruptive magmas, especially through eruptive after-action, as
sublimation, gaseous action, igneous-aqueous action, etc., by
which the heavy metals were in great part extracted from
such magmas. As the eruptive magmas, at least those of
deep origin, are admitted to contain a more or less notable
admixture of water, with other constituents of hydrous or
gaseous character, the formation of minerals on cooling and
the subsequent cycle of solution and reprecipitation, as above
described, will take place.
In this connection the following quotation is important:
"It is thought highty probable that under sufficient pressure
GENESIS OF QUICKSILVER ORE DEPOSITS. 29
"and at a high temperature there are all gradations between
"heated water containing mineral material in solution and a
"magma containing water in solution. If this be so, there
"also will be all stages of gradation between true igneous
"injection and aqueous cementation, and all the various phases
"of pegmatization may thus be fulh' explained." [C. R. van
Hise, 1 6th Ann. Rep., vol. XI, page 647.]
The foregoing explains the reason that the metals are origi-
nally deposited principally in the form of sulpho-compounds;
which, in the upper portion of the earth crust, in the belt of '
weathering, under the action of the various gases, especially
carbon dioxide and oxygen, and of organic bodies, are trans-
formed into various oxidation products thereof, including the
native metal. [See on this subject more particularly: F,
Posepny, Genesis of Ore Deposits; C. R. van Hise, Principles
of North American Pre-Cambrian Geolog}', i6th Ann. Rep.
U. S. Geological Sun'e}^ Pt. I; ibid.^ Physico-Chemistry of
Metamorphism, Bulletin Geol. Soc. of Am., vol. IX; J. L. H.
Vogt, Problems in the Geology of Ore Deposits, Genesis of
Ore Deposits, page 636 and following; etc.]
The opinion that quicksilver deposits are formed in accord-
ance with the general principles above described is based upon
obser\^ations at Steamboat Springs and Sulphur Bank, and
finds confirmation in the associated minerals within those
deposits which bear evidence of precipitation out of aqueous
solutions. The following observations on this subject are of
sufficient importance to be shortly discussed:
Most of these deposits show that at some time during their
history they have been the scene of intense solfataric action,
and a great many are in contact or in close proximity to
eruptive phenomena.
Mercury boils at 357*^ C, but volatilizes to some extent at
ordinary temperatures.
Liquid mercury combines with sulphur in the manufacture
of vermilion in the dry way, below the melting point of sul-
phur, 120° C. ; in the wet waj', sulphide of mercury forms
between 45° and 50° C. Hence the combination of mercury
and sulphur takes place between liquid mercury and sulphur.
That in the wet process a heat below 50° C. is insisted upon
would indicate that the combination of liquid mercury and
sulphur can only take place within the immediate vicinity of
30 QUICKSILVER RESOURCES OF CALIFORNIA.
the surface, as the proximity of igneous-aqueous action to the
quicksilver deposits during some time of their history will
cause the increase of heat in depth to be much more rapid than
the ordinary static rate of i° C. per loo feet. (At Sulphur
Bank, Dr. Becker gives the heat of the water of the Herman
shaft at the surface 128° F., and at a depth of 300 feet 176° F.)
In vapor form mercury combines with sulphur at high tem-
peratures, proof of which can be found in the bricks of old
furnaces wherein cinnabar and native mercury are often found
in large quantities; the mercurial vapors must have recombined
with free sulphur in vapor form and recr^'stallized as cinnabar.
The agency which causes the recombination of these disso-
ciated vapors, at practically the same temperature, is as yet
undetermined.
All these considerations have caused a great number of
operators of quicksilver mines to retain the old theory of ore
formation by sublimation, and to hold the opinion that mer-
cury is brought into the lithosphere, and possibh' even into the
belt of weathering, in the form of mercurial vapors. These,
under favorable conditions, form mercuric sulphide, which then
follows the cycle of solution and precipitation indicated by
Messrs. Becker and Christy, namely, a solution of a double
sulphide of mercury and sodium (HgS, nNaiS) in waters holding
in solution: alkaline-sulphides, -sulph5'drates, and -h3-drates,
or neutral or acid sodium carbonates partially saturated by
hydrogen sulphide; and a precipitation mainly due to decrease
in temperature and pressure or to dilution.
Dr. Becker [Mon. XIII, U. S. G. S., above cited, page 419
and following] thoroughly discusses this subject and gives
extensively his reasons for considering the cinnabar deposits as
exclusively formed by precipitation from solutions. Prof. S. B.
Christy [Am. Journal of Science, vol. XVII, 3d series, 1879, page
453 and following] had previously given his reasons why he
arrived at the same conclusion. He made several tests as to
the solubility of mercuric sulphide in different solutions under
varying conditions of temperature and pressure, and regarding
its precipitation out of those solutions. A short extract from
his article will be of great interest:
"The tests were made at temperatures varying from 200"^' to
"250° C, and pressures varying from 260 to 500 pounds per
GENESIS OF QUICKSILVER ORE DEPOSITS. 31
" square inch. The duration of the tests varied from three to ten
"hours, and in each case the cooling was allowed to take place
"gradually and undisturbed. Their result proved that waters
"containing solutions of alkali sulphides and some natural min-
"eral waters to which sulphydric acid had been added, will,
"under certain conditions of temperature and pressure, dissolve
"mercuric sulphide; that increase in pressure aids rather than
"retards this solution, and that cinnabar is deposited from such
"solutions in the crystallized form when temperature and pres-
"sure are slowly lowered, while the occasional occurrence of
" metacinnabarite, or black amorphous sulphide of mercury, was
"explained by the sudden dilution or cooling of the depositing
"waters, or the local mixing, during crystallization, of agents
"causing rapid precipitation."
Professor Christy in the course of these tests obtained out of
a solution of potassic sulphydrate wherein amorphous mer-
curic sulphide was placed, a coherent mass of crystals of cinna-
bar, perfectly simulating the crystals which occur in nature.
He further argues that while the deposition of cinnabar from
mercury in vapor form occurs in the masonry of furnaces,
condenser walls, etc., the same can not account for the same
action in ore deposits, because the high temperature required
to volatilize mercury and cinnabar would destroy the gangue
minerals almost invariably associated with the ore in nature,
such as dolomite, calcite, bitumen, and pyrites, which besides
are never found in the occurrences of cinnabar and mercury in
the masonr}^ of furnaces and condenser walls, directly traceable
to volatilization and sublimation.
There are some fundamental differences between quicksilver
ore and gold ore deposits, which must be noted. All the quick-
silver deposits worked up to the present time show a lack of
persistence in depth, and at a rather shallow depth in the
different deposits their cinnabar content becomes too low for
commercial purposes. The approach of this impoverishment
is in nearly every case accompanied with the occurrence of
native mercury, while in gold deposits generally, once the
sulphide zone is reached, the character of the ore remains
nearly permanent.
Dr. Becker attributes this phenomenon to the precipitation
of native mercury by dilution of the solution, or by the action
of decomposition products of organic matter; the latter causing
32 QUICKSILVER RESOURCES OF CALIFORNIA.
the presence of hydrocarbons so often found accompanying
quicksilver ores. [Mon. XIII, U. S. G. S., page 437.] That
the native mercury is mainly found in the lower parts of the
mines is ascribed by him to the fluidit}' and high density of
the metal. [Ibid., page 388.]
As to the precipitation of native mercury b}- dilution, when
the precipitation is caused suddenly, the product is a black
mass of metacinnabarite with a very small quantity of native
mercury [ibid., pages 429, 430, and 436] ; hence the copresence
of cinnabar and native mercury would involve a re-solution
and precipitation and slow cooling of the metacinnabarite
without affecting the native mercun- present.
The reduction of mercuric sulphide through decomposition
products of organic matter would relegate the locus of this
reaction to the upper portion of the deposit, and as those agents
are active at the present time, native mercury ought to be
found, at least to some extent, in the upper horizon of all
quicksilver deposits.
Prof. S. B. Christy remarks on the occurrence of native
mercury: "Unless w^e regard it as an efiect of local oxidation
"of a very stable compound, its appearance is well nigh inex-
"plicable upon either h3'pothesis" of production by sublimation
or deposition from solution. [Am. Journal of Science, vol.
XVII, 3d series, page 463.]
The oxidation of mercuric sulphide takes place at high
temperature; mercuric sulphate being formed in the condensers
nearest the furnaces, but not having been found in nature.
Whatever may be the cause of the formation of native
mercurs', its fluidity and density can hardly account for all
phenomena of its occurrence. In the Socrates mine, Sonoma
County, native mercury is found in fine globules within com-
pact rock, while in the fracture planes of the same rock cinnabar
is found associated with the native metal; if the cinnabar was
the original form wherein the metal was deposited, some traces
of it ought to be found in the compact rock, where the decom-
posing agents can not have been as active as in the fracture
planes. Original deposition as native metal and subsequent
transformation into sulphide appear here more probable.
The quicksilver deposits are closely connected with eruptive
phenomena — either the presence of eruptives, or intense solfa-
taric action. As Professor Vogt states: "In the exceedingly
GENESIS OF QUICKSILVER ORE DEPOSITS. 33
"numerous deposits in some way connected with eruptive
"processes, the nearness of igneous rocks must have caused
"increase of temperature (and also of pressure?). This is
"often so great as to exceed for heavy compounds the critical
"temperature." [Genesis of Ore Deposits, page 659.]
The source of the great heat in most of the quicksilver
mines can, in many cases, be traced directly to the chemical
reactions taking place at the present time. Chemical activity
being increased by temperature and pressure, it is only reason-
able to suppose that, at no great depth, conditions exist which
would keep the mercury in a gaseous state.
The suggestion of Professor Vogt: " With regard to younger
"veins especially, we must keep in mind a possible extraction
"from laccolitic magma in depth" [ibid., page 656], may
in many cases offer an explanation for the genesis of quick-
silver deposits, where no extrusive igneous rocks are found in
their vicinity. Erosion is the cause of the absence of quick-
silver deposits in older formations. This erosion is much more
considerable than generall)- taken into account. [See ibid.,
page 670.] Professor de Launay, comparing ore deposits oc-
curring relativel}- near the surface in less denuded regions with
those deep below the surface in strongly denuded regions, takes
as instance of the former quicksilver deposits, "which occur
"chiefly in recent rocks near volcanic eruptives, while from
"older ranges, partly destroyed by erosion, they have disap-
"peared with other debris."
The cinnabar deposits are in many cases connected with
alteration zones in the country rock, caused by silicification,
forming by preference in those zones. The latter, however, do
not uniformly contain cinnabar, and the same form of altera-
tion of the rocks is found throughout the Neocomian outside
of the quicksilver belts. This process of silicification is more
especially characteristic of the belt of cementation. [See above,
page 27.] The term cementation designates the binding to-
gether of the rock particles by infiltration of mineral materials
in solution, and their deposition as minerals in the interstices
of the rocks.
The process of serpentinization resembles that of silicifica-
tion. The material for the serpentine may be furnished
partly, or in whole, b}- the minerals present in basic sedimen-
3— QR
34 QUICKSILVER RESOURCES OF CALIFORNIA.
tary rocks, which are altered through this process, or the
material may come from extraneous sources. [Van Hise, i6th
Ann. Rep., Part I, page 691.]
As serpentine may replace quartz, the presence of cemented
and indurated sandstones, chalcedonite, phthanite, and serpen-
tine may represent various phases of the physico-chemical
process of cementation in the belt of fracture.
This silicification process forms different materials in different
localities. It forms a great quantity of black opal, containing
some quartz and chalcedonite (a mixture of opal and crystal-
line silica). A considerable portion of the sandstones of the
Coast Ranges show the effects of this silicification process, in
varying degrees.
The cinnabar forms in the cracks, seams, and fissures of the
silicified material. The richness of the cinnabar ore is to a
great extent dependent upon the size of the cavities favorable
for deposition and consequently upon the compactness of the
fissure-filling; hence rich ore bodies are principally found in
those parts where the fissure-filling has been crushed and
distorted.
COST OF MINING AND REDUCTION.
The cost of mining and reduction of quicksilver ores differs
very sensibly in the various mines. The nature of the ground
is one great cause of this difference. In some mines the
ground is such that little or no timbering is required. In
others, the ground is so bad that the stopes have to be tim-
bered and filled. In some mines the air is generally good,
while in others the heat is so great that the men work under
disadvantage.
The cost of timber and cordwood also varies very much, some
districts being well provided with timber, while others are at
considerable distance from the source of suppl)-.
'• I--?/
YTVTJOO
Geology by Win. Forstner, E.M.
MAYACMAS D
I — Sunrise. ") lo — Geyser, Sulphur,
2 — Cloverdale. Il — Black Bear Group.
3— Mercury. 12— Pluton Den.
4 — Manzanita. j 13 — Clyde.
5 — Albian. /■ Cloverdale Mine. 14 — Culver — Baer Group.
6 — Mattole. 15— Rattlesnake.
7 — Mount Vernon. 16 — Tunnel Site. )
8 — Philadelphia. 17 — Incandescent. '-
9 — Waterloo. J 18 — Almaden. )
No. Name OF Mine.
NO. N.4ME OK MINE.
19— Mate. 1
29 — Socrates.
20 — Eureka Nos. i and 2. [Eureka Con.
30 — Mercury.
21— Captain. f
31— Great Northern.
22- 1
23 — Cedar.
32-Hope.j. p^„^,,, p^^i,,^ ^
24— Quicksilver. ( Crown Point
34-Denver.
25— Queen Group.! Q. Mining Co.
35-)
26 — Lookout. 1
36 — V Lucky Stone Group
27 — Diamond. \
37—)
28 — Mercury.
38— Hurley.
N.AaiE OF Mi:
39 — Pacific.
40 — Hercules.
41 — Sonoma.
42—
43—
44—
45 — Pontiac.
46- "
47 — Boston.
48— Empire.
rn Point Quick-
ver Mining Co.
49 — Double Star.
50 — Occidental.
51 — Healdsburg.
52— Edith.
53— Cinnabar King Group.
54-Eugenie. )
55— Maud. [■ Bacon Con.
56— Dragon. '
57— Napa.
DISTRICT.
58— St. George, i
59— Golden Gate. ■ Bacon Con.
60— Eagle. \
61— Helen.
62 — Young America.
63 — Chicago.
64— Wall Street.
65 — ^Jewess.
66 — Middletown.
67-
Nameof mi:
68— Gem.
69 — Great Eastern.
70 — Hope.
71 — Iviverpool Con.
72 — Eureka Con. )
73— "
Great Western
-Standard Q. Co. 5
74-
75—
76-
1- Napa Consolidated.
1 — Eureka Con.
79— "
80— "
I— Contention.
82 - Minnesota.
83 — Manzanita.
S4 — Mercury.
S5 — Bone.
86 — Fanny.
Napa Consolidated.
88— South Side.'
89 — Corona.
90 — Napa Con.
91—
92 — Beecher.
93 — New Granada
94— Twin Peak.
95- "
Xi.. Namk of Mink.
96 — Ida Easly.
97— Old Discovery.
98— Twin Quartz.
99— Good Enough.
100 — Silver Bow. ')
loi— Phrenix. j
102— Red Hill. [ :jj(^jj ^^Q„
103— Starr. j
104— Pope. I
(05 — Washington. J
34
tary rockj
material n
Ann. Rep.
As serp(
and indurj
tine may
process of
This sili
localities,
some quar
line silica)
Coast Ran
varying de
The cini
silicified n
great exte:
for deposit
fissure-filli
those part
distorted.
qAK J
rri- 'Tj
./d/iHOTlIJAO
COS
The cost
ver>' sensil
is one gn
ground is
others, the
bered and
while in ot
disadvanta
The cost
districts be
considerab
A 3TATe
- c.tW3J
Obi
•ej3»*.« -
i
DISTRICTS NORTH OF SAN FRANQSCO.
MAYACMAS DISTRICT,
The Mayacmas District, as defined b}- Dr. G. Becker [see
Mon. XIII, U. S. G. S., page 368], embraces parts of Napa,
Lake, and Sonoma counties, along the Mayacmas range, of
which Mount St. Helena and Mount Cobb are the most promi-
nent mountains. [See geological map of portions of Napa,
Sonoma, and Lake counties quicksilver districts, in this Bul-
letin.]
Quicksilver deposits are found on both sides of the range;
the main belt, however, lies in its eastern part north of the range,
crosses it near Pine ^Mountain (between Mount St. Helena and
Mount Cobb), and lies principally south of it, west of Pine
Mountain in Sonoma County.
The general trend of the belt is northwest. In its south-
eastern part, in Napa Count3', it is in very close proximity to
a region of very intense and probably prolonged eruptive
action, covering Tertiarj- and post-Tertiary periods. The
center of eruptions in this region was probably' in the territory
bounded b}- Mount St. Helena, the Twin Peaks (or Sugar
Loafs), and High Peak; the flows have, however, spread over
a large adjoining territory. Outside of this are found a great
many other eruptive bodies in this district, of which the more
prominent are: The basalt body on Oathill, some smaller
ones in the territory of the ^-Etna Consolidated Company, an
andesitic eruptive body northeast of Oathill, Pine Mountain,
Col)b Mountain, and others. This district is hence a region of
intense eruptive action. Large masses of lava have covered
parts of it, and while partly eroded, extensive sheets of tufa
cover at present parts of it to a greater or less depth, and make
it ver>- difficult to determine the limits of the cores of igneous
rocks. The present deeply car\-ed topography of the region is
largely governed by the erosion of this capping.
The older rocks are mainly represented by sandstones, some-
times nearly unaltered, sometimes thoroughly altered into
(35)
36 QUICKSILVER RESOURCES OF CALIFORNIA.
schists, with all intermediary gradations. Serpentine is very
prominent, mostly a hard, dry variety, in places disintegrated
and pulverized b}- weathering, showing as large bare spots
along the ranges. Even where not bare, the serpentine can be
detected at a distance by a sparse vegetation, w^hile on the
balance of the surface a ver>' close growth of brush or grass is
found. The relation of the serpentine to the quicksilver
deposits is not clear. Most of these are associated with, or in
close proximity to, serpentine; but others, like those at Oat-
hill and Cloverdale, are entirel}' away from the serpentine;
and where the serpentine is verj^ prominent and continuous
over a certain width, no deposits of any value have been found;
as, for instance: between Oathill and the Mirabel around the
head of Bucksnorter Creek; on the ridge between Bear Creek
and Drj' Creek ; on the main ridge between the headwaters of
Dry Creek and Briggs Creek. Neither are workable quick-
silver deposits found in the serpentine. Where serpentine is
associated with any deposits, these are always contact deposits,
while both the Oathill and Cloverdale mines are in the sand-
stone.
The quicksilver deposits appear from their association with
the opaline rock, which is presumably an alteration product of
serpentine by silicification, to be related to the serpentine to
a certain extent. The fact that, where it is A-ery wide, no
paying deposits have been found, would indicate, however,
that either the sandstones contain the primary disseminated
metal, which is concentrated through some process of second-
ary concentration, or else in the large bodies of serpentine the
concentration took place only in those parts affected by contact
metamorphism. While this holds true only for the south-
eastern part of the district, it must be remarked that in the
northwestern part, in Dry Creek and Pine Flat districts, there is
in many cases an undoubted relation between the quicksilver
occurrence and igneous actions. In the Dry Creek district the
only deposit of any ascertained consequence is the Helen,
which lies very close to the tufas of Pine Mountain. There
are undoubted signs of igneous rocks in the Pine Flat district
on both sides of Big Sulphur Creek; some of these igneous
dikes run, as far as determined, in a direction which would
bring them near the ore deposits of the Eureka mine; others
were found near the Cloverdale mine. For a great number of
MAYACMAS DISTRICT. oi
deposits, these relations are not yet determined. Considering
the intimate relation of quicksilver deposits and aqueo-igneous
actions and the general geological conditions in this region, it
may, however, be expected that, at least, laccolitic relations
exist there.
Between the Corona and St. Helena Creek, a distance of
four miles in an air line, along the headwaters of Bucksnorter
Creek, the belt of serpentine is verj- wide. Between St. Helena
Creek and Bucksnorter Creek the Standard Quicksilver Min-
ing Company- has in the last few years spent a considerable
sum of money prospecting, but so far without any favorable
result.
To the west of the Great Western mine are the headwaters
of Dry Creek, a bowl-form basin nearly encircled bj' the main
ridge and by a ridge dividing Dry Creek from the drainage of
Putah Creek. Serpentine is very prominent in a great portion
of the Dry Creek basin, and again barren of any workable
deposits of cinnabar, notwithstanding some very prominent,
peculiar croppings, standing out boldly in the serpentine.
These croppings, especially prominent in the Wall Street and
Jewess grounds, consist of a network of white quartz seams,
mostly thin amorph quartz, with occasional concretions of
botryoidal form; the ground mass is a light yellow-brown,
ochreous mass; this material is locall}- called "dry bone," and
so far as yet observ'ed, never indicates a w^orkable ore deposit.
The same is found on the Bacon Consolidated and Cinnabar
King ground (Pine Mountain), and also in the Double Star
mine (Pine Flat). (Lawson's silica-carbonate sinter.)
Pine Mountain is a mass of andesitic tufa, most probably
with an eruptive core, of small dimensions and very steep
sides, and entirely disconnected from the Mount St. Helena
and the Mount Cobb groups of eruptives. Its main ridge is
not over 25 feet wdde, and about 300 feet long; elevation, 3475
feet. The tufa is of a light grayish color, and has spread over
a part of the adjacent ravines. No signs of basaltic rock could
be found on the ridge. The Helen mine is situated on the
eastern slope, near the edge of the tufa, and on the south-
western, western, and northwestern slopes are located a series
of mines, comprising the Cinnabar King and Bacon group of
mines. The northwestern slope is very steep and partly cov-
ered by tufa, which covers alternate beds of serpentine and
38
QUICKSILVER RESOURCES OF CALIFORNIA.
Fig. I. Section of uonhwest slope of Pine
Mountain, Sonoma County.
metamorphosed sandstones. At the contacts wide belts of
croppings show, partly in place, partly covering the side hill
with large bowlders. These croppings resemble very much
those of the Wall Street and Jewess. In the caiion continu-
ing below the old road from Middletown to Pine Flat a very
well-defined cropping on the contact of serpentine and sand-
stone is seen. [See Fig. i.] A great amount of work has
been done here; remnants
of old shafts and tunnels
are found everywhere on
the hillsides, but all work
is now abandoned. Sev-
eral pockets of very rich
cinnabar ore were found
at diSerent points at the
surface, but none appear
to have been found persist-
ent in depth.
The headwaters of Putah Creek are situated in a basin on
the south slope of Mount Cobb. In this basin are a great
number of hot springs, of which Anderson Springs are by far
the most prominent. These springs generally contain a great
amount of sulphur, and in several places sulphur deposition
and rock decomposition b}- sulphurous fumes are taking place.
Here, as in other parts of the district, cinnabar deposition
does not occur in or close to those places where hot waters and
vapors reach the surface. There are no cinnabar mines in this
basin — only a few prospects, which can scarcely be said to
give, up to the present, much promise of turning into mines;
a condition partly due to insufficient development.
The mines around Mount St. Helena have a considerable
supply of timber in their vicinity, although the ^Etna, Oathill,
Corona, Mirabel, and Great Western mines have made serious
inroads on the supply. The Oathill mine is the only one having
a sawmill. The other mines must use round timbers, or get
their timbers from the sawmills in Lake County at the foot of
Mount Cobb. In the Pine Flat district, the timber supply is
rather scant. There is one sawmill in the district. Round
timbers cost per set, including lagging, from $2.50 to $2.75;
timbers, 7 cents per linear foot; lagging, 3^ cents apiece;
-TT-
An
i^'
r^
v.,
f^.
.-J-
^^Sr
5-y
V? ^
L\
''K^,
\\jO\v4v Lake
\ /^hur»lpi(Lake
\<M
C 0 y o t * ^i> Gehnatdl lake
,Y<i'
j%
wjii 1 r '
-/'•
-^^^^iii^
''^^^^^-^r:^"'
[IZl [Z]
GEOLOGICAL MAP OF NAPA, SONOMA, LAKE, AND YOLO COUNTY QUICKSILVER DISTRICTS,
IssuKD BV California Statu Mining Bureau— Lewis E. Auburv, Statu Minbralouist, 1903.
CLEAR LAKE DISTRICT. 39
sawed square sets at mill, $2.15; lagging, 15 at 7 cents, $1.05;
cordwood averages from S2.50 to $3 per cord.
This district connects by several good roads with railroads.
The southeastern and central parts, by three roads to Calistoga —
one from Oathill, the toll road from Middletown, and the toll
road from the Great Western mine; distances, from 12 to 20
miles. The northwestern part connects with Calistoga and
Healdsburg, and for the most extreme northwestern portion
also with Cloverdale; distances, from 16 to 20 miles.
CLEAR LAKE DISTRICT.
The southern borders of Clear Lake and the adjoining terri-
tory* have been a region of great volcanic activity; a great
part of the territory south, southeast, and east of Clear Lake
bears evidence of having at one time been covered by lava
flows, most of the ridges being covered with eruptive
flows. [See Report State Mining Bureau of Cal., X, page 232.]
Whether these were ejected from a few large vents, or from a
great number of disseminated minor vents, has not yet been
determined. In close proximit}' to Clear Lake, at Mount Ko-
nockti or Uncle Sam, and in the territory northwest of Sulphur
Bank, such vents are undoubtedly located. These eruptions
took place at different periods, and ejected lavas of different
compositions. Mount Konockti is formed b)- later andesites,
which are also found to the northeast of the lower part of Clear
Lake; but in the close neighborhood of Sulphur Bank the
eruptives are priiicipall}^ but not exclusively, basalts. These
latter eruptions must have been recent, the basalt overlying
the Quaternary Cache Lake beds. To the northeast of the
lava flows in this district is a verj* extensive belt of serpentine;
but the rocks underlying the lava flows are, north of Putah
Creek, prominently sandstones and shales. [See geological
map of Napa, Sonoma, Lake, and Yolo counties quicksilver
deposits.]
Around Lower Lake lumber is worlh $17 per 1000 feet
(B. M.); round timber, 6 cents per linear foot; lagging, 6 cents
apiece.
This district finds its railroad outlet through Calistoga.
Lower Lake is 33 miles distant from that town.
'-5-^-
..-^
i^v^,
f^
CLEAR LAKE DISTRICT. 39
sawed square sets at mill, $2.15; lagging, 15 at 7 cents, $1.05;
cordwood averages from $2.50 to $3 per cord.
This district connects by several good roads with railroads.
The southeastern and central parts, by three roads to Calistoga —
one from Oathill, the toll road from Middletown, and the toll
road from the Great Western mine; distances, from 12 to 20
miles. The northwestern part connects with Calistoga and
Healdsburg, and for the most extreme northwestern portion
also with Cloverdale; distances, from 16 to 20 miles.
CLEAR LAKE DISTRICT.
The southern borders of Clear Lake and the adjoining terri-
tory have been a region of great volcanic activity; a great
part of the territory south, southeast, and east of Clear Lake
bears evidence of having at one time been covered by lava
flows, most of the ridges being covered with eruptive
flows. [See Report State Mining Bureau of Cal., X, page 232.]
Whether these were ejected from a few large vents, or from a
great number of disseminated minor vents, has not yet been
determined. In close proximity to Clear Lake, at Mount Ko-
nockti or Uncle Sam, and in the territory northwest of Sulphur
Bank, such vents are undoubtedly located. These eruptions
took place at different periods, and ejected lavas of different
compositions. Mount Konockti is formed bj^ later andesites,
which are also found to the northeast of the lower part of Clear
Lake; but in the close neighborhood of Sulphur Bank the
eruptives are principally, but not exclusively, basalts. These
latter eruptions must have been recent, the basalt overlying
the Quaternary Cache Lake beds. To the northeast of the
lava flows in this district is a very extensive belt of serpentine;
but the rocks underlying the lava flows are, north of Putah
Creek, prominently sandstones and shales. [See geological
map of Napa, Sonoma, Lake, and Yolo counties quicksilver
deposits.]
Around Lower Lake lumber is worth $17 per 1000 feet
(B. M.); round timber, 6 cents per linear foot; lagging, 6 cents
apiece.
This district finds its railroad outlet through Calistoga.
Lower Lake is 33 miles distant from that town.
40
QUICKSILVER RESOURCES OF CALIFORNIA.
1^
SULPHUR CREEK
DISTRICT.
The Sulphur Creek
district comprises the
headwaters of Sulphur
Creek, on the line be-
tween Lake and Colusa
counties, east of Clear
Lake. This region has
been considerablj- erod-
ed, a great amount of its
debris covering to a con-
siderable depth the coun-
try Ij'ing to the west
toward Cache Creek, a
distance of three miles
in an air line. The ridge
near the Abbott mine,
forming the watershed
between Cache Creek
and Bear Creek, is in
places covered with
wash gravel, some of
the pebbles being de-
rived from igneous rocks.
Two nearly parallel
belts of serpentine run
through the district [see
special map of the dis-
trict and Fig. 2] with a
northwest trend. The
western runs partly on
above-mentioned divide;
the serpentine is very
siliceous in character
and rather opaline. On
its eastern contact with
a belt of rather soft sand-
stone lies a zone of
crushed opaline. To the
west of this serpentine,
SULPHUR CREEK DISTRICT. 41
between it and the adjoining shales, is a zone of a light gray
or yellow material, containing inclusions (varying in size
from small pebbles to bowlders of considerable size) of obsid-
ian, chalcedonite, and opalinized serpentine. The matrix of
this breccia is a tufi, or better, a tuffoid (a tuff altered by
regional metamorphism, according to Miigge). [See Williams,
Litholog}', page 290.] The same material is found in the
Elgin mine.
The surface of this serpentine has been leached by acidic
w^aters, leaving a peculiar hard, siliceous material of a light
bluish-gray color, full of cavities, and occurring in thin slabs.
Near the surface the serpentine is generally not silicified, but
the ledge matter is largely a much crushed opaline rock, more
friable and less hard than the opaline in the tuffoid. This ser-
pentine belt is not very long and is surrounded by shales and
argillaceous sandstones. [See map of district.] To the east is
a wider and more continuous serpentine belt, at the western
contact of w^hich are located the Wide Awake, Empire, and
Manzanita mines.
The shales contain bitumen, sometimes forming heavy oil,
and sometimes lighter gaseous hydrocarbons. The waters
percolating through these formations are often charged with
hydrogen sulphide. Occasionally they form hot springs. A
hot sulphur spring at Blanck's Hotel [see map] was cut off by
the Wide Awake shaft when the latter was sunk from the 200
to the 300 foot level, at a distance of 1300 feet from the spring,
and a depth of about 300 feet below the spring, and never
reappeared, cold water now issuing from the same spring.
This proves that this spring was caused by hot ascending
waters, following a gentle slope of about 1300 feet horizontal
to 300 feet vertical. The great amount of mineralized waters,
the siliceous sinters and sulphur deposits formed by extinct
solfataric springs, and the still existing hot sulphur springs,
indicate strong irruptive action. As no igneous rocks appear
at the surface in the immediate neighborhood, this may have
been laccolitic. In the bed of Sulphur Creek a conglomerate
is constantly forming, the pebbles in the creek being cemented
by deposits from the water, which is charged with sulphur and
sulpho-salts.
The shales and sandstones occur unaltered and in various
stages of alteration. A belt of limestone passes through the
Manzanita property, course southeast, adjoining to the west a
42 QUICKSILVER RESOURCES OF CALIFORNIA.
belt of conglomerate, a water formation, similar to that now
forming in the bed of Sulphur Creek. About three fourths of
a mile farther on, in the same direction, but without any sur-
face connection with this limestone, is found a small body of
fossiliferous limestone, with fossils of the Cretaceous age
{Rhvnchonella whitJieyi).
In the Sulphur Creek district the cost of sawed timber is
very high, the nearest sawmill being 28 miles distant and the
roads very heavy; the mines use exclusively round timber at
8 cents per linear foot for 6 inches (smallest) diameter. Cord-
wood (oak) costs $s per cord.
KNOXVILLE DISTRICT.
The Knoxville district, situated at the junction of L,ake,
Napa, and Yolo counties, was in former times the scene of
much activity. A number of the mines then in operation —
Reed, Andalusia, Royal, and Grizzly— are closed down and
abandoned, and the newer prospects — Harrison, New Eng-
land, Red Elephant, etc. — have as yet disclosed nothing im-
portant.
The two mines at present in operation (the Boston and the
Manhattan) offer, however, many points of interest. These
mines are in proximity to a basaltic body ; the Manhattan is
in contact therewith, and the Boston is in very close proximity
and practically in line with the direction of the main fissure
through which the basalt was ejected. This basalt is the only
eruptive body coming to the surface in the district, and lies
on the contact between the large belt of serpentine which runs
in a southeasterly direction from Cache Creek and the unal-
tered Neocomian to the northeast thereof. This serpentine belt,
which reaches into Napa County and is several miles wide, con-
tains, as far as yet ascertained, only sporadic signs of cinnabar
ore, and it is very doubtful if any workable deposits will ever
be found therein.
There is no timber in the vicinity of Knoxville. It has to
be hauled from Lower Lake, 18 miles. Round timber, 8 inches
(smallest) diameter, costs 10 cents per linear foot. Cordwood,
oak, $5; pine, etc., $3.50 per cord. Oak is so much superior to
pine in the furnace that at $5 per cord it is not more expensive
than the latter at $3.50 per cord.
This district connects with the railroad at Rumsey, a dis-
tance of 15 miles; generally supplies are hauled from Napa,
40 miles distant.
QUICKSILVER MINES IN THE COUNTIES
OF CALIFORNIA.
COLUSA COUNTY.
Central Mine. — Sulphur Creek District. Empire Consoli-
dated Quicksilver Company, owner; R. A. Boggess, general
manager, Sulphur Creek, Colusa Count}'. Consists of the
Central, Dewe}^ and Little Giant claims, in Sec. 29, T. 14 N.,
R. 5 W. [See Report State Mining Bureau of Cal., XI, page 185;
XII, page 359.] This mine covers a small triangular territory
on the left bank of Sulphur Creek, and is traversed bj^ a ledge
with a northwestern strike, on the contact of a decomposed
rock, probably serpentine, and shales in which some ore was
found near the surface.
Elgin Mine. — Sulphur Creek District. Elgin Quicksilver
Mines, owner; C. F. Humphrey, president. No. 137 Mont-
gomer}' street, room 15, San Francisco. In Sec. 13, T. 14 N.,
R. 6 W. [See Report State Mining Bureau of Cal., XI, page
182; XII, page 359.] The mine is situated near the head of
Sulphur Creek, and is at present idle. The main tunnel is
caved in 120 feet from the entrance. The ledge matter is a
tuffoid very highl}' impregnated by sulphur, and decomposed.
The entire territory covered by this mine is so highly impreg-
nated by sulphur that attempts have been made to distill sul-
phur from the rock. Another tunnel, 60 feet below the main
tunnel, is also caved in; hot water, very high in sulphur, is
flowing out of it. A number of shallow openings on the line
of the croppings show on the dump some cinnabar-bearing
material. The excessive heat in the mine interfered to a certain
extent with its operation. Some quicksilver was, however,
made in a lo-pipe retort furnace belonging to the property.
Empire Mine. — Sulphur Creek District. Empire Consolidated
Quicksilver Company, owner; R. A. Boggess, general manager,
vSulphur Creek, Colusa County. This consists of four claims —
Empire, Hidden Treasure, Mercury King, and Mercury Queen.
44 QUICKSILVER RESOURCES OF CALIFORNIA.
In Sec. 28, T. 14 N., R. 5 W. [See Report State Mining Bureau
of Cal., XI, page 186.] There are several drifts and open cuts
on the propert)', but none showing any ore body of conse-
quence. The company is now sinking a vertical shaft in the
northwestern part of the propert}'.
Manzanita Mine. — Sulphur Creek District. Manzanita Gold
Mining Company, owner; G. V. Northey, lessee. Sulphur Creek,
Colusa County. In Sec. 29, T. 14 N., R. 5 \V. [See Mon.
XIII, U. S. G. S., page 367; Report State Mining Bureau of
Cal., X, page 160; XI, page 184; XIII, page 126.] This mine
was opened about 1865, but was worked onl}' for gold until
1892, when it was also worked for quicksilver, and up to lately
mostl}^ by surface work and short drifts. The rocks of a large
part of the territor}' covered by this mine consist of sandstones
and shales, intersected by narrow quartz seams, containing
gold, sometimes associated with cinnabar; these seams had
occasionally very rich spots, but as they are very thin, and
separated by wide blocks of barren country rock, their work-
ing was not very profitable and could onh- be carried on at all
by surface cuts, etc. The deposits occur on both sides of
Sulphur Creek ; on the west side of the creek the formation is
sandstone; on the opposite side of the creek it is more shaly.
In both places, extensive old works can be seen at and near
the surface. Bej-ond this surface zone the shaly country rock
east of the creek is barren. Farther down along the creek, on
the same side close above the mill, the sidehill consists of a
white rock, evidently the country rock leached by waters
coming from sulphur springs formerly situated higher up the
hillside. This leached material carries both gold and quick-
silver. The leaching process is, however, only superficial, and
the mineralization must be due to the action of the same
waters, for the countr}^ rock past this zone of leaching has
proven to be barren. At present the gold deposits are not
worked. The work is confined to the quicksilver deposit on
the northeastern part of the Manzanita claim, where the ore
carries only quicksilver and no gold. The shaft is on the top
of a knoll, at an elevation of 475 feet above Sulphur Creek.
A ledge of conglomerate, from 20 to 30 feet wnde, of the same
nature as the conglomerate now forming in the bed of vSulphur
Creek, crosses the hill in a northwesterly direction, and on the
southeastern sidehill siliceous sinters are found.
COLUSA COUNTY. 45
In the mine near the shaft a whitish friable material (leached
sandstone) carries sensible amounts of cinnabar. The ledge is
very winding in both strike and dip; the accompanying gouge
is also very irregular. The hanging-wall shale is in places
altered to a whitish material ver}^ similar to that above men-
tioned. The ledge material, especially in the lower 150-foot
level, is principally chalcedonite. In places conglomerate is
found on the foot wall of the ledge, but it is doubtful if the
real foot wall has been reached. This deposit shows plainly
that it is the result of deposition out of solfataric waters, as
well in the ore body as by their action on the adjacent rocks.
To the west of the deposit lies a belt of limestone, adjoining at
the west to a belt of conglomerate.
In the old workings are found some phenomena, which have
a bearing on the genesis of cinnabar ores. In an abandoned
tunnel, on walls which originally showed no signs of cinnabar,
a great amount of sulpho-salts is forming, accompanied in
places with cinnabar, generally as a coating of the wall, but
occasionally successive layers of silica have been found inclos-
ing a thin seam of cinnabar. As proof that this cinnabar for-
mation is going on at present, pieces of barren country rock
lying on the floor have been coated with cinnabar on the face
touching the wall similarly coated, while no signs of cinnabar
can be found on any other face, nor on any similar rock not in
contact with the wall. The cinnabar must hence have been
derived by exudation out of the wall rock. The tunnel is
perfectly dry, and the only water found therein on the floor is
some seepage from the surface after heavy rains, this cinnabar
formation taking place at a very shallow depth.
The reduction works of the Manzanita mine are specially
interesting, as the quicksilver ores are successfully concen-
trated, and the concentrates treated in retorts at a sensibly
reduced cost per ton of ore treated. [See chapter on Metallurgy.]
Wide Awake Mine (Buckeye).— Sulphur Creek District. W. H.
Martin, Crocker Building, San Francisco, and A. A. Gibson,
Sulphur Creek, Colusa Count5^ owners. In Sees. 28 and 29,
T. 14 N., R. 5 W. [See Report State Mining Bureau of Cal.,
XI, page 187; XIII, page 594.] The main workings consist
of a vertical shaft 500 feet deep, with some short drifts. This
shaft is now filled with water above the first level. Near the
46 QUICKSILVER RESOURCES OF CALIFORNIA.
northwest end of the claim is an open cut with some short
tunnels and winzes. Rich ore pockets have been worked out,
but do not seem to continue in any direction. The mine is
equipped with a very fine reduction plant consisting of a 24-ton
fine-ore furnace, which has, however, been scarcely used.
LAKE COUNTY.
Abbott Mine. — Sulphur Creek District. Empire Consolidated
Quicksilver Mining Company, owner; R. A. Boggess, general
manager. Sulphur Creek, Colusa County. Includes the Abbott
and Disturnell mines. In Sees. 30, 31, and 32, T. 14 N.,
R. 5 W. [See Mon. XIII, U. S. G. S., page 368; Report State
Mining Bureau of Cal., XI, page 239; XII, page 360; XIII,
page 595.] This mine was discovered in 1862. In 1870 a
furnace of a daily capacity of 10 tons was erected and operated
until 1879. The mine was idle from 1879 to 1889. In 1899
the property was equipped with a 40-ton Hlittner & Scott
W. , 8
Fig. 3. Abbott Mine, Lake County— Section over the serpentine.
furnace. The total production has been about 30,000 flasks.
Including the old works there are 15,000 linear feet of shafts
and drifts. The deepest working is 350 feet below collar of
the Boggess shaft. This mine lies on the southwestern con-
tact of a serpentine belt, strike northwest, with a shale country
rock, occasionally sandstone. The serpentine varies in width
from a few hundred feet to a quarter of a mile, and is about*
2>^ miles long. To the northeast is a belt of sandstone, rather
narrow in the southern portion, but widening rapidly going
northward. [See map of Sulphur Creek District.] The ser-
pentine is interstratified with beds of shales and sandstone [see
Fig- 3 — a crosscut on the road from the Abbott mine to
Sulphur Creek] ; the same alternations are found underground.
For instance, near the intersection of the Reardon tunnel
and the first level [see Fig. 4]; near the Boggess shaft in the
first level, where two serpentine ledges have been exposed [see
Fig. 5 J; in drift II of the old works [see Fig. 5], etc. To the
LAKE COUNTY.
47
west of the serpentine lies the body of brecciated tuffoid —
more especially described in the general description of the
Sulphur Creek district. The map of the mine workings indi-
cates that they follow generally the line of contact of the
tuffoid, wnth the shales lying west thereof. At some places,
as at the intersection of the Reardon tunnel and the first level
[see above], serpentine is found west of this contact. There
is no doubt that the same alternations of serpentine and shales
take place east of the territory at present opened. The exten-
sive slides found at the surface in Disturnell Caiion, and the
reverse dip found, the rocks having been tilted over by the
pressure of the sliding material, lead to the expectation of
irregularities in the un-
derground formations.
Near the Boggess shaft
this is ver}' clearly illus-
trated. The shales west
of the serpentine contain
some hydrocarbons. In
places petroleum is
found; in others, gases
of light inflammable hy-
drocarbons emanate from
the rock, or bubble up
through the water. A
few feet southeast of the
end of the Reardon tun-
nel in the first level is a mmeral spring containing carbonate
of magnesium, calcium, sodium, and lithium, and also some
sulphur compounds. The cinnabar ore forms in these bands
of serpentine, more especially in close proximity to the tuffoid;
exceptionally the ore is found in the shale. The gangue is
generally strongly crushed opaline. Metacinnabarite occurs
occasionally, but no native mercury has as yet been found.
The cinnabar is disseminated through the crushed opaline,
partly as face metal, but also in seams and pockets. The ore
zones contain a great amount of iron sulphides, in varying
quantities, rendering it very difficult to regulate the temper-
ature in the furnace. Very little gouge is found between the
ore bodies and the walls. The ground in the ore zones and
in the shales is often swelling, but the tuffoid stands very well.
Fig. 4. Abbott Mine— Plan near inter-
section of Reardou tuuuel and first
level .
48 QUICKSILVER RESOURCES OF CALIFORNIA.
In the lower 250-foot level at the Boggess shaft, an ore bod^'-
was found, averaging 30 feet in width and 1 50 feet long, which
pinched out in the intermediary level 50 feet above, reappear-
ing, however, in the upper 150-foot level. In the intermediary
level, 140 feet from the shaft, 50 feet of fair ore was found.
In the first (upper) level, two ore bodies were followed, and a
crosscut is started at the southeast end of the lower level to
cut the more easterly ore body. [See Fig. 5.]
The first level has been driven over 1500 feet, largely in the
hanging-wall shales, to find the ore bodies existing in the
northwestern part of the Lightner level, about 65 feet above
the first level. Two ore bodies, marked A and B, were found
and stoped. Near A, a shaft is sunk from the first level to tap
this ore body below, to a depth of 130 feet. The ore bodies
opened farther east by the lyightner level have not as yet been
reached by the first level. The territory between a point
250 feet west of the Boggess shaft and A, a distance of about
1000 feet in an air line, below the level of the collar of the
shaft, is practically unexplored ground; old surface workings
indicate that such exploration might lead to a discovery of
workable ore bodies.
The mine is equipped with a 48-ton Scott furnace. The ore
is dried on a special drier located between the crusher and the
furnace, having its own heating furnace.
The Anderson Prospects. — Mayacmas District. In Sees. 25 and
35, T. II N., R. 8 W. Owners, the Anderson family, Anderson
Springs, Lake County. On the ridge between Bear Creek and
the south fork of the Putah, in section 35, about half a mile
south of Anderson Springs, a seam of good cinnabar ore has
been to some extent opened up in a very much decomposed
sandstone. About one quarter of a mile southeast of Ander-
son Springs, in Sec. 25, T. 1 1 N., R. 8 W., at an elevation of 300
feet above the springs, the formation is strongly saturated with
sulphur, which has thoroughly decomposed the country rock,
wherefrom its local name of Sulphur Bank. The upper part
consists of thin, flat beds of quartzose rocks interbedded with
clay seams (possibly a series of chert beds, like the ledge mat-
ter of the Great Western, but too decomposed to be absolutely
classified). The quartzose rock carries on its fracture faces
cinnabar; when broken it proves to contain a great amount of
LAKE COUNTY. 49
iron sulphides. Its structure would indicate that the two
metallic sulphides were not deposited simultaneously. [See
1 6th Ann. Rep. U. S. G. S., Part II, page 448, 3d line from top.]
The softer decomposed clayey material does not contain any
cinnabar; this material was probably decomposed by the action
of the waters highlj^ charged with sulphur on the less compact
seams. This sulphur deposition must be of a different period
from that of the sulphides. Below these beds lies thoroughly
decomposed sandstone, having a nearly vertical bedding,
wherein lies a 2-foot seam of quartzose material, similar to the
more compact part of above described beds, standing parallel
to the dip of the inclosing sandstone and carrjdng some cinna-
bar. All the water at this Sulphur Bank is cold, while a
quarter of a mile distant are the hot sulphur springs and blow-
holes, from which hot sulphur vapors emanate, without anj'
formation of cinnabar ore.
Baker Mine.— Clear I^ake District. S. T. Palstine, Lower
Lake, Lake County, owner. In Sec. 16, T. 12 N., R. 6 W.
[See Mon. XIII, U. S. G. S., page 368; Report State Mining
Bureau of Cal., X, page 67; XII, page 360; XIII, page 595.]
Consists of the Baker and Trade claims. This mine lies on
a belt of serpentine cutting through the sandstones and prob-
ably abutting against the basalt bounding Soda Creek Valley
to the west. The lower tunnel crosscuts the formation, and as
the slope of the hill is very fiat, it gains very little depth. The
first 140 feet are in ver}' tough black clay, then 20 feet of serpen-
tine, when the ledge is reached, along which they have drifted
for 250 feet. In a stope 20 feet high, the seams have been
partially filled with quartz, upon which have been deposited a
coating of iron pyrites, which are coated with metacinnabarite.
