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A Memorial and Biographical History of Northern California (1891) (713 pages)

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Page: of 713

HISTORY OF NORTHERN CALIFORNIA. 245
been the following: W. D. Aylett. 1854; J.
R. Cook, 1880; W. T. Cressler, 187374; E.
J. Curtis, 1855-"56; John Daggett, 1881;
John A. Fairchild, 1867-68; G. F. Harris,
1875-76; Wm. Irwin, 1862-’63: J. K. Jobnson, 1885; W. J. Little, 1871-’72; S. L. Littlefield, 186364; J. K. Luttrell, 1865-66,
1871-72; R. M. Martin, 1869-'70; J. W.
McBride, 187374; Charles McDermit, 1860;
Peter Peterson, 1883; W. G. Procter, 1853;
P. C. Robertson, 1877-78; K.C. Scott, 1863—
64; Wm. Shores, 1869-70; F. Sorrell, 1861;
Elijah Steele, 1867-68; Thomas H. Steele,
1865-66; Caleb N. Thornbury, 1862; B. F.
Varney, 1857, 1863; A. B. Walker, 1858;
Wm. F. Watkins, 1859.
Three companies served from Siskiyou
County during the Rebellion, all of whom
were used on the frontier and in the Indian
wars on the cuast. Charles McDermit, Juseph
Smith and Robert Baird were the first captains.
The first newspaper in this county was the
Mountain Herald, issued June 11, 1853, by
Thornbury & Co., the proprietors being C. N.
Thornbury, W. D. Slade and S. F. Van Choate.
It was a four-page, sixteen-culumn paper, the
pages being only 9x16 inches in size. Small
us it was, it was a great achievement for a little
town over a hundred miles up in the muuntains.
In 1855 the Know-nothing party took posseseion ot the paper and renamed it the Yreka
Union, but this regime continued but a short
time.
Mining is still the leading industry in this
county, but agriculture is gaining upon it.
MINERALOGICAL,
Tlie following paragraphs are from the State
report:
Siskiyou County lies between the parallels
41° and 42° north latitude, and 121° and 124°
weet longitude. It is the central of the three
most northerly counties of the State, bounded
on the east by Modoc County, on the eouth by
Humboldt, Trinity and Shasta counties, on the
weet by Humboldt and Del Norte counties,
and ou the north by the State of Oregon. It
contains within its boundary lines 3,040 square
miles of territory, a very small portion of
which is arable. A large area, comprising
thirty-four townships, designated on the maps
as the Lava Bed Road District, and situated in
the extreme northeastern portion of the county,
adjoining Modoc, is, as its name implies,
covered with lava and unfit for cultivation. The
remainder, about two-thirds of the whole, ia
mineral land, and here the various kinds of
gold mining—quartz, placer, drift, and river—
that exist in California, are prosecuted.
This corner of the county includes a small
portion of the Jacustrine system of the State;
and the areas of water designated as the Lower
Klamath and a portion of Tule Lake, with
several of smaller dimensions, in the aggregate
cover 100 square miles of surface.
This county is suz generis. It has no counterpart on the Pacitie Slope. Within its borders are
found valleys and plains of arable Jand atan elevation of from 2,500 to 4,000 feet, surrounded by
beetling cliffs and serrated ridges that rise from
500 to 900 feet above sea level.
Scott Valley is situated near the central portion of the county at an eievation uf 3,000 feet.
Twenty miles from Mount Shasta this valley is
furty miles long by six miles in width, or about
240 sqnare miles in all, Etna, its principal
town, is at the head of the ‘ wagon-rvad navigation.” From this point supplies are sent by
pack animals to the Salmon and Klamath regions. A short line (six miles) of railroad is in
progress of construction from Montague Station,
on the line of the California and Oregon Railroad, to Yreka, the county-seat, which, when
completed, will be the terminus of the railroad
eystem in this county.
Volcanic cones are marked features in the
landscape of Siskiyou. In this county, particularly in the Klamath, Salmon, and Scott Ranges,
mountains lose their smoothly-rounded summits.
Table Jands are seldom seen; sharp, serrated
ridges have replaced them, with deep gorges
and precipitous cafions. An important change
is to be noted in the topographical features of
this county. The Coast and Sierra Nevada
Ranges are here merged into one. The strike,
or trend, of the stratification has been changed
trom west of north to north twenty degrees east.
The formation and metalliferous belts of Siskiyou are not so clearly defined as in the middle
and suuthern counties of the State, where they
are easily traced for long distances.