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: Dickson, James L., Head, James W., Levy, Joseph S., Morgan, Gareth A., Marchant, David R.
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London 2017
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.5621326
https://geolsoc.figshare.com/articles/media/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)