Cinnabar also forms in the serpentine associated with iron
pyrites. Farther on in the drift it forms in the fissures and seams
of serpentine, and is to a less degree associated with iron; yet
throughout the entire mine iron occurs verj- prominently in
association with cinnabar and metacinnabar. About 800 feet
north of this tunnel is a tunnel, course about north, 75 feet
long. The ledge matter is an opaline silica, carrying cinnabar
and iron pyrites, entirely different from that in the first named
tunnel where the gangue is tjuartz. A little southeast of this
tunnel and about 25 feet lower, another tunnel runs about east
4— OR
50
QUICKSILVER RESOURCES OF CALIFORNIA.
at right angles to the preceding, crosscutting the formation.
This tunnel is caved in, but judging from the material on the
dump it has reached the ledge. About 300 feet northwest of
this tunnel and 30 feet lower, a third tunnel has been run
S. 54° E., for 235 feet; then S. 24° E., 26^/^ feet to the opaline
ledge, where it is connected by a winze with the end of the
former tunnel; the ledge is about 25 feet wide. To the north-
west of these works a strong mineral spring is forming quite
a large mound on the hillside. The mine is equipped with a
lo-pipe retort furnace.
The Big Injun Group* — Mayacmas District. In Sec. 2, T. 10 N.,
R. 8 W., and Sec. 35, T. 11 N., R. 8 W.— on both sides of
y
f^ t' £> ay'yn C ly ^2
J?^
^«/A
r^r
1?,^yrfy.,.
fro<ffi/'rt.qt
Fig. 6. Big Injun Group, Lake County.
Bear Creek. Consists of two claims, the Big Injun and the
Digger Injun. The property is located on a very irregular and
disconnected line of croppings, showing only over a short dis-
tance south of Bear Creek, and apparenth" faulted or displaced
in the gulch through which that creek flows. [See Fig. 6.]
The country rock is serpentine and sandstone, very much mixed.
On the south side of the creek only surface indications of cin-
nabar are found. On the north side, cinnabar ore has been
found in man^^ shallow openings; in one, 3 inches of good
cinnabar ore is disclosed in a quartz seam in the opaline rock
over a length of 15 feet, but nothing assuring permanency in
depth has yet been developed.
[Since writing the above, these claims have been segregated.
The Big Injun belongs to the New Phoenix Mining Company,
LAKE COUNTY.
51
and the Digger Injun to the Congress Mining Company.
Theo. A. Bell, president, Behlow Building, Xapa.]
Chicago Mine (Ural). — Mayacmas District. In Sec. i, T. lo N.,
R. 8 W. About half a mile west of the Wall Street mine, and
nearly at the head of Dry Creek. [See Report State Mining
Bureau of Cal., XIII, page 595.] Owners, U. G. Schreves, of
Mirabel, Lake Count}', and others. In a large open cut, from
which former owners have taken 125 flasks of quicksilver.
PHuTu Xu. 1. CHICAGO PLANT.
with a short drift and a shaft 12 feet deep, is a ledge of hard
opaline rock, with only a little cinnabar in the cross fissures,
having a strike X. 23" W., and a dip to the southwest about
60°. This is overlaid by a seam carrj-ing cinnabar and also
some native mercury, in turn overlaid by one foot of softer
ledge matter carr^'ing fair values in cinnabar and native
mercur}-; then comes about 4 feet of more or less decomposed
serpentine, and then the serpentine hanging wall. The foot
wall is probably serpentine, but has not been uncovered. [See
Fig. 7.] A lower tunnel, 65 feet below the open cut, 80 feet
52
QUICKSILVER RESOURCES OF CALIFORNIA.
long, has a long stope 40 feet high to the surface and at the
breast a winze 16 feet deep; both on the same seam, which
here has a metal- carrying zone 3 feet wide, showing no native
mercury. [See Fig. 8.] A very crooked crosscut tunnel, 60
feet lower down the hillside, has not reached the ledge.
3 yy. I
Fig. 7. Section of Chicago Mine.
Fig. 8. Section of Chicagfo Mine.
Great Western Mine* — In Sees. 16, 21, and 22, T. 10 N., R. 7 W.
Owner, The Great Western Quicksilver Mining Company, E. W.
Newhall, president, Nos. 309-311 Sansome street, San Fran-
cisco; John Andrews, superintendent, Quicksilver, Lake Count}'.
[See Mon. XIII, U. S. G. S., page 35S; Report State Mining
Bureauof Cal.,XI,page64; XII,page36i; XIII,page595.] The
Great Western mine was opened in 1873, and has been a con-
stant producer since 1 874. The total production is about 90,000
flasks. There are about 18,000 feet of drifts and 11 50 feet of
shafts in the mine; the greatest depth of the workings is 750
feet. This mine is situated about two miles northwest of the
Mirabel and Bullion mines. The serpentine belt in the inter-
vening space is very wide and prominent, but as yet no work-
able cinnabar deposits have been discovered therein, nor on its
contact with the eruptives forming the main ridge northwest
of INIount St. Helena. Whether the latter are onl)- lava flows
from the igneous masses forming IMount St. Helena, or form
part of these masses, has not j'et been determined. At and
near the Great Western mine the serpentine belt is much nar-
rower, being confined between a wide sandstone formation to
the east and the above-mentioned bod}' of eruptive rocks.
The present workings are southeast of those in operation
54 QUICKSILVER RESOURCES OF CALIFORNIA.
when Dr. Becker examined the mine [see Mon. XIII, U. S. G. S.] ,
which explains some differences between the two descriptions.
The general strike of the ore body is northwest, with a south-
western dip of about 70°. The foot wall is a very hard sedi-
mentary rock altered by silicification, locally called greenstone.
The hanging wall, at least at the surface, is serpentine. The
ledge matter is formed by a series of thin beds of chert, having
their bedding planes
^^^'\^k.^^~-~)>-/ ^ parallel to the strike of
the ledge and interstrat-
ified with clay seams.
This chert is locally
called quartzite. The
dip of the serpentine is
flatter than that of the
ledge matter, and the
\- intervening, widening
S". vV space is filled with black
Fig. 9. Cross-section of Great Western Mine. Sita. [OCe -Tig. 9-J
The main working shaft
is sunk vertically in the foot-wall greenstone, and is on the
600-foot level, 340 feet northeast of the ledge.
The ore forms in the chert ledge, in a very irregular manner;
generally in the seams, and as face metal in the fractures of
the chert, but in the richer parts of the ledge disseminated
through the chert itself, associated with iron pyrites. The ore
bodies occur very irregularly in this chert zone, and the only
available indication for the occurrence of pay ore is the fact
that the mineralization is in general the strongest in those
parts where the chert beds have been more or less crushed.
The ore forms very seldom in the serpentine, but some bunches
of very hard and rich ore have been found in the serpentine,
without, however, any continuity. The black gouge is less
clayey and less foliated than generally in these ore deposits.
The increase in width of the hanging-wall gouge in depth is the
reason that no serpentine is uncovered in the lower workings;
and as no crosscuts have been run through the gouge to the
hanging-wall country in the lower levels, the persistency of the
serpentine in depth is not established. On the 600-foot level a
body of good grade ore, over 200 feet long and 50 feet wide, has
been opened up, which continues upward to about 70 feet
LAKE COUNTY. 55
above the 500-foot level. A "horse" has come in, and throws
the ore body somewhat out of its course, so that it has not yet
been reached in the 700-foot level. A drainage tunnel, 2200
feet long, runs through the foot-wall material, connecting with
the 500-foot level. This tunnel crosses some very narrow belts
of serpentine, but passes mainly through sandstone, until at
about 1 200 feet from the entrance it reaches a belt, 500 feet
wide, of decomposed, impervious shales, next to which lies the
foot-wall greenstone, about 450 feet wide, which is more or
less decomposed near the ledge, but at a distance of a few feet
therefrom becomes very hard and compact, and carries con-
siderable iron pyrites. [See Fig. 10.] This greenstone has
certainly not the appearance of being the source of the cin-
nabar, as the sandstone at Oathill, ^tna, etc. The formation
Fig. 10. Section over the Great Western Mine.
shows great displacement and distortion and great bowlders
of the neighboring series are found imbedded in the rock,
indicating strong dynamic action. On the strike of the ledge
ore is at present only extracted from one ore shoot, but the
company is doing considerable underground prospecting work
to find reserves for future development. The ore is treated in
a Litchfield furnace of 50 tons capacity.
Helen Mine (American).— May acmas District. In Sec. i,
T. 10 N., R. 8 W. About half a mile south of the Wall
Street mine, in the upper part of Dry Creek basin. Owner,
Andrew Rocca, Middletown, Lake County. [See Mon. XIII,
U. S. G. S., page 375; Report State Mining Bureau of Cal., XII,
page 362.] This mine is at present the only one in the Dry
Creek basin which produces quicksilver. It lies very close to
the tufas of Pine Mountain. The vein matter is a mixture of
opaline rock and serpentine, containing numerous inclusions of a
black flinty rock. The strike of the ledge is about due east and
west: its dip underground southerly, rather fiat, 30° to 40°.
56
QUICKSILVER RESOURCES OF CALIFORNIA.
The ledge lies at the contact of the sandstone and serpentine
[see Fig. ii], and can be readily traced on the surf ace for quite
a distance. In places the ledge crops out boldly above the sand-
stone, showing occasionally the cla}^ gouge, weathered to a
white color, indicating that the black color is principalh- due
to iron, probably in the form of mono-sulphide. At the north
end of the claim, eruptive rock (probably basaltic) shows on
the surface near the hanging w^all, but as no eruptive rock has
as yet been found in the underground workings, this may be a
flow from Pine Mountain. The cinnabar is accompanied by a
great amount of iron sulphide; it forms mostly in the fissures
and cracks of the vein filling, sometimes forming seams of
solid cinnabar an inch or more wide. The strike of these cin-
FiG. II. Cross-section of Helen Mine, Lake County.
nabar seams is parallel to the general strike of the ledge. In
the ore shoot the vein filling is less compact on the foot wall,
and the cinnabar seams are in places several inches wide, the
cinnabar besides permeating the entire rock. A gouge seam
separates this richer ore from the overlying relatively poorer
ore, which seems to indicate a movement during the period of
metal deposition, the gouge seam localizing the latter deposition.
[See Fig. ii.] The ore shoot, in fact, as far as at present
opened, shows cinnabar in nearly every fracture plane. The
ledge is reached by a crosscut tunnel, running nearly south,
through the foot-wall serpentine and driven to the hanging-
wall sandstone, which it reaches at a distance of 347 feet, with
140 feet of backs. The ledge as cut by the tunnel is 120 feet
wide, of which 100 feet is ore-bearing. The ore shoot has been
developed along the strike over a length of 80 feet. At the
breast of the tunnel a vertical shaft is in process of sinking,
which has cut through the vein and is in the foot-wall ser-
pentine. A lower tunnel, running about parallel to the one
LAKE COUNTY. 0/
above described, 1300 feet long, has not yet reached the vein,
due to its flat southerly dip.
A lo-retort plant, with a daily capacity of 1500 pounds of
ore, is in operation to test the value of the ore mined. The
great amount of iron sulphides carried by the ore necessitates
a very slow treatment, only one charge being treated per
twenty-four hours.
Jewess Mine. — Majacmas District. In Sees, i and 12, T. 10 X.,
R. 8 W.; Sees. 6 and 7, T. 10 N., R. 7 W. Some work has
been done on croppings of the same character and probabh'
belonging to the same body as those on the Wall Street mine,
on the opposite or southwest side of Dry Creek. These crop-
pings appear to be barren. A tunnel, run about 75 feet lower
down the sidehill, has caved in, but the dump shows no sign
of ore. Judging from common report no ore has ever been
taken out of this propert}'.
King of All Consolidated Group. — Clear I^ake District. Owners,
D. Jones, Xo. 137 Montgomery street, San Francisco; W. G.
Temper, Lower I^ake, Lake Count)^ In Sees. 29 and 32,
T. 12 N., R. 7 W. The group consists of the King of All,
Trejon, Cinnabar Queen, and Eagle Bird claims. This mine
is situated on a belt of serpentine, having a general northwest
trend. Bad Cailon Creek runs through this property and cuts
through the serpentine to the underlying schist. The lower
tunnel, a little above the bed of the creek, is in serpentine.
Its direction is nearly west. At about 100 feet from the mouth
a side drift is run in a northwesterly direction on a spur, with
a small stope showing the serpentine walls. The tunnel
passes two other spurs, and at 150 feet reaches what is con-
sidered the main ledge, which has a northwesterly course, with
dip nearly vertical. The tunnel is run 12 feet farther, the
breast being still in ledge matter. There is so much fire damp
in this mine that, as the air blower could not be used, it was
too dangerous to break any ore; hence the character of the
ledge matter could not be determined. The wall rock is in
places strongly decomposed, showing the action of solfataric
waters. To the northeast of the serpentine lies a large body
of tufas and volcanic bowlders, and about a mile north of the
King of All mine is Howard Springs, a region of ver>- strong
solfataric action, containing within a very small area forty-two
58 QUICKSILVER RESOURCES OF CALIFORNIA.
mineral springs, some hot, others cold, and of the most vary-
ing chemical composition. It is claimed that in the waters of
one of the springs, mercurial salts have been detected. The
ore composition in the King of All mine has most probably
some connection with the solfataric action at these springs.
The igneous rocks above alluded to belong probably to the
system of the Mount Konockti eruptives. That they are in
some way connected with the genesis both of the mineral
springs at Howard Springs and of the cinnabar ore deposits
at the King of All mine, appears very probable.
Lucitta Mine.— Clear Lake District. G. W. Pardee, E; G.
Pardee, B. R. Parrott, Lower Lake, Lake County, owners. In
Sees. 20 and 21, T. 13 N., R. 8 W. This property', on the
southern slope of Mount Konockti, or Uncle Sam, consists of
four claims: the Lucitta, Lucitta Extension N., Lucitta Exten-
sion S., and Lucitta Extension W. [See Fig. 12.] The work,
however, has been concentrated in the southern half of the
Lucitta claim. The entire formation is igneous, bowlders of
andesites being prominent, the intervening material being a
decomposed tufa bleached by solfataric action. White beds of
leached metamorphic shales are found in these igneous masses^
and occasionally bodies of cla3\ In the lower tunnel (No. i)
cinnabar has been deposited on the face of the bowlders and
in the decomposed tufa, occasionally forming bunches of ore,
apparently of good grade. Such an ore body is found in the
first crosscut [see Fig. 12]. In the middle tunnel (No. 2) the
country- rock is the same as in the lower tunnel. The best ore
is found in the side drift, 60 feet long, running southeast and
branching from the southwest crosscut near breast. Past the
crosscut the drift enters into very hard, barren material. The
ledge matter appears to be a metamorphic bleached shale, occa-
sionall}- gritty; while very much broken up, it shows a tendency
to a stratification dipping southwest. The material in the
upper tunnel (No. 3) is principally decomposed tufa, carrying
some ore. The main drift has caved at 100 feet from the
mouth, and two cur\'ed drifts have been run to reach the terri-
tory past the cave; the left-hand drift shows good ore in the
breast. The plan shows that this ore lies above that opened
in tunnel No. 3; hence this ore body is probably continuous for
a depth of 80 feet. A little higher up the mountain is an open
LAKE COUNTY.
59
pit, 25 feet deep. The walls are formed entirely by decomposed
and leached tufa, with bunches of cinnabar ore all through the
material. Similar bunches of cinnabar ore are found in the
decomposed tufa on the hillside all over the claim, but onh^ in
the middle tunnel a regular ledge is exposed, which, from the
appearance of the breast of the left-hand drift in the upper
tunnel, is probably covered up by the cave. A small prospect
Fig. 12. Lucitta Mine.
opening near the dump of tunnel No. 2 shows solfataric action,
and formations very similar to those at the surface at Sulphur
Bank. The mine is equipped with a lo-pipe retort furnace.
Middletown Mine. — Mayacmas District. In Sec. 7, T. 10 N.,
R. 7 W. ; about half a mile southwest of the Jewess. Owner,
W. H. Parsons, Middletown, Lake County. An outcrop
similar to that on the Jewess and Wall Street, on which some
work has been done on the top of the ridge, showing a small
amount of cinnabar through the ledge matter. The countr}^
rock is nearly all serpentine. About 90 feet lower a tunnel
60 QUICKSILVER RESOURCES OF CALIFORNIA.
35 feet long shows very hard, cherty material, carrying some
specks of cinnabar. A crosscut tunnel 50 feet long is started
about 200 feet below the upper croppings in very decomposed
country rock, probably schist.
Shamrock Mine* — Clear Lake District. Owners, J. C. Ansel,
Sulphur Creek, Colusa County; J. B. Mason and Swift,
Knoxville, Napa County. In Sees. 14 and 23, T. 13 N., R. 6 W.
It consists of the Shamrock and Shamrock Extension claims.
The mine is on Rocky Creek, a tributary of Cache Creek, in a
very extensive belt of serpentine, which to the southeast
extends to the Knoxville district. Rocky Creek makes a sharp
curve on the ground of this mine, forming a narrow peninsula,
about 100 feet above the bed of the creek, which has been
crosscut by two tunnels; the one starting from the up-stream
side has caved in and is inaccessible; the other, on the down-
stream side, runs in a course S. 60° W., first through 125 feet
of shales, then 75 feet through decomposed serpentine and
sandstone bowlders. At this poin^ drifts have been run
N. 68° W., and S. 68° E., mainly in gouge; but little ore can
be seen in these drifts.
Standard Quicksilver Company. — Mayacmas District. Z. W.
Christopher, superintendent, Mirabel, Lake County. This
company owns a large tract of land in the neighborhood of
Mirabel, on both sides of St. Helena Creek. [See Mon. XIII,
U. S. G. S., page 375; Report State Mining Bureau of Cal.,
VIII, page 325; XI, page 64; XII, page 360; XIII, page 595.]
The Mirabel, formerly the Bradford, which was opened in
1887 and at the time was a great producer, on the western
bank of St. Helena Creek, is considered worked out by the pres-
ent owners. It was abandoned in 1897, and has filled with
water. The total production of this mine was 30,590 flasks;
the greatest depth of the workings is 500 feet; 22,500 linear
feet of drifts were driven and 750 feet of shaft sunk. The
company has as yet not succeeded in developing any workable
deposits east of St. Helena Creek. On the west side, a little
to the north of Mirabel, in Sec. 23, T. 10 N., R. 7 W.,the com-
pany opened up the Bullion mine, nearly on a line running from
the Mirabel to the Great Western mine. This mine is located
on a ledge having a general strike about north (N. 8° \V.)
and dipping to the east. The dip of the ledge, rather steep
LAKE COUNTY.
61
near the surface, flattens out with depth, and consequently
the vertical shaft started in the hanging-wall sandstone
cuts the vein and enters the foot-wall serpentine. [See
Fig. 13.] The nature of the hanging-wall material, meta-
morphic sandstone, was ascertained while sinking the shaft;
against the vein lies a very wide belt of gouge, through which
no crosscut has been driven below the 450-foot level. The
ledge varies sensibly in width, but its average may be placed at
35 feet. The ore forms in ^ ,^^-
fissures running across the
vein, starting from the hang-
ing wall and feathering out
toward the foot wall; some-
times these cross fissures
occur close together and
then . form workable ore
bodies. This ore formation
would indicate a secondary
concentration of the mercury
from the sandstone; but
then the displacement which
caused the very heavy gouge
on the hanging wall must
have been posterior to the
ore concentration in the
ledge. Where the ledge is
barren, the opaline rock forming its filling is very compact.
The property is equipped with a 40-ton Hiittner & Scott
furnace, provided with a mechanical drawing apparatus, and
brick condensers provided with waterbacks.
Sulphur Bank. — Clear Lake District. Empire Consolidated
Quicksilver Mining Company, owner; R. A. Boggess, general
manager, Sulphur Creek, Colusa County. In Sees, i, 2, 3, 6, 8,
II, 12, 13, 17, 18, and 20, T. 13 N., R. 8 \V.,and Sec. 14, T. 13 N.,
R. 7 \V. [See Mon. XIII, U. S. G. S., page 254, etc.; American
Journal of Science, vol. XXIV, 3d series, page 23, et seq. ; Report
State Mining Bureau of Cal., X, page 238; XI, page 63; XII.
page 361; XIII, page 597.] The Sulphur Bank mine was opened
in 1875 and worked until 1883, during which period the Herman
shaft was sunk. Work was resumed in 1887 and continued until
Fig. 13. Section of Bullion Mine (Standard
Quicksilver Company).
62
QUICKSILVER RESOURCES OF CALIFORNIA.
1 897, during which period the Diamond and Babcock shafts were
sunk. In 1 899, work was again resumed and has been prosecuted
until the present time. The total production of the property has
been 92,000 flasks, the greater part being obtained from the sur-
face workings. This property has been extensively described and
discussed by several geologists, principally because it afforded
special occasion to study the relations between solf ataric waters
and the genesis of ore deposits. In Mon. XIII, U. S. G. S., a
very detailed geological map of the property is given.
PHOTO No. 3. WESTERN CUT— SULPHUR BANK MINE.
The deposit may be considered from two points of view:
the surface developments and the underground developments.
The surface developments in their present state give the im-
pression of an abandoned hydraulic mine, there being exten-
sive shallow cuts, more or less filled with bowlders of barren
igneous rocks. [See photograph of Western cut, Sulphur Bank
mine.] The igneous rock was determined by W. Jackson in
18S0 as augite-andesite, mainly because of the absence of
olivine; but in Mon. XIII, above cited, it is classified as basalt.
Sulphur Bank Mine.
-N .-'/p'c^'X-'-'
sp'
''vl«>jr
Stt'S
.<^^
^^'
I
LAKE COUNTY,
63
and the latter determination is generally accepted. These
basalt bowlders may be a flow from the craters, yet discernible
to the northeast of the bank, or may have been ejected from a
vent close to the bank, which has as yet not been uncovered.
Up to the present time this basaltic flow has been found every-
where overlying the altered sedimentaries. As the cinnabar
deposits are not restricted to the territory covered by the lava
flow at the Bank [see Fig. 14], and as most careful investiga-
tion has failed to disclose any cinnabar or mercury in the
undecomposed basalt, this basalt can not be the source of
the metal.
The upper crust of the lava deposit, to a thickness of a few
feet, consists of a white silica, the residue of the complete de-
composition of the basalt, by the combined action of the highly
-?a 3<i I fSouldt
arreL Si'rt.tt.rs
'3ac/^/< cCJ3^S« //i
Fig. 15. Sulphur Bank Mine— Elevation of Upper Wagon Spring Cut at (X).
sulphurous solfataric waters and the atmosphere, forming sul-
phuric acid (H.S + 40 = H.SO*), which decomposed all the
silicates in the rock and left the pure silica. Immediately
below the surface zone, where oxygen was not so abundantly
present, free sulphur was formed (H:;S -f O ^ H.O -f S). This
took place to such an extent that originally the property was
worked for sulphur. About 2000 tons of sulphur have been
extracted.
The basalt occurs in places as masses of bowlders, which
near the surface are surrounded by shells of decomposed
material of grayish color and very much disintegrated. Below
these bowlders and in places reaching very near the surface,
as in the bank of the Upper Wagon Spring cut [see Fig. 14 at
X and Fig. 15] and in the Apex cut, the basalt has a more or
less bedded form. When first uncovered, the basalt bowlders
have a rough surface; but when in contact with the atmos-
phere for a short time, their outer shell readily decomposes
64 QUICKSILVER RESOURCES OF CALIFORNIA.
and disintegrates, giving them a waterworn appearance. The
neighborhood of Sulphur Bank is at present a region of great
solfataric action, not so intense, however, as in the past. A
number of cuts have been run, covering a territory 2000 feet
long and See feet wide, and having a general northwestern
direction. These surface works are mostl}' in the territorj-
covered by the lava flow, but to the south, and especially to
the southeast in the Wagon Spring cut, near the Herman
shaft, the sedimentaries come to the surface. Iron, mosth' as
oxide, is extensively found in this surface zone; in places the
black coloring of the material is due to iron oxides. Sulphur,
as already mentioned, is also very prominent, in the forms of
free sulphur, metallic sulphides and sulphates, and free sul-
phuric acid. Hj'drocarbons, mostly in minute globules, are
also present. Mercuric sulphide (cinnabar) is one of these
metallic sulphides, and occurs in many places sufficiently con-
centrated in seams and pockets to form workable ore bodies.
In the bowlder zone it forms in the disintegrated material fill-
ing the interstices of the bowlders; in the bedded zone it
occurs in seams, which allowed the passage of the ascending
solfataric waters, and wherein the latter deposited the cinnabar
with a more or less gelatinous opaline silica.
Underlying the basalt are sedimentaries. It is greatly to be
regretted that the management of this property has not taken
pains to preser\-e geological descriptions of the underground
works, which are all caved in, except the Empire shaft, now in
progress of sinking. The latter is so tightly timbered, owing
to bad ground, that it ofiers no opportunit}' to study the forma-
tions through which it has passed. The following remarks
regarding the sedimentary formations are only fragmental and
are collected from dift'erent sources:
The sedimentaries consist of: the Cache Lake beds ( Quater-
nary- ) , conglomerates, sand beds, and argillaceous and calcareous
deposits, which are generally very friable and at Sulphur Bank
thoroughly decomposed by solfataric action. According to
Professors Le Conte and Rising these beds appear to be more
tilted to the east, near the Herman shaft, and nearer to the
volcanic vent or vents than westward near the Babcock and
Diamond shafts. Underlying the Cache Lake beds are the
Lower Cretaceous, Xeocomian rocks, prominently sandstones,
most highly metamorphosed. Professors Le Conte and Rising
LAKE COUNTY. 65
seem to assume that the Cache Lake beds belong to the same
period as these underl^dng sandstones, determined bj^ Becker
to be Neocomian. On the contact of the Cache Lake beds and
the metamorphosed sandstone is found a brecciated zone, which
in the neighborhood of the Herman shaft appears to be tilted
at a steep angle, dipping southward. On the line of cross-
section A B [see Fig. 14], the contact is also dipping south
between the Babcock-Diamond line and the Empire shaft, but
only at an angle of about 30°. [See cross-section C D.]
Taking low water in Clear Lake as datum, the depth of the
contact in the shafts is: Empire shaft, 185 feet; Babcock shaft,
100 feet; Diamond shaft, 90 feet.
The Quaternary beds are highly siliceous and interbedded
with strata of very loose material, acting as quicksand, disinte-
grated by the percolating solfataric waters. In the Wagon
Spring cut where they appear at the surface, the brecciated
zone, consisting of fragments of shale and sandstone inclosed
in a claye}' material, formed a channel for the ascending solfa-
taric waters, which deposited therein cinnabar and pyrites.
This deposit will be discussed hereafter in this chapter.
A great number of short tunnels, drifts, and winzes have
been run in the banks of the cuts, and shallow shafts have been
sunk in their bottoms, to excavate pockets of cinnabar ore. In
nearly every bank of the cuts formation of cinnabar is taking
place at the present time. Often, when breaking down the
cinnabar-carrying surface, no signs of cinnabar are found in
the uncovered surface. This formation of cinnabar, which can
not be an exudation product, may be explained by the fact
mentioned b}- Becker (Mon. XIII, page 260) that the waters
at the surface contain small quantities of mercuric sulphide in
suspension, but none in solution, caused b}' the presence of
ammonia. These suspended particles will be deposited on
arriving at the surface. In the Western cut a deposition of
cinnabar occurs, which, in the writer's opinion, can not be
explained except as a deposition from mercurial vapors. In
this cut a small shaft 12 feet deep was sunk, but had to be
abandoned on account of the peculiar gas occasionally occur-
ring in quicksilver mines, especially attacking the eyes of the
men, blinding them temporarily with intense suffering. (Some
claim this gas to be methane.) [See also Great Eastern Mine.]
5— QR
66 QUICKSILVER RESOURCES OF CALIFORNIA.
Near this shaft ver}- hot gases emanate from the floor of the
cut and form incrustations on a bowlder of basalt lying in the
proximity. These incrustations on the top of the bowlder show
signs of cinnabar, which can not come from any other source
than from these gases.
In the same cut not 20 feet interdistant, are two springs, one
cold, the other hot, from both of which gases are constantly
emanating, which would tend to indicate that the gases and
waters are not derived from the same source. The depth of
the surface workings has been limited by the water level. Shal-
low shafts prove that cinnabar occurs below the floor of the
cuts as well as in their banks; but the relation between the
cinnabar occurrence at the surface and that underground has
as yet not been clearly established.
The territorj^ developed by the underground workings does
not underlie that developed by the surface workings, except
for a slight portion near the Herman air shaft, and is much
more restricted than the surface workings. [See Fig. 14.]
Unfortunately all the old shafts have caved and are inaccessi-
ble. The Empire shaft, in process of sinking, has been started
with the purpose of reaching, by drifting, ore bodies presumed
to exist under the Western cut; these drifts will have to run
through the ground underlying the caved-in stopes of the
Diamond shaft. [See below.]
The Herman shaft is geologically the most interesting, as in,
these works connection might be traced between surface and
underground phenomena. The details available at the mine
are very deficient, but a description of the works in this shaft
in 1880 and 1881 is found in the above-cited article by Profes-
sors Le Conte and Rising, from which the following is quoted:
"The upper level, 210 feet, runs (in a course about N. 60*^ W. )
"from 70 to 80 feet in barren sandstone and shale, dipping
"about south, the rock being comparatively dry and cool; then
"cuts through a breccia, carrj'ing a great amount of hot waters,
"containing considerable alkaline sulphides, carbon dioxide,
"and hj'drogen sulphide; temperature, 160° F., with ver}' strong
"emanations of carbon dioxide. This breccia contained the
"ore. The level, of a total length of 232 feet, cut through this
"ore body and reached barren ground."
The plans of the works [see Fig. 16] show a second smaller
ore body, not mentioned in above description. Becker, who
LAKE COUNTY.
67
visited the shaft in 1887, states (Mon. XIII, page 263): "An
"important ore body was followed down; * * * the shaft
"is 417 feet deep, with seven levels. * * * This body has
"been worked out, and only the lowest portion was accessible.
"The small amount of ore remaining consisted of partially
"metamorphosed sandstones and shales carrying small stringers
"of cinnabar, quartz, and pyrite. I was not able to get satis-
f 6^
ML
^W
Fig. 16. Sulphur Bank Mine — Section and plan of Herman shaft.
"factor}' information as to the depth from the surface of the
"contact between the Lake deposits and the brecciated meta-
"morphic sandstones and shales."
The above quoted article of Le Conte and Rising continues:
"The lower level, 260 feet, reached the ore body at 136 feet
"from the shaft. The varying dips on the different levels show
"that the strata are very much broken up. The brecciated
"layer, which as in the Wagon Spring cut is composed of frag-
^^V >V^ Shale.
Cinnabar
ore.
68 QUICKSILVER RESOURCES OF CALIFORNIA.
"ments of shale and sandstone, forms also here the water
"channel. Where the ascending water is abundant, the matrix
"is hot mud; where the rock is drier, this has changed into a
"paste containing disseminated metallic sulphides, or into a
"regular indurated deposit from solfataric waters. The spaces
"between the fragments are sometimes only partially filled;
"the lining of the cavities is generally cinnabar, sometimes
"pyrites, or silica, or all of them; the silica grading from chal-
"cedonic into gelatinous. [See Fig. 17.] The ore deposit is
" not entirely confined to the breccia. Its form is ver}- irregular;
"sometimes ore bodies
"are separated b}- bar-
"ren rock, sometimes
"they enter the shat-
"tered sandstone, leav-
"ing the breccia. No
"free sulphur is found
" in the ore bodies. The
" irregularity' of the ore-
" bearing fissures shows
" that the shattering ef-
"fects were not confined to the brecciated strata."
Comparing this ore occurrence with that at the surface in
Wagon Spring cut, near the Herman air shaft, which is found
in a soft brecciated stratum several feet wide, consisting of
fragments of shale and sandstone with a matrix of blue clay
mud, through which hot alkaline waters at 125^ F., highly
charged with hydrogen sulphide and carbonic and boracic
acids, are ascending, and in which considerable cinnabar and
pyrites have been deposited, the conclusion is that both
deposits have probably the same genesis, though their relation
is not clearly established.
The following part of the quotation cited above from Mr.
Becker's work: "I was not able to get satisfactory information
* * * of the contact between the Lake deposits and the meta-
morphic sandstone and shale," indicates that in his opinion the
formation at the surface in Wagon Spring cut belongs to the
lake beds. No underground ore bodies have been found in
these beds, possibh^ due to the fact that these beds offered a
greater number, but more minute channels to the waters, and
Fig. 17. Sulphur Bank Mine— Ore
formation in Herman shaft.
LAKE COUNTY.
69
the ore deposition was subsequently less concentrated: for it
may be accepted as a fact that the cinnabar deposits at the
surface and underground belong to the same system of water
circulation.
From the accompanying section of the Diamond shaft [see
Fig. 1 8] it may be concluded that here the lake beds overlie
the metamorphic shales and sandstones [see also sections on
Fig. 14], rendering the assumption that such is the case in the
Herman shaft all the more probable. The material at the sur-
face in the Wagon Spring cut is so thoroughly decomposed
that it is impossible to decide this question by its study.
The accompanying sketch of the old works of the Diamond
shaft [see Fig. 18] shows the ore body in the metamorphic
sandstones underlying
the surface formations.
Judging from the plans,
the ore body was in
places 40 feet wide. It
is reported that at the
time the shaft collapsed
the lower level had not
reached the limits of
the ore body. Includ-
ing the results of the
workings of the Bab-
cock shaft (also col-
lapsed), the length of
this ore body may be
placed at 500 feet; but
it is doubtful if any of this ground will be available in the
future because of the collapse of both shafts, as this treacher-
ous ground is saturated clear to the surface with hot acidic
waters. Xo data are available to judge whether the ore
formed in a brecciated contact zone, or in fractures cutting
through strata; in other words, whether the ore bodies resem-
bled the upper part of the deposit in the Herman shaft, as
described by Le Conte and Rising, or the lower part, as
described by Becker.
The breccia in the Diamond and Empire shafts, judging
from dump samples, appears to be a fragmental sandstone
recemented by silica, which, being softer, offered more favor-
A7e/^pt7. ^.S/or^e^
Sulphur Bank Mine— Section of
Diamond shaft
70 QUICKSILVER RESOURCES OF CALIFORNIA.
able conditions for ore deposition than the more compact meta-
morphic sandstone. If, as it appears to do in the Empire shaft,
the formation becomes more compact in depth, the ore deposits
will probably accordingly decrease in value.
Summarizing, it may be stated that deposition from solfa-
taric waters is the prominent mode of ore formation, but that
mercurial vapors are present and probably play their part in
this process. The solfataric waters are highly charged with
active chemical agents, but the source from whence they derive
their mercuric contents is at present unknown; the igneous
bodies, however, to which the basalt surface flow belongs, are
certainly not the source thereof.
The increase in heat with depth in the Herman shaft is
worthy of note. At the surface, 128° F. ; at 200 feet depth,
160" F. ; at about 300 feet, 176° F. Assuming the surface heat
of 128° F., those at 200 and 300 feet depth, according to the
general rule of increase by static influence, would be respec-
tively 132° and 134° F. This shows that in regions of solfa-
taric action the increase in heat with depth is extremely rapid,
and that conclusions regarding physico-chemical phenomena
must take this rapid rate of increase into account, even for
zones of shallow depths.
The great heat, the chemical composition of the underground
waters and gases, and the character of the rock, render the
underground exploration of this property a ver}' serious under-
taking.
This property is equipped with four furnaces, of which one
is a Knox & Osborne 25-ton furnace, the others are Hiittner &
Scott furnaces, respectively of 40, 17, and 30 tons, and with a
furnace having nine q retorts.
Thorn Mine. — Mayacmas District. In Sec. 36, T. 11 N.,
R. 8 W. On the north side of Bear Creek, south of Anderson
Springs. Owner, D. H. Thorn, Anderson Springs, Lake
County. This prospect lies very close to the top of the ridge.
Near the surface some pockets of good ore were found, but
did not continue in depth. The underground works, 60 feet
below the upper works, show as yet no ore at all, and in the
upper works the ore bodies pinched out at a ver}- slight depth.
Utopia Mine.— Clear Lake District. In Sec. 25, T. 13 N.,
R. 6 W., about opposite Lakeport, near the east shore of Clear
LAKE COUNTY.
71
Lake. The Utopia Quicksilver Min-
ing Compan)', owner; M. S. Sayre, of
Lakeport, president. [See Report
State Mining Bureau of Cal., XIII,
P^ge 597-] The company is con-
templating opening this mine.
Wall Street Mine, — Mayacmas Dis-
trict. In Sec. I, T. lo N., R. 8 \V.
Owner, W. H. Parsons; postoflfice,
Middletown, Lake County. [See
Mon. XIII, U. S. G. S., page 375;
Report State Mining Bureau of Cal.,
XII, page 362.] The former owners
spent considerable mone)' in explora-
tion works, without satisfactory re-
sults. Their old workings are largely
caved in, the fur-
nace is destroyed
and its site prac-
tically obliterated.
In an old tunnel
(2440 feet eleva-
tion) [see Fig. 19]
there is a ledge
of hard siliceous
rock, carrying
some metal along
a seam, and pen-
etrating from that
seam into the
small fractures of
the rock, forming
a poorly mineral-
ized zone about
18 inches wide,
with a strike
northwest, and a
southwesterly
dip, which shows,
however, only
over a length of
40 feet, and about
50 feet along the
72
QUICKSILVER RESOURCES OF CALIFORNIA.
dip. This mineralized zone is apparently cut off to the east bj'
a body of hard, compact serpentine, and has not been found
past this point. Both walls are serpentine, and there is no
gouge on either wall. It appears as if a vein has cut through
the point of the hill, and only carried metal in the eroded
dome. The eastern branch directs toward the workings of the
Jewess, which have proven barren.
NAPA COUNTY,
Aetna Consolidated Quicksilver Mines. — Mayacmas District.
In Sees. 2, 3, and 4, T. 9 X., R. 6 \V. Owner, The .Etna
/JETN/l CON. MINES.
ONB MILE
Fig. 20. ^tna Consolidated Mines.
Consolidated Quicksilver Mining Company-, 70 Kilby street,
Boston, Mass.; B. M. Newcomb, Oathill, Napa County, Super-
intendent. [See Mon. XIII, U. S. G. S., pages 354, 371 ; Report
State Mining Bureau of Cal., XI, page 72; XII, page 362;
XIII, page 597.] This group of mines is situated at the
southeast end of the belt as at present developed. [See Fig.
20.] It comprises the Phcenix, Silver Bow, Red Hill. Star,
Pope, and Washington mines. These mines were formerly
74 QUICKSILVER RESOURCES OF CALIFORNIA.
large producers, but in the last few years have produced no
quicksilver. The property can hardlj' be described as lying in
^/ 9 oo'J
t^af-> ^/j/-a^£ ,
I itS'oo'J _
Tur- ri a./ A^' /.
-^/vr
Fig. 21. .5itna Consolidated Mines — Elevation at mouth of Tunnel Xo. 2.
James Creek canon [Mon. XIII, U. S. G. S., page 374], but
would be more properh' described as located on the northern
slope of a ridge running in a northeasterly direction from the
Twin Peaks and capped by lava.
■^v.
Ta//
Fig. 22. .Etna Consolidated Mines— Basalt dike. Silver Bow claim.
The serpentine in this region appears to be underlaid by
sandstone [see Fig. 21], being a break above tunnel No. 2 in
the Phoenix claim. Tunnel Xo. 7 runs toward a basalt dike,
which breaks through to the surface, and reaches the contact
at a depth of from See to 1000 feet. This dike shows at the
NAPA COUNTY,
75
surface for a length of about I ooo feet; the underground works
which run around the dike show it to be surrounded by sand-
stone. [See Fig. 22.] The basalt is cut of^ at the surface by
the same serpentine showing in Fig. 21 ; but from the fact that
the latter does not go through the sandstone, the surface
indications are not convincing that this basalt dike does not
connect with the main seat of eruption, having uplifted the
serpentine and broken through the sandstone. The tufa sur-
rounding the basalt is more siliceous and probably older than
the basalt. It overlies the sandstone but not the serpentine,
confirming the above supposition. The tufa overlying the
serpentine has prob-
ably been eroded.
For some reason, in
this region the tufa
is invariably found j
overlying the sand-
stone but not the
serpentine. In the
Star claim another
short dike of basalt,
about 100 feet long,
has been followed at
its contact with the
sandstone to a depth
of 600 feet.
The Washington
shaft disclosed a
boss of serpentine,
which carried a good body of ore, while in the sandstone but
little ore was found. [See Fig. 23.] In the Phoenix workings,
at tunnel No. 9, only sandstone was found underground in
the Red Hill claim, while the surface of that claim is almost
entirely covered by serpentine and its allied opaline rock; a
winze sunk from this tunnel follows a contact between igneous
rock and sandstone to a depth of 1000 feet.
All the sandstone in this neighborhood contains some cinna-
bar disseminated through it; but so far workable ore deposits
have only been found near the igneous rocks and the serpen-
tine, indicating a secondary concentration in connection with
the igneous rocks and the serpentine.
^^tna Consolidated Mines — Section of
Washington shaft.
76 QUICKSILVER RESOURCES OF CALIFORNIA.
The company is at present doing prospecting work, in order
to determine whether workable ore bodies can be found on the
contact with the large dike on the Silver Bow claim above
described. [vSee Fig. 22.]
Bella Union Mining Company. — This property is in Sees.
20 and 28, T. 7 X., R. 5 \V., one and a half miles south of
Oakville. [See Mon. XIII, U. S. G. S., page 377: Report State
Mining Bureau of Cal., XII, pages 364 and 365; XIII, page
599]
Boston Mine (formerly the Redington). — Knoxville District.
Boston Qviicksilver Mining Company, owner. B. M. Xewcomb,
general superintendent, Oathill, Napa County: J. B. Mason,
superintendent, Knoxville, Napa County. In Sees. 6 and 7,
T. II N., R. 4 W. [See Mon. XIII, U. S. G. S., page 284;
Report State Mining Bureau of Cal., XI, pages 69-72; XII,
page 363; XIII, page 599.] The Redington Quicksilver Min-
ing Company supposedly worked out the ground in the origi-
nal shaft and abandoned the works in 1882. In 1890 Mr.
McMillan started on a narrow seam of cinnabar several hundred
feet northwest of this shaft in the serpentine formation, which
upon development showed so profitable that the northwest
shaft was sunk and this territory worked until 1S98. The
present owners have reopened and retimbered the old shaft,
and by a systematic exploration not only found some good ore
bodies in the foot- and hanging-wall veins, but also opened up
large ore bodies in the serpentine lying in the inter\-ening
territory. This vein has supplied the majority of the ore
which the present company has passed through its furnace,
and shows at present large ore reserves. The result proves
again the great importance of systematic exploration work in
a quicksilver mine.
The ore bodies in this mine form in the same serpentine
which runs along the southwestern border of the mineralized
zone of the Manhattan mine. This belt extends for several
miles to the southwest, but, except at its contact with the Neo-
comian at Knoxville, does not contain a single ore body of any
consequence. The mineralized zone of the Boston mine has a
northwest strike, and dips at about 45° to the northeast. Its
cross-section is given in Fig. 24.
In the Neocomian sandstone, about 1200 feet northeast of
NAPA COUNTY. / /
the ore zone, some work has been done, confirming the fact
that cinnabar forms in the sandstones; tests of the latter taken
from various places indicate that cinnabar is disseminated all
through this lormation. Combining this fact with the absence
of cinnabar in the serpentine, even when in close proximity
to the igneous rocks in the Manhattan ground, and with the
fact that in the Boston mine the workable ore bodies are in
the serpentine, the suggestion offers itself that the genesis of ore
PHOTO No. 5. BOSTON QUICKSILVER MINK.
formation in this mine is similar to that in the ^tna mine —
secondary concentration of the ore disseminated in the sand-
stones connected in some way with the serpentine and igneous
rocks. While, as far as known, no igneous rocks are present
in this mine, basalt is known to extrude within half a mile
from it, and it is very probable that intrusions of igneous rocks
or laccolitic bodies may have influenced the concentration in
conjunction with the serpentinization process. This supposi-
tion finds confirmation in the fact that deposits from solfataric
springs can be traced from the Manhattan to the Boston mine.
78
QUICKSILVER RESOURCES OF CALIFORNIA.
The intense chemical actions which have undoubtedly taken
place in this zone, and the great amount and variety of sulphur
compounds found therein, indicate undoubtedly close connec-
tion with igneous actions, and can hardly be attributed exclu-
sively to the reducing agency of organic matter or ferrous salts
on waters carr^-ing sulphites or sulphates in solution. [See
Genesis of Ore Deposits, pages 34S-350.]
The mine is opened by two shafts. The original shaft, in
which the works are at present prosecuted, is on the southeast-
ern part of the mineral zone near the furnace. This shaft is
600 feet deep, but the lowest level at present in operation is at
390 feet. Below that level the works are under water. The
second shaft is 640 feet northwest of the furnace, and has been
sunk to a depth of 400 feet.
Fig. 24. Boston Miue — Section over the mineralized zone.
Footwall vein in opaline.
Narrow stratum of claj-.
Serpentinized breccia (20-40 ft.).
Silicified serpentine 100-200 ft. wide, inclosing
ore bodies forming the " serpentine vein."
Decomposed serpentine.
Hanging-wall vein.
Clay.
Shales 100-200 ft. ^de.
Sandstones carrs-ing some cinnabar.
The three parallel veins can be said to be inclosed in serpentine,
for the clay on the hanging-wall vein shows by its structure to
be decomposed serpentine. The gangue in the hanging-wall
vein is more or less decomposed opaline. That of the foot-
wall vein is also opaline, but much less decomposed. The ser-
pentine of the central vein is silicified. The ore forms in the
multitudinous seams traversing the serpentine, mainh' in a
direction parallel to the general northwest strike of the zone.
The ore shoots in the vein are very persistent in depth as far
as opened up, and up to 200 feet long. The vein fillings being
all siliceous, the cinnabar deposition is probably related to this
silicification. The entire mineral zone is, however, also highly
permeated with sulphur. In various places in the mine con-
siderable exudations of sulpho-salts are found. Iron pyrites
are also very prominent in the fissures, especially in or close to
NAPA COUNTY. /y
the cinnabar deposits. Experience therefore shows that con-
siderable contents of iron pyrites indicate the proximit}' of
bodies of cinnabar ores. The cinnabar occurs generally in
crystal form, often columnar. Occasional!}' acicular crystals
are found in the vugs. Some metacinnabarite is found, gen-
erally as coating of iron pyrite aggregates. The mine is
equipped with a 6o-ton Hlittner & Scott furnace.
