Historically, before the advent of
diversion of Klamath River water for agricultural
purposes, which started several decades after the
first settlers and miners came to the area, and
before artificial storage of river water for both
agriculture and power generation, Klamath Lake and
the main stem of the Klamath River quite often,
during late Summer and Fall, experienced low, warm
and polluted water flows. This was the nature of
the Klamath system as a result of inflow to Klamath
Lake being high in nutrients and with high normal
daytime temperatures through the month of September.
The problem was exacerbated by the fact that Upper
Klamath Lake is a large, shallow body of water with
relatively low fall inflow leading to large amounts
of algae blooms and other warm water pollution. It
is recorded that in some years when the area would
experience a hot day with a wind from the south,
evapotranspiration along with that wind would block
all downstream flows over the natural barrier at the
south end of the lake. Also, it is noted in John C.
Fremont’s report of his explorations in this area
that the lake water was too polluted for the horses
to drink. In addition to the above noted records, a
journal maintained by George Gibbs in the Fall of
1851 while a member of the Redick McKee treaty
expedition presents a very good description of
conditions encountered along the Klamath as well as
the Scott and Shasta Rivers. Excerpts from that
journal along with comments will be presented later
in this paper.
Recently, a document referred to as
the KBRA (Klamath Basin Restoration Agreement) which
lays out a proposed program for division of existing
water supplies within what is normally referred to
as the Upper Klamath Basin was released to the
general public and others. The area included in the
water agreement included all streams tributary to
Upper Klamath Lake and the Lost River. The KBRA was
formulated through a series of secret meetings among
invited interested parties and organizations. As
the negotiations progressed, parties not in
agreement with the general trend of the line of
thought were excluded from future meetings. One of
the pre-set conditions without which negotiations
could not proceed was removal of four power dams on
the main stem Klamath River. Removal of the dams
was expressed as a benefit to salmon runs within the
main stem Klamath by opening historical spawning
areas used by these fish. No consideration was
included in the document released in January, 2008
to remedy problems created downstream within
California by removal of the dams such as loss of
economical electrical power, loss in property values
to the home owners who would loose their lake front
environment to a canyon filled with contaminated
lake sediments, contamination of the river
downstream by those sediments that would be left
along the river bank for years to come during high
waters and, loss of flow control for the river
provided by existing reservoirs and properly
scheduled and controlled power generation.
At this point, a little background
leading up to existing problems seems appropriate in
order to understand the mind set leading up to KBRA
negotiations. The background expressed here is the
conclusion arrived at over time by a reasonably
intelligent individual keeping appraised of current
news items. The Upper Klamath Basin as described
above is located in a semi-arid region with limited
water supply. Much of the area is of volcanic
origin. Upper Klamath Lake is a large, shallow lake
fed by water sources high in nutrients and
experiences high water temperatures during late
summer and fall. Historically, high evaporation
rates reduced downstream flows to very low values,
and, at times were actually cut off intermittently.
Development of the Klamath Basin Irrigation Project
early in the 20th century provided storage of winter
flows to be used for summer irrigation of Project
lands. Later, development of the power potential
created by storage of winter flows was pursued by
private interests. Water supplies for agriculture,
while never over abundant, would become critical
during periods of drought. Later, after the
project had been operating for quite a number of
years, environmental interests began to believe that
the river system was being impaired by water
diverted for agriculture and by the existence of
power dams. Pressure was put on the power company
to remove the dams and then when re-licensing became
necessary, that pressure was increased many fold.
Meanwhile, court action against agricultural
interests increased leading to a court ordered
cut-off of irrigation water in the year 2001 which
was financially devastating to many Project land
owners. Thus when the secret negotiations leading
up to the KBRA promised relief from court ordered
water stoppages at the hands of environmental
interests in exchange for support in achieving dam
removal, many Project land owners were willing to
sign on (blackmailed). In spite of numerous
problems certain to take place on the Klamath main
stem, Dam opponents list the only benefit to be
restoration of the river so that hypothetical large
salmon runs can return. These opponents are either
so brainwashed into the idea that restoration of any
river system will lead to good things or they are so
dead set against any dam that they do not care about
the consequences. In the paragraphs below I will
attempt to paint a picture, mostly based on
descriptions given by George Gibbs, but also
enhanced by a lifetime of contact with the Klamath
River and knowledge passed on by three previous
generations of Klamath River residents.
