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Did Ancient Glaciers Shape Mars’ Surface? Deposits Found By Space Probe Hint Five-Mile-Deep Valley Was Carved By Ice

Sunday, April 1, 2012 19:20
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(Before It's News)

By Rob Waugh

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Huge glaciers might once have lurched through the 1,800-mile long Valles Marineris valleys on Mars.

The glaciers would have carried sulphur and dust from Martian volcanoes as they carved the five-mile-deep trough on the surface of the planet.

The new theory could explain deposits of sediment which were first seen by the Mariner 9 probe 40 years ago and which have puzzled scientists ever since.

 
Artist's impression of the Valles Marineris valley on Mars: Huge glaciers might once have lurched through the 1,800-mile long trough

Artist's impression of the Valles Marineris valley on Mars: Huge glaciers might once have lurched through the 1,800-mile long trough 

 
Mounds

Inside the canyon are vast mounds of layered sediments of enigmatic origins. In recent years, these huge mounds ¿ some that reach more than a mile in height ¿ have been shown to contain sulfate minerals, which are typically found in desert lake or shallow sea environments on Earth

New measurements by the Mars Reconnaissance Orbiter have lent weight to the theory that glaciers filled with volcanic ash and sulphur carved the Valles Marineris

New measurements by the Mars Reconnaissance Orbiter have lent weight to the theory that glaciers filled with volcanic ash and sulphur carved the Valles Marineris

‘Icy weathering might be a major part of the geologic story on Mars,’ said PSI Research Scientist Joseph Michalski, ‘The planet has been in a cold, frozen state for a long time.

'In the distant past, it was also cold, but volcanoes were much more active, periodically pumping huge amounts of sulfur into the atmosphere, which could have ultimately ended up trapped within ice alongside plentiful dust.’

Inside the canyon are vast mounds of layered sediments of enigmatic origins which have puzzled scientists for decades. 

A number of recent publications have suggested that the deposits were formed by water upwelling, where subsurface water breaches the surface during occasional upwelling events.

But the Michalski's team points out that the deposits are 'draped' over the canyon walls – and for the groundwater scenario to be true, the entire canyon would have had to be filled with sulphur.

For the deposits to have been left by water would have required more sulphur that would be available on the whole of Mars.

 
Inside the canyon are vast mounds of layered sediments of enigmatic origins which have puzzled scientists for decades

Inside the canyon are vast mounds of layered sediments of enigmatic origins which have puzzled scientists for decades

 

A recent scan of the surface showing the weathering on the walls of the canyon - thought to have been caused in an acidic, dry environment, as if by a glacier filled with volcanic debris

A recent scan of the surface showing the weathering on the walls of the canyon – thought to have been caused in an acidic, dry environment, as if by a glacier filled with volcanic debris 

 

As an alternative, Michalski and Niles suggest that the ILDs formed from massive, dusty ice deposits that once filled much of the canyon.

Such a scenario is consistent with the size, topographic configuration of the deposits, and with their mineralogy, which suggests weathering in an acidic, water-limited environment.

‘Icy weathering should be much more important than the Earth because Mars lacks liquid surface water to buffer chemical processes,’ Michalski said. ‘As was pointed out by the great mineralogist Roger Burns more than 20 years ago, icy systems should become very acidic on Mars.’

‘We are of the opinion that Mars has been cold and dry for quite a long time, and that during that time, the various cycles of dust deposition, ice precipitation and sublimation, and sulfur outgassing can explain quite a bit of the surface geology.

'Even so, the hypotheses are not without certain complications and uncertainties. It is our hope that more scientists will be begin to test these ideas.’

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