Corona Mine. — Mayacmas District. In Sees. 32 and 33,
T. 10 N., R. 6 W. [See Report State Mining Bureau of Cal.,
XIII, page 597.] The Vallejo Quicksilver Mining Company,
owner; J. B. McCauley, president and superintendent, Oathill,
Napa County. The mine is at the head of James Creek, on the
contact of a serpentine belt and the Oathill sandstone for-
mation. [See Fig, 25.] The ore occurs in a zone of black
chert rock, Ij'ing between a sandstone foot wall and probably
'c/f f ot^r /^ /y ■i'faC S en-/:>f>-j^ Z^-'-'-e '- — ^ -
^
in^
/S' tT' J'tV/ S ^
Fig. 26. Corona Mine — Section showing formation. Dip, S.W. 30*.
a serpentine hanging wall. [See below.] The general strike
of the zone is N. 45° W. Three ore shoots show at the sur-
face. The development consists mainly in a level which enters
the hill running very nearly west and crosscutting the sand-
stone foot wall for about 400 feet. The sandstone is here
mixed with some shales. At 400 feet, the tunnel cuts the vein
and follows it about 800 feet to the southeast, and 1 300 feet to
the northwest. The tunnel cuts the vein at the southeasterly
ore shoot, with about 130 feet of backs. The workable ore
body is here from 10 to 15 feet wide, the cinnabar forming in
fissures running through the opaline rock. Underlying the
latter is a white talc, wherein pieces of white and gray rock
are found, determined as phthanite, indicating that originally
a body of shales overlaid the sandstone and were silicified,
80 QUICKSILVER RESOURCES OF CALIFORNIA.
probably by the same solution which formed the overlying
chert beds. [See Fig. 26.] This ore shoot has in the past pro-
duced some rich ore, but at present no work is being done upon
it; the development work being centralized on the middle ore
shoot, which the tunnel cuts at a depth of 350 feet below the
surface. A vertical shaft, 100 feet deep, has been sunk from
the tunnel level on this shoot. The tunnel is driven northwest
to cut the third ore shoot. Part of the tunnel is run in the
sandstone foot wall, determining its persistency, but no cross-
cut has been run into the hanging wall. A ver}^ soft decom-
posed material overh-ing the ore body was crosscut to a width
of 35 feet, without finding unaltered material; hence the
assumption of a serpertine hanging wall rests on surface indi-
cations. The black chert wherein the ore makes is from 40 to 45
feet wide; it has a verj' irregular bedding system, which, if
any, may be said to be a little more prominent across the vein,
but the higher mineralized portions seem to follow the trend
of the ledge. The central ore shoot has been opened for a
length of 160 feet, and has been persistent in depth from the
surface to the present depth of 450 feet. The cinnabar forms
occasionally in such hard and compact material that it can
scarcely be understood how it found access 10 its place of depo-
sition. There is no apparent difference between the barren
and the cinnabar-bearing chert; the former may be in its
general texture a little more compact. A special feature of
this mine is the very great amount of sulphide of iron accom-
panying the cinnabar. The furnace, of 50 tons capacity, is
ver}' much like an ordinar}- Scott furnace; the ore is so highly
pyritous that very little fuel is required. This feature has the
objection that the heat in the furnace is ver}- irregular, and
generalh- far too high, entailing a great loss of mercurj-.
La Joya Mines. — The Standard Consolidated Quicksilver Min-
ing Company, owner. The property is in Sec. 24, T. 7 N.,
R. 6 W., three miles southwest of Rutherford. These mines
have been idle for several years and the works are caved in.
Regarding La Joya mine, Mr. von Leicht reported in March,
1S98, three known ore bodies, separated by barren stretches,
in an altered serpentine, cropping at the surface as yellow
ochery matter, on the contact of sandstone and serpentine to
the southwest of the former; strike northwest. The gangue
NAPA COUNTY.
81
minerals as reported are: silicates and calcites, no iron pyrites
or sulphur. Since this report was made some further explora-
tion work had been done. A 20-ton Fitzgerald furnace has
been erected, but not used as yet.
Manhattan Mine.— Knoxville District. Lake Mining Com-
pany, owner; R. B. Knox, Knoxville, Napa County. In Sec.
6, T. II N., R. 4 W., and Sec. i, T. 11 N., R. 5 W. [See Mon.
XIII, U. S. G. S., page 282: Report State Mining Bureau of
Cal., XI, pages 70-72; XII, page 363; XIII, page 598.] The
PHOTO No. 0. MAXH.\TTAX Ql'ICKSILVER MINE.
first work on this mine was performed at Johntown in 1863.
[See Fig. 27.] As the ore was reduced at the Redington mine
its product was credited to that property. Work was resumed
in 1 868 until 1877, then the mine was idle until 1884, but has
been in constant operation since that year. Total production,
about 1 5,000 flasks.
The study of this mine is especially interesting in regard to
the relation of igneous rock and the ore deposition. The ore
deposits are found in a belt having a general northwestern
6— QR
82 QUICKSILVER KESOURCES OF CALIFORNIA.
direction, lying between basalt to the northeast and serpentine
to the southwest. The basalt does not show at the surface in
a continuous line; the full red line on the plan of the mine
represents as nearly as possible the line of its vent. The ter-
ritory between the basalt and the serpentine is almost entirely
covered b}' tufa, except in the following places :
At Johntown is a small exposure of the "mudrock" in
which the original discovery of cinnabar in this mine was
made.
North of the furnace and close to the serpentine lies a large
body of chalcedony, formed most probably by mineral springs.
On the northwestern end of the property is found the hill
represented by section 3, showing a body of serpentine almost
entirely covered by tufa.
The underljnng countr}- rock is an altered Neocomian [see
Becker, Mon. XIII, page 464], crushed and altered into a
material which is found through the entire mine in various
conditions of hardness. Near water channels it is a dark-
colored clayey material, which grades into a light-gray rock
without any discernible cleavage or fissility, generally rather
soft, occasionally darker colored, very hard and fine-grained.
Its position near the eruptive rocks, and comparisons with the
silicified shales of the neighborhood of Mount Konockti, sug-
gest that the shaly country rock was crushed and ground by
the eruptive actions, and its original stratification destroyed.
The harder portions are probably the result of contact meta-
morphism, as they are generally found in contact with, or close
to, the igneous rock. This material is locally called "mud-
rock," and is found also in other mines. It was found in the
lower level of the Wide Awake shaft (Sulphur Creek), and in
some of the mines in San Luis Obispo County. On the con-
tact of the "mudrock" and the basalt occurs a breccia, gener-
ally very hard, locally called "niggerhead," probably fragments
of country rock recemented, due to the action of the adjoin-
ing basaltic extrusions.
Underground explorations have proven that the surface
indications in many instances do not represent underground
conditions. Sections i, 2, and 3 show that the presence of
basalt at the surface does not indicate an igneous dike per-
sistent in depth. The section of shaft No. 3 shows basalt
underlying 150 feet of breccia and "mudrock," while levels a
NAPA COUNTY. 83
and b show basalt near the surface and none in the under-
lying territory. The section over pit No. 3 (CC) shows how
basalt bowlders and tufa have spread over the country rock.
It would require systematic underground exploration to deter-
mine the exact location of the fissures through which the basalt
extruded. One fact is, hov/ever, beyond doubt: The eruptive
actions are intimately connected with the ore deposition.
Through the serpentine runs a very prominent cropping of
opaline material, near its northeastern boundary, which crop-
ping is almost continuous to the Boston mine, where large ore
bodies have been found therein. A great amount of explora-
tion work has been done on these croppings without disclosing
any ore, until recently a seam of fair ore, from 6 to 12 inches
wide, has been discovered therein, about 400 feet southeast of
the furnace.
All the territory between the basalt and the serpentine shows
the action of mineral springs, which have formed large beds of
sinter and other siliceous material.
Commencing at the southeastern part of the property are the
works on Soda Hill. The underground works are at present
inaccessible. At water level they encountered gas and water
highly charged with sodium, arsenic, etc. — salts. The opaline
ledge crops here ver\' plainly in the serpentine, and consider-
able work was done to explore it, but the ledge was found to
be absolutely barren. This hill is surrounded by knolls formed
by mineral springs now dried up. The surface of the hill is
covered by tufa, in which several shallow pockets of cinnabar
were found, but in the long tunnel (/;/) [see plan] driven
under the hill no ore was found. The formation proved to be
principally breccia. On the east slope of the hill an incline
shaft, 25 feet deep, was sunk on two parallel seams of black ore.
Northeast of Soda Hill (N. 50° E.) lies pit and shaft No. 3,
the most extensive works on the property. The pit is in the
form of an L. The north and south leg is 250 feet, the east
and west leg 200 feet long. The average depth is about 100
feet, and 120 feet at its deepest point. The walls of the
pit are partly basalt, more or less leached, partly tuf? and de-
composed breccia; in the northwest corner the "mudrock,"
exposed at Johntown, appears. The bottom of the pit shows
the richest in the northern part, but cinnabar ore scams are
found all through the formation, generally vertical, but follow-
84 QUICKSILVER RESOURCES OF CALIFORNIA.
ing the prominent seams in the rocks in ever}- direction. A
number of tunnels have been run from the pit into the adja-
cent territory-, especially toward the basalt to the east, but as
the pit walls are nearly vertical, their entrances are nearly all
inaccessible. A tunnel {a) [see section over pit], in the south-
eastern part of the pit, about 25 feet below the surface, which
is accessible, shows first decomposed breccia, partly carrying
some ore, partly barren. At 100 feet from the mouth solid
basalt comes in. On the contact of the breccia and the basalt
lies a belt of opaline rock, largely decomposed, but traversed
by hard ribs of undecomposed opaline, accompanied by seams
of ore. This material carries some lime. The same section
shows that at a lower level basalt is absent, verticall}- under
its occurrence in tunnel a, and that even were basalt found by
driving tunnel l^ further, this could hardly belong to the same
body as that found in a. Shaft No. 3 runs into basalt at a depth
of 150 feet [see section] and remains in that formation under-
h-ing "mudrock" to its bottom at 230 feet. The 150-foot
level, from which tunnel ^ is run, is mainly in very hard, dark-
colored breccia. At this level metamorphic sandstone replaces
the breccia and persists to the 200-foot level. [See sketch of
pit Xo. 3.] Below the 150-foot level the ore, which in the
breccia is scattered in seams and pockets throughout the forma-
tion, is concentrated in a contact between the sandstone and
the "mudrock," persisting below the 200-foot level, as far as
yet ascertained. The "mudrock" appears to surround the
sandstone. With the appearance of the sandstone is intro-
duced a change of the gangue from siliceous to calcareous,
calcite beginning to appear in the veins, while the waters con-
tain carbon dioxide. Here then the replacement of silica by
carbon dioxide takes place below a zone where silica predomi-
nates. This may be attributed to the influence of basalt on
the higher horizon, locally heating the rocks and hence
favoring the formation of silicates.
Adjacent and to the northwest of pit Xo. 3 lies the surface
exposure of "mudrock" at Johntown. This exposure does not
cover over two acres. The original discovery of cinnabar was
made here, but all the works are almost entirely obliterated.
Nearly north of Johntown, at a distance of about 600 feet, is
the southeastern end of a row of pits lying in a northwesterly
direction, pretty close to the ridge which marks probably the
NAPA COUNTY. 85
vent of the basalt extrusion. These pits are on a fissure called
the Bunkhouse vein. The ore occurs in lenses on which the
pits are sunk, the intervening spaces being nearly barren.
Occasionally large ore chambers are found in the ore lenses. The
ore forms in seams in the "mudrock," but prominentl}' in the
tufJ and in the breccia, and occasionally in limestone which is,
nearly always, only found in connection with the ore, near the
surface in nodules. In this connection it must be noted that
the Knoxville basalt carries a high percentage (7.72%) of lime
(CaO) [see Mon. XIII, page 159], and thus the lime in the
ore bodies may readih' be accounted for. Sections i and 2 give
details of the formation as exposed in the pits and levels run
from them. The development tunnel now being run in a north-
easterly direction cuts first through a whitish decomposed tuff,
then successively through basalt, breccia, ledge matter, and
"mudrock." The ledge matter, which dips away from the
basalt, is a fine-grained, hard, slightly silicified "mudrock," the
cinnabar forming principalh' on its contact with the breccia.
West of this deposit, near the serpentine, is a large deposit
of siliceous material (r), prominently chalcedony, partly of a
sintry nature formed by solfataric springs, the remnants of
previous igneous action, which has now ceased entirely. The
siliceous material is mostly in somewhat contorted beds, slightly
resembling the chert beds of the Cretaceous, dipping southeast-
erly and having a varjang thickness, rather inconsiderable.
This deposit, locally known as St. Quentin, is about 400 feet
long, in a northwesterly direction. Some isolated small knolls
of the same formation are, however, found farther to the north-
west. There are three pits on this deposit. The two southerly
pits are only separated by a wall of a few feet wide at the sur-
face. The third, most northerly, is .smaller and shallower. A
tunnel {e) has been run under this pit about 30 feet below the
surface in a breccia formed of fragments of various rocks
cemented by silica. At the breast some chalcedony is found.
The cinnabar occurs generally in the seams of the siliceous
beds, often mixed with sand, so that it can be removed with
scrapers out of the seams. In the eastern part of the deposit
the siliceous material is impregnated throughout with the
cinnabar in a microcrystalline condition, indicating a contem-
poraneous deposition of the cinnabar and the silica. No
macroscopical crystals of cinnabar are found anywhere in this
86 QUICKSILVER RESOURCES OF CALIFORNIA.
deposit. The ore has not been found to persist in depth in any
of the three pits.
To the north of the St. Quentin lies the basalt shaft and pit.
The vertical shaft lies north of the pit. At a depth of 130
feet, the lower level was run from the shaft under the pit,
which is about 400 feet long in a north and south direction.
Both shaft and pit start in basalt. At 130 feet "mudrock"
came in the shaft from the west. The territory under the pit
is also reached by a long tunnel (//), with a shaft at the end,
20 feet in depth, which communicates with a large chamber 40
feet wide, 45 feet high, and 80 feet long in the bottom, situated
under the pit, entirely excavated, having contained a large
body of good ore. The ledge on which the pit is located has a
north and south strike, varying from that of the other deposits.
It is entirely inclosed in basalt, and in depth abuts abruptly
against a stratum of hard sandstone, dipping slightly east,
from 2 to 6 feet thick; the ore only occasionally penetrating
slightly into seams of this stratum, which is underlaid by
"mudrock." This body of basalt, no feet high, is hence only
a surface flow, which is confirmed by {d) and (/). [See
below.] The ore bodies in the basalt were so profitable that
extensive explorations were made in the "mudrock" to find
their continuation in depth, but without result; hence the con-
clusion that the ore deposition is intimately connected with
the basalt, and that the hard stratum overlying the "mudrock"
prevented the solutions from entering therein, acting as an
impervdous stratum. The ledge matter is throughout asso-
ciated with calcite. [See above, Bunkhouse vein.] The ledge
pinched materially about 50 feet from the surface; at this
horizon the vein filling is limestone, containing narrow seams
of cinnabar. In the lower part it consists of very profitable
ore seams interstratified with seams of limestone about a foot
wide. In the northern end of the deposit "mudrock" is more
prominent.
A couple of hundred feet northwest of the basalt shaft
another north and south vein {b) has been worked in a
weathered basalt from i to 4 feet wide, and from 150 to 200
feet long. To a depth of 50 feet this vein was in places very
rich. At that depth, however, the rock suddenly hardened and
simultaneous!}' the vein became poorer, and had to be aban-
doned at a depth of 60 feet.
NAPA COUNTY.
87
To the southwest of the basalt pit, between this pit and pit
No. 3 of St. Quentin, a shaft {d) has been sunk to the under-
lying "mudrock" which was also found in a pit (/"i) west of
the basalt pit.
Extensive works (/.,) west of the basalt pit and northwest
of St. Quentin, near the serpentine, consist of a large open cut,
tunnels, and stopes, showing that large bodies of ore have been
taken out of this ground. The formation is leached igneous
rocks, chalcedony seams, and brecciated sandstones. Two
drifts have been run toward these works. The upper tunnel,
75 feet below the surface at the open cut, cuts through silica
concretions, then leached basalt, basalt, and on the contact of
the basalt with an altered sandstone a vein dipping southwest,
which, judging
from the old
stopes, contain-
ed a number of
ore bodies of
lenticular form.
The lower tun-
nel, 140 feet be-
low the same
surface, runs
mainly in serpentine material; at 300 feet it cuts across a vein
having a nearly east and west strike; an understope, 20 feet
deep and 70 feet long, shows that the ore body lies in hardened
contact "mudrock." A shaft 80 feet deep shows that the
basalt lies here north of the "mudrock," while in the upper
tunnel it lies south thereof. The stope [see cross-section,
Fig. 28] showed good ore, metacinnabarite, and some native
mercury in pockets next to the basalt. When the stope
reached the understoping in the lower tunnel, it was shown
that the lower vein had a cross strike to that on which the
vein understoping was done, and the latter was never found
below.
At the northwest end of the property is the knoll of which
section 3 gives a cross-section. Several small pockets of ore
were found in the tufa overlying the top. The tunnel (/)
cuts through the entire knoll, running for the greatest part in
serpentine. Ore was only found in the basalt near the
northern end. It forms in seams in the basalt. In some of
Fig. 28. Manhattan Mine— Section over the works at (/,).
88 QUICKSILVER RESOURCES OF CALIFORNIA.
these seams the main filling is formed by bands of iron pyrite,
with thin, intercalated seams of cinnabar; in others the filling
is opaline silica. The ore in the surface pockets carried also
considerable iron pyrite. The hill is mainly serpentine and
shale; the absence of basalt in the lower tunnel may be caused
by a fault, the upper part of the basalt having slid northeast
with the slope of the hill.
While the mine is not a great producer, it .s of great geologi-
cal interest, because the relations between the igneous rocks,
the countT}' rock, and the ore deposits can be so well traced.
The absence of ore deposits in the serpentine, even where it is
contiguous to the igneous rocks, must be noted. In opposition
to the ore occurrence in the Oathill mine, the ore deposits are
all contiguous to the basalt and do not extend to an}- distance
from it, except in the St. Quentin deposit, where the cinnabar
has been deposited from solfataric waters, which must have
been related to the basalt. Again, in the ^tna mine the pre-
vailing conditions indicate that the cinnabar was disseminated
through the sandstone, and formed into workable ore bodies by
secondary concentration in some way connected with the ser-
pentine and basalt, while in this mine all indications tend to
the conclusion that the igneous rocks are the direct source
of the cinnabar. In the neighboring Boston mine there are
reasons to suppose a course of ore formation similar to that in
the ^tna mine. Considering that the Boston and Manhattan
deposits are only one mile interdistant, and that from the
topograph}' it might be inferred that while not appearing at
the surface, the vent through which the basalt extruded in the
Manhattan persists toward the Boston, the entirely diSerent
nature of ore formation in these two mines is very noteworthy.
It is to be regretted that in no place in the Manhattan mine
has the commercial development of the ore deposits caused the
underground works to be run in a manner to determine the
vent of the basalt extrusion, or whether on or near this vent
deposits of greater persistence in depth would be found. The
fact that every deposit as yet opened in this mine terminates
in depth with the basalt, justifies the expectation that such
persistence might be the case.
The irregular basalt occurrences found in the mine are prob-
ably intrusions, which follow pre-existing fissures, joints, bed-
ding planes, or contacts, which would account for the lack of
NAPA COUNTY.
89
heat effect on the adjoining rocks by these igneous intrusives.
[See N. S. Shafer, Bulletin Geological Society of America,
vol. X, page 253.]
South of the furnace in the serpentine is an exposure of
breccia covering a couple of acres, which is used as building-
stone.
The mine is equipped with one coarse-ore and one fine-ore
Knox & Osborne furnace, both of 24 tons capacity. The
coarse-ore furnace is only used for about two months in the
year, the great majorit}'^ of the ore as it comes from the mine
being proper material for the fine-ore furnace.
J3 a ■!, o-/ t c 0 7-e ,
<
Fig. 29. Xapa Consolidated Miues. [See page 91.]
Oathill Mine (or Napa Consolidated Quicksilver Mines). —
Mayacmas District. In Sees. 27, 28, 33, and 34, T. 10 N.,
R. 6 W. The Napa Consolidated Mining Company, of Boston,
Mass., owner ; B. M. Newcomb, Oathill, Napa County, super-
intendent. [See Mon. XIII, U. S. G. S., page 355 ; Report
State Mining Bureau of Cal., XI, pages 65-72 ; XII, page 364 ;
XIII, page 598.] This property covers a large area of ground
between James Creek and Bucksnorter Creek. It has been for
years since its opening in 1876, and is still, one of the largest
producers in the State.
The cinnabar deposits in these mines lie entirely in a belt of
NAPA COUNTY.
91
sandstones, which abut and surround a core of basalt. The
sandstones occur in thin beds, with partings filled with attrition
products and clay. The stratification and also the mineralized
zone have a general tendency toward parallelism to this core.
[See van Hise, i6th Ann. Report, U. S. G. S., Part I, page 637.]
Nearing this core the stratification becomes more irregular and
contorted. The veins, practically fissure fillings in the sand-
stone country rock, are from a few inches to a few feet wide.
Their general plan is given in Fig. 29. They are in their strike
independent of the bedding planes, and carry generallj^ a clay
gouge on the foot wall. In places chambers have been formed
in the walls of the fissures, on that side of the vein where the
sandstone was not protected by a clay gouge from the action of
the percolating solutions.
A peculiar phenomenon
occurs at the crossing of
the Humboldt and Osceola
veins. In both veins near
the crossing shoots of good
ore, about 500 feet long,
were found. The Hum-
boldt vein, which is more
of a conglomerate nature
than any of the other veins,
persists on both sides of
the crossing ; but the Os-
ceola is hardly discernible
at the crossing point and makes only at a certain distance on
both sides of the crossing point. [See Fig. 30.]
The secondar}^ concentration of the workable ore bodies in
this group of mines must probably be attributed to the contact-
metamorphic action of the basalt core. It is, however, a note-
worthy fact that here the ore bodies do not persist to the basalt
core. The explanation may be that the heat and pressure due
to the intrusion of this large body of basalt raised the temper-
ature so high in the close neighborhood of its intrusion that
the mercury was carried off in vapor form and deposited in a
region where the temperature and pressure were lower. The
mine is equipped with two 50-ton Scott furnaces, one of which
was rebuilt in 1902 after sixteen years of service.
Fig. 30.
Xapa Consolidated Mines— Crossing
of two veins.
92 QUICKSILVER RESOURCES OF CALIFORNIA.
Philadelphia Mine. — Mayacmas District. In Sec. 26. T. 10 X.,
R. 6 \V. Owner. M. Pluth, of Oathill, Napa County. The
mine is located in the southeastern end of the divide between
James Creek and Pope Valley, running down from the Oathill
divide. The belt of serpentine running northwest from ,Stna
Springs along the southwest ridge of Pope Valley, crossing
James Creek, near its mouth, follows the divide for some
distance, and some promising float is found on top of the ridge.
A crosscut tunnel 270 feet below the ridge has not yet reached
the ledge; its breast is in basalt, indicating an igneous core in
this divide.
Red Elephant and Northern Light Mines. — Knoxville District. I n
Sec. 3, T. II N., R. 5 \V. The former mine is owned by \V. G.
Tremper, of Lower Lake, Lake County. The latter mine,
south of the Red Elephant, is owned by Fr. Josh, of Lower
Lake, Lake County. In the Red Elephant, a little surface
cinnabar has been found, but none of a number of shallow
cuts and pits show any cinnabar ore in place.
Summit Mine.— In Sec. 19, T. 7 X., R. 5 W. S. W. Keeney,
Xo. 563 Parrott Building. San Francisco, owner.
Twin Peaks Mine. — Mayacmas District. In Sec. 4, T. 9 X..
R. 6 W., and Sec. 33. T. 10 X., R. 6 W. Owners, B. A.
Wilson, F. Smyth, and H. Herrick, of Middletown, and J.
Hayes, of Harbin Springs, Lake Count}*; B. A. Wilson, super-
intendent, Oathill, Xapa County. This mine can only as
yet be considered as a prospect; it has, however, some good
ore, which is reduced in a small retort furnace. The cinnabar
ore is formed in the cracks and fissures of the opaline rock,
and is accompanied by a sensible amount of iron sulphides.
The ore body lies rather flat, and has a strike nearly north
and south, dipping about 30° to the west. Above the ore lies
a layer of grayish-green talc (probably decomposed serpentine),
which shows cinnabar all through it; above which lies a black
gouge, which in places shows clearlj' the structural forms of
the original opaline rock. The formation in this mine, which
lies close to the igneous bodies, is very much distorted; but
when found in place, the ore bodies will probablj' be found on
the same contact of serpentine and sandstone as the neighbor-
ing Corona mine. The property is equipped with a lo-pipe
retort, and the ore must have been of a good grade, as the
monthly product is reported to be 40 flasks.
SOLANO COUNTY.
93
SOLANO COUNTY.
St. John Mine.— In Sec. 33, T. 4 N., R. 3 W. The St. John's
Consolidated Quicksilver Mining Company, owner; Ch. Bone,
president; J. H. Sayre, secretary, room 5, No. 405 Montgomery
street, San Francisco; A. A. Tregidgo, superintendent, Vallejo,
Solano County. This mine was opened in 1873 and was oper-
ated until 1880, during which time it produced 11,530 flasks.
\\'ork was then abandoned until 1S99, when the present com-
pany resumed by reopening some of the old works.
A1-^\- /, o I 1 1 200
€fyv,'^";,...
-s^..
w. ,
■•■/■I
■/
■^•iW.. ...
— 6,
.•- e ■ -
Fig. 31. St. John Mine— Section east and west over main tunnel shaft.
The mine is located in a basin between Mount Luffman to
the west and Mount St. John to the east. These mountains
are characterized by the bold outcrops of two bodies of meta-
morphic sandstones. Nearh^ the entire inter\-ening surface is
covered by sandstone debris, but all the dumps of the old
tunnels show schist, and in some of the larger cuts the contact
of the .schists and sandstones can be found. The sandstones
especially those of the Mount St. John ridge, show a prominent
north and south fracture system. The schists probabh- lie in
a trough, having a general northern trend in the sandstone
1
1
^HH
I^^H
Hl^^''^ ^^^1
wSi
0
1^^
^"■""^^= *^^l
J^M
i^riH' ^^1
n
^^^^^K.^
Hi
^^^^^^^^^^^^^^ ''".^^^^■1
^1
K'
J • . "' I^^^B
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1," ^j'-'.'^. .; "T
PHOTO No. 8. ST. JOHN MINE AND FURNACE.
PHOTO No. 'J. ST. JOHN QUICKSILVER MINE.
SOLAXO COUNTY. 95
formation ; but whether the latter formation underlies the entire
territory has not as yet been determined. Fig. 31 shows that
below the level of the main tunnel another body of schists lies
in the sandstone. The contact of the sandstones and the
schists is ver>' irregular and intricate. The schists appear to
carry some magnesia, at least sulphate of magnesia forms
in the main tunnel in a couple of places. The ore croppings
are found at, or in close proximity to, the ridges of sand-
stone. There are a great amount of open cuts, drifts, and
shallow shafts on these croppings. The principal work, how-
ever, was done in the main tunnel, through which two distinct
ore bodies— the main tunnel ore shoot and the San Miguel
ore shoot — have been worked. The former was cut by the
main tunnel at a depth of 250 feet below the surface, and a
shaft sunk on it from that level to a depth of 180 feet. The
San Miguel ore shoot was reached by a crosscut about 100
feet long, at the end of which a shaft 180 feet deep was sunk,
all in sandstones. The latter works are at present inaccessible.
The main tunnel, course nearly north, which has been retim-
bered, reaches the old stopes at 11 20 feet from the entrance.
It runs through schists, near the entrance thinly bedded, con-
torted, in places showing slickensides, and becoming more
massive in depth. This material resembles very closely the
"mudrock" in the Manhattan mine. At 700 feet from the
mouth the tunnel intersects a sandstone dike, about 6 feet
wide, course N. 60° E.
The metamorphic sandstone is in places altered to quartzite,
and in other places is somewhat porphyritic. It shows zones
of fractures, nearly parallel with the contact, not over one to
one and a half inches interdistant. These are sometimes cut
off by a set of more irregular cross fractures, causing the rock
to break very irregularly, sometimes conchoidal. The ore
forms principally in the zones of parallel fracturing and adjoin-
ing thereto. Where the fissuring allowed it, the cinnabar was
deposited with a quartzose gangue. Often it forms face metal
on the fissure walls, which show signs of movements after the
deposition. Where the rock is more compact, small aggregates
of minute cinnabar crystals are disseminated through the rock,
generally associated with iron pyrite. The mineralization was
contemporaneous with, or anterior to, this metamorphism.
96
QUICKSILVER RESOURCES OF CALIFORNIA.
200
_J
/■£■£" r
Possibl}- the cinnabar was
originally diffused through
the sandstone and leached
//. out and concentrated during
^ the metamorphism of the
sandstone. At and below the
level of the main tunnel the
ore forms exclusivel}' in the
sandstone, but nearer the sur-
face it is found in the schists.
At the point of intersection
with the main tunnel ore
shoot, the main tunnel makes
an offshoot to the west to
avoid the old works [see Fig.
32], and continues then in a
northeasterly direction ( N.
20° E.). It passes first through
sandstone, and then follows
the northeastern contact be-
tween the sandstone and the
schists. Xo ore has as yet
been found in this drift.
Judging from the old stopes the ore body at the level of the
main tunnel was |si
about 70 feet long
and from 15 to 25
feet wide. Below
this level two ore
bodies were worked ^■^'^ -z-'^
from the shaft —
one west, the other
east and southeast
of the shaft — sep-
arated by about 60
feet of barren
ground. The stope
on the ore body
west goes down to
the 130-foot level,
where it forms a
Fig. 32. St. John Mine — Plan showing
main luiinel west of shaft.
^ Ore /30 /ei^e/
•IllUk " /80' "
Fig. 33. St. John Mine — Plan of works in main
tunnel shaft.
SONOMA COUNTY. 97
bod}- about 60 feet long and from 6 to 8 feet wide, having
a course of about N. 10° W., starting about 30 feet from
the shaft. [See Fig. 33.] The ore body east of the shaft
on this level is larger and more irregular. In the 180- foot
level the contact of the sandstone and schists east of the shaft
runs about N. 50° W. In the sandstone are found three zones
of cinnabar deposition running about parallel to the contact,
going from the latter southeast, respectively, one inch or less,
^y^, and 4 feet wide. The sandstone has not been cut through
by the crosscut, 54 feet long, from the northeast contact. The
stope is about 40 feet long on the strike. The shaft has lately
been sunk 50 feet deeper. In the 230-foot level the course of
the same contact is about north, but the works have not as yet
exposed any ore. The mine is equipped with two coarse-ore
shaft furnaces of the John Neat patent. For a detailed descrip-
tion of the plant, see the chapter on Metallurgy.
SONOMA COUNTY,
Almaden, Incandescent, and Tunnel Site Group. — Mayacmas Dis-
trict. C. C. Thomas and E. Grimmer, owners. Pine Flat,
Sonoma County. In Sees. 31 and 32, T. 11 N., R. 8 W.
Includes the Almaden, Incandescent, and Tunnel Site claims.
To the northeast of the Eureka mine. No development.
Bacon Consolidated Group. — Mayacmas District. Includes the
Edith, Maud, St. George, Golden Gate, and Eagle mines, in
Sees. II and 12, T. 10 N., R. 8 W. B. Getleson, owner, Mid-
dletown, Lake County. Idle.
Boston Group. — Mayacmas District. Wm. F. OXeary, A. C.
Huebner, and J. Conran, owners, Healdsburg, Sonoma County.
This group consists of three claims — the Boston, Earlene, and
Hope — in Sees. 3, 9, and 10, T. 10 N., R. 8 W. Two short tun-
nels are run on this property. The upper tunnel, very close to
the crest of the ridge, course N. 63° W., is 100 feet long; at the
breast a drift of about 25 feet long, on a course about north, is
run on the vein ; a thin seam dipping about 30° to the north runs
parallel with this drift and carried some cinnabar. The lower
tunnel, 75 feet below the upper, runs on the same course 320
feet; it cuts, at 230 feet from the entrance, a vein having a
7— yK
98 QUICKSILVER RESOURCES OF CALIFORNIA.
nearly north and south course. The hanging wall is too
decomposed to state the character of the rock; the foot wall is
sandstone. The vein filling is opaline rock, with a bedding
across the vein. In the north crosscut, 25 feet long, the vein
narrows at the breast; in the south crosscut, 10 feet long, some
ore was found near the main tunnel, but at the breast no
cinnabar was found.
Gnnabar King Group. — Mayacmas District. Cinnabar Mining
Company, owner; E.S.Rowland, secretary, Healdsburg, Sonoma
County. The group includes the Cinnabar King, Champion,
Pa3-master, Goodenough, and Helen claims, and two millsites on
the southwestern slope of Pine Mountain, in Sec. 11, T. 10 X.,
R. 8 W. [See repoirts State Mining Bureau of Cal., XI, page
461 ; XII, page 371 ; XIII, page 602.] This propertj- is the only
one on the west slope of Pine Mountain on which some work
has been done lateh-. The general course of the croppings is
northwest. Several open cuts show some ore on the dumps.
This ore forms in silicified serpentine, in seams parallel to the
strike. The dip of the ledge is southwesterly. There is on
the propert}' a shaft 55 feet deep, on a ven,- flat incline; a lower
tunnel, 660 feet long, at a level 200 feet below the collar of the
shaft; and an upper tunnel 87 feet below same collar. These
works are inaccessible,
Cloverdak Mine. — Maj-acmas District. In Sees. 3, 4, 9, and 10,
T. 1 1 X., R. 9 W. This includes the Cloverdale, Sunrise, and
Mount Vernon groups, the Mercun.- and Manzanita claims, and
some inclosing lands, on both sides of Big Sulphur Creek,
near the mouth of Squaw Creek. Owners, H. B. and C. A.
Lawley, The Geysers, Sonoma County. [See Mon. XIII, U.S.
G. S., page 376; Report State Mining Bureau of Cal., XIII,
page 603.] This mine was opened in 1S72, the furnace being
constructed in 1S75, and run for twenty-six months, producing
about 3200 flasks of mercurj'. The works were closed down
in 1878. Work was resumed in 1898 b}- the present owners,
who started the furnace in Xovember, 1S99. The latter has
run steadily for the last eighteen months, producing about 720
flasks. At the end of 1902 it was producing about 50 flasks
per month. The mine workings consist, besides several large
open cuts, of about 1500 feet of drifts and 150 feet of shafts.
On the Mount Vernon group very little development has been
SONOMA COUNTY. 99
done. A body of thinly-bedded cherty rock between sand-
stone walls has been opened up in the Mount Vernon claim by
a shaft and two tunnels. The latter, which are almost vertically
above each other [see Fig. 34] , show some face cinnabar on the
fissure planes of the chert. The strike of this body of stratified
chert is about northeast, the dip very irregular about southeast.
In the upper tunnel the seams between the chert beds carry
sulphur, the only similar occurrence seen on the property.
The property is traversed by several nearly parallel ledges of
thinly-stratified chert, inclosed by sandstone. These ledges
have generally a northwest strike and northeast dip. The
thickness of the chert beds varies from a half to three inches;
that of the clay seams from a knife blade to quarter of an inch,
except in one place, in the Murphy tunnel or No. 4 ledge,
where chert and clay
seams are for some dis-
tance much thicker. In
places, both the chert d//9<yo)^^
and clay are colored
light green by silicate of
iron. In the same tun- sf/9/0/^
nel the thick gouge
above the chert consists >0£.e''£ ,
e ,. . , Fig. 34. Cloverdale Mine— Section overworks,
for some distance of de- j^^„„t vemou claim.
composed sandstone and
clay interbedded like the chert formation. No serpentine is
found on the property — the country rock being all sandstone;
but on the ridge of the divide between Squaw Creek and Big
Sulphur Creek, above the mine, some porphyritic and dioritic
rocks are found, cutting through the sandstone which forms
the backbone of the ridge. The chert shows very plainly on the
lower part of above-mentioned dividing ridge, which has there
a general direction nearly east and west, and is cut at an
obtuse angle by those ledges.
Starting up the ridge from the furnace, the first ledge, No. i ,
about 25 feet wide, is barren at the ridge, but to the southeast,
in the Glory Hole tunnel, shows very good ore.
On the next ledge. No. 2, the former company twenty years
ago mainly concentrated its work, producing 3100 fiasks from
it. The ledge was worked both by open cut and in the Cat-
sin's tunnel. At present this ledge is worked on the south
SONOMA COUNTY.
101
slope of the ridge by three open cuts, forming a nearly continu-
ous line of workings [see photograph Fig. 35, Ki, K., and K3J ;
the open cut at the top of the ridge (Ki) is 60 feet high and
48 feet wide, and furnishes at present, practically without sort-
ing, all the ore run during the summer season through the
furnace, which has a capacity of 7 tons of ore per day and
produces from 45 to 50 flasks per month. The more compact
and regularly bedded part of the ledge carries the metal mostly
as face metal and incrustations in the fissures; the crushed
portions are much richer and carry the metal more in seams
and bunches.
/i//3
S <k tt £/ » f
Fig. 36. Cloverdale Mine — Plan and section of Murphy tunnel.
The next ledge. No. 3, is only separated from Xo. 2 b}' a
narrow belt of sandstone, and has been extensively worked by
open cut in the Old Ray workings on the north slope. It
shows onl}'^ slightly on the south slope of the ridge, principally
in the mouth of the Murphy tunnel. [6, Fig. 35.]
Ledge No. 4, or Murphy ledge, shows principally in the
Murphy tunnel. It is about 25 feet wide. [See Fig. 36.] The
chert beds are mostly from one to three inches wide, the gray
clay seams one quarter to one inch ; cinnabar ore making prin-
cipally on the faces, richer nearer the hanging wall, which is
peculiarly interstratified, as above mentioned, with clay seams
like the chert beds. These chert beds, wherein the cinnabar
102 QUICKSILVER RESOURCES OF CALIFORNIA.
ore makes, are ven,- similar to the ledge matter of the Great
Western.
The company has a small incline furnace of 7 tons capacity
per day, and a lo-pipe retort furnace.
Qyde Mine. — Mayacmas District. G. Hemmingwaj- and F.
Baumeister, owners, The Geysers, Sonoma County. In Sec. 24,
T. 10 X., R. 8 W., on the north fork of Little Sulphur Creek
(Devil's Den Canon). This mine is close to and partially
surrounded by the Culver- Baer property, and is located on
the same ledge of croppings as the Old Oakland (Lost Ledge
and Geyser) group of that property. The croppings show
very boldly on the northeast bank of the creek, and the latter
is full of large ore bowlders. The old works are inaccessible,
but on the dumps several tons of ore of a good quality are
found.
Crown Point (Sonoma) Mine.— Mayacmas District. The Crown
Point Quicksilver Mining Company, owner; S. S. Bogle, secre-
tary', Santa Rosa, Sonoma Count}'. It includes the Sonoma
Xos. 3 and 4, Hercules, and Crown Point Xos. 4, 5, and 6,
in Sec. 5, T. 10 X., R. 8 W. [See Mon. XIII, U. S. G. S.,
page 376; Report State Mining Bureau of Cal., XIII, page
603.] In former years rich surface pockets were worked to
advantage; they were situated adjacent to a serpentine belt,
ha\-ing general strike X. 48° W. [See map of Maj-acmas Dis-
trict, and Fig. 37.] Two tunnels (A and B), respectiveh- 325
and 200 feet long, and a shaft (C) 50 feet deep with a drift 40
feet long in the bottom, represent the later development work,
which has, however, as ^-et not disclosed any valuable ore
bodies. This work has been done in a very unsystematic
manner and proves little or nothing as to the future of the
property. The company started in the fall of 1902 some sj^s-
tematic prospecting work.
Culver-Baer Mine. — Mayacmas District. This is in Sees. 24,
23, and 14, T. II X.. R. 9 \V.. along the headwaters of the
north fork of Little Sulphur Creek (Devil's Den Canon).
It includes the Fairfax, Sunny Side, Republic, Bush, Colfax,
and Culver-Baer Xo. i and Xo. 2 claims, representing the
former Oakland and Geyser group; and the L'nion, Hard-
scrabble, Ridge, Black Bear, and West End claims, representing
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104
QUICKSILVER RESOURCES OF CALIFORNIA.
the Black Bear and Kentuck group. Owner, the Culver-
Baer Mining Company; president, A. V. McNabb, vSanta Rosa,
Sonoma Count^^; general manager, G. B. Baer. Cloverdale,
Sonoma County; superintendent, F. Baumeister, The Geysers,
Sonoma County.
This property covers the old mines of the Oakland and
Black Bear group. This mine was a producer from 1875 to
1879, producing about 6900 flasks, but was then shut down,
' Sa ^icLsto ^le.
Fig, 38. Section Culver-Baer Mine.
work being resumed only in 1901. [See Mon. XIII, U. S. G. S.,
page 376; Report State Mining Bureau of Cal., XII, page 371;
XIII, page 602.] The ledge is indicated by a persistent and
very strong cropping of ledge matter, with a general east and
west course, on the north bank of the canon, about 150 feet
wide, dipping north into the mountain, winding a little but
following rather closely a line parallel to the creek. [See
Fig. 38.] These croppings consist mostly of silicified foot- wall
sandstone, changed into a blocky material with a great num-
ber of quartz seams; sometimes serpentine (hanging wall),
SONOMA COUNTY. 105
also traversed bj^ quartz seams, occurs. This ledge material is
rather hard and compact. The ore is not making on the faces,
but mosth^ inside the rock; often while not appearing on the
surface, the pieces of rock prove rich in cinnabar when broken
up. Very little sulphide of iron accompanies the cinnabar.
Especialh- in the old Geyser claim, about opposite the new
furnace site, the cinnabar occurs in its rarer form of crystalliza-
tion in acicular (needle-shaped) prisms. Higher up the canon,
in the old Lost Ledge ground, the cinnabar occurs in the
ordinary tabular crystal form.
The old underground works in the Old Oakland and Geyser
group are caved in, and a crosscut tunnel driven by the pres-
ent company is also inaccessible. This tunnel, 890 feet long,
is on the level of the new furnace, reaching the ledge at a
depth of 375 feet below the old croppings, where it found ore.
The old works on the Lost Ledge ground (upper part of the
property) reached the same depth in the ore body.
The sandstone foot wall along the ledge is greatlj' eroded,
forming the creek. On the hanging wall is a narrow belt of
serpentine overlaid by a wide belt of sandstone. This belt of
serpentine seems to persistently accompany the outcrop. The
amount of ore in sight in the croppings, that can be quarried, is
so large that the company is erecting a 20-ton Fitzgerald incline
furnace, without undertaking for the present anj- further
underground development work.
The western part of the property, the Black Bear group,
covering the Old Kentuck ground, has been leased to W. T.
Brush and others, of Cloverdale, Sonoma County.
The croppings so prominent in the eastern part follow Devil's
Den Caflon into the Clyde mine, then turn a little northward
and re-enter the Black Bear group. In its western part they
are abruptly cut off by a body of serpentine, having a nearly
east and west course. The present lessees are cleaning out
some of the old works.
Double Star Mine, — Mayacmas District. In Sees. 2, 3, 10, and
1 1, T. 10 N., R. 8 W. The property is on the old road from
Middletown to Pine Flat, at the headwaters of Little Sulphur
Creek, and consists of the Double Star Nos. i, 2, and 3, Her-
cules, and Giant. Owners, Wm. Peters, of Healdsburg,
Sonoma County, and others. A vertical shaft was sunlc on
106 QUICKSILVER RESOURCES OF CALIFORNIA.
croppings identical with those on Pine Mountain, the Wall
Street, etc.; it has been abandoned and a crosscut tunnel run
1 70 feet below its collar, in the serpentine, which at 400 feet
from its entrance cut the fissure on which the shaft was sunk.
Short drifts were run both ways on the fissure, showing the
same material as on the surface, but no cinnabar ore. At 650
feet the tunnel reached sandstone, mixed with "alta"; drifts
were run both waj-s on the supposed contact, without dis-
closing any ore. The breast of the tunnel at 670 feet is in
mixed sandstone, gouge, and decomposed serpentine. It is, in
fact, doubtful if the real sandstone has as yet been reached.
Eureka Mine. — Mayacmas District, In Sec. 32, T. 11 N.,
R. 8 W., on the divide between Big Sulphur and Little Sulphur
creeks, to the northwest of the Socrates mine. Includes the
Eureka No. i and No. 2 (Old Flagstaff), Mate, and Captain
claims, and Eureka millsites; and the Electric, Creekside,
Trout, and King Arthur claims in Big Sulphur Creek, in Sec.
29, T. II N., R. 8 W. Owner, Eureka Quicksilver Mining
Company; C. R. Cormack, secretary. No. 215 Sansome street,
San Francisco. [See Mon. XIII, U. S. G. S., page 375.] A
belt of serpentine passes through the southern part of the
Eureka claims near the ridge of the hill, with a general strike
about northwest, and a southwesterly dip. [See Fig. 39.] This
serpentine forms the hanging wall of a contact, the foot wall
being sandstone. In the main tunnel, this arkose sandstone is
very much decomposed, the silicates having been largely
altered to clay by weathering. On the foot wall lies a heavy
gouge, and the ledge matter, which is cut at a depth of 170
feet, is very hard. In a higher tunnel verj^ fair ore was found,
the material being much softer. Two drifts have been run
from the main tunnel along the ledge, but have not as yet reached
any pay shoot. The hillside is very steep, and heavy slides
have occurred. The two bodies of thinly-bedded material
(probably chert) — one in the Captain, with a strike of N. 77° E.,
the other higher up the hillside on the Eureka No. i, strike
N. 23° W. — belonged probably to the ore body.
Lower down in the Mate is a body of very light- colored,
loose-grained sandstone, carrying quicksilver in the form of
cinnabar and of incrustations of black sulphide of mercury.
Sufficient work has not yet been done on this material to decide
SONOMA COUNTY.
107
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108
QUICKSILVER RESOURCES OF CALIFORNIA.
about the extent and importance of this deposit of quicksilver
ore. A thin seam of cinnabar ore, three inches wide at the
surface, has been cut by a tunnel at a depth of about 30 feet,
showing a width of one foot. The mine is equipped with a
20-ton Fitzgerald furnace, built in the latter part of 1902.
Great Eastern and Mount Jackson Mines.— Near Guerneville.
The Great Eastern Quicksilver Mining Company, owner;
A. Abbey, superintendent, Mercury, Sonoma County : or No. 44
Nevada Block, San Francisco. In Sees. 16 and 17, T. 8 N.,
Fig. 41. Section over the Great Eastern Mine.
R. 10 W. [See Mon. XIII, U. S. G. S., page 362; Report
State Mining Bureau of Cal., VIII, page 633; XI, page 460;
XIII, page 602.] These mines are peculiar in so far that they
are at a considerable aistance from all other workable deposits
and also from any known eruptives. The outcrop is prominent,
but only for a relative h' short distance (about 1900 feet), and
follows prett}' closely a belt of serpentine [see Fig. 40], cutting
through the irregularly metamorphosed rocks of the Coast
Range, probably of Neocomian age. The strike is very nearh'
east and west — in the Great Eastern, N. 75° \V.; in the Mount
Jackson, N. 63° W. The croppings stand almost vertical near
the surface, but in depth dip northeasterly. The sandstone
General Plan of
GREAT EASTERN MINE.
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110 QUICKSILVER RESOURCES OF CALIFORNIA.
foot wall has been considerably eroded, leaving the croppings
of the ledge in bold relief. [See Fig. 41.]
The main shaft is sunk vertically in the sandstone foot wall
to a depth of 500 feet, and the cross drifts from the shaft to the
vein on the various levels show that no serpentine occurs in
the foot wall. The hanging wall is serpentine. The croppings
[see Fig. 41] are about 200 feet above the level of the shaft,
and were worked through several drifts and cuts. At present
all the ore comes from the lower levels.
On the 500-foot level, a detached ore body has been found,
120 feet southwest of the main ore vein, in the foot-wall sand-
stone, and has been opened up for about 60 feet, showing
good ore. A raise 20 feet high shows that the top of this ore
body pitches southeasterly on a strike nearly parallel to that
of the main vein. The vein filling is ven," similar to that of
the main vein. The country adjacent to the deposit carries
a considerable amount of iron pyrites; strong emanations of
fire gas render work in this vein ver}- diflScult, as this gas
attacks the eyes of the miners. Efforts have been made to
collect this gas for analysis, but as yet have not succeeded.
