Valley formation on martian volcanoes in the Hesperian : Evidence for melting of summit snowpack , caldera lake formation , drainage and erosion on Ceraunius Tholus

@inproceedings{Fassett2007ValleyFO,
  title={Valley formation on martian volcanoes in the Hesperian : Evidence for melting of summit snowpack , caldera lake formation , drainage and erosion on Ceraunius Tholus},
  author={Caleb I. Fassett and James W. Head},
  year={2007}
}
Ceraunius Tholus, a Hesperian-aged volcano in the Tharsis region, is characterized by small radial valleys on its flanks, and several larger valleys originating near its summit caldera. All of these large valleys drain from near the lowest present portion of the caldera rim and down the flanks of the volcano. The largest valley debauches into Rahe Crater (an oblique impact crater), forming a depositional fan. Recent study of climate change on Mars suggests that many low-latitude regions… CONTINUE READING
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