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Gully formation in the McMurdo Dry Valleys, Antarctica: multiple sources of water, temporal sequence and relative importance in gully erosion and deposition processes

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posted on 21.11.2017, 16:22 by James L. Dickson, James W. Head, Joseph S. Levy, Gareth A. Morgan, David R. Marchant
Diurnal gully activity within Gully A during peak austral summer in January 2010, with average flow front advance of c. 8 m/day. Vantage point shown in Figure 4a (Site 1)

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