On the same level, inten-ening between the main ledge and
the serpentine hanging wall, is a ver>' hard crystalline rock of
a graj'ish color, showing some slight signs of serpentinization,
but having no resemblance to the chalcedonite found in other
quicksilver deposits. This hard rock has the advantage of
allowing the large stopes to be left without timbering or fill-
ing, notwithstanding the mine makes considerable water. On
one ore body the stope, from 10 to 35 feet wide, is carried to
the surface, being sustained by rock pillars left in the poorer
parts of the ledge, Avithout any stulling or filling. The same
stope is continued downward about 90 feet below the 500 -foot
level.
A vertical shaft is sunk, starting from the 500-foot level, on
the ledge, about 100 feet deep. At the bottom of the shaft in
the 5So-foot level the foot wall shows very plainly; the ore
makes in places clear to that wall with very little or no
gangue. Between the ore-carrying zone and the serpentine
hanging wall comes first the hard siliceous rock casing above
described, then a much softer zone of somewhat decomposed
serpentine, and then the hanging- wall serpentine. [See Fig. 41 .]
SONOMA COUNTY.
Ill
The ore forms in irregular lenticular bodies, more persistent
vertically than horizontall3\ [See Fig. 42.]
The ledge filling is generally a very hard crystalline rock,
fissured and cross-fissured in all directions, and recemented by
subsequent depositions. The ore forms principallj' in relativelj^
softer zones in this material. It carries less iron pj-rites in the
lower levels than at the surface, and the exudations of sulpho-
salts are also much less in the lower levels, rendering the
ventilation of the mine a relatively easy matter. In the ledge
filling are found bunches of soft, whitish, somewhat unctuous
material — a decomposition product. It is impossible, due to
the complete decomposition, to determine the character of the
original material. The material, locally called "caliche," is
sometimes barren, and sometimes carries sensible amounts of
Fig. 42. Great Eastern Mine— Plau showing the form of the ore bodies.
cinnabar, but its presence generally indicates the proximity of
cinnabar deposits. On the 580-foot level an exposure of the
crj'stalline fissured rock carrying cinnabar shows that some of
these fissures are rather wide, over an eighth of an inch, and
that the rock is recemented by quartz containing no signs of
cinnabar. Clearly, then, this recementation took place subse-
quent to the cinnabar deposition.
The absence of gangue, the hard siliceous material on the
hanging wall, and the character of the vein filling, all indicate
a very strong silicification (cementation) process, but of an
entirely different nature from that forming the chalcedonite
" quicksilver rock " so often associated with cinnabar deposits.
In the levels above the collar of the shaft in the surface crop-
pings some opaline rock is found, and the silicification (cemen-
112 QUICKSILVER RESOURCES OF CALIFORNIA.
tationj of the ledge matter is less distinct than in the lower
levels.
The mine is equipped with one 12-ton coarse-ore Maxwell
furnace, and one 16-ton fine-ore Hiittner & Scott furnace, using
brick and wooden condensers.
Great Northern Company ♦ — Mayacmas District. W. H. Jordan,
president, Xo. 131 1 Claus Spreckels Building, San Francisco.
Owns nine claims — Alta, Leota, r^Iinaoka, Little Giant, Colum-
bia, Bluejay, Happ}' Hooligan, Wizard, and , in Sec. 2,
T. 10 N., R. 8 W., and Sec. 33. T. 11 X., R. 8 \V., situated north-
east and parallel to the Old Denver. Xo important develop-
ment work has as j-et been done on this property.
Hope Mine. — Mayacmas District. Crown Point Quicksilver
Mining Company, owner; S. S. Bogle, secretary-, Santa Rosa,
Sonoma County. Includes the Hope Xos. i, 2, and 3 mines, in
Sec. 4, T.,io X., R. 8 \V. This group is on the southeastern
extension of the Eureka and Socrates belt of croppings. The
Hope shaft, very near the northwestern end line, is 80 feet
deep, sunk on these croppings, but at present is inaccessible.
A tunnel has been run partly on the contact and partly in the
serpentine hanging wall. The ledge filling is a siliceous
material, with a main Assuring parallel to the strike. At the
breast a crosscut shows that this fissure filling is 30 feet wide.
At the southeast end of this crosscut a winze 15 feet deep has
been sunk, but is at present caved in. There are ver>' few
signs of cinnabar in the tunnel or in the material on the dump.
Hurley Property. — Mayacmas District. Mrs. M. Hurley, 1820
Pacific avenue, San Francisco, owner. The property consists
of 160 acres in Sees. 4 and 5. T. 10 X., R. 8 W., to the
southeast of the old Sonoma mine. In this property is found
the continuation of the serpentine belt running through
the Sonoma, associated on both sides wnth sandstones. A
short surface tunnel near the falls of the creek, close to the
west line of the property, shows a ledge having a course nearly
X. 45° W., about 30 feet wide, dipping westward. The serpen-
tine belt on the property is generally prett}' narrow. Xear the
house in the east and west center of the property some crop-
pings show on the surface; on these are a shaft 50 feet deep
and a caved-in tunnel 150 feet long. It is claimed that some
cinnabar ore w^as found in the bottom of the shaft.
SONOMA COUNTY. 113
Lookout Group. — Mayacmas District. Judson Brown, Pine
Flat, Sonoma Count}', owner. Includes the Lookout and
Diamond claims, in Sec. 32, T. 11 N., R. 8 W.; parallel and
adjoining the Eureka Nos. i and 2 to the south. No develop-
ment of any importance.
Lucky Stone Group. — Mayacmas District. C. A. Grimmer,
Pine Flat, Sonoma County, owner. Includes the Last Chance,
Pay Reef, and Mother Lode claims, in Sec. 4, T. 10 N., R. 8 W.,
lying parallel and adjoining the Old Denver to the southwest.
On the Last Chance, the most northwesterly claim, old work-
ings show some cinnabar ore on the contact of serpentine and
sandstone.
Maricoma Mine (Santa Rita). — E. White and others, of Pine
Flat, Sonoma County, owners. In Sec. 36, T. 10 N., R. 8 W.
Three tunnels have been run on this property; the upper one
is 160 feet above the level of the lower tunnel. In the lower
tunnel a stope has been raised on an ore body about 6 feet
wide, having a serpentine foot wall and a sandstone hanging
wall, with a wide gouge on the foot wall, and containing some
good cinnabar ore. In the breast of the tunnel the contact
carries no cinnabar ore.
Mercury Mining Company. — Macaymas District. F. A. Hunt-
ington, president. No. 330 Montgomery street, San Francisco.
Owns the Boulevard, Boulevard Extension, Elizabeth, Espe-
ranza, and two other claims northeast of the Socrates mine,
and the Prince and Princess southwest thereof. In Sees. 32
and 33, T. 11 N., R. 8 W., and Sec. 2, T. 10 N., R. 8 W. No
important development work has as yet been done on this
property.
Missouri Mine. — Mayacmas District. L. W. Pittman, The
Geysers, Sonoma County, owner. In Sec. 25, T. 1 1 N., R. 9 W.
[See Mon. XIII, U. S. G. S., page 376; Report vState Mining
Bureau of Cal., XIII, page 603.] It lies to the northeast
of the Culver- Baer propert}'. This mine has been idle for
years and all workings are inaccessible. The Culver-Baer
Company is cleaning out some of these works to test the value
of the property.
Napa Mine. — Mayacmas District. In Sec. 11, T. 10 N.,
R. s W. Donzel Stoney, 40 Montgomery street, San Fran-
cisco, owner. Idle.
8— QR
114 QUICKSILVER RESOURCES OF CALIFORNIA.
Occidental and Healdsburg Group. — Mayacmas District. In
Sec. lo, T. lo N., R. 8 W. J. Stern, No. lo Battery street,
San Francisco, owner. Idle.
Old Chapman Mine. — W. A. Coalson, of Alexander, Sonoma
County, owner. It lies in Sees. 25 and 30, T. 10 N., R. 8 W.,
at the mouth of Sausal Creek canon, on Deer Creek. On the
south side of Deer Creek a line of croppings, course about
N. 15° W., runs down the slope toward the creek, but the
underground works have not disclosed any continuation of
ore in depth.
Pacific Mines (Crystal or Red Cloud). — Mayacmas District. In
Sees. 5 and 6, T. 10 N., R. 8 W. This, the northwestern
extension of the Sonoma mine, comprises the Crystal, Crystal
No. 2, Crystal Extension Nos. i, 2, 3, and 4. Owner, Pacific
Mining Company; A. Abbey, 611 Market street, Oakland;
A. Anderson, superintendent, Pine Flat, Sonoma County. [See
Mon. XIII, U. S. G. S., page 376; Report State Mining Bureau
of Cal., XIII, page 603.] The country rock is mostly altered
sandstone, through which the same belt of serpentine which is
found in the northwestern part of the Sonoma mine runs in
about the same strike, N. 48° W. [See Fig. 37.] On the sur-
face some croppings show at the southwestern contact of this
serpentine belt with the sandstone. A crosscut tunnel (Pacific
tunnel), direction nearly north, runs 265 feet below these crop-
pings. Starting in the countr}' rock southwest of the serpen-
tine, it cuts through another belt of serpentine 40 feet wide,
150 feet from the mouth, to the north of which is 60 feet of
broken ledge matter (called the Little Vein), upon which,
however, no work has been done. At 525 feet the tunnel
reaches the foot- wall gouge, then goes through 25 feet of very
much broken ledge matter, and at 550 feet reaches the serpen-
tine hanging wall, here about 75 feet wide. Short drifts have
been run both ways along the hanging wall, but no workable
ore bodies have as 3'et been found. The same contact has been
found in other workings; the croppings show plainly along the
crest of the ridge. A tunnel (A) running along the vein, and
starting at the southeast end of the hill, about 66 feet above
the level of the Pacific tunnel, has disclosed some promising
ore. In this tunnel a shaft 40 feet deep has been sunk, which
shows some very good ore. Another tunnel ( A^), about 40 feet
SONOMA COUNTY. 115
lower, and nearly parallel to tunnel A, has not yet connected
with this shaft.
Pontiac Group. — Mayacmas District. H. S. Beach and E.
Warner, of Pine Flat, Sonoma County, and C. Mobley, of
Healdsburg, Sonoma County, owners. Consisting of four
claims: Pontiac Nos. i, 2, 3, and 4, in Sees. 33 and 34, T. 11 N.,
R. 8 \V. No important development work has as yet been
done on this propert}'.
Rattlesnake. — Mayacmas District. H. C. Lightner, Parrott
Estate, San Francisco, and others, owners. In Sec. 31, T. 11
N., R. 8 W. [See Mon. XIII, U. S. G. S., page 376; Report
State Mining Bureau of Cal., XIII, page 603.] This mine was
worked in 1S74, but is at present abandoned and the workings
are inaccessible. In this mine the mercury was nearly exclu-
sively found in the native state, as in the Socrates. The country
rock, judging from the surface, is altered sedimentaries, with
occasional small occurrences of serpentine.
Socrates Mine. — Mayacmas District. In Sees. 32 and 33,
T. II N., R. 8 W., and Sees. 4 and 5, T. 10 N., R. 8 W. It is
on the divide between Big Sulphur and Eittle Sulphur creeks,
where the road from Calistoga to The Geysers crosses. Owners,
W. H. Jordan, No. 131 1 Claus Spreckels Building, San Fran-
cisco, F. A. Huntington, and T. W. Nowlin; H. Davey, super-
intendent, Guadalupe mine, Santa Clara County. This ledge
is on the same contact as the Eureka mine; the croppings show
very prominently and can be traced for a considerable distance
between the sandstone foot wall and the serpentine hanging
wall. The main tunnel [see Fig. 43] is run at a depth of about
200 feet below the top of the ridge, starting in the foot wall
material, which is decomposed sandstone mixed with shale and
clay. The average strike of the ledge is northwest, but the
gouge on the foot wall, which in the Eureka mine is very wide,
is much thinner; the ledge matter is soft opaline rock, very
much fractured and favorable to ore deposition. The quick-
.silver occurs mainly as native mercury, the fractures of the
opaline rock being filled with native mercury and some cinna-
bar, the more compact portion of the rock containing minute
globules of native mercury. A "horse" of serpentine about
2 feet wide runs through the vein. The ore on the foot-wall
gouge is softer and generally richer. In some places bunches
116
QUICKSILVER RESOURCES OF CALIFORXIA.
of native mercurj- are found in the sandstone, especially in the
southeast drift. The foot-wall black gouge carries oxides of
iron, calcium and magnesium, silica, silicate of magnesium,
and some free gases (probably free sulphide of h5'drogen and
carbon monoxide), which are ver}- noxious to the miners. The
occurrence of the quicksilver almost exclusively in the native
state causes unhealthy conditions underground and great loss of
mercury in blasting and handling the rock; the recovery of the
mercur}' from the ore is also a problem, which has as yet been
only partially solved.
At present the compau}- is passing the ore through a rotarj"
roaster, 27 feet long, 5 feet 8 inches in diameter, lined with
lo-inch firebrick, having a pitch of 6 inches, using wood as a
Fig ^3. Socrates Mine.
fuel. The rotation is very slow, and the draft is so regulated
as to control the amount of oxygen permitted to enter the fur-
nace. From this roaster the vapors pass through a series of
condensers to the stack, where it is claimed that the products
of combustion exhaust at 100° F. The results appear to be
very satisfactory to the owners.
Walker Mine. — Near Guerneville, in Sec. 7, T. S N., R. 10 W.
L. F. Walker, of Guerneville, Sonoma County, and M. C.
Meeker, of Camp Meeker, Sonoma County, owners. Some
surface deposits caused a tunnel 560 feet to be driven into the
mountain, which at 415 feet from its mouth crosscuts for 60
feet a material showing signs of strong silicifacation, and then
runs along the supposed center of this material for about 90
feet.
YOLO COUNTY. 117
Wall Springs Mine. - Near Guerneville, in Sec. 30, T. S N.,
R. 9 W. H. C. Wall, Hilton, Sonoma County, owner; Healds-
burg Quicksilver Mining Company, J. C. Hobson, of Hilton,
Sonoma County, lessee. A shaft, 70 feet deep, is in process
of sinking. It is claimed that the surface material (serpen-
tine) carries cinnabar, but in the material excavated from the
shaft no signs of cinnabar could be detected.
YOLO COUNTY.
New England and Harrison Mines.— Knoxville District. The
New England is in Sec. 26, T. 12 N., R. 5 W., and the Har-
rison is in Sec. 35, T. 12 N., R. 5 W.; the latter most
probably covering the ground of the Grizzly, mentioned by
Becker. M. W. Harrison, Knoxville, Napa County, owner.
[See Report State Mining Bureau of Cal., XII, page 363;
XIII, page 598.] Both mines lie in serpentine. The minerali-
zation is accompanied with silicification, forming a verj' hard
opaline material.
In the New England are abundant signs of decomposition
by sulphuric waters. Small blisters with an eggshell envelope,
containing oil and sulphur, are found in the rock. Up to the
present time, nothing of value has been exposed in this mine.
The Harrison tunnel was inaccessible. The dump shows
the ledge matter to be a very hard opaline, carrying some cr\^s-
tals of cinnabar in the seams.
In the wide serpentine belt to the southwest of the Manhat-
tan-Boston line occur croppings of opaline rock which have
been prospected for years without any result.
Reed Mine. — Knoxville District. Including the Royal or
Soda Springs mine. Merchants Exchange Bank, San Fran-
cisco, owner. In Sees. 23, 25, 26, and 36, T 12 N., R. 5 W,
[See Mon. XIII, U. S. G. S., page 283; Report State Mining
Bureau of Cal, XI, page 68.] This property was extensively
worked, producing 5650 flasks between 1875 and 1879, but has
been idle for a number of years. The works are caved in and
inaccessible. The surface geology shows that the deposits in
the Reed mine are located close to the line of contact of an
area of serpentine with unaltered fossiliferous rocks, the ore
bodies being contained in an opaline rock formation. The old
works of the Royal mine are located on a dike of the same
material, 20 feet wide, cutting through the serpentine.
Cropptngs
MAP OF THE LITTLE PANOCHE MINING DISTRICT.
DISTRICTS SOUTH OF SAN FRANQSCO.
FRESNO COUNTY.
Arambide and Aurecoechea Claims.— These are in Sec. 32,
T. 13 S., R. 10 E., and Sec. 5, T. 14 S., R. 10 E. Owner, George
Alferitz, care of Dellepiane & Co., 425 Battery street, San
Francisco. These claims are situated near the Providential
group of mines [see map of Little Panoche Mining District] ,
in the same formation of metamorphic sandstone, mixed with
some shale. In former 3'ears considerable mercury was taken
out of this property, but the works are now caved in and inac-
cessible, and the furnace is entirely obliterated.
Mexican Mine. — This comprises three claims (Mexican Mine
Xos. I, 2, and 3), in N.E. % of Sec. 22, T. 18 S., R. 13 E.
Owner, Manuel Santos, New Idria, San Benito County. The
developed part of the property lies in the northwest branch of
Cantua Creek, very close to the contact of the metamorphic
series and the Chico sandstones to the northeast thereof.
While the surface shows almost exclusively serpentine, the
underground workings have proven that this rock is in places
only a surface covering, the tunnels all passing the serpentine
in from 10 to 15 feet and entering into sandstone.
Tunnel No. i [see Fig. 44] is a short tunnel in sandstone,
heavily bedded, with a strike N. 13° W., dip S.W. 80°, through
which a seam 6 inches wide cuts on a strike N. 25° W., dip
N.E. 40°, carrying cinnabar associated with silica and oxides
of iron, oxidation product of iron sulphides.
Tunnel No. 2, on opposite side of the gulch, after passing
through 10 feet of surface serpentine enters into sandstone.
This tunnel has a course south, 60 feet long; 20 feet in a side
drift runs S. 45° E. about 30 feet, which cuts a narrow seam
of ledge matter, course S. 20° W. The breast of the tunnel
follows for some feet a fissure from 18 to 24 inches wide, carry-
ing cinnabar, the gangue being a dark yellov,' ochery material,
indicating that the unaltered ore will be found to carry a great
(119)
120
QUICKSILVER RESOURCES OF CALIFORNIA.
amount of iron sulphide. About 2 feet from the breast is a
shaft 30 feet deep on a narrow seam of ore.
A little above a line from Xo. i to Xo. 2 in the gulch is an
open cut 8 feet deep, showing fissures in the sandstone, dip-
ping northeast, filled with silica and seams of cinnabar asso-
ciated with iron sulphide.
FIG 44.
FLAN or
n£X/CAN M/NE
F/?fSNO CO UN TV
Below and to the northeast of these works in the gulch are
two tunnels: Xo. 4, running N. 10° W., 75 feet; then S. So*^ \\'.,
50 feet; projected to reach under Xo. i. This tunnel is entirely
in slate, but at the breast sandstone is coming in the roof. The
lower tunnel, Xo. 5, 300 feet long, course nearly east and
west, is entirely in slate. Xeither of these tunnels has reached
the ore deposits as yet.
FRESNO COUNTY. 121
Providential Group* — Owners, Thomas Flint, J. J. Croxon,
B. P. Stephenson, N. C. Briggs, A. Johnson, B. Vargas, of Hol-
lister, San Benito County. This group consists of seven claims.
[See map of Little Panoche Mining District.] The country rock
is metamorphic sandstone intermixed with some shale. The
strike of the sandstone is prominently north and south; that
of the shales east and west. The sandstones and shales have
a bluish-gray color. In the sandstone occur narrow, irregular
seams of white quartz. A more or less intricate system of
leached zones runs through the sandstone, which is apparently
leached to a dull white color by the action of some percolating
solution. The cinnabar is found in these zones, which is
accompanied by nearly continuous seams, from i to 2 feet
wide, of quartz colored brown b}- iron and in places forming very
large, perfect quartz crystals, indicating a deposition in open
places. The zones contain a great amount of oxide of iron,
forming yellow ocher and principall}' red oxide. The cinnabar
is found intimately associated with the red oxide. The crop-
pings are prominently indicated by the quartz seams. The
country rock is soft and has been very deeply eroded into ver}'
steep and deep gulches, and the course of the ledges is in places
obscured by probable slides. Their course is indicated on the
accompanying map. The material is ver}- deceptive. Rela-
tively very little cinnabar can be seen in the ledge filling, even
with a glass; but on washing the material, rich in disinte-
grated iron oxide, proves it to contain considerable amounts of
cinnabar.
The principal work has been done on the Providential and
Gabilan claims. In the former an incline shaft has been sunk
near the bottom of the gulch at a place where the ledge splits
in two. This shaft, course N. 74° E., on an incline of about
50°, is run along a slip, which stands nearly vertical and shows
considerable cinnabar. The bottom of the shaft is almost
entirely in a black gouge. A drift has been started S. 74° W'.,
to undercut the ground vertically under the collar of the shaft.
The sandstone is an arkose, nearly unaltered sandstone. The
work on the Gabilan, 880 feet higher, is on the top of the main
ridge; there is a shaft about 25 feet deep and some shallow
cuts, showing the same leached sandstone, wnth the quartz
seam running through the center of the mineralized zone; the
122 QUICKSILVER RESOURCES OF CALIFORNIA.
course of the ledge is here X. 54^ E., the dip 60^ southeasterly.
Some work has been done on the Buena Vista, southwest of the
Providential, showing the ledge to run north, dipping east 60°,
about 3 feet wide. The connection of this ledge with that of
the Providential can not, however, be traced on the surface.
KINGS COUNTY.
The mine (no name) in the X.W. ^ of the S.W. ^( of
Sec. 22, T. 22 S., R. 16 E., belonging to F. W. Hunter, C. F.
Francis, and G. H. French, of Parkfield, Monterey County, is
situated on Avenal Creek, east of Table Mountain, 14 miles from
Parkfield. The mine is at the contact of the serpentine and
the Chico sandstone. This contact forms a mass of rubble,
gravel, and partly cemented material, intermixed with bowl-
ders of sandstone and serpentine, and claj-, which it is claimed
on washing proves to contain cinnabar. There is a gray
sandstone resembling the sandstone carrj-ing cinnabar in the
Oceanic mine, which also here shows cinnabar. This material
is found underlaid by cemented gravel pebbles.
The serpentine on the south bank of the creek has all the
appearances of being a slide from the side of Table Mountain,
and has apparently pushed up the adjoining sandstone beds
and been partly projected within those beds. The countrj'^
has no mining timber, but a fair supplj' of fuel timber.
The mine (no name) in the S.E. J4 of the X.W. }.{ of Sec.
28, T. 22 S., R. 16 E., belonging to H. Dawson, of Lemoore,
Kings County, is on Table Mountain, 13 miles from Parkfield,
Monterey County. There is a shaft about 10 feet deep on
some fair croppings, but showing as yet no permanent forma-
tion.
The mine (no name) in the X.W. ^4 and X. }4 of the S.W
^ of Sec. 28, T. 22 S., R. 16 E., belonging to F. \V. Hunter,
C. F. Francis, and G. H. French, of Parkfield, Monterey County,
and Mrs. A. Smith, of Lemoore, Kings County, is on Table
Mountain, 13 miles from Parkfield, Monterey County. There
are a number of shallow surface openings on croppings which
show some cinnabar, but in no place has any permanent forma-
tion been disclosed.
MONTEREY COUNTY. 123
MONTEREY COUNTY.
Cholame Parkfield Mine. — In Sec. 35, T. 22 S., R. 14 E., and
Sec. 2, T. 23 S., R. 14 E.; 6 miles from Parkfield, and 32 miles
from the railroad at San Miguel. Owners, L. S. Patriquin,
G. W. Ford, and G. W. B. Anderson, of Parkfield, ^lonterey
County. This property consists of three claims, covering 4500
feet by 600 feet in width, in a course X. 60° W., following as
closely as possible a contact of serpentine and highly meta-
morphosed rocks of the Franciscan series. The outcrop of
these metamorphics is not ver>^ large. At both ends of the
property the surface is entirely in serpentine, which formation
forms the prominent surface rock of the vicinity abutting
against the Chico sandstone. It is highly silicified, and in
many cases only a surface flow; fiequently small areas of
Franciscan sandstone crop through the serpentine, while in
the gulches evidence can be found that shales underlie the
serpentine. The contact crosses a side ridge of the main
mountain range and the outcrop of the metamorphic rocks
covers the apex of this ridge. The contact has been reached
by two tunnels starting respectively from the southwest and
the northeast side of the ridge, both at about the same level,
350 feet below the highest point. The tunnel from the south-
west has just reached the contact at a distance of 964 feet from
its mouth, showing some cinnabar at the contact. The tunnel
from the northeast reaches the same contact 330 feet from the
mouth, and has been driven about 500 feet northwesterly along
the contact, showing some ore in several places. The line of
contact is very irregular, generally without any gouge, but
where there is any gouge, the slickensides show movements in
various directions, vertical and horizontal. The sandstone is
verj' much fractured and has been recemented by quartz, calcite,
and gypsum. Part of the serpentine has been highly silicified,
altered into a chalcedonic material. The cinnabar forms
principally in the fractured sandstone, but also occasionally in
the serpentine close to the contact. The tunnel from the south-
west side demonstrates that the cinnabar deposition in the
altered Franciscan sandstones is by no means restricted to the
contact. Several large ore pockets have been found in this
tunnel over 400 feet from the contact, and about 100 feet there-
from a peculiar deposit carr>-ing a very high percentage of free
121 QUICKSILVER RESOURCES OF CALIFORNIA.
sulphur, through which cinnabar is disseminated, -was cut and
followed for a few feet. The metamorphic rocks are very-
much shattered; large crevices, probably resulting from earth-
quakes, are frequently found. The entire formation has an
ochery character from oxidized iron sulphides, and in several
places can be seen the effects of the high heat resulting from
the oxidation of these sulphides. There are several surface
cuts wherein good ore has been found on the contact. The
richest surface deposit, carrying exceedingly rich ore in altered
sandstone, is cut off by a body of serpentine. A tunnel run 50
feet below this deposit shows a most irregular formation — flint,
serpentine, then a broken mass of bowlders of flint and meta-
morphosed sandstone mixed with clay, then again serpentine,
but no signs of ore. This rich surface deposit, showing seams
of nearly pure cinnabar and metacinnabarite in fracture planes
of flinty rock, is clearly not in place, but from where it has
moved to its present position is as yet an open question. The
neighborhood is very sparsely timbered, both in regard to
mining timber and for fuel purposes.
Dutro Mine. — This is in the San Carpojo district, in the south-
west corner of Monterey County, two miles in an air line from
the ocean, at the head of the west fork of San Carpojo Creek,
in the S.W. % of the S.E. % of Sec. 28, T. 24 S., R. 6 E.
Owner, Frank Dutro Martinez, Santa Maria, Santa Barbara
County; G. E. Van Gordon, of Cambria, San Luis Obispo
County, lessee. This property is situated on a line of croppings
running nearly east and west, in silicified Franciscan sand-
stone. As far as can be judged the ledge has a southern dip.
On the property is a shaft which is claimed to be 100 feet deep
and a drift about 40 feet on the ledge. These works are caved
in. Judging from the material on the dump the ledge matter
is of a flinty character, carrjdng sensible amounts of cinnabar.
The vicinity is well watered and timbered.
Table Mountain Quicksilver Mine. — This property is 12 miles
from Parkfield, and 38 miles from the railroad at San Miguel;
in Sec. 30, T. 23 S., R. 15 E. Owner, G. W. White, of Park-
field, Monterey County. This mine is located on top of Table
Mountain. The surface is nearly exclusivel}- serpentine. The
works are located nearly in the center of the claim; the lowest
tunnel at about 100 feet below the top of the mountain. At
present only one tunnel, 50 feet long, in decomposed serpentine,
SAN BENITO COUNTY. 125
course X. 60" E., is accessible. On the left side it shows, over a
distance of 30 feet, a seam carrying cinnabar, slightly dipping to
the northwest. In the decomposed serpentine are found bowl-
ders of flinty quartz carrying some cinnabar, but no permanent
formation has as yet been reached. At the southeast end of the
claim a shaft 10 feet deep has been sunk on a chalcedonic
material showing some cinnabar. Between these two work-
ings a tunnel has been started, course N. 40° E., in shale, 130
feet long, the breast being in decomposed serpentine. Below
the entrance of this tunnel the Chico sandstone is found abut-
ting against the serpentine. No ore has as yet been found in
this tunnel.
SAN BENITO COUNTY.
San Benito Count}' is traversed by two parallel mountain
ranges, the Gabilan and the Mount Diablo, which unite south of
the county in Monterey County. Only in the latter — the eastern
range — have quicksilver deposits of any consequence as yet
been developed. The^- may be segregated into three districts:
The New Idria district, in the southeastern part of the county ;
the Stayton district, in the extreme northeastern corner, taking
in small portions of Merced and Santa Clara counties; and a
third district, situated nearly in the center of the county in
the mountain cluster between San Benito creek on the west
and Tres Pinos and Panoche creeks on the east, which might
properly be called the Central San Benito district. The
geology of the districts will be treated separately. [See, also.
Report State Mining Bureau of Cal., XI, page 370.] They
are not referred to in geographical sequence, owing to the
alphabetical arrangement of the respective mines in this
bulletin.
Central San Benito District. — This district contains only a few
scattered mines on which development work has been per-
formed. It is located in the Mount Diablo range, which con-
sists mainly of rocks of the Franciscan series, in places
covered by or adjacent to younger formations. Its geological
features are mentioned in the descriptions of the Bradford and
Cerro Bonito mines, the two principal mines of the district. The
country- is well timbered, both for mining and fuel purposes.
The railroad outlet is at Tres Pinos.
New Idria District. — The New Idria, San Carlos, Sulphur
Spring, and Molina mines in this district were discovered in the
126 QUICKSILVER RESOURCES OF CALIFORNIA.
early 5o"s by miners who had worked near the present site of
the Aurora mine on what was at first supposed to be a silver
mine, but which proved to be a deposit of chrome iron.
The geological map of the quicksilver district in the southern
portion of San Benito County shows that this district contains
a belt of metamorphic rocks having a general northwest strike,
bounded on both sides by Chico formations, and consisting of
a belt of serpentine in the center, having to the northeast a
rather narrow belt of metamorphic rocks, mainly sandstone,
and to the southeast a much wider belt of metamorphic rocks,
containing, however, much more slate. The main deposits of
quicksilver ores are located very close to the contact of the
serpentine with these sandstones and shales. They form tw^o
parallel lines, one comprising the San Carlos, Aurora, and New
Idria mines, and the other the Picachos, Andy Johnson, and
Clear Creek mines. The Don Juan and Don Miguel mines are
outside of this contact belt, entirely in the metamorphic shales
and sandstones.
The mineralized deposits at New Idria are situated on a line
having a general northwestern trend. Between the New Idria
and San Carlos deposits, which are extensively developed, are
the Sulphur Spring and Molina mines, the former being the
only one found immediately in contact with the serpentine on
this line. The country' rock of the New Idria and the San
Carlos is ver>' similar; the rocks found in the lower tunnel of
the San Carlos are strikingly similar to those found in the New
Idria mine. The geological map of this section indicates that
the high peaks of the New Idria and San Carlos are formed of
sandstones and shales, while surrounded by serpentine. This
serpentine is generally a hard, light-colored variety, only occa-
sionally changed by silicification into black opaline rock. West
of San Carlos Peak is the Aurora mine, entirely surrounded by
serpentine.
Close to the metamorphic series the Chico is sensibly dis-
turbed, but only for a belt not over looo feet wide, past which
the Chico beds of drab-colored sandstone can be seen outcrop-
ping very regularl}' at the surface.
The serpentine is by far the prevailing rock of the meta-
morphic series. There are indications that in places the ser-
pentine appearing at the surface is only a surface occurrence
and does not persist in depth, as will be seen later herein, and
also in the description of the Mexican mine, Fresno County,
/A^tHH Si ^
SAN BENITO COUNTY.
127
situated on the northeastern contact of the same belt of the
metamorphic series. The serpentinization of the rock is very
irregular, and sometimes very light, while in other places the
rock is a talcose, bluish-green serpentine, with a more or less
conchoidal fracture. Inclusions of bodies of sandstone and
shale are found in the serpentine. On a ridge over a mile long,
having a course about S. 30° W., running from the divide south
of the San Carlos, along the headwaters of Clear Creek toward
the Picachos, and at the surface entirely formed of serpentine,
all gradations from sandstone to serpentine are found. In one
inclusion of a yellow sandstone, at least 100 feet by 50 feet at
the surface, seams of serpentine over a fourth of an inch wide
cutting through
the sandstone can
be seen. The ac-
companying pho-
tograph (No. 11)
of a thin section
(enlarged) con-
clusively proves
the serpentiniza-
tion of the sand-
stone. In the belt
between the ser-
pentine and the
Chico, a great part
of the sandstone
is so thoroughly
recrystallized by
metamorphic ac-
tion that it is very
difficult to decide in the field whether the material is meta-
morphic sedimentary^ or eruptive.
In the lower part of Clear Creek near its entrance into the
San Benito, a conglomerate is found on the hills, containing
pebbles of all kinds of rocks, including serpentine. This
region must have been a lake of large dimensions, as conglom-
erate is found 1 100 feet above the level of Hernandez. Another
appearance of conglomerate is found overlying metamorphic
sandstones and shales, at an elevation of 4700 feet (2150 feet
above Hernandez), forming the highest point of the mountain
cluster, which forms the big bend of San Benito Creek, south
of the Picachos (Dominic Peak).
PHOTO No. n. Thin Section of Sandstone and
Serpentine from Xew Idria District.
41 Diameters.
*i>llciili .ilcyivJijy
t: ^A/.
n
t ' ■
I
r jh cr o af "y
T
1
SAN BENITO COUNTY.
127
situated on the northeastern contact of the same belt of the
metamorphic series. The serpentinization of the rock is very
irregular, and sometimes very light, ^vhile in other places the
rock is a talcose, bluish-green serpentine, with a more or less
conchoidal fracture. Inclusions of bodies of sandstone and
shale are found in the serpentine. On a ridge over a mile long,
having a course about S. 30° W., running from the divide south
of the San Carlos, along the headwaters of Clear Creek toward
the Picachos, and at the surface entirely formed of serpentine,
all gradations from sandstone to serpentine are found. In one
inclusion of a yellow sandstone, at least 100 feet b}' 50 feet at
the surface, seams of serpentine over a fourth of an inch wide
cutting through
the sandstone can
be seen. The ac-
companj'ing pho-
tograph (Xo. 11)
of a thin section
(enlarged) con-
clusively proves
the serpentiniza-
tion of the sand-
stone. In the belt
between the ser-
pentine and the
Chico, a great part
of the sandstone
is so thoroughly
recrystallized by
metamorphic ac-
tion that it is very
difficult to decide in the field whether the material is meta-
morphic sedimentary or eruptive.
In the lower part of Clear Creek near its entrance into the
San Benito, a conglomerate is found on the hills, containing
pebbles of all kinds of rocks, including serpentine. This
region must have been a lake of large dimensions, as conglom-
erate is found 1 100 feet above the level of Hernandez. Another
appearance of conglomerate is found overlying metamorphic
sandstones and shales, at an elevation of 4700 feet (2150 feet
above Hernandez), forming the highest point of the mountain
cluster, which forms the big bend of San Benito Creek, south
of the Picachos (Dominic Peak).
PHOTO No. 11. Thin Section of Sandstone and
Serpentine from New Idria District.
41 Diameters.
12S QUICKSILVER RESOUKCES OF CALIFORNIA.
Along the lower course of Clear Creek and its drainage
serpentine and metamorphic sandstones are very intricately
mixed. For a considerable distance the creek and its tributa-
ries have cut their beds in the serpentine, while above on the
ridges sandstone is extensively represented, indicating that
the serpentine underlies the sandstone, which latter is generally
strongly silicified. The serpentine itself is generally silicified
to a certain extent, and the entire formation, at the surface
where the serpentine shows, looks as though the sandstone
has been eroded. Part of the serpentine is denuded of vege-
tation, and the material has deteriorated into a granular
mass ; but a great portion of the serpentine territory is covered
with brush. In some places in the region between Clear Creek
and San Benito Creek, the barren serpentine is capped by a few
feet of ferruginous chert, containing so much iron that the
entire rock has a brownish-red color. These patches are
covered with brush, and as the soil in the part of the serpentine
belt covered with brush has a much darker appearance than
that of the barren ground, which is light yellow to white, it
must be supposed that the iron contents of the serpentine have
a certain influence on the growth of brush. Whether the iron
content is due to the character of the rock which has been
serpentinized is as yet an open question.
The schists of the older series are found in a few places — in
the bottom of Clear Creek Caiion just above and below the
Clear Creek mine, and in San Benito Creek, near the south-
east corner of Sec. 22, T. i8 S., R. II E. In Clear Creek Canon
the schists underlie the serpentine, and are partly ver3^ much
distorted, but their strike is about N. 45° E., dip nearly verti-
cal southeast. In San Benito Cafion they are exposed on the
east side of the creek, the opposite side being formed of thinly
bedded shales, probabh- belonging to the Chico, having a south-
east strike and a southwest dip. The schists are not very
wide, and are inclosed in sandstones. Another small cropping
of schist is found a little higher up the creek at the New York
mine.
In San Benito Canon, near the Don Juan mine, the non-
conformity of the metamorphic series, with a strike nearly east
and west and a dip south, and the Chico on the other side of
the creek, with a strike S. 45°-6o° E., dip southwest, is strik-
ingly illustrated. Going up the canon above the old retort of
the Don Juan mine the metamorphic shales can be seen under-
I I Serpenlirg
I I /ie/omorp/>.
\ I Aoi^ Igneous
t i Bos/c /gneous
Geolojo' l>y Wi". Korstiier, E.M.
Geological Map of Stayton Mining District.
Issued by the California State Mining Bureau— Lewis E. Aubury. State Mineralogist, 1903.
SAN BENITO COUNTY. 129
lying the sandstones, which form nearly the entire surface of
Dominic Peak, the mountain between the elbow of San Benito
and Picachos creeks, except at its highest point (4720 feet),
1900 feet above the creek, which is covered by a conglomerate,
traces of which can be found nowhere on the mountain side.
Part of the sandstone is only slightly silicified, principally by
quartz seams in the fractures; but on the southern part of the
top of this hill, jasper is found in sensible quantity, while this
formation is rare on the hillsides. The sandstones are non-
conformable with the underlying shales. The chert beds are
almost entirely absent in this region. Only one very small
exposure in the lower part of Clear Creek has been observed,
which contains a great amount of iron oxide. Jasper is also
but slightly represented. In fact the silicification process has
not been so intense in this region as in other parts of the
quicksilver belt. The question might arise whether this
phenomenon has any connection with the small representation
of igneous rocks and the absence of mineral springs in this
region. The small extent of the later opalizing silicification is
also to be noted, no belts of opaline rock being found in close
proximity to the ore deposits, while such rocks are found to
some extent in the mass of serpentine.
The district is from 60 to 70 miles distant from the railroad
at Tres Pinos, San Benito County, with which it is connected
by two good roads from New Idria via Vallecitos Canon, and
from Hernandez down San Benito Creek.
The supply of timber is rather scarce. The price of cord-
wood is from $5 to $6.50 per cord; round mining timber, 11
inches at the small end, costs 12 cents and over per linear foot;
square timber, including freight from railroad ($12 to ^18 per
ton), costs $40 and over per 1000 feet (B. M.).
Stayton District. — This district is situated in the corner of
San Benito, Merced, and Santa Clara counties, and comprises
parts of these three counties, but being principally in San
Benito County is included within the latter. [See geological
map of the Stayton District.]
The surface rock of this district is prominently of igneous
origin and except in the northwestern part the underlying
sedimentaries are almost exclusively found in the bottoms of
the deeply -eroded gulches. The post-Tertiary igneous rocks
vary greatly in character; from very fine-grained, dark-colored
basic, basaltic rocks, to very fine-grained, hard, nearly white
9— QR
130 QUICKSILVER RESOURCES OF CALIFORNIA.
acidic rocks. The great majority is, however, a light grayish-
colored porphj^ritic rock, which Whitney [see Geology of Cali-
fornia, page 46] classified as trachyte, but which closely
answers the asperites described by Becker. [See Mon. XIII,
page 151.] There is no doubt that this district has been the
locus of repeated igneous eruptions, and that these different
igneous rocks represent various stages of magmatic differentia-
tion. [See Prof. \V. Brogger, Q. J. of the Geol. Society,
vol. L, page 29, and vol. LII, page 607 and following; J. P. Idd-
ings, ibid., page 609, and Bull. Phil. Soc. of Wash., vol. XII,
page 151.]
The sedimentar\' rocks belong to the metamorphic series,
prominently sandstones. At one place at the northwest foot
of Mariposa Peak, a small exposure of chert was found.
Some shales are also exposed, and at one place in I,os Banos
Creek, at the foot of the grade of the road from Staj'ton to
lyOS Banos, a fine compact conglomerate is found which may
probabl}' represent the conglomerate forming the basal mem-
ber of the metamorphic series, as described by Fairbanks.
[See Bull. Geol. Soc. of America, vol. VI.] This conglomer-
ate must not be confounded with the coarse conglomerate
forming at present in the beds of some creeks. Only at one
place in the northwest corner of the district, in the old Com-
stock property, is an exposure of serpentine noted, and this
not over 1000 feet wide, abutting to the w^est against schist
and to the east against a flow of basalt.
There are no hot springs in the district, but in the western
belt, sulphur emanations, principally carrying antimonious ores,
are very prominent, and the ledge matter and part of the wall
rocks in all the metalliferous deposits have been so thoroughh-
leached by sulphurous waters that the determination of their
original composition is extremel}^ difficult, if not impossible.
The ore deposition is undoubtedly posterior to the eruption
and consolidation of the volcanic rocks. At one place in the
Staj-ton mine, cinnabar can be found replacing some leached
minerals in the igneous rocks.
The district is about 16 miles from the railroad at Hollister,
San Benito County. The vicinity is practically void of mining
timber, but there is ample fuel timber at $3 per cord.
The following claims as nvimbered on the map are in this
district: i. Santa Cruz; 2. Mariposa; 3. Green Valley; 4. F,
Smith; 5. Cold Spring; 6. McLeod; 7. Badger; 8. Fairplay;
SAN BENITO COUNTY. 131
9. Santa Clara; 10. Pacific; 11. Last Chance; 12. North Star;
13. Stayton.
Andy Johnson Mine. — New Idria District, in Sec. 13, T. 18 S.,
R. 11 E., and Sec. 18, T. 18 S., R. 12 E. Thomas Flint, owner,
Hollister. This mine is located on the line of croppings men
tioned in the general description of the district, running from
the Picachos to the Clear Creek mine. All the old works are
inaccessible.
Aurora Mine ( formerly Morning Star ) . — New Idria District. In
Sec. 5, T. 18 S., R. 12 E. Owners, A. Leonard, San Benito;
Thomas Flint, Hollister; Estate of Ig. Ceseiio; S. E. Sadler,
No. 34 Steuart street, San Francisco; bonded to the Aurora
Quicksilver Mining Company, B. J. Potter, president. No. 165
East Twelfth street, Oakland. Contains eight claims, the
Aurora, Leonard, Molly O, Morgan, Aurora Extension, Morn-
ing Star, Sadler, and Traction. This property was discovered
in 1853 and efforts have been made at different times to pros-
pect it. The property is located on a line of croppings having
a course S. 15° E., situated south of San Carlos Creek at the
foot of San Carlos Peak, and running up about half wa)^ to
the top of the divide between San Carlos and Clear creeks.
These croppings are about 600 feet long and from 50 to 100
feet wide. Their course prolonged to the northwest would
come very close to the New Idria mine. They are entirely
surrounded by serpentine, and no other rock is found at the
surface; neither do the short tunnels and shallow open cuts on
the mine show any other material. The upper tunnel, 10 feet
long, is 275 feet above the furnace. Another tunnel, 25 feet
long, near the bed of the creek, is 25 feet above the same level.
Both show only serpentine. There is a large open cut on the
hillside in the croppings, from which some ore has been taken.
Above the latter is an open cut, 200 feet above the furnace
level, which is about 100 feet long and 30 feet high. The
course of its face is about northeast. In the northeastern half,
a horizontal stratum of opalized serpentine 3 feet wide and
carrying seams of cinnabar is found. This property is equipped
with a two-chamber Fitzgerald furnace.
Bradford Mine (formerly Cerro Gordo). — Central San Benito
District. In Sees. 3, 4, and 9, T. 15 S., R. 8 E. Owner, H. R.
Bradford, No. 7 North Market street, San Jose. This mine lies
on Tres Pinos Creek. The drainage of this creek is, up to
about one mile below the mine, in gravel beds lying nearly
132
QUICKSILVER RESOURCES OF CALIFORNIA.
horizontal. At Johnson's place, sandstone appears on the
south side of the creek, in narrow beds standing nearly vertical.
The sandstone belt runs along the west side of the propert}-; to
the east lies a wide belt of serpentine. Both the sandstone and
the serpentine have a northwesterly strike. The serpentine
as found in the mine workings dips northeast. [See Fig. 45.]
Elev.of collar 2280
Section
Tunnel
jnclmedShoH
plan
Fig. 45. Workings. Bradford Mine.
The western part of the serpentine consists of a highh- silicified
belt of varying width, in part opaline rock, carn.-ing some
cinnabar. Between this belt and the sandstone is a wide belt
of black gouge, and at least one other belt of black gouge has
been found in tunnel No. 2 in the silicified serpentine. The
width of the contact gouge between the sandstone and the
overlying serpentine is not known, but from surface indications
SAN BENITO COUNTY. 133
it must be rather wide. Where crosscut at the bottom of the
shaft [see Fig. 45] , the opalized serpentine between the gouges
is only 16 feet wide. The next gouge is at that place 160 feet
wide. This opalized serpentine crops out in a northwestern
direction past the boundar}' of the property, and north of the
creek. It carries some cinnabar, but as yet no body of work-
able ore has been found.
The incline shaft, following the contact of the opalized ser-
pentine with the underlying gouge, has been sunk 200 feet on
the incline. A tunnel has been run 160 feet vertically below
the collar of this shaft; it is 535 feet long, and reaches under
the shaft, but follows the contact of the opalized serpentine
and the overlying gouge. No ore bodies have been disclosed
by this work; however, the serpentine carries some cinnabar
throughout.
The surrounding country is well timbered. The mine is 18
miles from Tres Pinos railroad station, connected by a good
wagon road. The existence of cinnabar in the locality was
discovered in 1859 as an incident of the work of constructing
a wagon road by the New Idria Mining Company, and much
effort by various parties has since been expended in the pros-
pecting and development of the early find.
Butts Mine. — Central San Benito District. In Sec. 4, T. 16 S.,
R. 8 E. Wm. Butts, of Pine Rock, San Benito County, owner.
The country rock is a coarse sandstone, through which cuts a
ledge having a course nearly southwest, dipping north about
50°, wherein some sandstone occurs; seams of silica fill the
fractures of the sandstone, and carry a great amount of iron
oxides. The formation in the neighborhood of this ledge is
very irregular; shales, chert, and some serpentine are found all
intricatel}' mixed up. Except near the croppings of the ledge
no workable ores have as yet been found. A tunnel 300 feet
long has been run, and a shallow shaft about 20 feet deep has been
sunk. The property is equipped with a 2 Q retort furnace.
