The Salton Sea's Predicament
CLIP XX - VMP - North Shore
SLIDE 1
In 1905, a diversion was made on the Colorado river near its mouth, in Mexico,
for the purpose of conveying water to irrigate lands in the Imperial valley, California.
The diversion went sour
and the Colorado river changed course, flowing north toward the Salton Depression, with its lowest point at -287 feet below sea level,
to form the Salton Sea.
By 1907, the flow was finally controlled, but the accident made it patently clear that the Salton Depression
could hold a lot of water.
CLIP 3 - SS
SLIDE 2
Since 1928, the Salton Sea
has been the repository for the agricultural runoff of
the Imperial valley.
A mixture of salts and other chemicals have been flowing into the sea
for nearly a century.
A balance between runoff and evaporation keeps the sea from drying up, while
the salts continue to concentrate.
CLIP 6 - SS
SLIDE 3
The salts entering the Salton Sea can be traced to:
CLIP 7 - SS
SLIDE 4
Currently the Salton Sea is used as:
These uses are all artificial, because in the absence of agricultural runoff,
evaporation produces a dry lake bed.
CLIP 10 - VMP - East Shore
SLIDE 5
The Salton Sea restoration aims to reduce its salinity, currently about 30% saltier than the ocean and increasing.
A leading proposal would accumulate the salts in a smaller portion of the sea,
while reducing the salt content of the remaining larger portion.
This solution is unsustainable because the salts are not being physically removed, assuring
that future generations will have to cope with the ever increasing amount of salts.
Text: Victor M. Ponce
Music: Fernando Oñate
Camera: Juan Villaseñor
Editor: Flor Pérez
Credits: http://saltonsea.sdsu.edu
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Visualab Productions
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