I Heard It Rains Down in Mars
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Saturday, Aug. 31, 2013, at 8:00 AM
There are a lot of features on Mars that look similar to those on
Earth. It has mountains, volcanoes, ice caps, sand dunes, and more.
One of the more intriguing Martian features are alluvial fans: The
finger-like spreading of a channel in the surface. On Earth, this is a
feature of a flood of water, which travels along the channel downhill
until it reaches a flat surface. When that happens it spreads out,
creating the fan of littler channels.
The HiRISE camera on Mars Reconnaissance Orbiter has spotted many alluvial fans, but this one was so pretty I wanted to share it:
Channels carved by torrential floods on Mars... millions of years ago. Click to enaresenate.
Photo by NASA/JPL/University of Arizona
Photo by NASA/JPL/University of Arizona
This fan is on the inside of the rim of Mojave Crater, a
60-kilometer-wide (40-mile-wide) impact crater near the equator of Mars.
The structure matches an Earthly alluvial fan almost perfectly. Larger
boulders are heavier and can’t be carried as easily by floodwaters, so
they tend to stop soon after the terrain levels out. Smaller rocks can
travel farther, which appears to be the case here. The branches, the
shape, the direction: Everything indicates a flash flood on Mars.
What could have caused it? This part surprised me: It may have been due to rain,
water rain, that could occur after an asteroid or comet impact. For
example, ice under the surface could be melted by the impact, which would then rain down over a large area. This would be a temporary and local event, but could spark flash floods something like rainstorms do here on Earth.
But after that, gravity and terrain did the rest, on Mars as it is on
Earth. That’s actually rather astonishing: Given some basic and
fundamental principles, you can actually figure out how weather and
erosion processes work on another planet. And when you look at it, it
actually kinda reminds you of home.
The Universe is a pretty weird place. But pretty cool, too.
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