The neighborhood of the property contains some fuel timber,
but little mining timber. The distance from Tres Pinos rail-
road station is 21 miles by a good wagon road.
Cannon Mine. — Central San Benito District. In Sec. 4, T. 15 S.,
R. 8 W. A. C. Cannon, of Emmett, San Benito County,
owner. This property lies adjacent to and north of the Bradford,
184
QUICKSILVER RESOURCES OF CALIFORNIA.
on the same croppings. A drift 130 feet long has been run,
with a winze 30 feet deep in the silicified serpentine. At the
bottom of the winze is a drift 90 feet long, showing that the
serpentine carries some cinnabar, but without disclosing a pay
shoot.
T15S. EWE.
CERRO BENITO MINE
Cerro Bonito Mine. — Central San Benito District. In Sec. 31,
T. 15 S., R. 10 E., and Sec. 6, T. 16 S., R. 10 E. Cerro Bonito
Quicksilver Company, owner; H. R. Bradford, No. 7 North
Market street, San Jose, general manager; James Tread-
well, San Francisco, president; S. T. Kennedy, Llanada, San
Benito County, superintendent. This mine was opened about
SAN BENITO COUNTY. 135
1874 and worked by the old Cerro Bonito Company until 1876.
It is stated that the mine has produced about 800 flasks.
The present company, organized September, 1902, has been
working this property since then, and is at present reopening
the main tunnel. This work has proceeded to a length of
650 feet, the entire length of the tunnel being 930 feet. This
tunnel, as far as opened, is in the black gouge mixed with
some sandstone; from a shoot connecting with the old upper
works, some jaspery material has come down, showing some
cinnabar. The companj^ is also refitting the old 25-ton coarse-
ore furnace. The old workings consist of a great amount of
surface work and numerous underground works, which are
largely inaccessible; but those which can be entered show
development to have been very extensive. Up to the present
time the company has not reopened any large ore bodies.
The entire geology of the neighborhood is verj^ complicated,
and from what is disclosed in the works that can be entered,
no sufficient data can be collected to give a satisfactory^ and
clear description of the geology. Between the property and
Panoche Valley is a flow of basalt — probably a surface flow.
This appears, judged from surface indications, to be the only
igneous rock in the vicinity. The top of Cerro Bonito Hill,
which rises steeply, is surrounded by two lines of bluffs [see
map of the Cerro Bonito mine] , one forming the top itself, the
other from 200 to 300 feet lower and much more prominent,
especially on the north and northwest sides, where in places the
bluffs are 100 feet high. These bluffs are formed of a hard silice-
ous material, most probably a metamorphic breccia recemented
by silicification. Some black opaline rock is found through this
rock, and occasionally some sandstone. The true relation
between this breccia and the bedded sandstone can not be
traced from the present accessible development works. In
three places the breccia overlies the regularly bedded sand-
stone. Going northwest from the southern part of the prop-
erty these places are:
First — Sandstone tunnel (^) [see map], an extensive and
intricate network of underground drifts, winzes, and shafts, in
sandstone. At their western end a gouge is found dipping
from 10° to 15° in a westerly direction and carrying some ser-
pentine coming in from the roof and overlying the sandstone
which lies in nearly horizontal regular beds, especially in the
136 QUICKSILVER RESOURCES OF CALIFORNIA.
western part of the works; near the mouth of the works some
nearly vertical narrow seams of quartz cut through the sand-
stone.
Second — Farther northwest is an open cut (/), from which
extensive works run into the hill. In one of these the breccia
is found overlying the sandstone, dipping about 30*^ N., 40^^ E.
This breccia is found continuous to the old open cut works and
carries cinnabar all through, overl3dng a stratum of serpentine.
Third — Northeast of this work is a long tunnel {h) running
in a southwesterl}' direction. In this tunnel sandstone is found
underlying the breccia, which is for long distances replaced by
black gouge. Near the end of the opened part of the tunnel,
which is 815 feet long, the cross-section is in horizontally
bedded sandstone, with narrow seams of black clay and quartz,
which underlies the black gouge. On the hillside above this
tunnel are prominent croppings of the breccia.
The ore bodies in these works have never been connected
with those in the underground
works in the main tunnel, and
appear to be a separate deposit.
From the fact that in the sand-
stone tunnel cinnabar is found
in the sandstone, it must be
concluded that the ore deposi-
tion took place through water
Fig. 46. Elevation open cut ( ^ ), Cerro i i .,• .■, ■% .i •
Bonito Mine. chanuds cutting through this
sandstone; but the occurrence
of the recemented breccia so extensively overhing unaltered
and undisturbed sandstone is as yet unexplained. The large
bodies of black gouge (attrition products), showing very impor-
tant movements in the strata resting upon these same sand-
stone beds, render the explanation all the more difficult. It is
hardly conceivable that all this metamorphic material has been
moved into its present position by dynamic action finding its
center in Cerro Bonito Hill. The surface workings show a
stratum of serpentine, or may be serpentinized material, under-
Ij'ing the breccia forming the croppings and lying unconforma-
bly on the sandstones and shales. [See Fig. 46.] The croppings
southwest of the discovery point, wherein a short tunnel and
a shallow shaft are located, are much more serpentinized and
SAN BENITO COUNTY. 137
show some cinnabar all through in a softer, more weathered
material than in the other croppings.
The cinnabar forms generally in the hard, siliceous brecciated
material, which may be considered the gangue rock. It is
claimed that verj^ rich ore was found in the surface openings,
though none is at present visible; it was probably in the softer
and more open parts of the rock.
The vicinity of this mine is supplied with timber for both
mining and fuel purposes. The mine is 3 miles from Llanada,
a stage station 31 miles from Tres Pinos.
Clear Creek Mine and adjacent Boston Mine, also called the
Monterey Mine. New Idria District. In Sees. 2, 11, and 12,
T. 18 S., R. II E. Thomas Flint, of Hollister. owner. These
mines lie on a line of croppings which run from the northern
end of the Clear Creek mine in a direction about S. 30° E. to
the Los Picachos mine, in Sees. 19 and 20, T. 18 S., R. 12 E.;
passing through the Andy Johnson mine. They are not con-
tinuous, but show suflSciently to trace their line. These crop-
pings are of a light yellow ochery material, traversed by a
network of quartz veins and some serpentine seams. In places
the rock contains a great amount of iron oxide, becoming
brownish-red in color. The cinnabar appears to be scattered
all through the rock in those places where it is mineralized.
The upper croppings of the Clear Creek mine, 590 feet above
the level of the creek, have been extensively worked and a
road has been built from there to the furnace in the creek.
The lower croppings, 305 feet above the same level, also show
extensive operations, and some good ore can yet be found on
the dump. The cinnabar is scattered through the rock in
crystalline aggregates and along the fracture seams. While no
pyritic ore is found on the dump, it is more than probable that
it will prove to be the same mass of silica, highly permeated
with iron sulphide, found in the Los Picachos mine. Between
the croppings and the creek level some remnants of an almost
entirely covered-up tunnel can be seen, and a long tunnel has
been run on the line of the croppings about N. 30*^ \V. at the
level of the creek, but is at present inaccessible. About one
mile below this mine is a dismantled furnace.
Don Juan and Don Miguel Mines. — This group, also called the
San Benito, and sometimes the Cody mine. New Idria District,
138 QUICKSILVER RESOURCES OF CALIFORNIA.
is in Sec. 36, T. 18 S., R. 11 E., and Sec. 31, T. iS S., R. 12 E.
Estate of E. J. Breen, San Francisco, owner. The works are
inaccessible, but judging from the dumps the ore forms in a
shale interstratified with thin layers of sandstone, which in the
rock exposed to the air is colored brown by oxide of iron. The
cinnabar forms in the cross joints of the undisturbed rocks, and
in crushed pieces along the fracture planes. The main tunnel
is 45 feet above the level of the creek. The ore was followed
down with a shaft until the water came in too freely to be
handled. The strike of the croppings is northwesterly. To
the southeast they abut against a body of sandstone, which
can be seen, in the canon running into the San Benito above the
mine, to be overh'ing the metamorphic shales. The latter have
an east and west strike, dipping southerlj' 70°.
Fourth of July Mine,— New Idria District. In Sec. 18, T. 18 S.,
R. 12 E. Thomas Flint, of Hollister, owner. This property
is located on a line of croppings running about parallel to the
northeast and lower down the ridge than those of the Andy
Johnson. None of the old workings are accessible.
Mariposa Mine. — Stayton District. [See Santa Cruz Mine.]
New Idria Mine. — This property is situated in Sees. 29 and 32,
and parts of 28, 33, 34, and 35, T. 17 S., R. 12 E., and Sees.
3 and 4, T. 18 S., R. 12 E. The New Idria Quicksilver Mining
Companj-, owner; B. M. Newcomb, general superintendent. Oat-
hill, Napa County; J. G. Finch, superintendent. New Idria, San
Benito County. [See Mon. XIII, U. S. G. S., page 291 ; Report
State Mining Bureau of Cal., VIII, page 483; XI, page 373;
XIII, page 599.]
Several mines are embraced under this heading: as the
Washington, New Idria, Sulphur Spring, Molina, and San
Carlos mines. The mines were discovered and located in 1853,
and several of them have been operated to a greater or less
extent since that time almost continuously. The company
operating the property at present acquired it by purchase in
1895, and has since made manj- and extensive changes in the
earlier mining and reduction methods, so that the works of
to-day present a different aspect from those described b}- Dr.
Becker.
The New Idria mine is the principal and the largest profit-
producer of all the mines of the group. Several miles of
140
QUICKSILVER RESOURCES OF CALIFORNIA.
underground work have been developed in this mine, of which
over two miles are at present open.
The Xew Hope vein has not been w^orked for years, and
what Dr. Becker called the stockwercks forms at present the
N
X\:s 'Sha/es one/
Co
•some
sondsfone
New Id
ria
Shale
>■
L.
'Ivan 6frea/f/n /he A/e^ /dna /^/ne
StbLEl/ri
Fig 47. Xew Idria Mine.
main worked ore deposit, called the Xew Idria. [See Figs. 47
and 48.] This deposit has been followed downward to the
700-foot level. Its hanging w^all is the cla}- wall of Dr. Becker;
the foot wall is a shale. The Elvan vein has been extensivelv
SAN BENITO COUNTY.
141
worked, and is at present worked between the 500 and 700-foot
levels. The Bell tunnel is at present inaccessible.
The accompanying sketch [Fig. 48] shows that the deposit
has a southerly dip. The stratification of the rock in the ore
bod}' is, however, to the north.
/^ -longing tTa//
^ -foor Wa//
Fig 48.
The ore makes as a rule in a more or less metamorphic
sandstone, but occasionally in metamorphic shale. This deposit
is strongly marked at the surface by a line of very bold crop-
pings, in places standing out over 100 feet above the hillside.
The general course of these croppings is about S. 80° W.
The material of these croppings is a highly metamorphosed
sandstone, wherein some less altered sandstone occurs and
142 QUICKSILVER RESOURCES OF CALIFORNIA.
mixed with some indurated shale, in places containing a
great amount of pj^rites and their oxidation products. The
rock, especially the softer parts, is impregnated with cinnabar,
and small aggregates of cinnabar crystals are found dissemi-
nated through very hard rock. The fissures and cracks are
often found filled with cinnabar, accompanied with calcite and
some quartz. The ledge matter contains sensible amounts of
sulphur.
Near the western edge of the croppings a very good expo-
sure of the formation is found, showing the clay wall about
ID feet thick, course N. 50° E., dipping S.W. 65°, overlaid by
shales, and in its turn overlying sandstone.
The serpentine is a few hundred feet from the New Idria
vein at the surface, but does not form either wall permanently
as far as at present developed. In
the 500-foot level it occurs at the
western end overlying the clay wall.
[See Fig. 49.] In the 700-foot level
a gouge seam containing serpentine
is found in the ore body, which
would lead one to expect that at
greater depth the serpentine may be-
come the hanging wall.
'5 Referring to Figure 47, it can be
Fig 49. Section west end fifth sccu that the orc body lies on an arc
level. New Idria Mine. ^f ^ Circlc, the Walls ClOsing iu at
both ends. The Elvan vein is closely connected with the New
Idria ore body, but the New Hope seems to be independent
and, as Dr. Becker obsen-ed, does not appear to pass the clay
wall to the northwest.
The New Idria vein is very persistent in depth; in fact, shows
on the lowest level as good, if not better ore than in the upper
part of the mine. The width of the workable ore bodies is
very irregular. In places they are 100 feet wide; in other
parts of the mine the entire body between walls is either
barren or so low grade as to be unworkable. The average dip
may be placed at 50^-55°. The cinnabar content of the differ-
ent portions of the mine depends partly on the physical char-
acter of the rock. Where the latter is strongly crushed it
contains more cinnabar, yet in places very hard rock is so
thoroughl}' impregnated with cinnabar that it becomes good
SAN BENITO COUNTY. 143
workable ore. The presence of the cinnabar in this hard rock
can only be explained by deposition from solutions by circulat-
ing in sub-capillar>' channels, hence in the deep zone of rock
fiowage.
The ore is accompanied by sensible amounts of gypsum, due
probabh' to the great amount of sulphur already mentioned.
The clay wall is probably a gouge resulting from a movement
lietween the strata, which faulted the formation, and at the
place of faulting crushed the rock, thereby causing a zone emi-
nently predisposed for ore deposition. The clay wall has as
yet not been prospected any distance on either side of the Xew
Idria ore body. It is probable that other ore bodies will be
found on this line of fracturing. The ground in the mine is
rather heavy, requiring square-set timbering and filling in the
stopes.
Through a very well-conceived plan of chutes throughout the
mine and b)' the use of an old incline shaft connecting the 500
and the 700-foot levels, all ore broken in the mine can be sent
down to the latter level, from which point it is carried by
tramway to ore bins located on the hillside above the reduction
works, where, after passing over grizzlies, it is distributed by two
gravity tramways to the fine and coarse ore furnaces respec-
tively. A considerable portion of the ore treated is obtained
from the surface, part of it being from the croppings before
described, and part from the old dumps, the resultants of earl 5'
years' working. Much of this material finds its way to the
reduction works through the same channel as above described.
[See Fig. 47.] Thus the cost of its transportation from the
mine to the reduction works is minimized.
The timbers in the 700-foot level are coated with whitewash.
By this very simple method these mining timbers, which were
formerly covered by fungi and destroyed by the acids in the mine
water within a few months, now remain entirely sound after
having been in the mine over eighteen months.
The mine is equipped with a Scott fine-ore furnace handling
60 tons per twenty-four hours, and a coarse-ore furnace han-
dling nearly 100 tons per twenty-four hours. [See chapter on
Aretallurgy. page 197.]
San Carlos Mine. — Xew Idria District. This is in Sec. 4,
T. 18 S., R. 12 E., and forms one of the group of mines of the
144 QUICKSILVER RESOURCES OF CALIFORNIA.
New Idria Company. This mine was discovered in 1858 and
was worked to a very limited extent — more in the nature of
surface prospecting than as legitimate mining work; but in
later years discoveries of ver^- rich superficial ore bodies were
made, and were worked over quite an extent of surface, with
great profit to the owners. Late workings have so far failed
to discover any deep deposits of value. As will be seen from
the map of the district no serpentine appears at the surface in
the ground covered b}' this mine. The country rock is princi-
pally metamorphic shales and sandstone. Some of the rock
has the appearance of a probable igneous origin.
Plan
^ N70'L-I50
% oandsrone
% ° / i I
"S/ia/es I 1
Shty/e &^y^^^^^^^=::r-~~....^ front Elevaf/on
Serpent^
Fig. 50. Open cut, San Carlos Mine.
{a) Drift in altered shale.
(b) Sandstone carrj-ing some cinnabar.
( (/) Decomposed serpentine dipping a little north of east.
{/) Very hard silicified serpentine carrying cinnabar.
In the face of one of the open cuts [see Fig. 50] serpentine
is found containing sensible amounts of cinnabar. This ser-
pentine overlies the shales, and from the appearance of the cuts
both the shales and the sandstone carried cinnabar; but this
ore did not persist to any considerable depth. The ore formed
in all formations, but the channels through which it reached
the surface are as 3'et unproven.
Two tunnels have been run in a northeasterh- direction from
the northwest side of the peak under the open cuts, about 100
feet below their bottom. These tunnels run principalh- through
SAN BENITO COUNTY. 145
metamorphic shale. Some ore was found in them, but not in
such quantity or position as to justify the assumption that the
channel through which these extensive deposits at the surface
were fed has been intersected.
A crosscut tunnel, 260 feet below the latter tunnels and
started from the south side of the peak, is now iioo feet in,
running on a course nearly X. 60° W., but has not reached the
territory under the open cuts. This tunnel runs through meta-
morphic shales and sandstones. For the first 500 feet the strata
are much distorted and crushed, but after passing through
about 50 feet of indurated black cla^^ stratified in nearly verti-
cal beds and having a strike of about X. 70° W., the formation
becomes more regular, both the shales and sandstones having
conformable strata. Xearer the breast sandstones prevail,
while in the first part of the tunnel shales are the prevailing
material. In a gouge seam, standing nearly vertical and cut-
ting through sandstone, are found several quartz seams, some
having large quartz crystals. Gypsum and calcite are found
in the seams of the shales. Xear the breast the sandstone has
inclusions of fine-textured rock, and in some of the seams
carries chalcopyrite.
Philadelphia and New York Mines, — Xew Idria District. In
Sees. 23, 25, and 26, T. iS S., R. 11 E. Estate of E. J. Breen,
San Francisco, owner. They are located on a stratified shale,
colored deeply red with oxide of iron. These shales have a
strike about southeast, dip southwesterly, which strike brings
them about in the direction of the Don Juan mine, higher up
San Benito Creek. In the northwestern part of the property,
in the Philadelphia claim, considerable work has been done,
consisting of a tunnel 100 feet long, course northeast, a large
open cut in the steep hillside, and a smaller cut with a short
tunnel, 125 feet above the tunnel. There are no signs of cin-
nabar ore in the works or on the dump. In the New York
mine little or no work has been done.
Ramirez Consolidated Mine (formerly Los Picachos Mine).—
New Idria District. In Sees. 19 and 20, T. 18 S., R. 12 E.
\V. A. Stuart, and others, owners, Xo. 606 Montgomery street,
San Francisco. This mine derived its name of Los Picachos
from a series of bluffs cropping boldly above the hillside to au
146
QUICKSILVER RESOURCES OF CALIFORNIA.
elevation of from loo to 250 feet. These bluflEs belong to the sys-
tem of croppings showing at the surface in a line, having a
course X. 30^ W., from this mine across the Andy Johnson to the
north end of the Clear Creek mine, a distance of over four
miles. The croppings on this mine are not onh- bolder, but
also delineate both sides of a bod}- of siliceous rock cutting
through the serpentine countn,', having a width of from 300
to 600 feet. To the southeast thev can not be found further
PHOTO No. 13. LOS PICACHOS MINE (RAMIREZ CONSOLIDATED)
than the southeastern Picachos Peak. Beyond the creek cours-
ing around that knoll is only the barren serpentine, without
any trace of mineralization. At the surface the croppings are
highly colored by the oxidation of the iron pyrites, in places
mixed with chalcopj'rite. which is found in great amount in
the unaltered rock. In the weathered rock cinnabar is found
in the fracture planes in seams of more or less thickness; also
in bedding planes and in places in crushed zones of the rock.
In the unaltered rock, cinnabar occurs mainly as a coating of
vugs. After this cinnabar was deposited a posterior deposition
SAN BENITO COUNTY. 147
of silica took place, covering the cinnabar. The rock itself is
not impregnated with cinnabar, probably due to its compact-
ness. The face of the bluffs shows a stratification in the rock
forming the croppings; in the southeastern part of the property
the strata have a strike S. 40° E., dipping N.E. 60*^. The cin-
nabar is found in the bedding planes; in other places cinnabar
is found in the joint planes. In the northwestern part of the
mine these strata have a strike N. 30° E., and dip southeast.
The line of the croppings is not quite straight, while in the
southeast portion the strike is parallel with that of the crop-
pings; it is across that of the croppings in the northwestern
portion.
There are a great number of old workings, which at present
are inaccessible, and the remnants of an old furnace. The
present owners are doing some surface development, having
some good ore at the surface. The mine is equipped with a
i2-pipe retort furnace.
Santa Cruz and Mariposa Mines. — Stayton Mining District. In
Sees. 20, 21, 28, and 29, T. 11 S., R. 7 E.. at the western foot
of Mariposa Peak. H. French, of Lone Tree, San Benito
County, owner. [See Report State Mining Bureau of Cal., XII,
pages 365 and 366.] These mines are in a verj' thoroughly
decomposed igneous rock. The old works give out verj- strong
sulphur emanations. In former years they yielded some quick-
silver by retorting, but are at present virtually abandoned.
Stayton Mines, including the Gypsy, are located in Sees. 5 and
8, T. 12 S., R. 7 E., partly in San Benito and partly in Merced
counties. The Staj'ton Mining Company, owner; S. H. Smith,
secretary and general manager, Gilroy, Santa Clara County.
[See Report State Mining Bureau of Cal., VIII, page 350; X,
page 515; XI. page 371; XII, page 365; XIII, page 599.]
These mines were discovered early in the 70's and worked for
some years up to 1877. Considerable ore was taken out and
worked in one Q retort. The Gypsy mine, which now forms
part of this property, was worked in former years by several
parties. The last separate owner, the San Benito Mining
Company, erected a lo-ton fine-ore Scott furnace, which, how-
ever, was never put in practical operation. It is stated that
this property has produced between 800 and 1000 flasks by the
retorting process.
10 — QR
148
QUICKSILVER RESOURCES OF CALIFORNIA.
The mines are located on both slopes of the main ridge of
the Mount Diablo range. The principal cinnabar deposits are
to the east of the range, mostly accompanied by some stibnite;
but some cinnabar-carr\-ing veins are found west thereof, in
which territory, however, the principal ore deposits are exclu-
sively stibnite.
The workings on the cinnabar deposits are very shallow;
the deepest workings in the Excelsior mine are not over 140
feet on the dip of the vein. [See g, map of Stayton Mining
District.] A tunnel (/) over 1200 feet long, in a direction
nearlj' perpendicular to the general strike of the mineralized
zone, cuts the formation at the deepest point at a vertical
depth of about 300 feet. It is inaccessible, but judging from
the dump the material is princi-
palh*, if not exclusively, igne-
ous. The strike of the mineral-
ized zones east of the main
ridge is nearly north and south,
and from south of the cabin to
g, a distance of over three
fourths of a mile, the cinnabar-
canying ledge matter is exposed
in several places, dipping west
at an angle of about 45*^. To
the east of this zone lies in its
southern part a belt of basalt. The ledge matter is an altered
rhyolite, containing besides cinnabar, iron sulphides, gypsum,
and occasionally some stibnite. In the southern part, North
Star {b) and Graybuck {a) workings [see Fig. 51], this ledge
matter is associated with a belt of chalcedonic quartz, and in
places the cinnabar has formed as cavit}- filling associated with
quartz cr^'stallization. This ledge matter contains bunches of
iron pyrites, in places rich in copper. In the northern part at
g the cinnabar forms in a material which to the naked eye has
the appearance of a breccia, but under the glass is shown to
consist of a dark-colored, close-grained quartz, the darker
coloring being due to iron and antimony minerals, with inclu-
sions of much lighter-colored quartz. The ledge filling then
shows strong sulphurization and silicification actions, both
contemporaneous with the ore deposition. The main ledge is
accompanied by a number of small fissures striking a little
Fig. 51.
Section at Graybuck shaft,
Stavton Mine.
SAN LUIS OBISPO COUNTY.
149
■ 1 /,i
// ^
QVi
Drawr
\
^
>.rthyoi\y
i^ A-^^
SAN LUIS OBISPO COUNTY, 149
east of south and dipping nearly vertical, running from the
west to the main ledge both in strike and dip, a number of
which contained some very rich ore, especially near the sur-
face, but none has as yet been followed to its contact with the
main ledge; hence the question whether or not they belong to
the same fracture system is as yet unanswered.
As above stated, antimony forms the principal metallic ore
west of the ridge, yet two cinnabar deposits are found there,
close to the top of the main ridge. One, the Pacific (//), is
situated on a belt of sandstone running north and south, dip-
ping east 75°, having a seam of cinnabar ore i8 inches wide.
In close vicinity are found stibnite croppings, striking north-
west and dipping northeast. The other cinnabar deposit (/),
near the road on the divide, is associated with a prominent belt
of leached siliceous rocks, showing very peculiar cavities.
SAN LUIS OBISPO COUNTY.
General Geology. — The Santa Lucia range and its spurs cover
the northwestern part of San Luis Obispo County, in which
section are located nearly all the quicksilver deposits of the
county. They are located in zones separated by large sections
of country, which sections, as far as yet ascertained, are barren.
In the northwestern part of this territory near Pine Mountain
there is a line of cones formed of rhyolite, having a general
northwestern direction. The cones, while close together, are
not connected at the surface. Near Pine Mountain, among the
debris of the rhyolite covering the slopes of the cones, are
found bowlders of diorite, indicating prior igneous eruptions.
In the Adelaide and Oceanic districts some scattered
exposures of rhyolite are found, which have no apparent rela-
tion to each other; hence nothing can be inferred relative to
the dislocations which caused these eruptions. The serpen-
tine lies principally on the west slope of the main ridge, where
it has caused enormous slides, due to its deterioration by
atmospheric influences. Its principal exposure is at Cypress
Mountain, where, at several places, its contact can be seen
with the underlying partly altered sandstones. The entire
appearance of the serpentine mass tends to the supposition
that it is an altered peridotite. In one place on the northwest
slope of the mountain some signs of induration by contact met-
148 QUICKSILVER RESOURCES OF CALIFORNIA.
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- !>ff)0JAR3V«»« 3TAtT3 /
eoet
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SAN LUIS OBISPO COUNTY. 149
east of south and dipping nearly vertical, running from the
west to the main ledge both in strike and dip, a number of
which contained some very rich ore, especially near the sur-
face, but none has as yet been followed to its contact with the
main ledge; hence the question whether or not they belong to
the same fracture system is as yet unanswered.
As above stated, antimony forms the principal metallic ore
west of the ridge, yet two cinnabar deposits are found there,
close to the top of the main ridge. One, the Pacific (//), is
situated on a belt of sandstone running north and south, dip-
ping east 75°, having a seam of cinnabar ore i8 inches wide.
In close vicinity are found stibnite croppings, striking north-
west and dipping northeast. The other cinnabar deposit (/),
near the road on the divide, is associated with a prominent belt
of leached siliceous rocks, showing verj' peculiar cavities.
SAN LUIS OBISPO COUNTY.
General Geology. — The Santa Ivucia range and its spurs cover
the northwestern part of San Luis Obispo County, in which
section are located nearly all the quicksilver deposits of the
county. They are located in zones separated by large sections
of countr}-, which sections, as far as j-et ascertained, are barren.
In the northwestern part of this territory near Pine Mountain
there is a line of cones formed of rhj'olite, having a general
northwestern direction. The cones, while close together, are
not connected at the surface. Near Pine Mountain, among the
debris of the rhyolite covering the slopes of the cones, are
found bowlders of diorite, indicating prior igneous eruptions.
In the Adelaide and Oceanic districts some scattered
exposures of rhyolite are found, which have no apparent rela-
tion to each other; hence nothing can be inferred relative to
the dislocations which caused these eruptions. The serpen-
tine lies principally on the west slope of the main ridge, where
it has caused enormous slides, due to its deterioration by
atmospheric influences. Its principal exposure is at Cypress
Mountain, where, at several places, its contact can be seen
with the underlying partly altered sandstones. The entire
appearance of the serpentine mass tends to the supposition
that it is an altered peridotite. In one place on the northwest
slope of the mountain some signs of induration by contact met-
150 QUICKSILVER RESOURCES OF CALIFORNIA.
amorphism of the adjoining sandstone can be found. The Fran-
ciscan series are prominently represented b\- sandstones, which
are ^"ery irregular in texture, grading from entirelj^ unaltered
arkose sandstones into completely' metamorphosed sandstones,
nearly, if not entirelj- quartzite. and these various phases are
intimately mixed, without any traceable S3-stem of gradation.
Adelaide District. — This district comprises the main range from
Cypress Mountain, in Sec. i, T. 27 S.. R. 9 E., to the Madrone,
in Sec. 22, T. 27 S., R. 10 E., with the territory on the north-
east slope, covering the headwaters of Las Tablas and El Paso
Robles creeks. The rocks of this district belong prominently
to the Franciscan or metamorphic series, principally sandstones,
with occasionally some shales, and in a few places exposures of
chert beds. One wide body of serpentine is found at Cypress
Mountain, extending southward past the headwaters of Santa
Rosa Creek. The whole belt has a northwest trend, and a nar-
rower and shorter belt of serpentine lies west thereof. In the
northern part of the district, on the main ridge, north of
Cypress Mountain, is an exposure of rhyolite, belonging to the
scattered exposures above mentioned; it has a northern trend,
but is of relatively small dimensions.
The territory comprising this district must at one time have
been covered by the Chico series. It is bounded on the east
and northeast by the Chico sandstone, and in places larger and
smaller patches of the same are found on the top of the ridges,
the Franciscan rocks being exposed lower down the hillside or
in the canons. At the contact, the Chico sandstones are so
much broken up and contorted that it is impossible to give any
data as to the strike and dip of the beds.
A line of croppings which can readily be followed runs in
a northwesterly direction through this district; though more
or less parallel to the direction of the main ridge of the Santa
Lucia range, this line is clearly independent thereof. These
croppings, starting from the southern part of the district in the
Madrone property, run continuously through the La Libertad,
Josephine, Alice, Modoc, and Elizabeth mines. Then the^'
become much less prominent and only show occasionally in
the ridge between Johnson and Carmine creeks and farther
north toward the Cypress Mountain group. The Karl and
Mahoney mines are situated on a belt entirely disconnected
from these croppings.
SAN LUIS OBISPO COUNTY. 151
The ore in this district is generally a whitish quartzose
material, containing small inclusions of serpentine, the cinnabar
forming principally in the seams, which show signs of later
silicification. The cinnabar is often accompanied by sensible
amounts of iron sulphides, which by their oxidation near the
surface give an ochery yellow color to the ore. As a rule, the
ore carries more iron sulphides as the cinnabar contents
increase. The ore bodies are contiguous to more or less exten-
sive strata of dark-gray to black-colored clays, mixed with
bowlders of lighter gray-colored sandstones. They are of the
same nature as that of the black clays, generalh^ associated
with quicksilver deposits — "alta," only here they are almost
invariably indurated. Their outcrops frequently accompany
those of the ore bodies; the}- are of a light gray color, having
the appearance of a disintegrated sandstone, traversed by a
network of narrow seams of an ochreous yellow color; in places
small inclusions of serpentine are found. This material, while
contiguous to the ore deposits, is always barren of cinnabar.
A great amount of work has been done in this district, espe-
cially between 1S67 and 1872; but in no mine, except the Karl,
has sufficient development work been done to enable one to
judge as to the behavior of the ore bodies in depth. In several
properties the surface disclosures would fully justify systematic
development work. The policy, however, seems generally' to
be to hunt for pockets of rich ore, which is treated in retort
furnaces, instead of opening large bodies of furnace material.
Oceanic District* — This district is situated on the west slope of
the main Santa Lucia ridge, and covers the headwaters of the
north fork of Santa Rosa Creek, Cooper Creek, and Oceanic
Creek (the three northern forks of Santa Rosa Creek) and the
divide between Santa Rosa and San Simeon creeks to the south
fork of San Simeon Creek, including Sees. 8, 9, 10, 11, 12, 13,
14, 15, 16, 17, and 24, T. 27 S., R. 9 E., and Sees. 18 and 19,
T. 27 S., R. 10 E. The geology of this district is very com-
plicated. The rocks belong almost exclusively to the Fran-
ciscan series, except in the southeastern corner, where the
younger formations overlie this series.
There are several scattered exposures of rhyolite in this
district, which apparently, however, have no relation to the
location of the ore deposits. There are very clearh- defined
lines of croppings. having a northwestern direction; one. start-
152 QUICKSILVER RESOURCES OF CALIFORNIA.
ing in the Vulture mine, crosses the divide and runs through
a part of Cooper Creek basin; another, starting southwest
thereof, crosses the divide between Cooper and Oceanic creeks,
on the ground of the Oceanic No. 2 mine, and runs through
the Oceanic mine. A third line of croppings lies northeast of
the latter, and may be those of a second or back ledge found
formerly in the old works of tunnel No. 4 and below in the
upper shaft levels of the Oceanic mine. These croppings go
some distance farther northwest, but do not reach the divide
between Santa Rosa and San Simeon creeks. On this divide a
ver}^ bold line of croppings starts northward, forming a con-
tiguous line of bluffs about a quarter of a mile long, flanked
on both sides by serpentine, which, however, appear not to
carry any cinnabar. The principal material of the croppings
is a rather light gray, flinty quartz.
The principal rocks exposed at the surface are, besides the
rhyolite above mentioned, sandstone, shales, some chert, and
occasionally some serpentine. The sandstone is generally
much decomposed, with a brownish or greenish gray color, but
not nearly as much silicified as in the Adelaide district. The
deep erosions and the fact that the country is continually slid-
ing, lead to the supposition that a large part of the underlying
rock is more or less serpentinized, which is confirmed by the fact
that in most of the gulches the hard sandstone is found under-
laid b}" shales or serpentine.
In the Lehman property the younger sandstones are found
impregnated with cinnabar in close vicinity to the rocks of the
Franciscan series, which would tend to show that the period of
ore format on was posterior to that of the deposition of those
Upper Cretaceous or Eocene rocks. As this deposition was
contemporaneous with, or closely following, a strong process of
silicification, the highly siliceous character of the ledge matter
of most of the mines is readily explained, the Franciscan series
having already undergone a prior process of silicification.
Pine Mountain District. — This district is characterized by the
great amount of exposures of rhj'olite. These rocks are lying
in a series of prominent knolls, the debris covering such wide
territory that it is impossible to give any estimate of the width
of the belt, which, however, is certainly from 100 to 400 yards
wide. The outcrops are not continuous, but are separated by
SAN LUIS OBISPO COUNTY. 153
short exposures of the Franciscan series. To the west lies
a wide belt of serpentine, which rock only shows to the east
in the territory of the Pine Mountain group. The entire
western slope of the main ridge and that part of the eastern
where the serpentine occurs, show extensive slides. Near
Rocky Butte, the Chico sandstone lies quite close to the igneous
rocks. The enormous amount of debris prevents the obser\-a-
tion of any contact metamorphic phenomena. Some bowlders
of diorite are found, but none in place. The location of these
bowlders would sviggest that the vents through which the
rhyolite was ejected were old lines of fracturing. The ore
deposits are all very close and more or less parallel, but not,
as far as yet developed, in direct contact with the igneous rocks.
San Carpoio District. — This district, in the extreme north-
western corner of the county, includes part of Monterey
Count}'. This countrj^ is very deeply eroded and the sidehills
are ver}^ steep. The country between San Carpojo Creek and
the ocean is prominently a highly silicified Franciscan sand-
stone. To the east of the creek and forming the backbone of
the main ridge is a wide belt of serpentine, along which, on
its western line, runs a belt of croppings, which, it is claimed,
can be traced from Pine Mountain to the northern watershed
of Salmon Creek, where cinnabar has been found in these
croppings. In the basin forming the headwaters of the west
fork of San Carpojo Creek runs a minor, more local, parallel
belt of serpentine, west of which are the croppings on which
the Dutro mine is found, and on the ocean slope detached
patches of serpentine can be found. There are through this
country, besides the cinnabar outcrops, several outcrops of gold
ore, on some of which prospecting is being done.
The Adelaide and Oceanic districts are not very well tim-
bered. On Cypress Mountain some durable cypress mine-
timber can be found, and to the north thereof there is some
good pine timber. The amount of available fuel is also
restricted. The Pine Mountain district is better provided with
timber. The Pine Mountain mine is equipped with a small
sawmill, and there is considerable fuel timber in this district.
The cost of timber in the Adelaide district is : round timber,
7 cents per linear foot ; lagging, 6 cents apiece ; cordwood,
$3.25 per cord. In the Oceanic district, round timber, 3^
154 QUICKSILVER RESOURCES OF CALIFORNIA.
cents per linear foot, to which must be added $8 per load for
hauling; lagging, ^j4 cents apiece; sawed timber, $15 per
1000 feet (B. M.); cordwood (pine), $4 per cord.
The Adelaide district connects with the railroad at Paso
Robles, distant from 1 6 to 20 miles. For the southern part of the
district steamship connection is made at Ca3'UCOs, distant about
12 miles. The Oceanic district is from 16 to 19 miles from San
Simeon, another steamship shipping point. The Pine Moun-
tain district is about 10 miles distant from San Simeon.
Alice and Modoc Group. — This lies in Adelaide District, in Sec.
17, T. 27 S., R. 10 E. California Consolidated Mining Com-
pany, owner; Wm. A. Stuart, No. 606 Montgomer}- street, San
Francisco. There are most probabh- two separate ore deposits
in this property. [See Fig. 52.] One, having a course X. 50°
E., and a southeasterly dip, is worked from the surface down
to a drift (n) 75 feet deeper (vertical), and showing there over
a length of 40 feet on the strike, the ore bod\' going farther at
both ends. The width of the ore body is certainly S feet, but
the roof is still in ore. From this level an understope 35 feet
deep on an incline of about 45° is in progress. Another ore
body, having a course N. 70"^ E., and a southeasterly dip, lies
about 200 feet south of the former. It is opened from the sur-
face to a level (/?) 30 feet (vertical) lower, where it is worked
out to a length of at least 60 feet on the strike, and a width of
from 6 to 7 feet. Below this level it has been partially worked,
and a chute connects this work with the lowest tunnel (c),
which is on a level with the retort, and 215 feet vertical below
the upper works. At the point where the chute connects with
this tunnel, 583 feet from mouth, the course of the ore body is
nearly east and west, dip south. The same ore body is cut by
the tunnel 460 feet from mouth, showing a width of 10 feet,
and standing nearly vertical. The propertj' is equipped with
two i2-pipe retort furnaces.
Bank Mine. — Pine Mountain District. In Sec. 36, T. 26 S.,
R. 8 E. E. S. Rigdon, of Cambria, owner. The country rock
of this property is entirely serpentine; the ledge matter is a
highly silicified serpentine, carrying cinnabar, which latter is
also sparingly disseminated through the adjacent serpentine
wall material. The tunnel was caved and inaccessible. The
SAN LUIS OBISPO COUNTY.
155
156 QUICKSILVER RESOURCES OP CALIFORNIA.
croppings indicate a very flat ledge, strike nearly east, dip north,
which is well charged with cinnabar.
Cypress Mountain Group. — Adelaide District. In Sees, i and 2,
T. 27 S., R. 9 E. J. H. Follis, of San Francisco, and E. Smith
and W. S. Forrington, of Paso Robles, owners. This group of
mines is located near the only exposure of igneous rocks
appearing in this district, and near the prominent serpentine
exposure of Cypress Mountain. The dike of rhyolite, about
three quarters of a mile long and 800 feet wide, runs about
N. 30° W. On the west side lies a readily traceable line of
croppings, which has, however, onl}^ been superficially opened
at one point, in the northwest corner of section i, by the
Columbia tunnel; the material taken out of this tunnel pros-
pects ver\' fairly in cinnabar. Most of the work has been done
on the northeast side of the rhj'olite dike; on this side the
croppings are not very plain, and scattered. In one tunnel an
ore body has been cut about 10 feet wide, in a black claj- gouge
with sandstone bowlders; whether a ledge or a lens of ore can
not be stated. On the hanging wall, but apparently belonging
to the ledge filling, is a stratum of chert}^ quartz about 12
inches thick.
Doty Mines. — Pine Mountain District. This property com-
prises five claims lying adjacent to the northwest of the Quien
Sabe mines, in Sec. 14, T. 26 S., R. 8 E. Doty Brothers, of
Cambria, owners. The lower tunnel, about 75 feet above the
creek level, is inaccessible. Judging from the dump the ore
deposit is formed in highh' silicified serpentine. Some of the
quartz seams have in their center a verj^ narrow seam of cin-
nabar; in other samples the cinnabar forms in the center of
quartz bunches, indicating that the cinnabar deposition is con-
nected with the silica formation, but posterior to the latter.
A short tunnel, 25 feet above the lower tunnel cuts very near
the entrance, a ledge having a course nearly east and west,
about 20 feet between walls. The hanging wall is a very
coarse sandstone. The gouge is very solid, the dip nearly ver-
tical. The foot wall, while too near the surface to be abso-
lutel)' determined, is probably shale, the foot-wall gouge
being much softer; its dip is verj^ flat, nearing the hanging
wall on the dip.
SAN LUIS OBISPO COUNTY. 157
Elizabeth Mine.— Adelaide District. In Sec. 17, T. 27 S.,
R. 10 E. H. Eppinger, of San Francisco, owner. This
property lies adjacent to the Alice and Modoc, on a line
of croppings running N. 30° W. Some surface openings
show that bunches of ore have been taken out. The rocks
show some signs of cinnabar. A crosscut tunnel, running
east toward these croppings, was inaccessible. The dump
showed nothing except cla3'ey material. Another tunnel, run-
ning from the road in a southeasterly direction, about east of
the retort, was also inaccessible. The property is equipped
with a lo-pipe retort furnace.
Eureka Group. — Adelaide District. In Sees. 6 and 7, T. 27 S.,
R. 10 E., and Sees, i and 12, T. 27 S., R. 9 E. Mr. R. Wear,
of Paso Robles, owner.
George and Josephine Group. — Adelaide District. In Sees. i8
and 20, T. 27 S., R. 10 E. L. G. Sinnard, of Paso Robles, and
J. Tartaglia, of Klau, owners. [See Report State Mining Bu-
reau of Cal., X, page 580.] This group lies between the Alice
and Modoc and the Ea Eibertad mines, and shows some surface
croppings and some shallow tunnels. When formerly worked
a small furnace was erected on the property. The old works
are inaccessible.
Karl Mine.— Adelaide District. In Sec. 33, T. 26 S., R. 10 E.
The Karl Quicksilver Mining Company, owner; J. Bagbj-, of
Klau, San Euis Obispo County, superintendent. A line of
croppings runs through this property, entering it in the south-
western part on an east and west course, but turning very
shortl}' after entering the propert}' to a southeastern direction.
The character of the croppings also changes a little, in so far
as they get a little less ochery than at their point of entrance.
The workable ore bodies have been exclusively developed in
the southeastern part of the propert}-. A great amount of
open cuts and extensive underground works have been made.
The company has developed two principal ledges, running
nearly parallel N. 50^ W., dipping northeast, but approaching
each other on the dip. The most southwestern ledge is localh-
called the serpentine ledge. Its foot wall is a belt of serpen-
tine from 20 to 40 feet wide, rather siliceous in places, as in
the tunnel wherein the shaft is located, taking a chalcedonic
158 QUICKSILVER RESOURCES OF CALIFORNIA.
character; this serpentine, however, does not appear at the
surface, but is capped to a depth of from 20 to 30 feet by the
croppings of the gouge accompanying the ore deposit. The
ledge matter of the serpentine ledge is a loose, coarsely-granu-
lated quartz, carrying iron and mercury sulphides. The entire
mass has a grayish-green color. Under the glass scarcely a
trace of serpentine can be found among the granules. The
color is given by the accompanying clay, which must be derived
from the serpentine. In this loosely-granulated quartz are
found bowlders of a very hard chalcedonic quartz and of a
laminated, somewhat calcareous material. Some of the bowl-
ders carry sensible amounts of cinnabar and pyrite; others are
entirely barren, and their relation to the surrounding country
rock is not clear. The hanging-wall material of this ledge,
which forms also the foot wall of the second ledge above men-
tioned, is a slightly metamorphosed sandstone. Immediatel}^
on the ledge lies a heavy claj-, colored green probably by sul-
phate of iron. The parallel ledge forms in a zone of what
appears to be a crushed country rock, probably of a quartzose
character, but having some clay in it, probably as a result of
the attrition. The ore contains considerable iron pyrite and
some free sulphur.
Both these ledges are well developed in the incline shaft
sunk from tunnel No. i, at an angle of 60°, to a depth of 155
feet from the level of the tunnel. The collar of the shaft is
125 feet below the surface. There are wide stopes in the ser-
pentine ledge above the lower level, and the parallel ledge is
also opened, showing clearl}- the difference in character of the
two ore bodies, which, however, in this level are much closer
together than at the surface.. The strike of the ledges in the
lower, or No. 3, level is N. 45° W.; the average dip is N.E. 45".
Crosscutting in the same level in a direction N. 35"^ E.
from shaft about 100 feet, the parallel ledge above mentioned
is cut, showing also important ore bodies. The foot wall of
the ore zone is a chalcedonic material, probably serpentine
altered by silicification, and colored green by sulphate of iron.
This is underlaid bj' a dark-gray indurated clay mixed with a
lighter, grayish-colored sandstone.
A great part of the product of this mine has been derived
from large open cuts. At present, however, the main ore sup-
SAX LUIS OBISPO COUNTY.
159
ply comes from the works in tunnel No. i. The furnace is an
8-tile Scott fine-ore furnace, with fourteen brick condensers
and ten stave barrel condensers.
Kismet Group. — Adelaide District. In Sec. 7, T. 27 S.,
R. ID E. F. D. Frost and E. Smith, of Paso Robles, owners.
The group comprises the Kismet, Margaret, and Alice C.
claims. A short tunnel on the Alice C. claim shows some
cinnabar-carrying rock near the mouth.
PHOTO No. U. I-.\ LII!ERT.\D MINE.
La Libertad Mine. — Adelaide District. In Sec. 21, T. 27 S.,
R. 10 E. Libertad Quicksilver Mining Company (G. A.
Trafton, of Watsonville, Santa Cruz County, president), lessee ;
owner, D. McEwen, Cambria, San Luis Obispo County. This
mine is located on the contact of a prominent belt of serpen-
tine and a sandstone belonging to the metamorphic series.
The general trend of the croppings is northwest. While the
croppings would indicate a regular strike of the ledge, the
underground works have as yet only developed ore bodies hav-
160
QUICKSILVER RESOURCES OF CALIFORNIA.
ing difierent strikes and dips, which latter are, however, all
eastward or in the hill, as the accompanying sketch of tunnel
No. 2 will indicate. [See Fig. 53.] These ore bodies lie in a
dark- gray indurated clay, intermingled with a great number
of sandstone bowlders carrying some serpentine. This material
appears to be the contact zone of the sandstone and serpentine.
The ore bodies are formed by rather hard quartzose bodies of
a whitish color, having small serpentine inclusions, the cinna-
N
LIBERTAD
'
'
*^^ ^0 TUNNEL No. 2. 1
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bar forming principally in the seams, sometimes one fourth of
an inch wide, in a crystalline form.
Following about the same southeasterly strike, the croppings
can be traced, until about a quarter of a mile below the retort
the ledge crosses the creek, where the exposure shows the
ledge with a width of from 8 to 10 feet, having a very rich
streak from 6 to 8 inches wide, carrying metacinnabarite asso-
ciated with the cinnabar; course N. 50° \V., dip northeast; the
ledge matter being prominently of a flinty character, and with
a sandstone foot wall. The ledge in its southeasterly strike
diverges from the serpentine and is entirely in the sandstone.
SAN LUIS OBISPO COUNTY. 161
This exposure is loo feet below the bottom of the shaft in
tunnel No. 2, the lowest ore exposure in the northwestern part
of the property, and distant therefrom about 1500 feet in an
air line.