The Journal used herein is titled
“GEORGE GIBBS’JOURNAL OF REDICK MCKEE’S EXPEDITION
THROUGH NORTHWESTERN CALIFORNIA IN 1851” Edited and
with annotations by Robert F. Heizer. ARCHEOLOGICAL
RESEARCH FACILITY, Department of Anthropology,
University of California, Berkeley. 1972. As
explained by Mr. Heizer, George Gibbs was a well
educated man with a law degree from Harvard
University. After practicing law for a while, he
came west to Oregon and subsequently learned some of
the language of Indian tribes along the Columbia
River. He came to California in time to sign on as
interpreter for the Redick McKee Treaty expedition.
On Saturday, September 27th the expedition reached
the vicinity of the junction of the Klamath and
Trinity rivers and then returned to this vicinity on
or about November 13th after having traveled along
the Klamath main stem to Scott River, up Scott River
to Scott Valley then exploring the Shasta Valley.
Along the way, Mr. Gibbs recorded his observations
concerning local Indian tribes, the River and the
surrounding area. It must be remembered that the
first mining parties to visit the Klamath took place
in 1850,
2
the year prior to the McKee
expedition and, in view of the difficult terrain, no
large scale mining operations had been started.
On September 29th, while near the
junction of the Trinity and Klamath Rivers about 35
miles upstream from the mouth of the Klamath, Mr.
Gibbs gave a general description of the two rivers.
In part he said “Like the Klamath, the Trinity runs
during it’s whole length through mountains; It is in
size about half that of the Klamath, and it’s
waters, likewise rapid, are of transcendent purity;
contrasting with those of the latter stream which
never lose the taint of their origin. The other
principal branches of the Klamath, Salmon, Scott’s,
and Shaste rivers, will be spoken of hereafter.”
Note: It is significant that Mr.
Gibbs should speak of the waters of the Klamath as
tainted while this far downstream from it’s source.
Besides the major tributaries mentioned above,
approximately 100 tributaries of lesser sizes enter
the Klamath above his location. Some of these such
as Indian Creek, Elk Creek, Camp Creek among others
contribute a significant amount of cold, clear water
into the Klamath even during Fall months.
“Thursday, Oct. 9th. The business of
the treaty being concluded, the camp broke up
to-day, -- A couple miles above the forks, we
reached the Hai-am-mu village, -- At this village
there was a large fish-dam: a work exhibiting an
extraordinary degree of both enterprise and skill.
-- The whole dam was faced with twigs, carefully
peeled, and placed so close together as to prevent
the fish from passing up. -- The labor of
constructing this work must, with the few and
insufficient tools of the Indians, have been
immense. -- Slight scaffolds were built out below
it,” ( at an opening in the dam) “from which the
fish were taken in scoop-nets; -- Similar dams to
this exist on the Klamath, a few miles below the
forks, and about fifteen above this one: and there
is another upon the Trinity, -- They form a frequent
cause of quarrel among the bands inhabiting
different parts of the rivers.-- Almost all the fish
taken in the autumn have a diseased appearance; the
skin being discolored in large blotches.”
Annotation No. 53 by Heizer: “ Dams
or weirs which completely closed the stream to fish
ascending to spawn could have been effective in
preventing salmon from proceeding further upstream
than the dam and thus denying others from partaking
in the run. The Kepel dam on Klamath River (Kroeber,
Handbook, pp. 58-60) was torn down after ten days of
operation, not because it was inefficient, but
because tribes upstream (Hupa, Karok, and Shasta)
would insist on their share of the salmon run.”
Note: Above statements raise
questions about the overall size of fall salmon runs
in the mid-1800’s. If the runs were as large as
some presently speculate, there would be no way
that the Indian, using dip net and spears, could
have caught
3
enough of the migrating salmon to impact upstream
needs. Also, the fact that the salmon were
diseased looking after only coming this far up the
river, low river flows along with diseases were
already taking it’s toll. A large salmon die-off in
the mid-Klamath in about 1915 has been documented
by the Ca. Div. of Fish and Game as having been
caused by a gill disease endemic to the Klamath
River.
