A research team led by Brown University has documented dozens of channels carved by melted water from glaciers located in the midlatitude region of Mars. The glaciofluvial valleys were carved in Mars' most recent epoch, the team reports, supporting the idea that the Red Planet was home to diverse watery environments in its recent past. Results are published in Icarus.
Planetary scientists have uncovered telltale signs of water on Mars -- frozen and liquid -- in the earliest period of the Red Planet's history. A new claim, made public this month, is that a deep ocean covered some of the northern latitudes.
But the evidence for water grows much more scant after the Noachian era, which ended 3.5 billion years ago. Now Brown University planetary geologists have documented running water that sprang from glaciers throughout the Martian middle latitudes as recently as the Amazonian epoch, several hundred million years ago. These glaciofluvial valleys were, in essence, tributaries of water created when enough sunlight reached the glaciers to melt a thin layer on the surface. This, the Brown researchers write, led to "limited surface melting" that formed channels that ran for several kilometers and could be more than 150 feet wide.
The finding is "more than 'Yes, we found water,'" said Caleb Fassett, postdoctoral research associate in geological sciences and lead author of the paper published in Icarus. "What we see now is there's this complex history of different environments where water is being formed."
Caleb Fassett, with Brown research analyst James Dickson, professor James Head III, and geologists from Boston University and Portland State University, analyzed 15,000 images snapped by the Context Camera (CTX) aboard the Mars Reconnaissance Orbiter to compile the first survey of glaciofluvial valleys on Mars. The survey was sparked by a glaciofluvial valley that Dickson, Fassett, and Head spotted within the Lyot crater, located in the planet's middle latitudes. The team, in a paper last year in Geophysical Research Letters, dated that meltwater-inspired feature to the Amazonian.
In his survey, Fassett found dozens of other Amazonian-era ice deposits that spawned supraglacial and proglacial valleys, most of them located on the interior and exterior of craters in Mars' midlatitude belt. "The youthfulness (of the features) is surprising," he said. "We think of [post-Noachian] Mars as really, really cold and really, really dry, so the fact that these exist, in those kinds of conditions, is changing how we view the history of water on the planet."
What makes the finding even more intriguing is that the Brown planetary scientists can study what they believe are similar conditions on Earth. Teams from Brown and Boston University have visited the Antarctic Dry Valleys for years, where the surfaces of glaciers melt during the austral summer, sparking enough meltwater to carve a channel. The team will return to the Dry Valleys later this year to continue the study of this microclimate.
"It's sort of crazy," said Dickson, a member of the Brown team who stayed in the Dry Valleys for three months last year. "You're freezing cold and there's glacial ice everywhere, and it gets just warm enough that you get a river."
Fassett plans to search for more glaciofluvial valleys as more images come from the CTX, which has mapped roughly 40 percent of the planet.
Contributing authors include Joseph Levy of Portland State (who earned his Ph.D. at Brown last year) and James Marchant of Boston University. The research was funded by NASA.
- Fassett et al. Supraglacial and proglacial valleys on Amazonian Mars. Icarus, 2010; 208 (1): 86 DOI: 10.1016/j.icarus.2010.02.021
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