Southwest of the creek, the ledge crops out again. Panning
from the dirt showed here free mercury, which does not show
on the northeast side of the creek. The mine is equipped with
a lo-pipe retort furnace.
Lehman Mine. — Oceanic District. In Sec. 13, T. 27 S., R. 9 E.
F. Lehman, of Cambria, owner. This is in the Upper Cre-
taceous or Eocene sandst6ne; this sandstone is a white, fine-
grained material, with conchoidal fracture; when broken the
fracture planes have a black color and emit a bituminous odor.
Strike nearly east and west, dip S. 30°. In the seams of this
rock is a dolomitic gangue, carrj'ing some cinnabar. The
developments consist of a tunnel 40 feet long, about 200 feet
below top of ridge, and a couple of shallow open cuts.
Madrone Mine. — Adelaide District. In Sec. 22, T. 27 S.,R. loE.
Madrone Quicksilver Mining Company, owner, 233 S.Broadway,
Los Angeles. The development on this property consists
entirely of surface work; the deepest accessible point is not
over 25 feet below the surface. These surface works show
very good ore, and in one place a well-defined vein, running
nearly east and west and dipping very steep northward. The
hanging-wall material could not be determined. It carries in
places sensible amounts of bitumen. Next to the hanging
wall occurs a hard flinty material carr\'ing some cinnabar; then
comes softer ochreous rock, in places ver>' rich in cinnabar;
and then a breccia on the foot wall, carrs-ing some cinnabar.
The foot wall is the indurated grayish clay and sandstone
bowlders found in all the mines in the vicinity. The property
is equipped with a lo-pipe retort furnace.
Mahoney (Buena Vista or Gould) Mine.— Adelaide District. In
Sec. 33, T. 26 S., R. 10 E. J. J. O'Toole, Parrott Building, San
Francisco, owner; A. Gould and G. Bell, of Klau, San Luis
Obispo County, lessees. This mine lies east of and adjacent
to the Karl, and very close to the Chico sandstone, which east
and southeast of it apparently overlies the Franciscan series.
Considerable work has been done in former times, and also by
162 QUICKSILVER RESOURCES OF CALIFORNIA.
the present lessees, but no regular formation, either of ore
deposition or of country rock, has as j'et been developed. The
ore is scattered in bunches through a partially indurated clay
material mixed with sandstone bowlders, verj' similar in char-
acter to the foot wall of the ore zone in the Karl. Some of
these ore bodies are of considerable size (one 400 feet in from
tunnel No. i was from 10 to 15 feet wide and about 30 feet
high), but they are without an}- regularity of arrangement.
This property is equipped with a lo-pipe retort furnace.
North Star Mine (formerly Santa Maria). — San Carpojo Dis-
trict. In Sec. 13, T. 25 S., R. 6 E. William Gillespie and
J. H. Ailing, of San Simeon, owners. It lies to the southeast
of the Polar Star.
Oceanic Mine. — Oceanic District. In Sees. 15 and 21, T. 27 S.,
R. 9 E. Oceanic Quicksilver Company, owner, No. 2 Baker
Block, Los Angeles; A. B. Thomas, president; E. W. Carson,
of Cambria, superintendent. [See Report State Mining Bureau
of Cal., VIII, page 531; X, page 5S0; XII, page 366.]
This mine was actively operated from 1876 to 1879, and pro-
duced 7400 flasks of quicksilver in that period. The mine was
onl}' sporadically worked from that time until the present com-
pany came into possession. The latter has reopened the mine
and just completed a Scott fine-ore furnace with a minimum
daily capacity of 60 tons.
The development of this mine has been done partly by open
cuts and partly by underground work. From the surface work-
ings large bodies of ore have been worked out, their general
strike being N. 55° W., dipping southwest. The ore bodies
show considerable width, and their faces show that consider-
able ore is yet available for surface work, carn'ing sufficient
cinnabar to be considered satisfactory furnace material. The
underground works consist of several tunnels; the lowest tun-
nel. No. 4, cuts the vein at a depth of 250 feet below the sur-
face. From this level a shaft has been sunk on the vein. The
lowest level at present in operation in this shaft is 185 feet
below the level of tunnel No. 4. The vein changes its dip to
the northeast about 100 feet below the level of the tunnel. The
dip, how-ever, is nearly vertical. The strike of the vein is
N. 60° W. The southern, or foot wall is a shale "mudrock,"
which material is rather prominent in the neighborhood of this
SAN LUIS OBISPO COUNTY. 163
mine and is very similar to the "mudrock" in the Manhattan
and other mines. The real hanging, or northern, wall has not
been reached in the underground works. On the ledge matter
lies a belt of black clay, with inclusions of harder material very
similar to that composing the foot wall. A crosscut lOO feet
in length in the 185-foot drift has not cut through this clay
selvage. The ledge matter proper (or the matrix wherein the
ore makes) is a coarse grayish sandstone, rather compact,
through which aggregates of cinnabar crystals and iron sul-
phide crystals are disseminated, the cinnabar not being con-
fined to seams in the sandstone. The sandstone slakes very
sensibh^ when exposed to the air, and carries some lime. These
bodies of sandstone are rather close to the hanging wall. They
are inclosed in the black clay, are not continuous, and lie with-
out any regularity in the fissure, nor is the sandstone persist-
ently ore-bearing. As far as observed, they are not connected,
although it is not improbable that such is the case, as the clay
can hardl}' have been the channel for the mineral-carrying
solutions; they must have found their channel in the less
imper\-ious sandstone.
Oceanic No. 2. — Oceanic District. In Sec. ii, T. 27 S.,
R. 9 E. F. Lehman, of Cambria, owner. This property is
located on the ridge between Cooper and Oceanic creeks, on a
line of croppings running toward the Oceanic ground. There
are some old tunnels, which are caved in.
Pine Mountain Group. — Pine Mountain District. Consists of a
group of twenty-two mining claims and several tracts of tim-
ber land situated on and around Pine Mountain, mostly on the
east slope of the mountain, in Sees. 3, 10, and 11, T. 26 S.,
R. 8 E. The American Exploration and Development Com-
pany, owner; M. Hoytema, care Jabish Clement, No. 212 San-
some street, San Francisco, and San Simeon, San Luis Obispo
County, general manager. [See Report State Mining Bureau
of Cal., \'III, page 531; X, page 580; X, page 581 — Ocean
View.]
The principal workings are situated on the east side of the
body of rhyolite forming Pine Mountain, which is the most
southern of three eruptive cones, verj' close together, but not
connected and of slightly varying material, lying along the
backbone of the main ridge. The igneous rock has covered a
II— (2R
164
QUICKSILVER RESOURCES OF CALIFORNIA.
large territory on both sides with debris. The country rock
belongs to the Franciscan series — shale, sandstone, and ser-
pentine, the latter principally on the coast slope and in the
southern part of the property from the Pine Mountain tunnel
to the Little Almaden. East of the rh3'olite of Pine Mountain,
a line of croppings can
be traced along the foot
^ of the main eruptive
<*? body, but has, in many
'' ^^ places, slid down the hill-
side. Most of the work-
^ '^ ings in the Bucke^-e, Little
Almaden, and possibly
the Pine Mountain, are
located on such slides, but
the Ocean View tunnel probabh- cuts
the ledge in place.
The main workings are : The Ocean
View lower tunnel, just below the
camp, 1300 feet long, still in progress
of drifting. The course of the tunnel
is S. 25° W. [see Fig. 54] ; the first
400 feet are in shale and a black clay
gouge, then come 10 feet of rhyolite.
An upraise leads here to a short drift
15 feet above the tunnel level, show-
ing some ore in a serpentine quartzose
material. The main tunnel con-
tinues in this latter material to 610
feet from entrance, then to 7S6 feet
in black cla}^ gouge, where it cross-
cuts the main ledge on a very obtuse
angle. The course of the ledge is
nearly south, dipping east. The material is a flinty quartz,
stained in places grayish-green by silicate of iron. The cin-
nabar occurs principally as paint, especialh" in bunches. Past
this ledge to the breast the tunnel is in black gouge. Above
the level of this tunnel considerable work has been done. A
winze runs up 65 feet and two levels have been run above the
tunnel level. There are also two old upper tunnels. Out of
'2815
Fig. 54. Lower Ocean View
tunnel, Pine Moun-
tain Mine.
SAN LUIS OBISPO COUNTY. 165
these works ore has been taken and treated in the pipe retort
furnace.
On the Buckej-e a shaft has been sunk on verj' good crop-
pings, and a drift 350 feet long, S. 76° W., has been run, which
connects with the bottom of the shaft at a depth of 78 feet, 300
feet from the entrance. The ore at the lower level is a flinty
quartz. The surface is covered with rh3'olite bowlders. The
tunnel shows that the country is shale, and for the last 200 feet
serpentine. This work is, however, most probably in a slide
from the main body.
On the Pine Mountain a tunnel running nearly west is 300
feet long. The countrj^ rock is serpentine. The tunnel is
inaccessible. Judging from the dump, the tunnel has cut
serpentine and in the face shale.
The lyittle Almaden is an open cut. Work has been done on
a large body of croppings in a body of serpentine, which shows
clearly evidence of sliding.
Polar Star Mine (also called Santa Clara, or Black Hawk). —
San Carpojo District. In Sec. 13, T. 25 S., R. 6 E. Owners,
Public Administrator, G. E. Van Gordon, E. S. Rigdon, M. W.
Minor, and R. A. Minor, of Cambria; S. N. Hitchcock, C. D.
Hitchcock, F. H. Little, and W. Eittle, of San Simeon; H. H.
Carpenter, of San Luis Obispo; P. A. H. Arate, of San Luis
Obispo. [See Report State Mining Bureau of Cal., X, page
581; XII, page 366 — Black Hawk.] This is an old mine; it
has been worked sporadically since 1870 by different owners.
There is a great amount of surface ore on the south side-
hill of San Carpojo Creek, covering near the creek a distance
of 250 feet, running 750 feet up the hillside and narrowing to
about 40 feet at an altitude of 310 feet vertically above the
creek; this surface zone is from 6 to 20 feet deep. \^ery rich
ore has been found in this territorj^ but as yet the vein has
not been exposed. Some exposures of what is probably the
southern wall would indicate that the vein had an east and
west trend. The country rock is almost exclusively highly
silicified Franciscan sandstone. The property is equipped with
a two Q retort furnace in good order.
Quien Sabe Mine. — Pine Mountain District. Contains three
claims; Ouien Sabe Nos. i, 2, and 3, in Sec. 14, T. 26 S.,
R. 8 E. G. E. Van Gordon and M. W. Minor, of Cambria,
166 QUICKSILVER RESOURCES OF CALIFORNIA.
owners. The line of these claims is in a northwestern direction.
All the work has been done on the northeastern claim, which
abuts with its north end line against one of the branches of
the Arroyo del Pinal. The igneous rocks of Rock}- Butte lie
very close and parallel to the east side line. The intervening
space is in Franciscan sandstone. The two eastern claims are
located so as to cover a ridge of serpentine, having sandstone
on both sides. On both contacts are lines of croppings, charged
with cinnabar. Those on the west contact of the serpentine
are, however, the more prominent. An open cut on the west-
ern croppings shows good ore. The ledge matter is flinty
material. Some garnets can be found in this rock. Both cin-
nabar and metacinnabarite occur in the vein matter. On the
eastern croppings a shaft loo feet deep has been sunk. The
character of the ore is very similar to that of the western
croppings. From the creek level a tunnel has been started
nearly on the center line of the northeastern claim. This tun-
nel, 240 feet long, has not yet reached the ore deposit. Its face
is in black gouge, with inclusions of gra3'ish sandstone and
igneous rock. At a distance of 750 feet it will be under the
w^orks above described, at a depth of 230 feet.
Rinconada Mine. — In Sees. 21 and 28, T. 30 S., R. 14 E. Mrs.
Theresa Bell, of San Luis Obispo, owner. [See Report State
Mining Bureau of Cal., X, page 581; XII, page 366.] This
propert}' consists of two claims and two millsites, located about
12 miles southeast from Santa Margarita, a station on the
Southern Pacific Railroad, and 20 miles from San Luis Obispo.
The property was worked from 1875 to 1883, and equipped
with two furnaces — one of 20 tons, the other of 60 tons capacity.
It was shut down in the latter j-ear and practicall}'- abandoned.
It was relocated in 1897. In 1898 a lo-pipe retort furnace was
erected, but in 1901 the then owner, Mr. Petreida, died, and
since that time no work of any consequence has been done on
the property.
The country- rock is almost exclusively serpentine. Some
shale exposures are found in the bed of a creek about a quarter
of a mile west of the main workings. The mine is located in a
basin formed by a bend of the mountain ridge, and apparently
filled by material broken ofi the ridge. Through this basin
runs a line of croppings showing very boldly in the northwest-
SAN LUIS OBISPO COUNTY. 167
ern part of the Tenderfoot claim and in a cliff about a quarter of
a mile northwest thereof, the entire interv-ening surface being
covered b}^ large bowlders of croppings. Due west of the first
named place, topographicallj- above this line of croppings in a
gulch, croppings are also found. The main works consist of
extensive open cuts, principally worked in the 70's, with short
drifts and inclines — all in the croppings; a j^ellow ochery mate-
rial held together by a network of chalcedonic quartz seams.
A gulch, course N. 45"^ E., runs at the northeastern foot of the
ridge on which the croppings are located, and three tunnels
have been run under these croppings. The upper tunnel near
the head of the gulch, 115 feet below the top of the ridge, is
caved in. Judging from the dump this tunnel was run in ser-
pentine and shale. Lower down the gulch is another short
tunnel, about 50 feet long, entirely in serpentine. About 500
feet lower down in the gulch and about under the northeast
edge of the croppings, 50 feet lower verticallj^ than the first
tunnel, is the third tunnel, running south about 200 feet, then
S. 35° E., 200 feet. This tunnel is in serpentine. The breast
is at the contact of the serpentine and the sandstone. About
30 feet from the breast, short crosscuts have been run on a
fissure, having on the southeast wall a black clay gouge; a
shaft or winze has been sunk in the northeast crosscut, but is
covered up and is inaccessible. The country in the neighbor-
hood is well supplied with oak timber for fuel purposes, but
mining timber is rather scarce.
Sunset View Quicksilver Company. — San Carpojo District. Con-
sists of a cluster of mines in Sees. 13 and 18, T. 25 S., R. 6 E.
Jose Mariano, of San Simeon, owner. This is southeast of the
North Star.
Vulture Mine. — Oceanic District. In Sec. 24, T. 27 S., R. 9 E.
F. Eehman, G. E. Van Gordon, and E. S. Rigdon, of Cambria,
San Luis Obispo County; A. F. Benton, of San Miguel, San
Euis Obispo County; and G. W. Harris, of Pleyto, Monterey
County, owners. This property is located on croppings of
black, flinty, siliceous rock, more or less charged with cinna-
bar, in a belt of serpentine. Only very shallow surface work
has been done, so that nothing which determines the persistence
in depth or the form of the deposit has been disclosed. In one
168 QUICKSILVER RESOURCES OF CALIFORNIA.
open cut a stratum of clay from 2 to 3 feet wide is exposed,
which on panning shows to carry sensible amounts of cinnabar.
William Tell Mine,— Adelaide District. In Sec. 32, T. 26 S., R.
10 E. A. J. Brunoni, of Cambria, owner. This lies to the west
of the Karl mine, on the same ledge of croppings. A tunnel
60 feet long has been run, but no pay ore has been found as yet.
Wittenberg Mine. — Oceanic District. In Sec. 8, T. 27 S., R. 9 E.
D. F. Wittenberg, of Cambria, owner. This mine lies against
a wide belt of "mudrock," but judging from the surface indi-
cations, is underlaid by serpentine. All works are inaccessible
at present. The owner is at work reopening them.
SANTA CLARA COUNTY.
The New Almaden district lies southeast of San Jose, and
covers part of the northeasterlj^ foothills of the Gabilan range,
and a portion of the Santa Clara Valle5^ [See map of the
New Almaden Mining District.] Through the latter run two
spurs of low hills having a general northwestern direction,
both diminishing in elevation in this direction and disappear-
ing a couple of miles southeast of San Jose, where the valley
covers the entire territory between the Gabilan and Mount
Diablo ranges. One of these spurs, the Santa Teresa hills,
runs between the Arroyo Seco and Coyote Creek, and the other
between Coyote and Silver creeks. The New Almaden and
Guadalupe mines are situated on a ridge which forms the
southeastern boundary of that part of the Santa Clara Valley
having a general direction N. 45° \\ ., and connected at one
point with the main body of foothills of the Gabilan range.
This ridge is cut through at the southeast by the Las Animas
cafion, a very deep incision, in which are located the hacienda
and furnaces of the New Almaden mine. It deer-eases gradu-
ally in elevation going to the northwest, and is cut ofi north-
west of the Guadalupe mine by the caiion of Capitancillos
Creek.
These three ridges are to a great extent formed by serpen-
tine, especially the two first named. The serpentine is asso-
ciated with metamorphic sandstone and j aspilites. Large bodies
of croppings can be found in each of these ridges, having also
a general northwestern trend, but not coinciding with the back-
bone of the ridges.
tola'J/IoM A'
TDIMT.
fEVERGREEN/
■'>■ ' 7 f • <. >. ir.
ILLSDALE
STATION :.
Mo EOENVALE
^'^s-.^ STATION
^.o^
Orat^n by CNararrtore.
Green = Str[>enline, Vellou ^Melamorphk Seri-s BUit = Miocent
MAP OF THK NEW ALMADEK MINING DIvSTRICT.
Issued l>y the Califoniia State Mining Bureau - Lewis E. Aubury, State Mineralogist, 1903.
SANTA CLARA COUNTY. 169
In the New Almaden ridge the most extensive ore bodies
have been found in and close to Mine Hill, the highest peak of
the ridge, lying in its southeastern part. From this point going
northwestward the croppings, while not continuous, can be
traced along the ridge into the territorj^ of the Guadalupe mine,
a distance of about 3)^ miles. At the surface the serpentine
shows in large detached bodies surrounded by the sandstones
and shales of the Franciscan series and having a general north-
western trend. This general direction of the serpentine
exposures is important in connection with its occurrence
underground, proven in the New Almaden mine. The line of
ore croppings runs from Mine Hill to the America shaft, pass-
ing about 600 feet southwest of the Randol shaft. The under-
ground workings in this territory have shown that the fissures
wherein the ore bodies have formed have invariably a serpen-
tine foot wall; hence the serpentine must be considered to
occur underground in a continuous bod}^ through this entire
territory and to be in places covered by overlying sandstones
and shales. Southwest of Capitancillos Creek lies another
parallel exposure of serpentine, contiguous to which the out-
crops of the Costello mines are found. The Santa Teresa and
Bernal mines are located in the serpentine of the Santa Teresa
hills, and the North Almaden or Silver Creek mine close to
those of the most northern ridge. In the latter a great part of
the serpentine is very highly altered by silicification, as also
the sandstones, a great portion of the rocks being jaspilites.
The western slope of the adjoining Mount Diablo range is
nearly exclusively formed of shales.
In this district the occurrence of cinnabar-carr>4ng ore
bodies is clearly closely allied to that of serpentine, and as the
New Almaden was the first extensively worked quicksilver
mine in California, this association explains the reason why,
for a considerable lapse of time, cinnabar ores were, in the
opinion of most quicksilver miners, considered related to this
rock formation. The croppings consist of a more or less
weathered material having usualh' an ochreous color from the
oxidation products of the iron sulphides, and traversed by a
network of quartz seams, from a knife blade to quarter of an
inch wide. Overlying the ore bodies is almost invariably found
a body of clay, generally black, and containing more or less
inclusions of a dark-gray sandstone. As this clay overlies the
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>.ftr«\*>«.>A ."S ^^ tv•«x>•^t
:c ;:\M - \r-zH
SANTA CLARA COUNTY. 169
In the New Almaden ridge the most extensive ore bodies
have been found in and close to Mine Hill, the highest peak of
the ridge, lying in its southeastern part. From this point going
northwestward the croppings, while not continuous, can be
traced along the ridge into the territory' of the Guadalupe mine,
a distance of about 3^ miles. At the surface the serpentine
shows in large detached bodies surrounded by the sandstones
and shales of the Franciscan series and having a general north-
western trend. This general direction of the serpentine
exposures is important in connection with its occurrence
underground, proven in the New Almaden mine. The line of
ore croppings runs from Mine Hill to the America shaft, pass-
ing about 600 feet southwest of the Randol shaft. The under-
ground workings in this territory have shown that the fissures
wherein the ore bodies have formed have invariabl}' a serpen-
tine foot wall; hence the serpentine must be considered to
occur underground in a continuous bodj- through this entire
territor\- and to be in places covered by overlying sandstones
and shales. Southwest of Capitancillos Creek lies another
parallel exposure of serpentine, contiguous to which the out-
crops of the Costello mines are found. The Santa Teresa and
Bernal mines are located in the serpentine of the Santa Teresa
hills, and the North Almaden or Silver Creek mine close to
those of the most northern ridge. In the latter a great part of
the serpentine is xery highly altered by silicification, as also
the sandstones, a great portion of the rocks being jaspilites.
The western slope of the adjoining Mount Diablo range is
nearly exclusively formed of shales.
In this district the occurrence of cinnabar-carrj-ing ore
bodies is clearly closely allied to that of serpentine, and as the
New Almaden was the first extensively worked quicksilver
mine in California, this association explains the reason why,
for a considerable lapse of time, cinnabar ores were, in the
opinion of most quicksilver miners, considered related to this
rock formation. The croppings consist of a more or less
weathered material having usually an ochreous color from the
oxidation products of the iron sulphides, and traversed by a
network of quartz seams, from a knife blade to quarter of an
inch wide. Overlying the ore bodies is almost invariably found
a body of clay, generally black, and containing more or less
inclusions of a dark-gray sandstone. As this clay overlies the
170 QUICKSILVER RESOURCES OF CALIFORNIA.
ore bodies it has received the name of "alta " (Spanish — " over,"
"above"). At the surface this "alta" crops as a light-gray
material, resembling disintegrated sandstone, traversed by a
network of ver\- thin, yellowish-brown seams, often very much
like a bunch of very fine roots. In places the same material
can be found in the Xew Almaden mine several hundred feet
below the surface, forming part of the "alta." The same surface
Shale I Croppin gs ^jSerpentine
~e/o ~% /20'
Fig. 55. Section near R. R. B. shaft, Xew Almaden property.
cropping of "alta " can be seen in San L,uis Obispo County. [See
general description of Adelaide district.]
In a few places a good section of the formation has been
exposed at the surface, as for instance, the R. R. B. shaft of
the Enriquita mine, northwestern part of the Xew Almaden
mine, and near the Randol shaft of same mine. [See Figs. 55
and 56.] Both these sections indicate that the hanging wall
Serpentine\ 4l_\^j^f\ il v\— —
FiG. 56. Section on road above Randol shaft, Xew Almaden Mine.
proper may be a shale, which, however, is so decomposed at
the surface that nothing can be said as to its actual character.
About 300 feet below the collar of the R. R. B. shaft, in the
Eldridge tunnel, the same formation can be seen underground,
that is, the serpentine foot w^all, the vein and the overhing
"alta"; but as no crosscut has been driven through the latter,
no further information as to the character of the hanging wall
proper is available. The clay "alta" is but an attrition prod-
uct of the movement of the walls of the fissure, and hence to
call the "alta" a wall of the vein, as is frequenth' done, is
a misuse of geological terms. The rocks of the Franciscan
series in this region show a great amount of silicification. The
chert beds are, however, almost entirely unrepresented.
SANTA CLARA COUNTY. 171
To the west of the New Almaden ridge a belt of bedded
sandstone is exposed. The beds are from. 3 to 5 feet thick and
interbedded with thinner beds of shale. The sandstone is
rather coarse, and has been classified by Dr. Becker as Miocene.
[See Mon. XIII, U. S. G. S., page 312.] The strike is about
east and west, dip northerly, not over 20°. The country- west
of the New Almaden ridge and south of Capitancillos Creek,
belonging to the Gabilan mountain system, consists almost
exclusively of the sandstones and shales of the Franciscan
series, with occasionally some jaspilites. A small exposure of
serpentine was found about two miles west of the New Alma-
den ridge, close to the main ridge. West of the serpentine
belt which lies west of the New Almaden ridge, south of Cos-
tello's house, a small exposure of glaucophane schist was
found. A body of rhyolite lies in the northern part of the
New Almaden ridge, having a nearly east and west strike and
being about two miles long. To the east smaller bodies of
rhj'olite are found, probably the continuation of the same bod}-,
which must be covered up in the inten'ening space. This
eruptive body apparentlv has no relation with the ore deposi-
tion in this district.
The general character of the ore tends more to the conclusion
that the ore deposition was a feature of an intense silicification
of the fractured parts of the serpentine; that the fractured zone
was a favorable channel for the percolating solutions, which
dissolved the ferro-magnesian silicates and other salts of the
rock, and replaced them by silica, calcite, dolomite and allied
minerals, sulphides of iron and occasionally of mercury ; these
channels being limited on one side by the impermeable stratum
of clay, the "alta"; on the other side, by the limit of fracturing
of the serpentine.
There are some small areas of limestone in this district. The
most prominent are along the south bank of Capitancillos
Creek, where near the Guadalupe mine a limekiln was in
operation at one time. It appears, however, that the product
was not quite satisfactory, which was due to the presence of
bitumen in the rock.
Bernal Mine. — This is situated on the east slope of the Santa
Teresa hills, about 8 miles southeast of San Jose and near
Edenvale station, on the Southern Pacific main line. Ygnacio
172 QUICKSILVER RESOURCES OF CALIFORNIA.
Bernal, No. 207 Balbach street, San Jose, owner. This prop-
erty is traversed by a ravine having a northeasterly course,
draining into Coyote Creek; on both sides of this ravine, but
especially on the northwest side, where the workings are
located, are found some ver^^ prominent croppings. The lat-
ter are entirely surrounded by serpentine, but as far as ascer-
tained do not connect with those on the southeast slope of the
ravine. The direction of these croppings is about northwest.
A tunnel, course nearly west, about 215 feet long, is run on the
contact of the "alta" and the serpentine; about 30 feet from
the breast a good exposure of the formation shows the vein to
dip slightly northeast, with a clay gouge on both sides. A
short crosscut to the left shows that the overlying gouge is at
least 15 feet wide. The gangue is of a ver>- calcareous nature.
Nearly 200 feet above this tunnel, on the top of the ridge, a
shaft 65 feet deep has been sunk on the croppings, showing
some good ore on the dump. About 20 feet southeast of this
shaft a shallower shaft, not over 20 feet deep, on the same
croppings, shows a more ochreous vein material.
Comstock Mine. — This lies in the extreme southeastern corner
of Santa Clara Count}', in Sec. 19, T. 11 S., R. 7 E., really
belonging to the Sta3-ton Mining District. H. French, of Lone
Tree, San Benito County, owner. [Report State Mining Bureau
of Cal., XII, page 367.] The property is at present abandoned.
Some old surface workings and remnants of an old furnace can
5-et be seen. The mine is located on the only surface exposure
of serpentine found in the Stayton Mining District. The ore
found is a black chalcedonic quartz.
Costello Mine. — This lies on the southwest side of Capitancillos
Creek, about 1^2 miles southeast of the Guadalupe mine, and
opposite the Enriquita mine of the New Almaden propert}'.
M. Costello, of New Almaden, Santa Clara County, owner.
The principal workings in this propert}' are located on the
sidehill, about 400 feet above the level of Capitancillos Creek;
below these, considerable limestone is found in the debris
covering the sidehill, and also some croppings of the same rock,
but at the level of the works this rock does not occur. The
works consist of several shallow cuts and drifts in the debris
covering the hillside. One tunnel reaches through the latter
into the serpentine. In a crosscut from this tunnel a sand-
SANTA CLARA COUNTY. 173
Stone was found having on the fracture planes a thin black
coating of iron and carrying some cinnabar. All through the
debris pieces of ore are disseminated, composed of fragments of
a flinty material, generally in a matrix of quartz; occasionally
the matrix resembles the tuffoid of the Abbott mine. Lake
County. The character of the ore is entirely different from
that in the New Almaden ore bodies. No ore deposits in place
have yet been found.
Guadalupe Mine. — This mine is on Capitancillos Creek, lo
miles south of San Jose. The Century Mining Company,
owner; H. C. Davey, president, F. A. Lueddeman, secretar}^
San Jose, Santa Clara County; San Francisco office, room 131 2,
Claus Spreckels Building. [See Report State Mining Bureau
of Cal., Vm, page 542; XIII, page 600; Mon. XIII, U. S. G. S.,
page 326.] This mine was discovered in the early 50's, being
acquired soon after its discovery by the Santa Clara Mining
Association of Baltimore, Md., and was operated by that com-
pany until the mine was bought by the Guadalupe Mining
Company of California in 1875, when large surface improve-
ments in the way of reduction works and mining machinery
were installed and extensive mine development work was
prosecuted. Up to 1886 the mine produced 55,910 flasks of
quicksilver [see Mon. XIII, U. S. G. S., page 11], and then
remained idle until 1900, when H. C. Davey organized the
Century Mining Company-, which has remodeled the reduction
plant, started to unwater the mine, and is at present passing
through the furnace a great part of the old dumps and some
fillings of the upper parts of the old works. The unwatering
of the mine has proven a very difiicult undertaking, as the
works are at a shallow depth under Capitancillos Creek, which
drains a large section of the country.
From the plan of the old works it can be seen that the ore
body developed b}' the main vertical shaft, located on the
south side of the creek, had a northwest strike and southwest
dip. The second level, 300 feet below the collar of the shaft,
connects with an incline shaft started on the opposite bank
of the creek and following the vein on its dip. The main
shaft was only sunk to the sixth level (625 feet). From this
level an incline shaft was sunk, from which the seventh,
eighth, and ninth levels were driven. Ore was only developed
174 QUICKSILVER RESOURCES OF CALIFORNIA.
in the seventh and eighth levels. Besides these works several
other shallower shafts and drifts were run, all practically inac-
cessible.
The property is equipped with two 20-ton coarse-ore fur-
naces and two 40-ton fine-ore furnaces, modeled according to
the Davey patent.
Hillsdale Mine, or old Chapman mine, formerly known as the
Chaboya mine, about two miles from San Jose, near Hillsdale
station, lies on the east slope of the northwestern end of the
Santa Teresa hills. Oscar Promis, No. 246 South Third
street, San Jose, owner. There are a great number of excava-
tions in the hillside, which, however, reach scarceh' any depth,
as the crest of the hill is not over 100 feet above the level of
the valley. At present these workings show ver^^ little ore.
They must at one time have produced quicksilver ore, as the
remnants of an old furnace are still on the premises.
New Almaden Mine. — This property lies 1 3 miles south of San
Jose, and covers a territory of 8580 acres. The Quicksilver
Mining Company, owner; A. I^. Baile}^ 20 Nassau street, New
York, president; Thomas Derby, New Almaden, Santa Clara
Count}^ superintendent. [See Mon. XIII, U. S. G. S., page 310
and following; Report State Mining Bureau of Cal., VIII, page
541; X, page 604; XII, page 370; XIII, page 600.]
This property is the oldest known quicksilver mine in the
United States. It was first worked in 1824 b}^ Antonio Sunol,
lyuis Chaboya, and Robles, and was known as the Chaboya
mine. In 1845, Andreas Castillero, a Mexican army officer,
"denounced" the mine under the name of Santa Clara mine.
After the admission of California into the United States, Castil-
lero and his associates leased the mine for sixteen years to the
banking firm of Barron, Forbes & Co. The name of the mine
was at the same time changed to that of New Almaden. Ir
1864 the property came into the hands of the present owner.
This mine produced in the earlier years comparativelj- rich
ore, but in later years the richness of the ore has very much
decreased and that now worked is of about the general average
grade of that in the other large quicksilver mines of the State.
The table on pages 176 and 177 gives its production up to the
year 1896.
Bueno yisfa Shaft
/fandol Tunnel
Sec f ion A A
^ MoinShaft' J \ i, '-^,
A
'. fforr/ S/!aft
Washingfon %1
Shaff •<'
^S>
ffatf Turfte/
SCALCIN nCT
I . I Ore bodies y/ren /n Map of Or. Beefier ftSS.
\' I Ore bocfies cfefe/ofiecf /afer
Ore Uoilies in the New Almaden Mijic.
SANTA CLARA COUNTY,
175
The mine workings cover a ter-
ritory of about 2'^ square miles, ex-
clusive of those in the northwestern
part of the property. The greatest
depth of these workings is 2450 feet
below the top of Mine Hill, which is
used as the datum point for all under-
ground workings. In this territor)^
eighteen shafts have been sunk, and
the underground excavations would
be about 84 miles long. The greater
part of these extensive workings are
at present inaccessible; the Mctoria
shaft, a short distance to the south-
west of the Randol shaft, and the
Harr}' shaft, on the southeast slope
of Mine Hill [see map, Fig. 57], are
the only two shafts at present in
operation. The deepest workings at
present followed are 1000 feet below
the datum point; and below 1300 feet
the mine is filled with water.
The ground in that part of the
mine now in operation is remarkably
good. A majorit}' of the large stopes
are held up with scarcely any timber-
ing, and onl}^ in some parts of the
mine is square-set timbering required.
Most of the gangways require only
occasional timbering for short dis-
tances. The ground in the Randol
shaft formerly worked was, however,
much heavier.
The gangways are driven on the
contact of the clay gouge, locall}-
called "alta," which overlies the ore
bodies, and where the ore bodies are
absent, on the contact of the "alta"
with the serpentine foot wall, locally
called "greenstone."
The ore forms principally in "stock-
wercks" (that is, in large zones of
176
QUICKSILVER RESOURCES OF CALIFORNIA.
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SANTA CLARA COUNTY.
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178
QUICKSILVER RESOURCES OP CALIFORNIA.
fracturing), and in reading the following description it must
be borne in mind that when speaking of veins in the New
Almaden mine, this term does not indicate a well-defined
fissure, but that the ore deposition has taken place along zones
of fracturing. Judging from the great width of the "alta,"
the result of attrition caused b}' the movements of the rock
niNE HILL
Fig. 58. Section of Mine Hill, New Almaden.
Strata, from the wave-like form of ore deposits, from the fact
that parallel zones of ore deposition are found, and finally from
the character of the vein filling, which shows repeated fissuring
and refilling, resulting in a ribbon formation in the seams, the
conclusion must be drawn that this fracturing was persistent
during a long period of time.
The ore deposits are limited on their hanging-wall side
by the "alta," an
'Gi'onfpZv^^^ impermeable stra-
tum through which
no water circula-
tion could pass.
The foot-wall side
is persistently ser-
pentine, hence it
must be concluded
that in this mine
the serpentine is associated with the cause of fracturing of the
other rock strata, and this would lead to the conclusion that
here the serpentine must be considered as an alteration prod-
uct of intrusive peridotites, not as an alteration of strata of
the Franciscan series. This conclusion finds confirmation by
a section of the country from Mine Hill toward the Washing-
ton shaft. [See Fig. 58.] The fracturing has taken place on
Fig.
59. Section over Santa Rita West, Giant Powder
slopes, New Almaden.
SANTA CLARA COUNTY.
179
both sides of the serpentine, which apparently can not be con-
sidered otherwise than as an intrusive body having uplifted the
rocks of the Franciscan series.
The ore bodies form principallj^ in those parts of the zones
where the dip of the " alta " is very flat, as indicated in Fig. 59 —
an ideal section over two connected stopes, which have both
produced considerable amounts of ore. The contact of the
PHOTO No. 16. DL'.MP OF NEW ALMADEN MINE WORKS.
" alta" with the underlying vein filling, and where this is miss-
ing with the serpentine, is very tortuous in both directions,
vertically and horizontally, so that in the gangways, which,
as above mentioned, follow this contact, it is an exception to
find a straight line of any length. The stopes are locally
called "labores." The material which fills the zones of frac-
turing and wherein in places cinnabar forms, is generally
rather hard and siliceous, traversed by a network of seams
12— QR
180
QUICKSILVER RESOURCES OF CALIFORNIA.
of quartz and dolomite, showing repeated Assuring and filling
containing some inclusions of serpentine, the cinnabar forming
principally in connection with the seams. In places the vein
filling has more of an ochreous character, the matrix being
more or less leached out, leaving only the network of seams
intact.
The San Francisco vein is mainly composed of this ochreous
PHOTO Xo. 17. DUMP OF GREY SHAFT AND MINE HILL,
XEW ALMADEN.
ore, wherein are found bodies of ven,- hard rock, resembling
diorite, verj' irregularly fractured. In this vein, the ochreous
material lies on the serpentine, no gradual change taking place
from the former into the latter, which for from 8 to lo feet from
the vein is changed into a clayey material, gradually changing
into hard serpentine.
The general character of the vein filling indicates that, as in
most of the other quicksilver deposits in the State, the deposi-
SANTA CLARA COUNTY.
181
tion of cinnabar has been associated with the process of silici-
fication, which characterizes the alteration of the rocks of the
Franciscan series.
The general direction of the seams in the vein filling is not
parallel to the line of contact with the "alta." The "alta"
is often indurated near the vein, and is then locally called
"cab." This is especialh' the case in the upper workings. In
PHOTO No. is. VICTOKl.\ SHAFT, NEW ALM.\DEN.
the lower levels, it has more the character of a moist clay ; the
inclusions of gray sandstone, so frequent in the mines of San
Luis Obispo and San Benito counties, while not absent, are
much less prominent. Possibly associated with this change in
the character of the "alta" is a difference in the distribution
of the cinnabar in the pay shoots. In the upper workings the
part nearest to the "alta" is seldom the richest, the cinnabar
forming more plentiful at from 5 to 8 feet below the "alta,"
182
QUICKSILVER RESOURCES OF CALIFORNIA.
while in the lower workings the richest ore is invariably close
to the "alta."
The contact between the "alta" and the vein filling is very
sharplj' marked, but there is a gradual change of the above
described vein filling into the material of the serpentine foot
wall, the vein material gradually carrying more serpentine,
until its has entirely changed into the latter. The hanging
PHOTO No. 19. SANTA ISABEL SHAFT, NEW ALMADEN
wall is a shale, judging from surface exposures. Underground,
no crosscut through the "alta" to the hanging wall was seen.
[See Figs. 55 and 56.]
In some parts of the mine, especially in the lower workings
(as/, i), in the drift from the Santa Isabel shaft, southwest to
the American shaft [see plan, Fig. 57], heavy flows of gas were
encountered, principall}^ if not exclusively, consisting of car-
bon dioxide, which in that drift were so strong as to force the
SANTA CLARA COUNTY.
183
company to abandon the work. It is generally supposed that
this gas is generated by the decomposition of the calcite and
dolomite, which are abundant in those parts of the mine, both
in the vein filling and in the " alta."
In order to give an intelligible description of the formation
of the ore bodies in the New Almaden mine, the old works, at
present inaccessible, must be taken into account. The magnifi-
PHOTO No. 20. RANDOL SHAFT, NEW ALMADEN.
cent map of the underground works in the office of the com-
pany gives ample opportunity to do this. A reduced copy of
this map, up to the date of its publication, 1887, is found in
sheet IX of the atlas of Mon. XIII, U. S. G. S. The accom-
panying plan [Fig. 57] gives an outline of the ore bodies
opened up in the mine. The later works are located princi-
pally in the upper levels.
One nearly continuous series of ore bodies {a) lies on a line
184 QUICKSILVER RESOURCES OF CALIFORNIA.
Starting near the main shaft and going in a northwesterly
direction to about 400 feet northwest of the Santa Rita shaft,
a distance of about one fourth of a mile. These ore bodies are
worked to a depth of not over 700 feet below datum level (top
of Mine Hill). In the southern part, near the main shaft, the
ore bodies are intricately overlying each other. [See Fig. 57,
crosscut AA, a west-east section over this part of the mine.]
This may be due to the intrusive serpentine body in Mine Hill
before mentioned.
A second series of ore bodies {b) lies to the east, and runs
nearly parallel to the former. It begins a little southwest of
the Harr3' shaft, and runs to about the Day tunnel, where
it connects, by a series of stopes about 400 feet long, with
the first mentioned series. These workings go from 400 feet
below datum in their southeastern part to 650 feet at the
northwestern end.
Running a line from the Giant Powder stope to the Santa
Maria shaft, the general direction of the veins south of this
line, judging from that of the gangwaj^s, which as stated
above are run along their hanging contact, is about north
with an east dip. North of this line the ore bodies appear to
change their course and to lie on a nearly southwest strike
with a northwest dip. In this latter part of the mine there
are two distinct zones of mineralization — the western zone
{c), which connects directly with the first above-mentioned
series, and the eastern zone {</), which appears to be separated
from the second series {b) by a nearly barren zone, in which,
however, not only does the vein persist, but the two zones
mentioned by Dr. Becker (Mon. XIII, U. S. G. S., page 320
et seq. ) make their appearance, there being two levels run
on the 900-foot and looo-foot levels on their hanging-wall
contact. From the 700 to the 1 700-foot level, there is a barren
zone between these two mineralized zones {c and d). On
the latter level a body of ore was worked between them,
but judging from the map of the underground workings of the
company, *below this level, no ore bodies were found in the
intervening space. [See plan. Figs. 57 and 60, which give a
general idea of this system of ore deposit.]
In the 1400-foot level, Santa Isabel South, running toward
the Washington shaft, about 700 feet south of the Santa
dol Shaft
jT Col/<"'
SCAL£ W r££T
O so /OO 200 300
Fig. 60.
Plan of the Clay Walls, New Almaden Mine.
From Atlas, Monograph XIII, V. S. G. S.
SANTA CLARA COUNTY. 185
Isabel shaft, and near the breast of the 1400-foot level south-
west running from the same shaft toward the America shaft,
some ore was found. If these ore bodies could be proven to
be connected, they would be found to lie in the prolongation
of the strike of c and d, and there would appear to be a line of
cross-fissuring, a very possible occurrence in a country as
disturbed as the vicinity of the New Almaden mine.
In the knoll southeast of Mine Hill are the Cora Blanca
workings, which in former times yielded quite good ore. At
present a tunnel is run between the Cora Blanca and Grey
shafts in this hill, which has cut a small ore body; the latter
has, however, an entirely different appearance from that in the
other workings, the gangue consisting of fragments of jaspery
material recemented by silica, calcite, and dolomite. The cin-
nabar is here associated with some iron pyrite.
The most northwestern works on the property, known as the
Enriquita mine, are located about i % miles northwest of Mine
Fig. 61. Section in Enriquita Mine, New Almaden.
Hill. The lowest working is a tunnel starting on a very promi-
nent body of croppings, which in the tunnel forms a sandstone
traversed by a very close network of seams refilled by quartz
and calcite. At 840 feet from the entrance the tunnel enters
the serpentine and splits. The left-hand drift runs to the
bottom of the R. R. B. shaft, and then follows the contact of
"alta" and vein material, which at the breast disappears,
leaving the "alta" directly overlying the serpentine. The
right-hand drift also reaches a similar contact and stops at the
contact of the "alta" and the serpentine, showing that there
is here also a repetition of strata. [See Fig. 61.] Above this
level, about 150 feet below the surface, a body of very good
ore was worked in former years, from which about 10,000
flasks were obtained.
The mine is equipped with two coarse-ore furnaces of 12
tons capacity each; two medium-sized ore (granitza) furnaces,
one of 36 tons, the other of 18 tons capacity; and two fine-ore
(tierra) furnaces, one of 36 tons, the other of 24 tons capacity.
There is very little or no mining timber available in the
186 QUICKSILVER RESOURCES OF CALIFORNIA.
vicinity. The company uses exclusively Oregon pine, costing
$i8 per I coo feet (B. M.). Cordwood is not very abundant,
and costs $5. 85 per cord. The company uses oil as fuel under
the steam boilers in both hoists.
Santa Teresa Mine* — This is situated on the east slope of the
Santa Teresa hills, about 8 miles southeast of San Jose, near
Edenvale station, on the Southern Pacific main line. The
Santa Teresa Quicksilver Mining Company, owner; R. B. Har-
per, of San Jose, superintendent. Three tunnels have been run
in the mountain. [See Fig. 62.] The lowest tunnel, 700 feet
^Mt'f, Surface
Tunr) el
^e/n
'£___^' Top of Ridge (835)
Fig. 62. Sketch of works in the Sauta Teresa Mine. Scale, i":=2oo'.
long, reached the vein at 550 feet from the mouth; its course
is nearly south. It turns to the left on the vein and is driven
in toward the territory under the two upper tunnels in order
to reach the pay shoot in the vein, which apparently dips east-
ward. The middle tunnel, no feet above the former, course
S. 8° \V., 325 feet long, is in serpentine. It cuts the ledge 228
feet from the mouth. There is no selvage or gouge between
the ledge and the serpentine. The ledge stands nearly vertical;
the tunnel has not yet passed through the ledge into the oppo-
site wall. The upper tunnel is 85 feet above the middle tunnel,
course S. 22^ W. It cuts the contact of the serpentine and the
ledge at 220 feet from the mouth, and a few feet farther turns
to the right in the ledge and runs 187 feet in this direction.
SANTA CLARA COUNTY. 187
About 50 feet from its turning point is a vertical shaft, which
connects with the middle tunnel about 90 feet from the point
where the latter cuts into the ledge, showing that the ledge
dips north. Between these two tunnels, farther on, a raise goes
from the upper level to the surface no feet, all in ledge matter.
On the level of the upper turtnel several drifts and crosscuts
have been run in the ledge matter, showing the latter to be
ver}^ extensive.
The country rock is all serpentine. The ledge matter varies
greatly in character. It is apparently an alteration product of
serpentine through silicification, subsequent to a fracturing of
the material. The fissures have been filled by quartz and cal-
cite, the silicification varj'ing in difierent zones of the ledge,
probably due to a varying degree of fracturing. In places
inclusions of nearly unaltered serpentine are found. In others,
as for instance, in an intermediate short level run from the shaft
37 feet above the middle tunnel, the rocks contain a great
amount of cavities. Considerable ochreous material is found,
probably due to the oxidation of iron pyrite. A 50-ton Scott
furnace is in course of construction.
Silver Creek Mines. — This was formerly the North Almaden
mine, on the east side of Silver Creek, near Evergreen, about
8 miles from San Jose. Silver Creek Quicksilver Mining Com-
pan}', owner; H. R. Bradford, president. No. 7 North Market
street, San Jose. [See Report State Mining Bureau of Cal.,
XII, page 367; XIII, page 600.]
Access to mine refused to Field Assistant.
Wright Mines. — These lie on Llagas Creek, about 3 miles
south of the hacienda of New Almaden, 25 miles from San
Jose. Mrs. A. Rodgers, owner. No. 1801 Leavenworth street,
San Francisco. [See Report State Mining Bureau of Cal.,
XII, page 370; XIII, page 601.] This property was worked
to some extent in former years, producing some good ore; but
sufficient work has not been done in later times to judge of the
possibilities of the property.
188 QUICKSILVER RESOURCKS OF CALIFORNIA.
STANISLAUS COUNTY.
