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

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)

Bibliographic Details
Main Authors:	James L. Dickson, James W. Head, Joseph S. Levy, Gareth A. Morgan, David R. Marchant
Format:	Dataset
Language:	unknown
Published:	2017
Subjects:	Geology Gully formation McMurdo Dry Valleys flow front advance deposition processes Diurnal gully activity sequence source Vantage importance Figure 4 peak austral summer Site gully erosion Austral Antarc* Antarctica
Online Access:	https://doi.org/10.6084/m9.figshare.5621326.v1 https://figshare.com/articles/Gully_formation_in_the_McMurdo_Dry_Valleys_Antarctica_multiple_sources_of_water_temporal_sequence_and_relative_importance_in_gully_erosion_and_deposition_processes/5621326

Description
Summary:	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)