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Volume 055-3 - July 2001 (8 pages)

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The Story of the Cascade Canal
By A. Dale Johnson © 2001
The Hydraulic Mining Era
Y 1855 HYDRAULIC MINING HAD BECOME THE
most prevalent and fruitful method of mining the “goldbearing gravels” in Nevada County. It was essential that hydraulic mines have a water supply high above the gravel
beds—but that was not where the water was! Water soon
became big business with ditches springing up everywhere.
The Cascade was one of those ditches, built in 1857-60, and
became part of the largest of all water companies, the South
Yuba Canal Company. By 1869 this company had 200 miles
of canal costing $1,500,000—and there were nearly 600
miles of canals and ditches in all of Nevada County.
The Rock Creek, Deer Creek and South Yuba Canal
Company (later shortened to South Yuba Canal Company)
completed the most visionary and fantastic water project
ever in California with its South Yuba Canal. This canal
took water from the South Yuba at elevation 4675 feet, high
up in the mountains, just below the present Spaulding Dam,
and took it down the Bear Valley a distance of 16 miles,
where smaller distributing canals took the water to the
various mining areas.
It was a “wholesale” facility, or the equivalent of a moderm freeway, in terms of transporting large amounts of
\ water. The South Yuba Canal started with over one mile of
six-foot wide by five-foot deep flume bolted to a ledge
blasted into the sheer cliff below the diversion. (This section is now made of pipe and is visible from the Bowman
Lake Road.) From the lip of the Bear Valley, flume, ditch
and tunnel construction continued for fifteen miles, where it
tunneled 3100 feet through the ridge to reemerge within the
Deer Creek/Yuba drainage. This project was completed in
1857 at a cost of $500,000.
This canal made it possible to get large quantities of
water to almost any place it was needed, because its elevation was well above the gold-bearing gravels. The main distribution canals were Chalk Bluff (built in 1858), Ridge
(1858), Cascade (1860), and Dutch Flat (1865)—and all
went to major hydraulic areas.
The Cascade had its own water right of 1400 miner’s
inches, but also used water from the South Yuba Canal. The
genius of the South Yuba Canal system was the high mountain storage—most notably Meadow Lake (1858) at 7515
feet elevation and Fordyce (1874) at 6400 feet. This allowed the spring run-off to be captured and rationed out
late in the summer, when most streams would have dried up
otherwise.
(>
Nevada County Historical Society
Bulletin
VOLUME 55 NUMBER 3 JULY 2001
X yy,
You Bet, Hunt’s Hill, Quaker Hill, Scotts Flat and Buckeye
Hill. This area was found early on to be one of the best
“gravel-mining” areas. It sat squarely as part of the path of .
the “ancestral Yuba River” flowing north from the Dutch
Flat area toward the Washington ridge.
Little York township straddled the ridge separating the
Deer Creek drainage and the Greenhorn Creek arm of the
Bear River. This area ranges in elevation from 2900 feet (at
Scotts Flat on the north) to 3300 feet at the top of the saddle
near Quaker Hill (site of current Cascade Shores community), and then down to 2600 feet on the south side to
Greenhom Creek. Gold-bearing gravel was exposed on
both sides of this saddle, part of the path of the ancestral
river.
Initially, most of the mining activity took place on the
Greenhorn side, using water from Greenhorn Creek. One of
those early sites was Buckeye Hill, which may have been
the site where hydraulic mining was first developed (instead of the Buckeye Hill near Nevada City). Anthony
Chabot, Eli Miller and Edward E. Matteson crossed the
plains together and started their mining activity as partners
at this location in 1852. An account by Mr. G. E. Poore of
Red Dog indicates the process was actually first used there
in early 1853, and then the machinery was duplicated, at the
request of Mr. A. B. Caldwell, and placed into use at his
American Hill mine in Nevada City. Edward E. Matteson
was in charge of the American Hill operation in 1853, so,
whichever version is correct, he was still very much a part
of the invention, along with Miller and Chabot.
A key player in the Cascade story was Amos T. Laird,
one of the biggest gravel miners in Nevada City. He had
considerable standing in the community, as indicated by his
designation as a commissioner for the first election held
after the formation of Nevada County in 1851. He was also
a member of the “Nevada Rifles” (a volunteer militia company), along with future California Supreme Court Justice
Niles Searls.
Laird consolidated claims in the Gold Flat area and
brought in his own ditch to sluice the area. This ditch exfo". The Cascade Canal came into use as the way to get water
~into what formerly was known as Little York township,
which included the mining areas of Little York, Red Dog,
perience apparently led him to get into the ditch business in
a big way. He then partnered with Thomas Chambers to
build the Cascade Canal to deliver water to the Little York