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Post Info TOPIC: Salar de Uyuni


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Salar de Uyuni
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Mapping one of the flattest parts of the planet will help satellite calibration.
A precise topographical map has been made of one of the flattest places on Earth: the salar de Uyuni, a vast plain of white cemented salt in the mountains of Bolivia. The ground survey, aided by global positioning systems (GPS), shows variations in elevation of less than a metre across an area almost half the size of Wales.

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HILLS AND VALLEYS IN EARTH'S LARGEST SALT 'FLAT'
Using a new twist on standard Global Positioning System (GPS) technology, a team of scientists has found that Earths largest salt flat is rougher than expected, according to a new report led by Adrian Borsa of Scripps Institution of Oceanography at UC San Diego and published in Geophysical Journal International.
Borsa and his team studied the salar de Uyuni in southwestern Bolivia, which is both a popular tourist destination and a potential calibration site for Earth-orbiting scientific instruments. It had never before been surveyed on this scale using modern techniques.  Although the salar appears to be perfectly flat to the eye, by applying an innovative method of error correction to their data, the team was able to identify broad features ranging in height from a few centimetres to half a metre and extending over distances of tens of kilometres or more.
Earlier maps do not show any surface relief on the salar de Uyuni.  By mapping the surface to the accuracy of a few centimetres, the research team uncovered previously hidden features -- hills, ridges and valleys -- and opened the salar for use as a ground reference site for highly accurate satellite-based ranging instruments.  

We had no idea these features existed, but they matter to anyone who uses the salt flat to calibrate satellite altimeters  - Dr. Adrian Borsa.

The scientists' most unexpected finding was that the broadest topographic features on the salar correlate well with the increase in the strength of gravity at the surface that results from dense rock buried underneath salar sediments.  Just as the ocean surface rises over denser seamounts, the salar surface also rises and falls to reflect the subsurface density variations. This effect has never before been observed on land.

Source RAS

Latitude: 20° 19' 60 S, Longitude: 67° 42' 0 W

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