Tuesday, Oct. 14th. Speaking of
native dogs owned by the Indians, Gibbs states:
“Unfortunately salmon blood does not kill them, as
it does dogs of a more generous breed.”
Note: Salmon poisoning of dogs is
another disease endemic to the warm waters of the
Klamath.
Wednesday, Oct. 15th.—“Here we
encamped at the mouth of Clear Creek – These Indians
complained of hunger, and seemed really destitute.”
Monday, Oct. 30th. – “In camping on
the Klamath, it is necessary to seek the
neighborhood of the brooks, especially at this
season; as the water, never pure, is now offensive
from the number of dead salmon.”
Annotation No. 69 by Heizer: “There
may be some connection between the Yurok idea that
the waters of the Klamath are “poisonous” (Kroeber,
Handbook, p. 69), and the dead salmon which, after
the spawning run, contaminate it,”
Note: During my younger years on
the Klamath, 1931 to 1940, I never personally
observed dead salmon lying along the banks while my
mother, born in 1909, told of being directed, as a
young girl, by her grandfather to get sharp sticks
to throw the dead fish back into the river.
However, I was constantly warned to never swallow
Klamath River water. By the time of my younger
years, some of the power dams were in place which
improved late summer and Fall flow conditions.
Tuesday, Oct. 21st. – Speaking of the
Scott River: “while in the summer and fall it is
fordable almost anywhere.”
Monday, Oct. 27th. While exploring
the Shasta Valley – “The river itself, wandering
through arid plains, becomes tepid and unfit for
use,”
Wednesday, Nov. 12th. On the return
trip downstream the party camped overnight near the
mouth of the Salmon River. “The salmon fishing was
still going on; but the greater part of the fish
exhibited an unhealthy appearance.
4
Removal of power dams from the main
stem of the Klamath River will not restore the river
to a condition more favorable to human or fisheries
habitation as shown by the above notes. Loss of
storage used to generate electrical power during
times when natural flow would be inadequate will
likely throw the river back to a diseased condition
of low, warm, polluted water flows. Also, the
Klamath is not referred to as an upside down river
just by chance. The fact that the river water is
warm and polluted at it’s source and improves the
further downstream you go is not a normal situation
and without the help of colder water stored in the
reservoirs, this situation will be exacerbated.
Start of the fall salmon run quite often is delayed
because of inadequate flows over the bar at the
river mouth. Salmon collect in the ocean near the
mouth waiting for adequate, cold water. If a
coastal storm opens the bar before flows from the
upper river have cooled and increased, the salmon
will be in real trouble before reaching their
destination.
There is no known documentation from
the period of early exploration and settlement of
the upper Klamath Basin that indicates the existence
of spawning salmon above Upper Klamath Lake. The
existence of fish bones found at village sites has
led to the belief that they were caught near those
locations when, in fact, they were most likely
caught downstream and carried to the village. If,
by chance, a few salmon did manage to migrate into
the Upper Basin on exceptional water years does not
mean that a permanent run could be established that
far upstream following removal of the dams.
It is true that these power dams have
no storage space dedicated to flood control;
however, just the fact that they are there provides
a certain degree of protection. The dam operators
must maintain storage necessary for protection of
the structures by evaluating potential inflow and by
making releases ahead of unusual events. A flood
generated in the upper basin capable of causing
significant damage downstream of the dams is a
definite possibility. During the early spring
months of 2008 all of the players were in position
to cause a disastrous flood originating in the upper
basin except for the kicker. That kicker being a
warm rain which would have melted the several inch
blanket of snow spread over the large upper basin
area. Such a condition existed in the Columbia
Basin area of Eastern Washington in 1949 and the
kicker did show up. Look up the record of flows in
Crab Creek.
For the sake of us all that call the
Klamath home, including the Coho salmon who did not
reside in the mid to upper Klamath prior to
construction of dams, PLEASE do not restore the
Klamath River.
5
By:
Glen Briggs
B.S., Civil Engineering
Oregon State University
1960
Civil Engineer, retired
Dept. of Interior
Bureau of Reclamation
1960 to 1987
6
(Posted with the permission of
the author)