The Kendrick gazette. [volume] (Kendrick, Idaho) 1892-1968, 1904-12-09
MINES IND MINING NEWS
ITEMS or lNTEREsT GATHERED
DURING THE PAST WEEK.

"s"sS VW"SSe 49, EtVPaS"uo tS1 ssS
winters Work on Their Properties
In idaho, Montana ans Oregon
Mine Operations Of British Column
bIa Are srlsk-Many Accidents and
Personal Events.
Waldemar Lindgren Of the United
States geological survey, assisted by
G. w. Stose and II. R. johnson, under
took a geological reconnaissance in
1899 across the bitter Root range and
the Clear water mountains in Montana
and Idaho. Mr.. Lindrgen wrote a re-
port Of the work, giving particular
attention to the mineral deposits Of the
region studied, and it is now available
as professional paper No. %, and may
be obtained free Of charge, on applica-
ton to the director Of the United
States geological survey, Washington.
d. c., It is the only paper ever pub.
lished on the geology Of the district.
The region described in this report
is bordered on the south by the Salmon
river and on the north by the north
fork of the Clearwater. The Bitter
Root range, which attains an elevation
Of $1,000 feet, merges into the great
dissected high plateau Of the Clear
water mountains. These descend rather
abruptly to the plateaus of the Camas
prairie and Cold Springs prairie, which
form part Of the Columbia river lava
plateau. This plateau has a general
elevation Of $500 to 5000 feet, and is
built up Of horizontal lava flows. From
great glacial cirques in the western
slopes Of the Bitter Root range the
Salmon river and the several forks Of
the Clearwater river find their way
westward through canyons from 5000
to 5000 feet deep. The canyon of the
Salmon is especially remarkable for its
great length and depth.
The area indicated forms a wild and
very sparsely populated mountain re-
gion, which is heavily timbered except
on the highest ridges. The geology Of
the region is comparatively simple.
The main Bitter Root range and the
larger part of the Clearwater noun
tains consist of a massive biotite gran
lite, or, to define it more correctly, Of a
quartz mennonite, which is the north.
ward continuation Of the great batho-
lith of the same rock that occupies 60
large an area in southern central
Idaho. A very remarkable fault Of ex-
ceptional lentgh and displacement sep
arates the eastern slope Of the Bitter
Root mountains from the valley Of the
same name.
The valuable minerals contained in
this area are confined chiefly to the
western slope Of the Clearwater noun
tains. The most important are the
gold deposits, which in the
fissure veins and gravels. At the foot
of the Bitter Root mountains, some 10
miles north of Hamilton, Mont, is the
remarkable Curlew mine, where a body
Of galena was found in a fissure that
had limestone and quartzite as it's foot
wall and the gravels Of the Bitter Root
valley q hanging wall. On the upper
south fork of the Bitter Root river
prospects Of copper, sivler and silver
lead ore have been worked. Hughes
creek, in the same vicinity, contains
gold bearing gravels which have been
worked for many years.
Elk City, whree mineral deposits
were discovered in 1869, is the centre
Of the gold mining industry on the
west slope. Gold to the value of sew
eral million dollars was extracted there
from late tertiary bench gravels, and
placer mining is still prosecuted on a
small scale. Quartz veins have also
been opened in the old mining district.
The we'll defined quartz veins of
Buffalo Hump, discovered in 1897, are
actively worked, though not ON a very
large scale. These deposits occur in
granite rocks, accompanied by contact
metamorphic states. Florence, located
40 miles southwest of Elk City, is an
other of the old placer camps, dis
covered about 1851. The gravels were
rich and the camp has yielded gold ia
the value Of many million dollars. Al
present a few placer and quartz mines
are worked there also. Pierce City,
on Orofino creek, about 80 miles north.
northwest Of Elk City, is also q well
known placer camp, discovered In
1861, and worked continuously since
then. The present yield from these
placers is probably about $3OO.0 90 pc,
mum. The gravols occur as creek
aluvium and as benches up to 500 fee,
above the persent drainage level.
Quartz veins have also been found neal
Pierce, and many of them are now
worked on a small scale. The VEIN
occur IN gneises and chists. The tota
production Of this gold. bearing region
is at the present time probably abou
$1,000 90 per annum.
Coal of fair quality has been foun,
on the upper South Fork of the Bite
Root valley, and the beds are here as
ISOLATED with rhyolote. The develop
ments have not yet shown the extent o
this occurrence. Ignite Of fair quail
ity aslo occurs on Orofino creek below
Pierce, and is associated with basalts
but the beds are probably not THO
enough to make development prof1ta
BILE.
British Columbia Mines.
CRANKY smelter treated 1850 ton