Summit Group of Mines. — These consist of the South Summit,
North Summit, Grayson, Martin, Hayward, White Oak, and
Hopkins claims, and four millsites, in Sees. 20 and 29, T. 6 S.,
R. 5 E., principally in Stanislaus Count}', but partly in Santa
Clara County, on Red Mountain, about 50 miles from San Jose
and 40 miles from Livermore. The Phoenix Quicksilver Min-
ing Company, owner; H. G. Stevenson, Hobart Building, San
Francisco, president; E. P. Xewhall, Deforest, Santa Clara
Count}-, superintendent. [See R.eport State Mining Bureau of
Cal., XIII, page 603.] This property was discovered in the
70's by Mr. Waterford, who turned it over to the Martin
Brothers, of Pleasanton. The Messrs. Martin worked it on a
small scale and erected a 5-ton furnace and afterward sold it to
Mr. A. Hayward and associates, who recently formed the com-
pany which is the present owner. It is opened by several tunnels
and shafts, which show that there are three distinct zones of
mineralization: The Summit vein, having a strike N. 15° E.,
and a southeasterly dip; a belt of sandstone, having a north-
westerly strike, crossing the Summit vein (if it continues past
the latter is, however, not yet determined); and the Gray-
son vein, having also a northwesterh- strike, with a north-
easterly dip.
The Summit vein is developed by four tunnels and a shaft
40 feet deep on the top of the ridge. The vein is well exposed
in tunnels Xos. i and 2, which are connected by an incline
shaft. Considerable understoping has been done in Xo. i, and
from Xo. 2 a shaft has been sunk first verticalh- until it reaches
the ioot wall and then along the foot wall at an angle of 54°.
The vein is overlaid by "alta." The foot wall is in sandstone
altered by silicification. The understopes of Xo. i on the foot
wall show a large ore body ; one crosscut, 40 feet long, has not
reached the overlying "alta." The ledge matter is a serpen-
tine, altered into an opaline rock. The cinnabar is remarkabl}^
disseminated through the silica in fine aggregates of cr3'Stals.
Especially in the upper tunnel a great portion of the ore is
weathered into a soft ochreous material, due to the oxidation
of the iron sulphides. There is considerable lime in the
gangue. The Gravson ledge is more of a sandstone character.
STANISLAUS COUNTY. 189
with cinnabar coating the fracture planes; the ledge carries
also considerable ochreous material. The erection of a 50-ton
furnace is contemplated. The manufacture of the brick for
this has been started.
Adobe Valley Mine.— In Sec. 24, T. 6 S., R. 5 E. The Stanis-
laus Quicksilver Mining Company, owner; H. G. Stevenson,
Hobart Building, San Francisco, president; E. P. Newhall,
Deforest, Santa Clara County, superintendent. This property is
at present idle. A vertical shaft, about 180 feet deep, has been
sunk, but is filled with water to just below the 100-foot drift.
The country rock is apparently a bedded sandstone. The pres-
ence of considerable black clay gouge indicates that strong
movements have taken place. The rock and the ledge matter
carr}' a great amount of sulphur, occurring as iron and mag-
nesia sulphides, and where these have been decomposed, as
sulphates and free sulphur. The sandstone in places is impreg-
nated with cinnabar, associated with iron sulphide, but the
works are not enough advanced to admit of judging about the
value of the deposit.
Orestimba Mine. — This is on Orestimba Creek, in Sees. 25 and
36, T. 6 S., R. 5 E. The Hazard Quicksilver Mining Company,
owner; H. G. Stevenson, Hobart Building, San Francisco, presi-
dent; E. P. Newhall, Deforest, Santa Clara County, superin-
tendent. The property is at present idle. A short tunnel with
several crosscuts, about 200 feet above the creek level, shows
that the country rock is a silicified shale.
OUTLYING COUNTIES.
EL DORADO COUNTY.
Bernard Mine.— This is in Sec. 4, T. 8 N., R. lo E. The Ber-
nard Quicksilver Company, owner. ly. C. Osteyee, 212 San-
some street, room 11, San Francisco. [See Mon. XIII, U. S.
G. S., page 384; Report State Mining Bureau of Cal., XII,
page 359.] This property was first developed in the 6o's,
by G. Folger, of Jackson, Amador County, under the name of
the Amador Quicksilver mine. The present owners have re-
opened the old works, which consist of a vertical shaft about
75 feet deep, connecting with a tunnel about 65 feet lower
than the collar of the shaft, starting on a southerh' course,
about in the same direction as the strike of the slate, and turn-
ing nearl}^ at right angles to the right about 1 80 feet from its
mouth. Both the shaft and the tunnel are entireh* in the gray
slates of the Mother Lode region, which show some cinnabar
on panning. After passing the bend, the tunnel crosscuts the
the slates, and for about 25 or 30 feet the walls are coated with
vermilion. This coating appears, however, to be only super-
ficial, as when breaking down the rock no signs of it are found
on the new fractures. This tunnel being very old, this ver-
milion may be a recent deposition. About a quarter of a
mile west of these works a belt of serpentine runs through
the countrj'.
TRINITY COUNTY.
Surface indications of quicksilver ores are found in several
places throughout Trinity County, but active mining for this
metal has only been done in the northeastern part of the county,
between Crow Creek, a tributar}^ of the east fork of Trinity
River, and the north fork of the east fork of Trinity River.
The surface country rock of this section is principally serpen-
tine, which is generally very hard; on the east and west
ridge forming the northern boundary of the basin wherein the
TRINITY COUNTY.
191
quicksilver ore bodies occur, a great amount of the chr3-sotile
variety of serpentine is found, which, however, is entirely
absent nearer the mineralized section. The Emerald tunnel
cuts through the formation in a part of the territory, showing
little or no signs of mineralization, hence afiording opportunity
to judge about the rock formation of the country in general.
It starts in serpentine, but at the breast, about 250 feet in, the
material is a diabase altered into greenstone. The material
wherein the ore bodies form, being also altered igneous rock,
it is ver}- probable that the serpentine is in this territory- an
alteration product of igneous rocks. The exposures of metamor-
phics, prominently sandstones, are principally located west of
the mineralized zone, on the slope toward the North Fork. One
192 QUICKSILVER RESOURCES OF CALIFORNIA.
small exposure of igneous rock (quartz porph5-r\^) was found
near Crow Creek.
The material wherein the ore bodies form has been very
much altered; it is probably a feldspar porphyr}-. Occasion-
ally small detached exposures of croppings are found in the
serpentine. Thej- have an ochreous appearance, and their rela-
tion to the ore bodies developed underground is as yet unde-
fined. The works of the Altoona mine being at present
inaccessible, the obser^^ation of the underground ore appearance
was limited to a depth of 120 feet, the greatest depth at which
ore bodies are developed in the Integral mine.
Altoona Mine. — This lies in Sec. 22, T. 38 N., R. 6 \V., and
comprises the Trinity, Altoona, and part of the Blockade
mining claims. The Altoona Quicksilver Mining Company,
owner, 206 Sansome street, San Francisco. [See Mon. XIII,
U. S. G. S., page 366; Report State Mining Bureau of Cal.,
VIII, page 643; X, page 716; XII, page 371 ; XIII, page 603.]
The Altoona Quicksilver Mining Company acquired this prop-
erty in 1875, but prior to that time some surface work had
been done and relatively considerable quicksilver extracted.
In 1879 the mine was closed down by litigation, and so
remained until 1894, when work was resumed, a Knox &
Osborne fine-ore furnace erected, and the underground develop-
ment work energetically pushed. A vertical shaft was sunk
to a depth of 450 feet, from which five levels were driven; in
the lowest level another vertical shaft was sunk 152 feet deep,
from which two levels were driven. In all there are seven
levels, covering a territor>^ of 1600 feet in a northwesterly
and II 20 feet in a northeasterly direction; within which four
different veins were worked to a depth of about 600 feet.
Three of these veins come together at the lowest level, forming
a mineralized zone about 400 feet long and from 4 to 50 feet
wide. The fourth vein has no connection with the other, and
lies about 400 feet southwest; it has been worked from the
third (350 feet) to the first (140 feet) level. The mine makes
a very large amount of water, requiring several large pumps
and a boiler capacity of 140 H. P. to keep it unwatered, causing
a high cost of operation per ton of ore worked; and when, in
1902, part of the reduction plant was destroyed by fire, the
mine was shut down, and the water stands now about 18
TRINITY COUNTY.
193
inches above the floor of the upper level. The furnace has
lately been repaired, and the material of the dumps is run
through with satisfactory result.
The production of the mine has been: prior to 1S75, 1500
flasks; from 1875 to 1879 (retorts), 8010 flasks; from 1894 to
1902 (furnace, 70 months), 19,671 flasks; total 29,181 flasks.
Carr Mine* — This is in Sec. 22, T. 38 N., R. 6 \V., and consists
of one mining claim. G. Carr, of Carr\'ille, Trinity County,
owner. Some surface work of no consequence has been done.
PHOTO No. 21. ENTRANCE— CASTELT-A DEVELOPMENT TUNNEL, INTEGRAL MINE.
An exposure of croppings is found on this mining claim in the
road between the Altoona and Integral mines.
Integral Mine. — This is in Sees. 14, 15, 21, 22, 23, 27, and 28,
T. 38 N., R. 6 \V., and consists of forty-six mining claims and
several timber sections. The Integral Mining Company,
owner; E. W. McGraw, 324 Pine street, San Francisco; Frank
A. Mahon, superintendent, Integral, Trinity County. The
geology of this property is treated previously in the general
description of this district. Some croppings are found between
194
QUICKSILVER RESOURCES OF CALIFORNIA.
the mouth of the Castella tunnel and the sawmill, but no ore
bodies have been cut by this tunnel. Serpentine is also under-
ground the principal country rock. In this serpentine lies
a body of highly altered rock, probably an altered feldspar-
Verr/ca/W/nze b^
fween 40' a 80'/e/eL
Probab/e /imifs of porphyry on SO'/ei/el.
" •• '• ••/20' ••
Serpentine.
„, , freo)
Blacksmifh
shop
Fig. 62a. Underground workings of Integral Mine.
porphyr>% as far as ascertained in the form of an irregular
lens, with a northwesterly dip. In the parts of the lens which
carry ores the material is thoroughly decomposed by the action
of the mineral-bearing waters, which deposited there in iron
and mercury sulphides, the former being largely, if not entirely
TRINITY AND OTHER COUNTIES. 195
weathered into iron oxides, decomposing the gangue rock and
giving it a yellow and black color.
The principal system of underground works consist of a
shaft, from which four levels, respectively 40, 80, 120, and 180
feet below its collar have been driven, and an intermediate
level at lOO feet. [See Fig. 62a.] The 180- foot level connects
through a vertical winze with the Castella development tunnel,
which is 120 feet vertical lower; and from this winze a drift
and side drift have been run 25 feet below the 180- foot level.
By connecting the points where the serpentine has been cut
in the different drifts an approximate representation of the
form of the above-mentioned lens of porphyry containing the
ore bodies has been given. A great amount of surface work
(assessment work) on a number of the claims has been done,
without, however, disclosing anything of importance. The
property is equipped with a 24-ton fine-ore Knox & Osborne
furnace.
Trinity Mine. — This consists of three claims, Trinitj' Nos. i,
2, and 3, in Sees. 21 and 22, T. 38 N., R. 6 \V. Messrs. Riesch-
ling, owners.
OTHER COUNTIES.
Besides the above described mines, there are a number of scat-
tered cinnabar deposits, none of which have been developed
to any great extent, in various sections of the State.
In Contra Costa County, near Mount Diablo, some cinnabar
has been found. [See Mon. XIII, U. S. G. S., page 378.]
In Del Norte County [see above cited, page 366, and Report
State Mining Bureau of Cal., XII, page 198] some prospect-
ing for cinnabar has been done near the northern border of
the county on Diamond Creek, an eastern tributary of the
north fork of Smith River. The Mercury- group, near the
mouth of Diamond Creek, is owned by Israel Dietrick and
others. The Diamond Creek group lies near the head of the
same creek, close to the State line.
In Mariposa County a cinnabar occurrence is mentioned by
Professor Whitney. [See Geological Survey of California,
vol. I, page 230.]
13— QR
196 QUICKSILVER RESOURCES OF CALIFORNIA.
In Santa Barbara County [see Mon. XIII, U. S. G. S., page
382; Report State Mining Bureau of Cal., VIII, page 537;
X, page 596; XII, page 366] are the Los Prietos mines in the
Santa Ynez range. These produced in former years some
quicksilver, but have been idle for a number of years. Another
occurrence of cinnabar has been mentioned near the Cuch-
amma River (the Eagle Quicksilver mine).
In Shasta County a cinnabar deposit has been to some extent
developed; it is 30 miles northeast of Redding, in Sees. 4 and 5,
T. 32 N., R. I W. The Clover Creek Cinnabar Company,
owner. F. P. Primm, president. Redding.
In Siskiyou County [see Report State Mining Bureau of Cal.,
XII, page 370; XIII, page 602], near Oak Bar, on the head-
waters of the west fork of Beaver Creek, in the northern part
of the county, some cinnabar deposits have been worked to a
slight extent by the Siskij'ou Quicksilver Mining Company
(G. V. Snow, president), of Oak Bar; the company has also
erected a small furnace.
The Barton-Lange is another property; H. J. Barton, owner,
Oak Bar. Both properties are non-producers.
Some cinnabar was found in the sluice-boxes of the hydraulic
mines in Horse Creek, in this county.
METALLURGY*
The subject has been extensively treated by Crookes and
Rohrig in "Practical Treatise on Metallurgy," vol. I (1868);
by Kgleston in "The Metallurgy of Silver, Gold, and Mercury
in the United States," vol. II (1890); also by Prof. S. B.
Christy, in vols. XIII and XIV (i 884-1 886), "Transactions
of the American Institute of Mining Engineers," and in "The
Imperial Quicksilver Works at Idria" (1884), by the same
writer; also in many technical papers, among which the "Min-
ing and Scientific Press" of 1878 and 1879, giving a transla-
tion of Mr. Kuss's description of the Almaden mine in Spain;
and further, in many European technical publications.
The scope of this paper is a statement of the present condi-
tion of the quicksilver industry of California, and hence the
older methods, no longer in use in this State, and those used
in Europe and elsewhere, will only be alluded to where neces-
sary for a thorough understanding of the subject.
The extraction of mercury from ores containing sulphide of
mercury and occasionally native mercury (the only forms
wherein mercurial ores of commercial importance are found)
can be classified as the metallurgical process of distillation.
It is accomplished by subjecting the ores to a certain degree of
heat, applied by one or the other of two methods: in tightl}"-
sealed retorts, wherein the ores are heated without coming in
direct contact with the products of combustion of the fuel; or
in large furnaces, where the heat and products of combustion
of the fuel pass direct into the ore mass and are carried off
with the heated mercuric vapors, to be subsequently condensed
in large cooling chambers. The retorts are generally of cast-
iron. The Fitzgerald furnace may, however, be classified as a
continuous brick retort furnace.
The essential difference in the two methods lies in the fact
that the vapors given off by the ores in the retort furnaces are
separated from those resulting from the combustion of the fuel.
(197)
19S QUICKSILVER RESOURCES OF CALIFORNIA.
Professor Christy, in his exhaustive study on Quicksilver Con-
densation [Transactions American Institute of Mining Engi-
neers, vol. XIV. page 237], found that in the products of
combustion of an average furnace-day at New Almaden, run-
ning on 3 per cent ore, those of the fuel amount to nearly 80
per cent of the total; hence the fumes from a retort furnace out
of which the mercun,- must be separated, are much smaller in
quantity and moreover less complicated in composition, so that
the liquefaction of the mercury is rendered much easier and
less costly. The theoretical advantage is, however, entirely
obliterated by practical disadvantages which restrict the use of
retort furnaces to a few exceptional cases. Their capacity is
small, and the relative labor and fuel expense consequently
ven,- high, so that even for rich ores they ofier a ver}- unprofit-
able method of treatment. Unless the ores are ver>' free from
iron sulphide, quicklime must be added, to prevent the recombi-
nation of the mercury and sulphur in vapor form at the mouth
of the exit pipe, where sudden cooling takes place. The use
of retort furnaces, except for the treatment of soot and of con-
centrates, maj' as a rule be considered bad practice. It must
be acknowledged that their erection in the case of prospects
and new mines has often been favored, because the cost of con-
struction is low, and the}' oSer the mine owner, who has only
a limited capital at his disposal, the chance of getting some
immediate returns out of his mine. This, however, is done at
the cost of the future of his property, for in order to get any
results he is forced to extract onl)- the ver>- rich ore. thereby
very materially reducing the average of the bulk of his ore
bodies. Besides, it may be stated that, with a few exceptions,
the products of those retort furnaces have scarcely ever paid
for the work of extraction, let alone that of the development
of the property.
It was stated previously that these furnaces might be prop-
erly employed for the treatment of concentrates. In the text-
books treating on this subject, it is generally claimed that:
"The attempts of mechanical concentration of quicksilver ores
" have usually not been successful, because the cinnabar is so
" friable that a greater portion floats ofi with the water."
[Egleston, above cited, page 804.] Air. G. V. Xorthey, at the
Manzanita mine, in Colusa County, has, however, been \ery
successful in concentrating the ore of that mine. The ore is
METALLURGY.
199
first crushed rather fine, and then passed through a 5-foot
Huntington mill. [See Fig. 63.] The pulp passes through a
concentrating plant, having a capacity of from i to 2 tons per
hour, depending upon the gangue. The plant consists of five
bumping-tables, the pulp going first to one table and from this
is divided over the four other bumping-tables. The tailings
are elevated and sized. The heavier pass over a Bartlett con-
Plan and e/eyat/on of Concentrating System.
Manzanita Mine .
a= Crusher
b'-Huntington /»//// (^Ty^
c,ci= Bumpirfg Tables
e= Tailings Concentrators 1 f^*' ^^^^s^^\s^'^
/ = Eievator
r I
r=t
3\ ■!::
C
' "
e_
D
centrator, and the lighter over a belt vaimcr without side shake.
This plant is driven by a 25-horsepower Harding distillate
engine, using 15 gallons of distillate per twelve hours, laid
down (including 28 miles teaming from Williams) at 20 cents
per gallon, or $3 per twelve hours. The plant requires one
concentrator and two helpers.
The concentration varies according to t'.ie amount o: iron
200
QUICKSILVER RESOURCES OF CALIFORNIA.
pyrites in the ore. When the latter are scarce it may reach a
high figure, but generally the concentration will be about 20
to I. When high in iron pyrites the concentration ratio will
be too low to produce a material which can be profitably handled
in a retort furnace.
The concentrates are dried and retorted in a lo-pipe retort
PHOTO Xo. 22. PIPE RETORT FURNACE. M.A.NZAXIT.\ MINE, COLUS.A^ COUNTY
furnace, which has some features worth noting, [See Fig. 64.]
B}' using arches around the pipe spaces, each retort can be
taken out separately without interfering with the working of
the others. Each retort has a separate mercury outlet, allow-
ing opportunity to judge about its workings, and the water
circulation through each water jacket can be regulated sepa-
rately. The firebox is placed to the side of the first retort,
instead of under it, enabling the easy discharging and charging
METALLURGY,
201
of this retort. B}' placing the door of the retort inside the
wall, cooling of the space against the door and consequent
accumulation of mercury at that point are prevented. The
charge is from 75 to 80 pounds of concentrates per shift, with
the necessary lime, against 150 pounds of raw ore. Two fur-
nace men are required — one per shift.
The expenses of this plant are about $25 per day for labor,
202
QUICKSILVER RESOURCES OF CALIFORNIA.
fuel, repairs, etc. The lo-pipe retort, with suitable ore, can
handle the total product of the concentrating mill, running day
and night, concentrating from 20 to 24 tons. The total cost
of the plant, not including the mill building, is approximatel3':
25 H. P. engine $1,000.00
Rock-crusher 250.00
5-foot Huntington mill 1,500.00
5 bumping-tables 1,000.00
Concentrating table 500.00
I elevator 100.00
Fittings, pipes, etc 150.00
Contingent expenses 500.00
I pipe retort, with building and drier
$5,000.00
. 2,000.00
$7,000.00
j7,uou.uu
This plant in three months turned out 330 flasks of mercurj-;
^ / / 1. i
4 I ron pipe from re/ort
Fig. 65. Condensing plant soot retort, Boston Mine.
and since the visit of the writer, has continued to be operated
with about the same results.
This pipe retort furnace may be considered as an example of
the best practice for such an installation • the condensing prac-
tice is especially very well conceived.
At the Boston mine (Knoxville), the soot is treated in a
retort furnace using a condenser formed b}' a wooden box,
surrounded by water, which is constant!}^ renewed, the exit
pipe from the condenser being partly immersed in the water
covering the top of the condensing box. [See Fig. 65.]
Another arrangement of flues under the pipe retorts, by
which the parts of the pipes nearest the front and back walls
receive the greatest heat, has been patented by Messrs. Johnson
and McKay. [See Fig. 66.] The exit pipes of these furnaces
are only 6 feet long, without any attempt at cooling; under
METALLURGY.
203
their lower end runs a wooden trough wherein the mercury is
collected, and a loose burlap sheet is thrown over the end of
the pipes and the trough. Whether this installation suffices
to condense all the mercury vapors is very doubtful.
Two different forms of cast-iron retorts are used. The pipe
retorts vary from lo to 12 inches in diameter, and from 7 to 9
feet in length, those of 12 inches diameter being generally the
shortest. Their capacity is then from 5.22 to 5.9 cubic feet.
There must be left sufficient space in the retort so that during
the roasting process a sufficient amount of free oxygen will be
present to carry off the other vaporized products outside of the
mercury. Professor Christy [above cited, vol. XIV, page 236]
calculates that i kilogram of ore, containing 0.75 kilogram of
faxed material and carrying 3 per cent of quicksilver, requires
0.067 cubic meter of air at 0° C. and 760 mm. pressure in
JOHNSON a M^ KAY
FURNACE
ltl///llllri}l,},l,,,,,Tr7r,
order to carry the sulphur off as sulphur dioxide, or at the heat
in the retorts, which can be placed at 100" C. when charging,
v^=v^ (i+cz /); 7' = o.o67 (1+^^^)^0.091 cubic meter, which
reduced to pounds and feet gives for i pound of ore, 1.46 cubic
feet of air. In most cases the ores carry sufficient iron sul-
phides to make the addition of some quicklime very advisable,
which will absorb the freed sulphur, according to the equation,
4 HgS + 4CaO = 4Hg+3CaS + CaO, vSOa. The sulphur freed
from the reduction of the iron sulphides to ferrous sulphide
(FeS.= FeS-f-S) will also be absorbed by the quicklime. The
preceding indicates that the practice of filling the retorts
almost completely with ore is wrong; a charge of about 150
pounds of ore, filling about one third of the retort, is the most
preferable. The retorts must be kept at a relatively low heat,
not exceeding that required for the volatilization of the mer-
cury, from 375° to 400*^ C. ( = 750'^ Fahr. ). The distillation
of cinnabar (HgS4-20 = HgH-SO,) takes place at about 360° C.
[Crookes and Rohrig, above cited, page 505.]
204
QUICKSILVER RESOURCES OF CALIFORNIA.
The charge generalh- remains twelve hours in the retort,
but at the Helen mine, Mr. Rocca has found that with his
highh- pyritiferous and rich ore he obtained better results by
leaving the charge twenty-four hours in the retort and keeping
the heat at its lowest limit.
METALLURGY.
205
The Ch retorts are generally i8 inches wide and 12 inches
high in the center, giving them an area of i square foot, and
from 7 to 9 feet long. Their charge capacity is consequently
larger. Their cost is also much higher — $200 apiece, against
$25 for a pipe retort.
The opinions of quicksilver operators differ very much on
the relative merits of pipe retorts and q retorts, both having
their adherents; but for soot furnaces those of the q retorts
are probably in the majority.
Mr. C. Fitzgerald has applied the principle of heating the
ore without bringing it into direct contact with the products
of combustion of the fuel to a continuous retort furnace. [See
Fig. 67.] This furnace con.sists of an inclined, arched channel
of firebrick (angle 35°) with a tile floor. It has a charging
hopper at the upper end and a discharge chamber with door at
the lower end. The flames from the fire chamber pass under
this ore chamber along two center flues, return along two out-
side flues, pass to the top of the arch at the lower end, and go
from the upper end to the smokestack. The vapors from the
ore chamber are conducted through an iron exit pipe, which
is placed near the upper end of the ore chamber and is water-
jacketed outside of the furnace, to two condensers. In the sec-
ond condenser an air current for exhaust is created by a water
spray under 100 feet pressure, working on limestone to catch
the flour mercury. The capacity of each chamber is rated at
10 tons per twenty-four hours, using one cord of pine wood. In
practice the capacity is less. Three of these furnaces have been
lately erected — one at the Culver-Baer mine, one at the Uncle
Sam mine, both in Sonoma County, and one at the Aurora
mine, San Benito County.
The reduction of quicksilver ores on a large scale is con-
ducted in California in shaft furnaces. The evolution of these
furnaces from the primitive forms can be found in detail in the
above-mentioned metallurgical works. Suffice to say that at
present continuous furnaces are exclusively used. They may
be subdivided into coarse-ore and tile furnaces, the former only
treating lump ore; the latter medium-sized and fine ores.
A reduction plant may be divided into two parts: the fur-
nace and the condensing plant. The latter is just as impor-
tant as the former. The requirements of a good furnace are:
that it burns the rock, that is, that all the quicksilver is elim-
206 QUICKSILVER RESOURCES OF CALIFORNIA.
inated from the ore when said ore is discharged and thrown
over the dump; that the charging be done in such a manner as
not to allow the escape of any considerable portion of the
fumes, thus preventing loss in mercury, and especially danger
to the health of the employes; and finally, that the furnace does
its work with a reasonable consumption of fuel.
The main portion of the masonry of a quicksilver furnace
is built of ordinary brick. The furnace of the Corona mine
in Napa County is an exception, being built of tufa instead of
common brick. Only those parts which are exposed to the
action of the fire and the products of combustion are lined with
firebrick. The common bricks are generally burned on the
spot, and very often the operators accept and build their fur-
naces with very inferior material, the result being that even
when dried and heated with the greatest care, large cracks
appear in the furnace, which are not only detrimental to the
regular march of the furnace, but cause a great decrease in its
quicksilver production, which, it is true, is not a complete loss,
as the metal forms in the furnace bricks as native metal and
cinnabar and can be recovered after tearing down the furnace,
but which still is a very unprofitable metallurgical treatment.
Another cause of rapid deterioration of furnaces is found in too
rapid driving, which can only be obtained by raising the
temperature in the furnace, generally to a degree which will
destroy in a relatively short time the refractory material used
in the furnace construction in those parts most exposed to the
high heat of the flame. From the data given subsequently on
furnace practice, it will be seen what a great difference there
is between the time the ore remains in the furnace in different
reduction works.
As in all other metallurgical processes, the end to be obtained
is not perfection from a metallurgical standpoint, but from a
commercial standpoint. As in a gold mill it is often good
practice to neglect the extraction of a small percentage of gold
out of the ore, so in furnace practice the amount of ore passing
through the furnace and the amount of fuel used must be
governed bj^ the condition of obtaining the largest results at
the lowest cost per unit of produced metal. This depends to a
great measure on the special conditions existing in different
plants.
It may be here stated that the superintendence of a quick-
PHOTO No. L'3. CORONA FURNACE.
PHOTO No. 24. TUFA FURNACE IN COURSE OF CONSTRUCTION, CORONA
QUICKSILVER MINE.
208 QUICKSILVER RESOURCES OF CALIFORNIA.
silver reduction plant requires a great amount of technical
knowledge, both practical and theoretical, and a constant
personal super\-ision ; to put such a plant in the hands of any-
bod}' who is not thoroughly competent will invariably lead to
disappointment and financial loss.
The coarse-ore furnace is simplj- a shaft in which the ore is
dumped from the top, extracted at the bottom and heated
directly by the flame from the fireplace, the products of com-
bustion passing through the ore column. The lumps vary in
diameter from 3/^ to 9 inches. Various types of these furnaces
are at present in operation.
Exeli Continuous Furnace. — This furnace was first introduced
in 1 87 1 at Idria, Austria, b}- Bergrath A. Exeli. Two of these
furnaces are in use at Xew Almaden — furnaces Xos. 7 and 9.
Fig. 68 represents this type of furnace, of which a ver}- complete
description is given by Egleston [above cited, page 85 7] and
S. B. Christy [above cited, vol. XIII, page 561]. These iron-
clad furnaces, built in 1874 and 1875, are still in operation,
treating 1 2 tons of ore ever}' twent3'-four hours; the ore remains
forty-eight hours in the furnace. While it is generally taken
for granted that ores carrjdng a great amount of metallic
mercury can not well be handled in shaft furnaces, these two
furnaces in former j-ears gave verj' satisfactory results when
burning the ore from the 1500-foot level, Randol shaft, which
contained large quantities of native mercur5\ The charge con-
sists of about 1600 pounds of ore. These two furnaces require
two men per shift, and burn each 0.605 cord of wood per twenty-
four hours. The cost of treatment per ton is :
Labor $0.4166 (')
Fuel 0.3025 (^)
Total J0.7191
/ \ 4Xt2.so » ti/L I \ o.6o5X$6.oo .
(i) :lrl£—5_. =$0.4166 (2) ^^^^ = K).3025
24 12
IRON CLAD SHAFT FURNACE
(CONTINUOUS)
SECTION A B
ELEVATION
HORIZONTAL SECTIONS.
Fig. 68. Exeli Furnace. Scale \i"=i'.
210 QUICKSILVER RESOURCES OF CALIFORNIA.
Knox-Osborne Coarse-Ore Furnace. — This furnace was patented
in 1872. [See Fig. 69. J Formerl}- a number of these furnaces
were in use, but in later years their number has been greatly
reduced. One furnace is in use at the Manhattan mine (Knox-
ville), and the old furnace at the Cerro Bonito mine, San Benito
County, has been renovated. [For description, see Egleston,
above cited, page 841.]
Some fine ore can be charged with the lump ore, but only
sparingly, other^'ise it will choke up the passages between the
lumps, through which the products of combustion of the fuel
must freely circulate. The inventor ob\dated this by adding
some pieces of wood to the fine ore when much of this material
was contained in the charge, but this did not fully obviate the
trouble ; and besides, the addition of fine ores materially reduces
the daily capacity of the furnaces. Consequenth', since the
general introduction of the tiled furnaces, only coarse ore is
charged into the various coarse-ore types of shaft furnaces.
The cubic content of the furnaces is about 75 tons, and as it
handles about 24 tons per da}-, the ore remains about three da3's
in the furnace. The wood consumption on coarse ore is from
one to one and a half cords of oak per twenty-four hours.
Three men per shift are required.
Luckhardt Continuous Coarse- Ore Furnace. — This furnace was
used in former years at several mines, but at present none are
working in California. [See Egleston, above cited, page 838.]
Neat*s Coarse-Ore Furnace. — Patented by John Neat. [See
Fig. 70.] Two of these furnaces are at the St. John mine, Solano
County. This furnace has no fireplace. The ore is charged with
coke in alternate layers, using from 3^^ to 4 per cent of coke,
depending on the draft in the furnace. The drawing space in
the bottom of the furnace is open, leaving access to the air
and furnishing the draft. The top of the furnace consists of
a hopper, with doors at the bottom, moved by levers from the
charging floor. At this floor there is besides a cover with a water
seal, and provided with a glass panel to judge of the condition
of the charge. When the latter is at red heat a charge is with-
drawn from the bottom. This is done bj^ withdrawing the
fork (c), resting on the bar {d). The drawing is done at inter-
vals varying from i^ to 2}( hours, according to the draft,
-D
I '
Hat=ii
Lk
'Mill I I
iffiTitTTiTni-nTiirniii-nifTTiirftTT^ '.;
imn 111111111
14— QR
212
OUICKSILVER KESOURCES OF CALIFORNIA.
which is dependent upon atmospheric conditions. The ore
must be in pieces of i}^ inches or over. Judging from the
Charging Hopper
^^.
>^
^c/
/ran p/afe f/oor
Discharging Fork and
Door.
COARSE ORE FURNACE.
JOHN NEA TS' RAT.
furnace dump, a certain amount of clinkering takes place in
the furnace.
METALLURGY.
213
New Idria Coarse-Ore Furnace* — [See Fig. 71.] This furnace
has been designed by Mr. B. M. Newcomb, the general superin-
tendent of several of the principal quicksilver mines in the State.
\
>'
*^o
^Q
J '
/•
-) 1
-^
J
Su/ptjffff -
.\
T
X
J ^ '■
V
Cc:
V^'l
~)
^j'^:.
\
^
7---'
I
As will be seen from the sketch, the fire is applied on both
sides of the charge, which is only 4 feet through, and 6 feet
long in each compartment at the level of the top of the fire
chambers, and is heated at three sides, while besides, as it
214
QUICKSILVER RESOURCES OF CALIFORNIA.
comes .nto the fire
chambers, the charge
spreads, thus causing
its speedy heating to
the highest tempera-
ture in the furnace.
The depth of the dis-
charge doors below
the level of the fire
chamber gives the ore
a chance to cool off,
and to give off the
mercury vapors not
volatilized during its
passage in front of the
fire chamber. This
furnace is 17 feet
wide, 24 feet through
at the level of the fire
chamber, and has a
total height of 42^^
feet from drawing
floor to charging
track. It handles from
90 to 100 tons per
twenty-four hours; its
cubic capacity is 2400
feet, hence the ore
remains a little above
twenty-four hours in
the furnace. It is
run by two shifts of
five men each — one
furnace man, two
chargers, and two
drawers — and requires
not quite 2 ' - cords of
wood per day. The
excessively low fuel
consumption is parth'
due to the high per-
centage of iron sul-
phide in the ore.
METAIJ.rRGV.
215
The fine-ore furnaces belong nearly all to the tile furnace
type, with the exception of:
Livermore Furnace. — [See Fig. 72.] Only two of these fur-
naces are at present in operation — one at the Cloverdale mine,
the other at the Culver-Baer mine, both in vSonoma County.
The latter is a reconstructed Fitzgerald furnace. For more
detailed description of this furnace, see Egleston, above cited,
page 887.
The tile furnaces generally adopted in California are the
Fig. 72. Longitudinal section. Modified I.iverinore quicksilver furnace.
Litchfield, the Knox & Osborne fine-ore; and the Hiittner
Scott.
Litchfield Furnace has been in operation at the Great Western
mine, Lake County, for a number of years, and has given
good satisfaction, although admittedly consuming more fuel
than the Hlittner-Scott furnace. It resembles closely the lat-
ter, except that the heat ascends in the ore chambers between
the walls and the tiles, instead of being forced to pass over the
tiles.
Knox-Osborne Furnace» for fine ore, is used in the Manhattan,
Altoona, and Integral mines. This furnace has a capacity of
24 tons per day. It consists [see Fig. 73] of two ore chambers,
across which the inclined tiles are placed in a checkerboard
manner; the two upper rows of tiles are of cast-iron, the others
of fire clay. The ore glides down along the channels formed
by the inclined places. The double fire chamber is at one side
^.F-
H-f
.9 €/
PHOTO No. 26. CLOVERDALE REDUCTION PLANT.
PHOTO Xo. JT. GRK:A r WKSTEKX (jriCKSILVER MINING CO REUl'CTION PLANT.
218
QUICKSILVEU RESOURCES OF CALIFORNIA.
of the ore chamber. The partition walls between the fire
chamber and the first ore chamber, between the ore chambers,
and between the second ore chamber and the first dust cham-
ber, are pierced with pigeon holes, through which the flames
pass, heating the tiles and the ore. The partition wall between
the first and second dust chamber, both of which form an
integral part of the furnace, has five openings 3 feet high on
the level of the floor of the fireplace, creating a down draft
PHOTO No. 28. MANHATTAN FURNACK.
in the furnace. The second dust chamber is provided in its
outer wall with a large opening near the top, through which
the fumes pass into the first condenser, which is built at the
Integral mine contiguous to the furnace. The top of the fur-
nace is open ; the charge is placed directl}^ on the upper rows
of tiles; the down draft above mentioned being deemed suffi-
cient to prevent the escape of gases from the furnace.
Huttner-Scott Furnace,— [See Fig. 74.] This furnace repre-
sents the latest evolution of quicksilver furnaces in California.
Originally only used for fine ores, it has been modified to burn
METALLURGY.
221
Fig. 75. Tiling of Furnace Xo 3. New Alniaden.
also medium-sized ore, up to 3 '2 inches. It is extensively
described and discussed by Egleston [above cited, page 864]
and Christy [above cited, vol. XIII, pages 553 and 566]. The
tiles form a zig-
zag plane, along
which the ore
fed from the top
slides down
through the fur-
nace until finally
discharged at its
bottom through
the drawing pit,
being gradually
heated on its de-
scending course.
The size of the
ore lumps which
can be treated in
this furnace is governed by the distance between the edge of
one shelf to the face of the next below it, called the shelf-slit.
This distance was 3 inches in the first furnaces. Since then
it has been increased; the general dimensions now used is
5 or 6 inches, allowing medium-sized ore to be charged. In
furnace No. i, New Almaden, built in 1880, the shelf-slit is
8 inches, the largest
'^ used in any furnace
^ of this type.
'^ Generall)- the tiles
'Z are flat; their largest
^ commercial dimen-
'^ sions are 3 inches
by 15 inches by 36
^ inches. They are im-
ported, and cost, laid
down in San Fran-
cisco, $3.50 apiece.
Larger tiles, or those of special form, cost more. The detail
sketch shows the manner in which the tiles are secured in the
ore chamber.
Furnace No. 3, New Almaden, has a different form of tiles.
[See Fig. 75, and \ol. XIII. above cited, page 575.] These
Tiling oT Cerniak-Spirek furnace.
222
ouicksilvp:r kesoukces of California.
tiles have not proven as satisfactory as the flat ones. In Europe,
however, a similar form of tile is commonly used in the Cermak-
Spirek furnace. [See Fig. 76.]
All the Hiittner-Scott furnaces have the lire chambers on
one side of the ore chambers, and a vapor chamber on the other
side, except the Wide Awake furnace at Sulphur Creek. Colusa
County, where a fire chamber is placed on lioth sides of the ore
PHOTO Xo 3,1. FURXACK PLANT. IXTEGKAL MIXE. TKINirV COUXTY.
chamber. Mr. Gibson claims that thereby the capacity of the
furnace is materially increased without increasing the fuel
consumption. Mr. Robert Scott is of the opinion that one set
of fire chambers is sufficient to heat the ore which can be put
through the furnace to the required temperature.
The Hiittner-Scott furnaces are made of various capacities,
which are governed by the number of ore chambers in the
furnace, and by the height of each ore chamber. Following is
a table giving the dimensions of some furnaces:
METALLURGY.
223
s-inoH
-2 ° '.
>!? is?
■jaqtunx
Hex- a
^ .
c
S
1§§ 1
^K<
a 2
u c
Sx
nt
til SlIIBUIdH
aSJBij^ ajiiij.
■XjpBflB^
•jndino XjiBa
'j:^ r:c tr, r^ fr. ^
S. f^ rO Tf ■* ro
■s::^ is?
.V ir, -r ■* t» o
■t;:^; :s ;se <: S2
.J> t^ M o 0> CO >0
<, - - " •- -
^ ^
to W \0 to M ^2
2 5 a s,
.:^ j^ j^ ^ ^
— — _ ^ u
x. /. y. y. £ ~ p.
r •: - 3. a ai;
- /^ r. -x «; O
224
QUICKSILVER RliSOURCES OF CALIFORNIA.
At the New Almauen, some furnaces, viz., Xos. 3 and S, are
entirely surrounded by iron plates, and are called "ironclad
furnaces." This method of inclosing a furnace gives very good
satisfaction, but is very expensive. Generally furnaces are
inclosed in a wooden framework strengthened by iron tie rods.
In order to prevent this wooden framework from catching fire,
especially near the cracks in the furnace, which are almost
inevitable, it is advisable to surround them with asbestos, 2
t "
PHOTO No. 31. K.-VRL FrR.\.\Cl.. r-AX LUIS OBISPO COUNTY
inches thick. [See Fig. 84.] The later furnaces are commonly
of a daily capacity of 10, 20, 30, and 50 tons. The principal
materials entering in these furnaces are:
lo-Toii. i)o-Toii. so-Tou.
Common brick No. 150,000 300,000 400,000
Firebrick " 12,000 20.000 30,000
Tiles " iSS 360 42S
Cement bbls. 25 40 50
Fire clay.
Timber for frame.
Iron for frame, grates, hopper ^ etc.
METALLURGY.
225
The price of the firebrick is $32.50 per 1000 at San Francisco.
The price of tiles 3 inches by 15 inches bv 36 inches is S3. 50
apiece.
When the ore is charged moist in the furnace a great amount
of water vapor will be formed, which not only increases the
already excessive amount of fumes out of which the mercury
must be condensed, but also the formation of a great amount
of sulphuric acid and of sulphates, both of which are very
injurious to the condensers. The opinion of operators as to
}-"lG 77. Ore Drier, Utilizing exhaust Ml uiii
the desirable degree of dryness of the ore before charging dif-
fers. Some claim that for good practice absolutely dry ore
would be preferable, while others consider a relatively super-
ficial drying sufficient. In dry climates sun dr>ing ma}- in
cases then suffice. In many furnace plants the ore is dried by
spreading over iron plates on the top of the first condensers.
In other plants, for instance at the Oathill. Great Eastern, etc.,
a special drier is used. [See Fig. 77.] The exhaust steam
Fig. 78. Ore drier. Special furnace at Abbott Mine.
15— QR
228
OUICKSILVliR RESOURCES OF CALIFORNIA.
from the engine driving the fan is passed through coils under
the platform on which the ore is spread. At the same time,
at Oathill, exhaust steam is brought into the first condenser.
At the Abbott mine, a special furnace is used to heat the plat-
form of the ore-drier. [See Fig. 78.] Sixty tons of ore can
be dried in twenty-four hours, using two cords of oak wood.
The ore charged in furnace No. 3, at New Almaden, passes
through a brick shell surrounding a condenser, and provided
with a series of tiles placed at an angle of 45°, thereby obtain-
ing the double result of drj'ing the damp ore and materially
increasing the condensation in the condenser.
Again in other furnaces the ore is only dried while in the
charging hopper and
partly in the upper part
of the furnace. At the
Manhattan furnace a
special flue conducts the
fumes from the upper
three rows of tiles to the
first brick condenser.
These fumes are prin-
cipally water vapor, but
yet contain some mer-
cur}' vapors. At the
New Idria furnace,
where the fumes ema-
nating from the upper
part of the charge are highly sulphuric, due to a great amount
of iron pyrites in the ore, the device indicated in Fig. 79 has
been adopted, which has proven ver}' effective. The pipe (e)
goes to a special blower, from which the fumes are conveyed
to the smokestack. Mr. Robert Scott proposed to dry the ore
in the top of the furnace and to csLvry off the fumes there
formed by making the tiles of the upper three rows of cast-
iron and hollow, and passing the fumes through these hollow
tiles, instead of over the charge. [See Fig. So.] In order to
prevent the clogging at the top of the furnace, rakes worked
by levers from the charging floor are used. [See Fig. Si.]
Mr. H. C. Davey divides the furnace into two vertically super-
imposed compartments. In the lower part the roasting takes
place as in the Hiittner-Scott furnace. The upper part is
^y/J///h'//3y////^
— <-
Fig. 79. New Idria fine-ore furnace. Method of
conveying fumes from top.
4 — Counterweight, chained. B — Furnace hopper.
C — Iron door D — Track for side dumping car.
E — Cast iron pipe (12'" to blower and smokestack.
Fig. So. Top of the modified Scott furnace. Scale %"-^i'
232
QUICKSILVER RESOUKCES OF CALIFORNIA.
heated, by a separate furnace, only to the temperature required
to dry the ore. The ore falls through a narrow vertical throat
from the upper into the lower compartment of the furnace. In
the modified plan of Mr. Scott, above mentioned, this end is
attained bj' bars and rakes. [See Fig. So.] To cause the ore to
move down gradualh' while charging, the throat below the
hopper must have the same width as the shelf- slit.
234
QUICKSILVER RESOURCES OF CALIFORNIA.
The discharging of the furnace is also done in various ways.
[See the detailed plans in Egleston and Christy, and plans in
Figs. 73, 74, and 82.] Generally the hood of the flue carr^'ing
off the fumes emanating while discharging is close to the tim-
ber ib), causing danger of hot dust accumulating against the
frame timbers, and rendering it difficult to remove the dust.
This is obviated by the construction shown in Fig. 83.
The general arrangements of
furnace plants are shown in
Fig. 84 (Oathill furnace), Fig.
85 (Abbott furnace), and Fig. 86
(St. John furnace), and several
photographs. The plan of the
New Almaden is given on a
large scale in the works of
Egleston and Christy, above
cited. Most of the furnace
plants have been gradually en-
larged, and as their site is nearly
alwa^-s in a mountainous region,
this gradual enlargement has
often forced, by lack of proper
room, the condensing plant to
be built in a ver\- irregular
manner.
The condensing of the fumes
emanating from the furnace and the recovery of the mercury
offer a very complicated problem. The distillation heat of
cinnabar is 360° C, or 680° F., hence the fumes must leave the
furnace at a temperature higher, but as near as possible to it;
the theoretical product being mercur}- in vapor form and
sulphur dioxide (HgS^20 = Hg+S0,).
In good practice the temperatures of the fumes as they leave
the furnace appear to come very near to this limit. [See
Christy, vol. XIV, above cited, page 226.]
Fig. S3. New Idria fine-ore furnace.
Details of drawing door.
A — Sheet iron hood carrying away
fumes. B — Bracing rod and hood
(asbestos covering). C — Iron door in
iron-lined chute. D — Ore car.
-xk ^^0
v^Nfj.! i i
y
^-^A.
i>-^'
f
■ 1^-
i
T
I
;Fi'
i< iiitiihjil :ai-»nl .' '•.'sstnu) bnr. ?no9tti»baoo io noU'i-v
Fig. 84.
General plan of reduction works. (Mineral Industry.)
Vertical section ol condensers and furnace on A B. (Mineral Industry.)
furnace and elevation showing condensers. (Mineral Industry.)
^^JK »»»»'>\ ■^%»iWo'^
>^v>l4**')
•-rf-
IS
♦.%M*VT
A^-»\\vA->'\«>6
'v<i.'-.>'Qt\»'b ^wW r'aV.qi^"
^
^ TR
wpyfc^w^*-^
J L__ JinjJ.
^1 *^ * V
'1
^.
j »»<VAU"\
i
1
5.
a
j',0
^
>
i^
(.-{i)Hnbu( iBwniM) .a^iow noiioubsi to ujslq IbtousO
236
QUICKSILVER RESOURCES OF CALIFORNIA.
Temperature Determinations as Taken by Mr. J. R. Smedberg,
February, iSSo, with Furnace No. 9, New Almaden.
Degrees
Celsius.
1. Lowest peep-hole (above fireplace) 823^
2. Next higher 946
3. Next higher 878
4. Topmost peep-hole (near furnace throat) . . . 372
5. Entrance to first brick condenser* 190.6
6. End of second brick condenser 37.8
7. End of first glass and wood condenser 25.6
S. End of second glass and wood condenser. . ; 17.8
9. End of third glass and wood condenser .... 15.6
10. End of fourth glass and wood condenser. . . 14.4
11. End of fifth glass and wood condenser 14.4
12. End of sixth glass and wood condenser ... . 13.9
13. End of wooden flue, entrance to sidehill
flue
Degrees
Fahren-
heit.
1612
701
375
100
78
64
60
5S
58
57
Fall in
Degrees
Celsius.
iSi.r
I52.S
12.2
7.8
2.2
1.2
0.0
O.:
Fi&. 55. sketch showing method of handling ore at Abbott Mine, Lake County.
According to this table, the cooling takes place principally
in the down-take and in the two brick condensers, the fumes
being cooled to a temperature of 37.S- C, and moisture begins
already to appear. It is to be regretted that the results of
similar temperature determinations on a modern Hiittner- Scott
plant are not available.
".After passing through the iron down-take, see description of furnace.
