Everything about Badwater Basin totally explained
Badwater is a
basin in
California's
Death Valley, noted as the lowest point in
North America, with an
elevation of 282
feet (85.5
m) below sea level.
The site itself consists of a small
spring-fed pool of water next to the
road; however, the accumulated
salts of the surrounding basin make it undrinkable, thus the name "Badwater". The pool does have
animal and
plant life, including
pickleweed, aquatic
insects, and the
Badwater snail.
Adjacent to the pool, where water isn't always present at the surface, repeated freeze-thaw and evaporation cycles gradually pushed the thin salt crust into curiously hexagonal honeycomb shape.
The pool itself isn't actually the lowest point of the basin, which is several
miles to the west and varies in position. However, the salt flats are hazardous to traverse (in many cases being only a thin white crust over mud), and so the sign is at the pool.
Geography
At Badwater, significant rainstorms flood the valley bottom periodically, covering the salt pan with a thin sheet of standing water. Each newly-formed lake doesn't last long though, because the 1.9 inch average rainfall is overwhelmed by a 150-inch annual evaporation rate. This, the United States' greatest evaporation potential, means that even a 12-foot-deep, 30-mile-long lake would dry up in a single year. While flooded, some of the salt is dissolved, then is redeposited as clean, sparkling crystals when the water evaporates.
History
Not long ago, during the
Holocene (about 2000-4000 years ago), the climate was quite a bit wetter than today. So wet that streams running from nearby mountains gradually filled Death Valley to a depth of almost 30 feet. Some of the minerals left behind by earlier Death Valley lakes dissolved in the shallow water, creating a briny solution.
The wet times didn't last. The climate warmed and rainfall declined. The lake began to dry up. Minerals dissolved in the lake became increasingly concentrated as water evaporated. Eventually, only a briny soup remained, forming salty pools on the lowest parts of Death Valley's floor. Salts (95% table salt - NaCl) began to crystallize, coating the surface with a thick crust about three to five feet thick.
Other
Badwater is the starting point of the
Badwater Ultramarathon, which ends high on
Mount Whitney (the highest point in the
Continental United States), 85 miles (137 kilometers) to the west.
Further Information
Get more info on 'Badwater Basin'.
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