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Ridges on Mars Suggest Ancient Flowing Water

By Guest PostFebruary 2, 2013Scienceactive hydrology, ancient martian subsurface, applied physics lab, biosphere, brown university, craters on mars, curiosity rover, flowing water, fluid flow, fossils of cracks, fracture conduits, gale crater, habitable environment, hydrothermal fluid, hypothesis, jack mustard, johns hopkins university, landing site, lee saper, mars reconnaissance orbiter, martian surface, mineral hardened material, minerals, NASA, nili fossae, nilosyrtis, orientation data, planetary exploration, regional scale volcanism, ridges, subsurface hydrology, surrounding rocks

Ridges in impact craters on Mars appear to be fossils of cracks in the Martian surface, formed by minerals deposited by flowing water. Water flowing beneath the surface suggests life may once have been possible on Mars.

PROVIDENCE, R.I. [Brown University] — Networks of narrow ridges found in impact craters on Mars appear to be the fossilized remnants of underground cracks through which water once flowed, according to a new analysis by researchers from Brown University.

The study, in press in the journal Geophysical Research Letters, bolsters the idea that the subsurface environment on Mars once had an active hydrology and could be a good place to search for evidence of past life. The research was conducted by Lee Saper, a recent Brown graduate, with Jack Mustard, professor of geological sciences. (more…)

Meteorite Shockwaves Trigger Dust Avalanches on Mars

By Guest PostDecember 18, 2011Scienceairblast, alfred mcewen, atmosphere, basketball court, craters on mars, dark streaks, dust avalanches, dusty surface, equator, erosion, hirise camera, impact crater, jay melosh, kaylan burleigh, mars global surveyor orbiter, martian surface, meteorite, olympus mons, plate tectonic processes, red planet, shock wave, solar system, tallest mountain, university of arizona

Dust avalanches around impact craters on Mars appear to be the result of the shock wave preceding the actual impact, according to a study led by an undergraduate student at the UA.

When a meteorite careens toward the dusty surface of the Red Planet, it kicks up dust and can cause avalanching even before the rock from outer space hits the ground, a research team led by an undergraduate student at the University of Arizona has discovered.

“We expected that some of the streaks of dust that we see on slopes are caused by seismic shaking during impact,” said Kaylan Burleigh, who led the research project. “We were surprised to find that it rather looks like shockwaves in the air trigger the avalanches even before the impact.” (more…)

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Ridges on Mars Suggest Ancient Flowing Water

Meteorite Shockwaves Trigger Dust Avalanches on Mars