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Volume 052-2 - April 1998 (8 pages)

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Nevada County Historical Society
Bulletin
Volume 52, No. 2 April 1998
Lake Englebright
By Bedford Lampkin
Lace ENGLEBRIGHT IS LOCATED on the Yuba River
approximately equidistant between Marysville and Grass Valley. The county line between western Nevada County and
eastern Yuba County runs up the middle of the lake. The lake
is formed by the Upper Narrows Dam and was built in 1940
and is maintained by the Corps of Engineers.
Named for Harry Englebright of Nevada City, a mining
engineer and legislator, the dam never was used for its original purpose. But it is a fitting tribute to a deserving man and
an attractive and useful addition to our state’s resources.
The lake is open all year. There is a modest fee for the use
~ of the small boat launching ramp located adjacent to the
picnic area. Camping areas are available, but can only be
reached by boat. Visible across the lake from the launching
ramp is a private concessionaire marina (licensed by the
Corps of Engineers) and an armada of houseboats.
The building of the Upper Narrows Dam is just one facet
of a larger picture. The dam was born of a fierce battle fought
on a personal level and on a legislative and judicial level.
Initially the conflicting interests were the valley farmers and
the hydraulic mining advocates.
THE CONTROVERSY
Hydraulic mining began in approximately 1852 as a fairly
harmless occupation. Early on in the gold rush, the valuable
metal could be found in the stream beds of the Sierra foothills
with little effort. But in short order, with the arrival of many
men intent upon taking the treasure, gold became more difficult to come by. The very primitive technology of the earlier
argonauts was replaced by techniques for extracting gold
from relatively large amounts of ore-bearing gravel. In time
this led to the first attempts at hydraulic mining. Some would
give credit to Anthony Chabot (Lake Chabot, Chabot Junior
College near Oakland, etc.) for building a 50-foot wooden
penstock to provide water pressure, attaching a canvas hose
f™ and attacking a mound of gravel and washing the resultant
slurry down a lengthy sluice box. Edward E. Matteson is
given credit for attaching a metal nozzle to the hose making
the procedure more efficient. The idea caught on rapidly.
Within a few years the technology had advanced such that
large-bore metal nozzles were used to blast and wash the
gravel ridges. At the same time the building of ditches and
flumes, tunnels and pipes accelerated to provide the high
pressure water necessary for the operation.
The water that had impacted the gravel now ran its course
into sluices of thousands of feet in length wherein the heavier
gold particles were captured in the cleats fastened to the
bottom of the sluice. The lighter material was carried further
downhill by the weight and velocity of the water in its
gravitational flow. The sluices were cleaned of their gold
content every few weeks or months.
The gravel and fine dirt that washed downhill would
collect in huge amounts. When the winter rains came, the
waste material from the hydraulic operations would continue
its downhill travel through the various water courses, until it
reached one of the major rivers that arrived in California’s
Central Valley. The Feather, Yuba and Bear Rivers were all
major contributors to the deposits of debris which came to be
known as “slickens.” The Yuba River had the reputation as
being the worst offender in this regard. Hydraulic mining was
a lucrative business and money in it was invested by large
corporations as far away as England. In conjunction with
hydraulic mining, the water companies that invested in
ditches, flumes and reservoirs was also big business.
Early on, farmers had speculated what the effect would be
when the mine tailings reached the valley. For several years
there was little effect to be seen, but in the 1860s heavy rains
brought large amounts of debris into the rivers and subsequently into the valley.
The heavy rains continued for several years. The assault of
mine tailings continued in the valley with the result that river
beds rose and slickens began to cover the farm lands adjacent
to the river. Cities such as Marysville and Yuba City were
forced to build dikes to protect themselves from the raging
waters, but there was little that individual farmers could do to
stop the flow of sand and gravel covering the land.
The first legal action took place in 1873, when several
farmers pooled their resources and sued the Spring Valley
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