«^ —
Co
I
u-
- — i:
— «»
METALLURGY.
239
The fumes as they leave the furnace are far from resembling
the theoretical product of distillation of mercuric sulphide.
These are mixed with the roasting products of the ore, to wit:
water vapor, carbon dioxide, and mechanicalh' entrained ore
dust; and the products of combustion of the fuel, to wit: water
vapor, carbon dioxide, and mechanically entrained ash. In
Volume XIV (above cited), page 234 and following, Professor
Christy gives a detailed study of these fumes and their
PHOTO Xo. 36. GRE.A.T EASTERX FURNACES.
behavior, and the conditions for a well-constructed condensa-
tion plant. When coming in contact with cool surfaces, the
fumes deposit a solid material known as "soot," consisting of
the ore dust, ash, some tarry hydrocarbons, and the products of
the decomposition of the CO^ into CO and O. The most
important condensed constituents are water, sulphates of
iron, alkali mercury, and sulphuric acid. The water absorbs
from the condensed vapors, sulphurous acid, chloride of
ammonia, hydrocarbons, etc. The sulphuric acid, especially
when present in large quantities, as in the case when roasting
240
QUICKSILVER RESOURCES OF CALIFORNIA.
highl)^ pyritiferous ores, is a most troublesome product, as it
attacks every material out of which condensers are constructed.
The soot is an intermediate product, which is only detrimental
when it forms in excessive quantities. It has the advantage
of retaining the minute globules of mercurj^ which form at the
moment of sublimation and would otherwise be carried ofi by
the gases. [Mist loss, see vol. XIV, above cited, page 233.]
Spirek [ly'Industria del Mercuria in Italia, page 14] mentions
the fact that the soot causes the mercury contents of the
fumes to be below the saturation point.
The products of the condensers are: for the hot condensers
near the furnace, mainly dry quicksilver and soot mixed with
ore dust; farther on, quicksilver, acid water (containing mainly
sulphuric acid), and damp soot; for the last condensers, acid
waters, holding various sulphates in solution, colored black by
the soot, and carrying some very finely divided quicksilver;
,(r
' Side£/er
•lecond Col/echha
^U3^| i aunder
Fig. SS. Installation to save flour mercury, Xew Almaden.
finally, for the flues to the smokestack, nearly dry soot with
very little quicksilver, rarely visible to the naked eye.
The quicksilver is collected in inclined troughs running
along the outside of the condensers. [See Fig. 87.] The
water vapors contain some very finely divided mercury, which
floats on the water brought down by their condensation. At
New Almaden, a special installation has been constructed to
save this quicksilver [see Fig. 88, which explains itself], and
considerable quicksilver is thus secured. Even repeated passage
through such settling boxes will not save all the minute
quicksilver globules.
The draft in the fire chamber of the furnace and the passage
of the fumes through the furnace and the condensing plant to
the smokestack are caused and regulated by the introduction
of a blower in the course of this travel. Sometimes a fire draft
at or near the stack is added, and at the Xew Idria furnace an
METALLURGY.
243
auxiliary blower is used. At the Abbott furnace the blower
is placed between the first and second condensers — a verj-
unusual location.
The condensing plant, as above stated, must answer the
double purpose of cooling the fumes and causing the deposition
of the liquefied quicksilver. Professor Christ}' [above cited,
vol. KIV, page 207] concisely states the various difiiculties
PHOTO No. JJ. OCEANIC QUICKSILVER REDUCTIOX PL.^NT, SAN LUIS
OBISPO COUNTY.
encountered in this operation, as follows: "The quicksilver
"fumes furnish often less than one per cent by volume of the
"products of combustion with which they are mixed."
When Professor Christy wrote this (1885), the mines were
running on much higher grade ore than at present; 0.5 per
cent is a fair average (even probably a little too high) of the
ore now passing through the various furnaces in the State.
The volume of the fumes produced is [see above cited, page
236], per kilogram of ore, 0.185 cubic meter, at o" C. and 760
mm. Hg: that of the vaporized quicksilver
244 QUICKSILVER RESOURCES OF CALIFORNIA.
I cu.m. >; o.oos
:^ — ^ = 0.00058 cu. m.,
8.96 ^
or 0.31 per cent of the total fumes.
"Even the weight of the quicksilver is inconsiderable com-
" pared with that of the gases which pass through the con-
" denser."
Under the present conditions as above mentioned their per-
centage would be:
Hg =0.005 kilogram.
CO2 = 0.100 •'
SO. = 0.040
N =0.132 "
Water vapor = o. 100 "
Total weight of dr}- gases
at 0° C. and 760 mm. Hg = o.377 "
Weight of quicksilver vapor
at 0° C. and 760 mm. Hg = 0.005 " or 1.3 per cent of total weight.
Professor Christy continues: "These facts add greatly to the
"difl5culties of condensation. For in the first place, the heat
"must be extracted from the fumes in order that the quick-
" silver may be liquefied. Next, the whole volume of the gases
"must pass through the condensers at a certain velocity, in
"order to maintain the draft of the furnace. The minute
"condensed globules of liquefied quicksilver are likeh' to be
"carried oflf in the form of 'mist.' The gases which escape from
"the condensing S3'stem are necessaril}- saturated with quick-
"silver vapor at the temperature of escape." (This loss is,
however, very small. Assuming, as Professor Christy does
[page 245], an average escape temperature of 20° C, the cal-
culated loss would be 0.83 per cent of the total yield [see
Table XIII, page 243] ; while according to Mr. Spirek [see
above, page i S] the soot prevents the fumes from being satu-
rated with mercury vapors.) " Then there is the ever-present
"mercurial soot, which requires separate treatment. The
"quicksilver itself is read}- to escape from any crack or crevice
"of the condensers, either as a liquid or a vapor. Finally, as
"soon as the condensers become cool enough to act effectively,
"they are attacked by the dilute sulphuric acid formed from
"the oxidation of the sulphurous acid in the fumes. This
"agent slowly attacks and destroys almost ever\- material out
"of which the condensers can be made."
To combine the effects of cooling and deposition of the quick-
silver in the most preferable manner, three factors must be
PHOTO No. -JS. INTERIOR VIEW OF REDUCTION WORKS,
NEW ALMADEN— HACIENDA.
PHOT(J No. -1-1. NEW IDRIA, SHOWING ROUND WOODEN FLUE: AND WOODEN
TANKS USED FOR CONDENSERS.
246
QUICKSILVER RESOURCES OF CALIFORNIA.
considered: the length of the path of the vapors in the con-
densing system, the interior volume of the system, and the area
of the cooling surface. It is to be regretted that very little data
regarding these conditions in the diflferent furnace plants are
available.
Mr. Robert Scott considers the condensing room required for
a 40-ton furnace 17,000 cubic feet, and for a 50-ton furnace,
20,000 cubic feet, which must be increased as the ore diminished
PHOTO No. 45. RETORTING SOOT, GREAT EASTERN MINE.
in grade. Professor Christ}- [above cited, page 224] gives this
data for furnace No. i at New Almaden. The totals are: Path
of vapors from furnace to top of chimney, about 1000 feet;
interior volume, 26,667 cubic feet; cooling area, 18,653 square
feet; ratio of cooling area to interior volume is 0.69. It must
be remarked that the brick condensers give onl}- a ratio of 0.5.
In the brick condensers at present built by Robert Scott, the
interior volume is about 1927 cubic feet; the cooling area,
922.5 square feet; giving about the same ratio.
Following is a table furnished by Mr. E. W. Carson, super-
intendent of the Oceanic Quicksilver Compam-:
METALLURGY.
247
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METALLURGY.
249
The ratio of the cooling area and interior volume is here for
the total plant H^ ol = 0-39) mainly due to the unscientific
construction of the brick condensers (built before Mr. Carson
arrived on the property), which show a ratio of I'VrW ^^^
f ^ff» respectively about 0.28 and 0.27. Mr. Carson has tried
to remedy this to some extent b}- cooling the top of the first
two chambers by water. In fact, this plant as constructed a
few years ago was a striking example of the result when met-
allurgical work is placed in ignorant hands.
-z'C
Fig. 90. Knox Ironclad Condenser.
A great number of different condensers, built on varying
plans and with varjdng material, have been devised. Their
details can be found in the works above cited. At present the
following are in use in California:
Brick condensers are constructed in different dimensions,
from 9 by 5 feet, 5 feet high (the small brick condensers at the
Great Western mine in Lake County), to 8 by 16 feet, 29 feet
high, at the Oceanic. The condensers at present built by Mr.
Robert Scott are 14^4 by 8 '2 feet inside, 22 feet high from
Fig. 9! . Water Tank Condenser.
METALLURGY.
251
^^
i f
1,
!
y y
lower part of floor to top of building, with a central partition
wall to deflect the fumes on their passage, an inclined bottom
with a spring of 15 inches, and earthenware exit pipes. The
side walls are 9 inches thick. They are generally arch-topped,
sometimes covered by iron plates. [See Fig. 89.] Each con-
denser is separated from the one adjoining and connected by
earthenware pipes; the first and second by iron flues.
To hasten the cooling of the fumes, narrow iron tanks con-
nected by cast-iron pipes have been placed in some plants,
mainly in the first condenser at the end walls, water circulat-
ing through the installa-
tion, called "waterbacks."
[See vol. XIV, page 216.]
At the Karl mine, San
Luis Obispo County,
8-inch tile pipes, through
which water circulates,
have been placed in the
first four condensers.
At the New Idria mine,
stone is' used for the
construction of some con-
densers.
The iron condensers at
present used are generally
of the Knox type. [See
Fig. 90, and Egleston,
above cited, page 846.]
Where the ore does not
carry too much iron
sulphide, they stand very well. At the Manhattan mine, on
the coarse-ore furnace, seven iron condensers were installed
behind two brick-dust chambers. These have been used from
1874 to 1877 and from 1885 to 1887 continuously, and from
1889 to the present date about two months every year. All
joints are luted with Portland cement.
Another iron condenser, the "water tank condenser" [see
Fig. 91], is used at New Almaden for furnaces Nos. 7, 8, and 9.
[See Egleston, page 860.] These condensers give very good
satisfaction.
^Jte
The Baker Flue.
252
QUICKSILVER RESOURCES OF CALIFORNIA.
The farther the parts of the condensing plant are from the
furnace, the more they are exposed to the deteriorating effects
of waters carr^dng sulphuric acid, and experience has taught
that wood is the onlj- material which will resist the eSects to a
great extent, especially pitch pine, hence the use of wooden
constructions in those parts of the plants which are not exposed
to too high temperature. At New Almaden the wooden Baker
&
a" Tile P/pa
Q"TJIe Pipe
t /// / /// / / //// /7Z
£:jei/a t/'on , ^sech'on .
Fig. 93. Wooden Condenser Box. Corona Mine.
flue [see Fig. 92] has been used for years. Stave pipe flues are
now frequently'' used also for connections between brick con-
densers and for smokestacks. Wooden condensers are fre-
quenth'' constructed, especiall}- in the form of barrels. Those
at the New Idria coarse-ore furnace have a diameter of 8 feet
and are 14 feet long. Similar wooden barrel condensers are
also used at the Karl mine, Oceanic mine, etc. The great
difficulty with these stave constructions lies in the iron bands,
which are corroded, especially in the lower half of the circle,
METAIXURGY,
253
which at the New Idria have been replaced, as an experiment
by wooden bands made of wheel felloes.
At the Corona mine a wooden box has been erected between
the fifth brick condenser and the flue to smokestack. This
box is IOC feet long and traversed by 8-inch tile pipes for air
Fig. 94. Soot-Cleaning Machine.
circulation, in order to cool the fumes. [See Fig. 93.] The
blower is between the fifth condenser and this box.
In the smaller mines the soot is still worked by hand as de-
scribed by Egleston [above cited, page 810, and vol. XIV, page
230], but in the larger mines, soot machines are used. [See
Fig. 94.] Generally the residue is treated in retort furnaces,
but at New Almaden the residue is re-charged in the fine-ore
furnace.
ELEVATIONS.
Elevations for which no authorities are given are from barometrical observations
during field work for the Quicksilver Bulletin, by Wm. Forstner, Field Assistant.
COLUSA COUNTY.
Feet.
Central mine — Main tunnel 1675
Divide between Colusa and Lake counties, at crossing of road
from Sulphur Creek to Abbott mine 2125
Elgin mine — Main tunnel 2275
Empire mine — Tunnel at southeast end 1715
Tunnel in Sulphur Creek 1475
Manzanita mine — Shaft 1950
Sulphur Creek — Blank Springs Hotel 1575
Schoolhouse 1525
Wide Awake mine — Office 1600
EL DORADO COUNTY.
Bernard Quicksilver mine — Tunnel 925
Canon — Store 900
Placer^-ille *i830
FRESNO COUNTY.
Arambide mine — Tunnel 1440
Corner of Fresno, Kings, and Monterey counties 3145
Little Panoche Pass 1800
Mexican mine — Cabin 3640
Providential mine — Tunnel 1600
Ridge on Gabilan claim 2480
KINGS COUNTY.
Avenal Creek at mouth of Bull Pen Gulch 1530
LAKE COUNTY.
Abbott mine — Office 2000
Shafthouse 2050
Adams Springs 2725
Anderson Springs 1475
Baker mine — Retort furnace 1375
Brown's mill on Kelsey Creek 1650
*s P. R. R. Co.
(254)
ELEVATIONS. 255
Feet.
Bullion mine — Collar of shaft 1540
Chicago mine — Cabin 2700
Clear Lake 1340, + 1400, i 1310
Divide between Adobe and Kelsej' creeks near Kelseyville 1725
Divide between Lake and Sonoma counties —
Crossing Great Western tollroad 2675
Crossing road from Helen to Bacon mine 3210
Pine Mountain 3475
Crossing old road from Middletown to Pine Flat 3300
Crossing road from Middletown to Dewey's mill 3200
Mount Cobb, eastern rim 4500
Mount Cobb, northwest point 4050
Geyser Rock, northwest of Mount Cobb 3660
Glenbrook 2300
Gordon Springs 2500
Great Western mine — Store 2080
Helen mine — Furnace 2760
Howard Springs 2180
Jewess mine — Cabin 2525
Kelseyville 1435
King of All mine — Lower tunnel 1875
Lakeport 1400
Lower Lake 1400
Lucitta mine — Retort furnace I975
Middletown 1200
Middletown mine — Upper works 2400
Mirabel — Office Standard Quicksilver Co. 1460
Mount McGuire 2750
Red Elephant mine — Cabin 1S25
Road from Lower Lake to Abbott mine-
Forks of Bartlett Springs and Abbott roads 1415
Divide at head of Phipps Creek 1570
Crossing Cache Creek 1050
Road from Lower Lake to Knoxville —
Crossing branch of Soda Creek at Baker mine 1315
Morgan Valley schoolhouse 2475
Road from Middletown to Glenbrook —
Divide between Putah and Keisey creeks 2650
Road from Middletown to Oathili —
Bridge over Bucksnorter Creek 1190
Sulphur Bank mine — Office 1450
Collar of Diamond shaft 1345
Collar of Empire shaft 1345
Collar of Herman shaft 1365
Wagon Spring cut, bottom 1390
Western cut, bottom 1325
Thorn mine — Tunnel 2040
t Treadwell. J Clear Lake Water Co.
256 QUICKSILVER RESOURCES OF CALIFORNIA.
MERCED COUNTY.
Feet.
Cathedral Peak 3450
Saddle between Cathedral Peak and Mariposa Peak 2850
Stayton mine — Cabin 2880
Old furnace (Gj^psy) 2400
MONTEREY COUNTY.
Cholame and Parkfield mine — Top of ridge 3460
Dutro mine, at head of west fork of San Carpojo Creek 1630
Parkfield 1540
Table Mountain — Top of ridge 3300
Table Mountain Quicksilver mine — Cabin 3190
NAPA COUNTY.
^tna mine — Basalt ridge, Silver Bow claim 2050
Office and Tunnel No. 7 1240
Tunnel No. 5 1400
Tunnel No. 2 1600
^tna Springs 800
Boston mine (Knoxville) — Office 1275
Calistoga *363
Corona mine — Boiler house and tunnel i960
Manhattan mine (Knoxville) — Office 1925
Oathill mine — Office 2025
Philadelphia mine — Works on ridge 2040
Road from Calistoga to ^ijtna Springs —
Summit of Howell Mountain 2250
Flat between Twin Peaks 2440
Forks of road to Oathill 2160
Road from Middletown to Calistoga —
Toll house at Mount St. Helena 2300
SAN BENITO COUNTY.
Antimony Peak, Stayton District 3150
Aurora mine — Furnace 3S25
Bradford mine (Cerro Gordol — Office 1820
Cannon mine — Tunnel 1560
Cerro Bouito mine — Main tunnel 2775
Office 2440
Top of Cerro Bonito hill 3250
Clear Creek mine — Old Monterey furnace 2800
Lower workings 311°
Upper workings 3660
Divide between San Carlos and Clear Creek, crossing of road from
New Idria to Hernandez 44J^o
*S. P. R. R. Co.
ELEVATIONS. 257
Feet.
Dominic Peak 4720
Don Juan mine — Old furnace 2785
Elkhorn 1 100
Emmett schoolhouse 1140
Henrietta Peak, Stayton District 3480
Hernandez P. 0 2540
Hollister *286
Llanada P. O., Panoche Valley 1540
Los Picaclios mine (Ramirez Cons.) — Retort furnace 4600
Mariposa mine, Staj-ton District — Old works 2700
Mariposa Peak 334o
Mount Venado 4660
New Idria mine — Croppings on top of hill 375o
Furnaces 2720
Mine boarding-house 334o
North Idria Peak, knoll above furnaces 3640
North San Carlos Peak 4660
Office 2590
San Carlos mine tunnel 4500
San Carlos Peak 4980
Upper fall, San Carlos creek 3720
Panoche divide 2240
Panoche P. 0 1250
Park Mills 1440
San Benito 1540
Shiver mine, Stayton District 2460
Tres Pinos *5 1 2
SAN LUIS OBISPO COUNTY.
Alice and Modoc mine — Retort furnace 1900
Bank mine — Main tunnel 345
Cambria 60
Cholame P. O 670
Cypress Mountain mine — Cabin 2425
Cypress Mountain — Plateau 2900
Divide between Hughes and Santa Rosa Creek on road to Cambria . 2350
Divide between San Luis Obispo and Santa Margarita, on wagon
road 1550
Doty mine — Lower tunnel 2000
Elizabeth mine — Retort furnace 1950
El Paso de Robles * 722
Exline mine — Tunnel loio
Karl mine — Furnace 1080
La Libertad mine — Retort furnace iSoo
Lehman mine 1975
Madrone mine — Retort furnace 1950
*s. P. R. R. Co.
258 QUICKSILVER RESOURCES OF CALIFORNIA.
Feet.
Mahoney mine — Retort furnace 1140
Oceanic mine — Furnace 400
Main tunnel 770
Oceanic mine No. 2 1575
Pine Mountain — North end of ridge 3125
Top of ridge + 3560
Pine Mountain mine — Ocean View tunnel 2815
Office 2940
Sawmill 3010
Polar Star mine — Cabin 200
Rinconada mine — Croppings 2040
Furnace 1750
Rocky Buttes -j- 3444
Ouien Sabe mine — Lower tunnel 1945
San Luis Obispo * 23S
Santa Margarita * 996
Vulture mine 1460
SANTA CLARA COUNTY.
Bernal mine — Works on ridge 650
Comstock mine, Stayton District — Furnace 1400
Costello mine — Main tunnel 1000
Guadalupe mine — Furnace 340
Guadalupe schoolhouse 290
Hillsdale mine — Old furnace 120
New Almaden mine — America shaft 1560
Mine Hill top . 1600
Randol shaft 1220
Office 1335
R. R. B. shaft, Enriquita 950
San Jose 60
Santa Teresa mine — Office 26c
STANISLAUS COUNTY.
Adobe mine — Collar of shaft 1900
Orestimba mine 2250
Summit mine — Office 2250
SONOMA COUNTY.
Bacon Consolidated mine iPine Mountain) — Old furnace site 2900
Boston mine (Pine Flat) — Cabin 2525
Cinnabar King mine — Cabin 2900
*s. P R. R.Co.
t U. S. Coast aud Geodetic Survej-.
APPENDIX
17— QR
CALIFORNIA STATE MINING BUREAU.
This institution aims to be the chief source of reliable
information about the mineral resources and mining indus-
tries of California.
It is encouraged in its work by the fact that its publications
have been in such demand that large editions are soon ex-
hausted. In fact, copies of them now command high prices in
the market.
The publications, as soon as issued, find their way to the
scientific, public, and private libraries of all countries.
STATE MINERALOGIST.
The California State Mining Bureau is under the supervision
of Hon. Lewis E. Aubury, State Mineralogist.
It is supported by legislative appropriations, and in some
degree performs work similar to that of the geological surveys
of other states; but its purposes and functions are mainly
practical, the scientific work being clearly subordinate to the
economic phases of the mineral field, as shown by the organic
law governing the Bureau, which is as follows:
Sec 4. It shall be the duty of said State Mineralogist to make,
facilitate, and encourage special studies of the mineral resources and
mineral industries of the State. It shall be his duty: To collect statistics
concerning the occurrence of the economically important minerals and
the methods pursued in making their valuable constituents available for
commercial use; to make a collection of typical geological and miner-
alogical specimens, especially those of economic or commercial impor-
tance, such collection constituting the Museum of the State Mining
Bureau; to provide a library of books, reports, drawings, bearing upon
the mineral industries, the sciences of mineralogy and geology and the
arts of mining and metallurgy, such library constituting the Library
of the State Mining Bureau; to make a collection of models, drawings,
and descriptions of the mechanical appliances used in mining and
metallurgical processes; to preserve and so maintain such collections and
library as to make them available for reference and examination, and
open to public ihspection at reasonable hours; to maintain, in effect, a
bureau of information concerning the mineral industries of this State, to
consist of such collections and library, and to arrange, classify, catalogue,
and index the data therein contained, in a manner to make the informa-
tion available to those desiring it, and to provide a custodian specially
APPENDIX. 263
qualified to promote this purpose; to make a biennial report to the
Board of Trustees of the Mining Bureau, setting forth the important
results of his work, and to issue from time to time such bulletins as he
may deem advisable concerning the statistics and technology of the
mineral industries of this State.
THE BULLETINS.
The field covered by the books issued under this title is
shown in the list of publications. Each bulletin deals with
only one phase of mining. Many of them are elaborately
illustrated with engravings and maps. Only a nominal price
is asked, in order that those who need them most may obtain
a copv.
THE REGISTERS OF MINES.
The Registers of Mines form practically both a State and
County directory of the mines of California, each county being
represented in a separate pamphlet. Those who wish to learn
the essential facts about any particular mine are referred to
them. The facts and figures are given in tabular form, and
are accompanied b}' a topographical map of the county on a
large scale, showing location of each mineral deposit, towns,
railroads, roads, power lines, ditches, etc.
HOME OF THE BUREAU.
The Mining Bureau occupies the north half of the third floor
of the Ferry Building, in San Francisco. All visitors and resi-
dents are invited to inspect the Museum Librar}', and other
rooms of the Bureau and gain a personal knowledge of its
operations.
THE MUSEUM.
The Museum now contains over 16,000 specimens, carefully
labeled and attractively arranged in showcases in a great, well-
lighted hall, where they can be easily studied. The collection
of ores from California mines is of course very extensive, and
is supplemented by many cases of characteristic ores from the
principal mining districts of the world. The educational value
of the exhibit is constantly increased by substituting the best
specimens obtainable for those of less value.
These mineral collections are not only interesting, beautiful,
and in every way attractive to the sightseers of all classes, but
are also educational. They show to manufacturers, miners,
capitalists, and others the character and quality of .the economic
264 QUICKSILVER RESOURCES OF CALIFORNIA.
minerals of the State, and where the}' are found. Plans have
been formulated to extend the usefulness of the exhibit by
special collections, such as one showing the chemical com-
position of minerals; another showing the mineralogical
composition of the sedimentar}-, metamorphic, and igneous
rocks of the State: the petroleum-bearing formations, ore
bodies, and their country rocks, etc.
Besides the mineral specimens, there are many models, maps,
photographs, and diagrams illustrating the modern practice of
mining, milling, and concentrating, and the technology of the
mineral industries. An educational series of specimens for
high schools has been inaugurated, and new plans are being
formulated that will make the Museum even more useful in the
future than in the past. Its popularity is shown by the fact
that over 100,000 visitors registered last year, while many
failed to leave any record of their visit.
THE LIBRARY.
This is the mining reference library of the State, constantly'
consulted by mining men. and contains between 4,000 and
5.000 volumes of selected works, in addition to the numerous
publications of the Bureau itself. On its shelves will be found
reports on geology, mineralogy, mining, etc., published by
states, governments, and individuals; the reports of scientific
societies at home and abroad; encyclopaedias, scientific papers,
and magazines; mining publications; and the current litera-
ture of mining ever needed in a reference libran,'.
Manufacturers' catalogues of mining and milling machinery
by California firms are kept on file. The Registers of Mines
form an up-to-date director}' for investor and manufacturer.
The librarian's desk is the general bureau of information,
w^here visitors from all parts of the world are ever seeking
information about all parts of California.
READING-ROOM.
This is a part of the Library Department and is supplied
with over one hundred current publications. A'isitors will find
here various California papers and leading mining journals
from all over the world.
The Library and Reading-Room are open to the public from
9 A. M. to 5 p. M. daih', except Sundays and holidays, and from
9 A. M. to 12 M. on Saturday's.
APPENDIX. 265
THE LABORATORY.
This department identifies for the prospector the minerals he
finds, and tells him the nature of the wall rocks or dykes he
may encounter in his workings; but this department does not
do assaying nor compete with private assa3'ers. The presence
of minerals is determined, but not the percentage present. Xo
charges for this service are made to any resident of the State.
Many of the inquiries made of this department have brought
capital to the development of new districts. Many technical
questions have been asked and answered as to the best chemi-
cal and mechanical processes of handling ores and raw mate-
rial. The laboratory is well equipped.
THE DRAUGHTING-ROOM.
In this room are prepared scores of maps, from the small
ones filling only a part of a page, to the largest County and
State maps; and the numerous illustrations, other than photo-
graphs, that are constantly being required for the Bulletins
and Registers of Mines. In this room, also, will be found a
ver}- complete collection of maps of all kinds relating to the
industries of the State, and one of the important duties of the
department is to make such additions and corrections as wijl
keep the maps up to date. The seeker after information
inquires here if he wishes to know about the geology or topog-
raphy of an}' district; about the locations of the new camps,
or positions of old or abandoned ones; about railroads, stage
roads, and trails; or about the working drawings of anything
connected with mining.
MINERAL STATISTICS.
One of the features of this institution is its mineral statis-
tics. Their annual compilation by the State Mining Bureau
began in 1893. Xo other State in the Union attempts so elab-
orate a record, expends so much labor and monej- on its com-
pilation, or secures so accurate a one.
The State Mining Bureau keeps a careful, up-to-date, and
reliable but confidential register of every producing mine,
mine-owner, and mineral industry in the State. From them
are secured, under pledge of secrec)', reports of output, etc.,
266
QUICKSILVER RESOURCES OF CALIFORNIA.
and all other available sources of information are used in
checking, verifying, and supplementing the information so
gained. This information is published in an annual tabulated,
statistical, single-sheet bulletin, showing the mineral produc-
tion by both substances and counties.
TOTAL GOLD PRODUCT OF CALIFORNIA— 1848 1906.
1S48 $245,301
1849 . 10,151,360
1850 41,273,106
1851 75-938.232
1852 81,294,700
1853 67,613,487
1854 - 69,433,931
1855- 55485.395
1856 _ 57,509,411
1857 43,628,172
1858 46.591.140
1859 -- 45.846.599
i860 44,095,163
1861 41,884.995
1862 38,854,668
1863 23,501,736
864 $24,071,423
865 17.930.858
866 17,123,867
867 18,265,452
868 17.555.867
869 18,229.044
870 17.458,133
871 17.477.885
872 15,482,194
873 15.019,210
874 17,264,836
16,876,009
876 15,610,723
877 16,501,268
878 18,839.141
879 19,626,654 ,
880 _ $20,030,761
881 19,223,155
882 17,146,416
883 24,316,873
884 13,600,000
885 12,661,044
886 14,716,506
887 13,588,614
888 12,750,000
889 11,212,913
890 12,309,793
891 12.728,869
892 ... 12,571,900
893 12,422,811
894 13,923,281
895 - 15.334.317
1896 _ $17,181,562
1897.. - . 15,871,401
1898 15,906,478
1899 - 15.336.031
1900 15.863,355
1901 16,989.044
1902 16.910.320
1903 16,471,264
1904.. 19.109,600
1905.. 19.197.043
1906 18,732,452
Total.. _ 1,452,785,763
TOTAL QUICKSILVER PRODUCT OF CALIFORNIA— 1887-1906.
Flasks.
1887 33,760
1888 33.250
1889 26,464
1890 22,926
1891 22,904
1892 27,993
1893 30,164
1S94 30,416
1895 36,104
1896 30,765
1897 26,648
1898 31,092
Value.
51,425,000
1,413.125
1,190,500
1,203.615
1,036,386
1,139,600
1,108,527
934,000
1,337,131
I. .075, 449
993,445
1,188,626
Flasks.
1899 29,454
1900 26,317
190I 26,720
1902 29,552
1903 32,094
1904 28,876
1905 24,655
1906 19,516
Total for 20
years ... 569,670
51,405,045
1,182,786
1,285,014
1.276,524
1,3.^5,954
1,086,323
886, 08 1
712,334
523,215,465
APPENDIX.
267
MINERAL PRODUCTS OF CALIFORNIA FOR 1906.
The yield and value of the mineral substances of California
for 1906 was as follows, as per returns received at the State
Mining Bureau, San Francisco, in answer to inquiries sent to
producers:
Asbestos Tons
Asphalt Tons
Bituminous Rock . .Tons
Borax (Crude) .... Tons
Cement Bbls
Chrome Tons
Clays (Brick) M
Clays (Pottery) . . . .Tons
Coal ; Tons
Copper Lbs
Fullers' Earth Tons
Gems
Glass Sand Tons
Gold
Granite Cu. ft
Infusorial Earth . . . Tons
Gypsum Tons
Lead Lbs
Lime Bbls
Limestone Tons
Macadam . . Tons
Manganese Tons
Magnesite (Crude) Tons
Marble Cu. ft
Mineral Paint Tons
Mineral Water Gals
Natural Gas M. Cu. ft
Paving Blocks M
Petroleum Bbls
Platinum Ounces
Pyrites Tons .
Quicksilver P'lasks
Rubble Tons
Salt Tons
Sandstone Cu. ft
Serpentine Cu. ft
Soda Tons
Silver (Commercial Value)
Slate Squares
Tungsten
Zinc Lbs
70
77,756
16,077
58,173 I
1,286,000 I
317
277,762 2
167,267
24,850
28,726,448 5
440
9,750.
329,810.
2,430-
21,000.
338,718.
689,268
80,262
1,066,164.
I
4,032
31,400.
250.
1,585,690.
168,175.
4,203.
32,624,000.
91.46.
46,689
19,516
489, 208 .
101,650.
182,076.
847.
12,000.
10,000.
206,000.
$3,500
777,560
45,204
182,410
.941,250
2.859
538,848
162,283
6r,6oo
522,712
10,500
497,090
13,375
.732,452
344,083
14,400
69,000
19,307
763,060
162,827
870,887
30
40,320
75,800
1,720
478,186
109,489
173,432
238,020
1,647
145,895
712,334
547,519
213,228
164,068
1,694
18,000
817,830
100,000
189,100
12,566
Totals $46, 776,085
Quicksilver was produced in Lake, Napa, San Benito, San Luis
Obispo, Santa Clara, Solano, Sonoma and Trinity counties.
268 OnCKSILVER resources of CALIFORNIA.
MINING BUREAU PUBLICATIONS.
Publications of this Bureau will be sent on receipt of the
requisite amount and postage. Only stajnps, coin or money
orders will be accepted in payment. Do not send personal
checks.
Address all communications regarding publications to
Librarian.
(All publications not mentioned are exhausted.)
SALE OF MINING BUREAU PUBLICATIONS.
Under Section 8, amendment to the Mining Bureau Act,
approved March lo, 1903, your attention is respectfully called
to that portion of the amendment which states:
"The Board (Board of Trustees) is hereby empowered to fix
a price upon, and to dispose of to the public, at such prices,
any and all publications of the Bureau, including reports,
bulletins, maps, registers, etc. The sum derived from such
disposition must be accounted for and used as a revolving
printing and publishing fund for other reports, bulletins, maps,
registers, etc. The prices fixed must approximate the actual
cost of printing and issuing the respective reports, bulletins,
maps, registers, etc., without reference to the cost of obtaining
and preparing the information embraced therein."
Report XI — 1S92, First Biennial - .- — $i.oo
Report XIII— 1S95, Third Biennial.-' . .-
Bulletin Xo. 6 — '•Gold Mill Practices in California" (3d edition)
Bulletin No. 9 — •Mine Drainage. Pumps. Etc " Bound -.
Bulletin Xo. 15— "Map of Oil City Oil Fields, Fresno County, California"
Bulletin No. 23 — 'Copper Resources of California" _ _-.
Bulletin No 24— "Saline Deposits of California" _ 50
Bulletin No. 27— "Quicksilver Resources of California"- . .75
Bulletin No. 30— 'Bibliography- Relating to the Geolog>-, Palaeontology
and Mineral Resources of California," including list of maps .50
Bulletin No. 31 — "Chemical Analysis of California Petroleum" -
Bulletin Xo. 32— "Production and Use of California Petroleum" -
Bulletin Xo. 36 — "Gold Dredging in California " (2d edition)
Bulletin Xo. 37- "Gems and Jewelers' Materials of California." (2d ed.)
Bulletin Xo. 3S— "Structural and Industrial Materials of California"
Bulletin Xo. 42 — "Mineral Production of California" — 1905
Bulletin Xo. 43— "Mineral Production of California for Xineteen Vears"-
BuUetin Xo 45 — ".Auriferous Black Sands of California" ...
Bulletin Xo. 46 — ''Index of Mining Bureau Publications ' .- ...
Bulletin Xo. 47— "Mineral Production of California"— 1906
Bulletin Xo. 4S— "Mineral Production of California for Twenty Years"-..
Bulletin Xo. 49— "Mines and Minerals of California" -
California Mine Bell Signals (Cardboard) -
California Mine Bell Signals (Paper)
Gold Production in California from 184S to 1906
Register of Mines, with Map, .\mador County
Register of Mines, with Map, Butte County -..
Register of Mines, with Map. El Dorado County
Register of Mines, with Map. Inyo County - -.
Register of Mines, with Map, Kern County 25
Register of Mines, with Map, Lake County
Post-
rice.
Il.OO
1. 00
age.
$0.15
.20
•50
.60
.04
.oS
■05
•50
.02
.12
■75
.08
■50
.oS
■50
.oS
•75
.20
.02
.02
.10
.02
•30
.06
02
...
.02
•05
.02
•03
.02
.02
•25
.oS
■25
.oS
■25
.oS
■25
.oS
•25
.08
•25
.OS
APPENDIX. 269
Post-
Price, age.
Register of Mines, with Map, Mariposa Couuty $0.25 $0.08
Register of Mines, with Map, Nevada County ... .25
Register of Mines, with Map, Placer County .25
Register of Mines, with Map, San Bernardino Countj' .25
Register of Mines, with Map, San Diego County 1 25 .08
Register of Mines, with Map. Santa Barbara County 25
Register ot Mines, with Map. Shasta County 25 .08
Register of Mines, with JIap. Sierra County _ 25
Register of Mines, with Map, Siskiyou County .25
Register of Mines, with Map, Trinity County 25
Register of Mines, with Map, Tuolumne Countj- . 25
Register of Mines, with Map. Yuba County ..... __. .25
Register of Oil Wells, with Map, t,os Angeles City .35
Map of Mother Lode . . .05
Jlap of Desert Region of California _ • 10
!Map Showing Copper Deposits in California ._ 05
Map of Calaveras County .._ .25 .03
Map of Plumas County .25 .03
Mineral and Relief Map of California .25 .05
Map of Forest Reserves in California (Mounted). 50
Map of Forest Reserves in California (Unmounted) .30
In Preparation —
Map and Register of Madera County.
Report on Minaret District.
Bulletin — "Revised Edition Copper Resources of California."
Samples (limited to three at one time) of any mineral found
in the State ma}- be sent to the Bureau for identification, and
the same will be classified free of charge. /Vo samples will be
determined if received from points outside the State. It must
be understood that no Assays or Quantitative Determinations
zvill be made. Samples should be in a lump form if possible,
and tnarked plainly with name of sender outside of package,
postoffice address., etc. No sajnples will be received unless
charges are prepaid. A letter should accompanj- sample and
a stamp should be enclosed for repl)-.
Address all samples and communications regarding samples
to Laboratory.
LAW RELATING TO MISREPRESENTATION OF MINES BY ANY
OFFICER OF A CORPORATION TRANSACTING BUSINESS IN
CALIFORNIA.
Section i. Anj^superintendent, director, secretary, manager,
agent, or other officer, of any corporation formed or existing
under the laws of this State, or transacting business in the
same, and any person pretending or holding him.self out as
such superintendent, director, secretary, manager, agent or
other officer, who shall willfully subscribe, sign, endorse, verify,
or otherwise assent to the publication, either generally or
privately, to the stockholders or other persons dealing with
such corporation or its stock, any untrue or willfully and
fraudulently exaggerated report, prospectus, account, statement
270 QUICKSILVER RESOURCES OF CALIFORNIA.
of operations, values, business, profits, expenditures or pros-
pects, or other paper or document intended to produce or give,
or having a tendency to produce or give, to the shares of stock
in such corporation a greater value or less apparent or market
value than they really possess, or with the intention of defraud-
ing any particular person or persons, or the public, or persons
generally, shall be deemed guilty of a felony, and on conviction
thereof shall be punished b}- imprisonment in State prison, or
a county jail, not exceeding two years, or by fine not exceeding
five thousand dollars, or by both.
Sec. 2. All Acts and parts of Acts in conflict with this Act
are hereby repealed.
Approved March 22, 1905.
INDEX.
Page.
Abbott mine 46
Adelaide district 150
Alice and Modoc mine 154
vEtna Consolidated mines _ 7J
Alta .- no
Alloona mine 192
Baker mine 49
Bitujneu in cinnabar ore deposits
25, 41,47, 161
Boston mine "6
Central San Benito mining district _. 125
Cerro Bonito mine 134
Chertbeds - 17
Chert beds and ore deposits 54, 99
Clear Lake district - 39
Cloverdale mine 98
Colusa County, Mines in :
Central .. . 43
Elgin 43
Empire - 43
Manzanita 44
Wide Awake 45
Concentration of quicksilver ores 198
Concentration plant, Cost of 202
Condensation of the furnace fumes... 234
Condensers, Brick __ 249
Products ._ 239
Waterbacks.. 251
Watertank 251
Wooden _ 252
Condensing-box, Boston mine 202
Condensing, Principles of.. 243
Contra Costa County, Cinnabar in 195
Corona mine 7'J
Cost of mining and reduction
34,201,208,214
Cost of timber and wood
3><, 39, 42, 129, 130, 153, 186
Cretaceous formations 16
Culver-Bacr mine 102
Del Norte County, Mines in . . 195
Draft in furnace plant. (See " Fur-
naces.")
Dry-bone 37
Elevations 254
El Dorado County, Mine in 190
Eureka mine . .. 106
Franciscan series . 12
Fresno County, Mines in :
Arrambide and Aurecoechea 119
Mexican 119
Providential group 121
Furnaces : Page.
Data regarding tile furnaces 223
Discharging methods 235
Exeli, continuous 208
Fitzgerald. 205
General arrangement of plant.... 234
Hiittner-Scott 218
Knox & Osborne coarse-ore 210
Knox & Orborne fine-ore 215
Litchfield .- 215
Livermore 215
Luckhardt _ 210
Ore-drying systems 225
Material for 206, 224
Neat's 210
New Idria coarse-ore 213
Products of combustion of 198
Requirements of 205
Retort. (See "Retort Furnace.")
Temperature in... 234
Tiles 221
Furnace fumes. Composition of_ 239
Furnace plant, Draft in 240
Gas in the mines 65. 110
Geological table of the Cretaceous
period __ 16
Geology of the quicksilver belt in Cali-
fornia.. _. 12
Granite, Description of 14
Granite, Its occurrences in the Coast
Ranges . _ 12
Great Eastern and Mount Jackson
mines ._ 108
Great Western mine 52
Guadalupe mine 173
Heat, Increase with depth under-
ground - --- 70
Helen (American) mine 55
Igneous rocks. 21, 39, 129, 149, 152, 163
Igneous rocks and ore deposition. ..21, 28,
36. .58, 62, 71, 77, 81, 91, 130, 148, 156, 191, 194
Integral mine 193
Karl mine 157
Kings County, Mines in 122
Knoxville district.. 42
Lake County, Mines in :
Abbott 46
.Anderson 48
Baker 49
Big Injun (New Phoenix Mining
Co.) 50
Chicago (Ural) 51
979
INDEX.
Lake County. Mines in : Page.
Digger Injun (Congress Mining
Co) 50
Great Western _ 52
Helen (American) o.i
Jewess 57
Kingof All 57
Lucitta 5S
Middletown .59
Shamrock ._ 60
Standard Quicksilver Company
(Mirabeland Bullion) 60
Sulphur Bank 61
Thorn 70
Utopia 70
Wall Street 71
La Libertad mine 159
Little Panoche mining district 119
Lucitta mine 58
Madrone mine.. 161
Mahoney (Buena Vista or Gould) mine 161
Manhattan mine 81
Manzanita mine 44
Mariposa County, Cinnabar ore in 195
Mayacmas district 35
Metacinnabarite 25, 31
Metacinnabarite, its occurrence
..47,49,79, 124,160,166
Mercury and heat 29
Mercury, Occurrence of native 31
(See, also, ''Native Mercury.")
Metallurgy- 197
Metamorphic series. Age of . 12
Xon-conformitj' with theChico... 128
Metamorphism of the older series in
the Coast Range 19
Mining timbers, Protection of 143
Mist-loss.. 239,244
Monterey County. Mines in :
Cholame-Parkfield.. 123
Dutro 12-1
Table Mountain 124
Mudrock... 82
Xapa Countj", Mines in :
-Etna Consolidated 72
Bella Union.. 76
Boston 76
Corona. — 79
Lajoya 80
Manhattan
Northern Light 9
Oathill... - SO
Philadelphia 92
Red Elephant 92
Summit _ 92
Twin Peaks 92
Xati ve mercurj- 32, 115, 110
Xeocomian series 12
Xew.Almaden mine 174
New Idria district _ 125
Xevi- Idria mine — 138
Page.
Oathill (Xapa Consolidated) mine 89
Oceanic district 151
Oceanic mine 162
Pine Mountain district 152
Pine Mountain mine 163
Polar Star mine 165
Pre-Cretaceous series 12
Price of quicksilver (annual since 1S50) 10
Production of quicksilver (Annual
since ia50) .. 30
Production of quicksilver at Xew Al-
raaden . 176
Quicksilver ores and antimony ores... 148
.\ud chalcedony 85
.^nd cherts 54, 99
-■ind copper 14S
.■\nd gold ores 44
And Igneous Rocks. (See "Igne-
ous Rocks")
And Sandstone. 'See "Sand-
stone.")
And Serpentine. (See "Serpen-
tine ")
Description 24
Genesis of 26
Formed by solution and precipita-
tion 30,65,171
Formed by sublimation 30
Forming at the present time 45, 65
Quicksilver rock 20
Ramirez Consolidated (Las Picachos)
inines 145
Retort furnaces 197. 203
Cost of._ 202,205
Johnson & McKay 202
G. V. Xorthey 200
San Benito County, Geologj- of 125
San Benito Countj-, Mines in :
.\ndj- Johnson 131
Aurora 131
Bradford 131
Boston. (See " Clear Creek.")
Butts 133
Cannon 133
Cerro Bonito 134
Clear Creek 137
Don Juan and Don Miguel 137
Fourth of July 138
Mariposa — 138
Xew Idria l'>8
Philadelphia and Xew York 145
Ramirez Consolidated (Los Pica-
chos) 145
San Carlos _ U3
Santa Cruz 147
Stayton 147
San Carpojo district 15!
Sandstones 17, 93, r21, 1'2C, 13.5
Sandstones and ore deposits
91,95, 104, 119,121, 138. 141, 161,163
INDEX.
273
Page.
San Luis Obispo County, Geology of.. 149
San Luis Obispo County, Mines in:
Alice and Modoc 154
Bank mine 154
Cypress Mountain 156
Doty 156
Elizabeth 157
Eureka 157
George and Josephine. 157
Karl . 157
Kismet 159
La Libertad 159
Lehman. 101
Madrone _ . 161
Mahoney (Buena Vista or Gouldj.. 161
North Star _ 162
Oceanic 162
Oceanic No. 2 163
Pine Mountain .. 163
Polar Star 165
Quien Sabe 165
Rincouada 166
Sunset View . 167
Vulture .- 167
William Tell 168
Wittenberg _ 168
Santa Barbara County, Mines in. 196
Santa Clara County, Geology of. 168
Santa Clara County, Mines in :
Bernal 171
Comstock 172
Costello 172
Guadalupe 173
Hillsdale 174
New Almaden 174
Santa Teresa.. 186
Silver Creek 187
Wright- - 1S7
Santa Teresa mine.. 186
Serpentine, Its derivation 13, 33, 127
Serpentine, Relation to cinnabar de-
posits 36,46,
75, 76, 88, 104, 106, 108, 114, 132, 142,
144, 149, 154, 157, 160, 166, 168, 178, 190
Serpentine, Surface occurrences
74, 119,123,187
Silicification and cinnabar deposits... 33
Silicifications process 19, 180
SiU-er Creek mine 187
Siskiyou County, Mines in 196
Socrates mine 115
Solano County, Mine in— St. John ... 93
Sonoma County, Mines in :
Almaden, etc. 97
Bacon Consolidated 97
Boston 97
Cinnabar King 98
Sonoma County, Mines in : Page.
Cloverdale 98
Clyde _ 102
Crown Point. 102
Crystal. (See " Pacific")
Culver-Baer 102
Double Star 105
Eureka 106
Great Eastern 108
Great Northern 112
Hope 112
Hurley 112
Lookout 113
Lucky Stone '. 113
Maricoma 113
Mercury Mining Co 113
Missouri _ 113
Mount Jackson. (See "Great
Eastern.")
Napa 113
Oakland. (See "Culver-Baer.)
Occidental and Healdsburg 114
Old Chapman.- 114
Pacific 114
Pontiac 115
Rattlesnake .... . 115
Socrates 115
Sonoma. (See "Crown Point.")
Walker 116
Wall Springs .. 117
Soot 239,214,253
Standard Quicksilver Co. (Mirabel)... 60
Stanislaus County, Mines in :
.\dobe Valley 189
Orestemba 189
Summit 188
Stayton district.. 129
Stay ton mine 147
St. John mine... 93
Sulphur Bank mine 61
Sulphur Creek district. 40
Summit group 188
Trinity County, Geology of 190
Trinity County, Mines in :
Altoona 192
Carr 193
Integral 193
Trinity 195
Tuffoid 41
Twin Peaks mine.. 92
Water, Underground circulation 28
Waters. Composition of underground. 66
Yolo County. Mines in :
New England and Harrison 117
Reed : 117
Royal 117
Zones of the earth crust 26
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