The Naturalist in Vancouver Island and British Columbia, Volume 1 (of 2)Lord, John Keast
History
The Naturalist in Vancouver Island and British Columbia, Volume 1 (of 2)
Lord, John Keast
British Columbia -- Description and travel; Natural history -- British Columbia; Vancouver Island (B.C.) -- Description and travel
_March 27th._—A good sleep has worked wonders. I find Grass Valley a
romantic little mountain town, about 2,200 feet above the sea-level, on
the western slope of the Sierra Nevada, owing its existence entirely
to gold-mining. Visited Mr. A.’s mill—a magnificent quartz-crusher.
Nine stamp-heads, each 900 lbs. in weight, are worked by one of Watts’
engines. The fine-dust gold is collected on blankets, or bullocks’
hides with the hair on, over which the water washes it, as it comes
from the stamp-heads. Some of the most productive gold deposits in
California were discovered in and about this quaint little place. I
descend a shaft 240 feet deep. The gold is distributed through the mud
and silt of what was clearly an ancient riverbed.
_March 28th._—Ride on horseback to Nevada and Hunt’s Hill. Nevada is
a clean pretty _city_, with gay shops, brightly-painted houses, and
planked streets. Near it are the famed hydraulic washings. The gold is
disseminated through terraces of shingle conglomerates, often three
hundred feet in thickness. These terraces are actually washed entirely
off the face of the country, by propelling jets of water against them,
forced under great pressure through a nozzle. To accomplish this, the
water is brought in canals, tunnels, and wooden aqueducts, often forty
miles away from the drift. This supply of water the miners rent.
As we near the washing-spot, in every direction immense hose, made
of galvanized iron, and canvas tubes six feet round, coil in all
directions over the ground, like gigantic serpents, converging towards
a gap, where they disappear. On reaching this gap, I look down into
a basin, or dry lake, 300 feet below me. The hose hangs down this
cliff of shingle, and following its course by a zigzag path, I reach a
plateau of rock, from which the shingle has already been washed. A man
stands at the end of each hose, that has for its head a brass nozzle.
With the force of cannon-shot water issues, in a large jet, from this
tube; and propelled against the shingle, guided by the men, washes it
away, as easily as we could broom a molehill from off the grass.
The stream of water, bearing with it the materials washed from out
the cliff, runs through wooden troughs called ‘flumes,’ floored with
granite; these flumes extend six miles. Men are stationed at regular
distances to fork out the heavy stones. Throughout its entire length
transverse strips of wood dam back a tiny pond of mercury; these
are called _riffles_—gold-traps, in other words—that seize on the
fine-dust gold distributed throughout the shingle. The ‘flumes’ are
cleaned about once a month, and the gold extracted from the mercury.
Masses of wood occur, in every stage of change, from that of pure
silica to soft asbestiform material, and pure carbon.
Public-domain text, read in full here on John Shaqi.
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