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

Flow advance in Gully A and pond generation on the floor of South Fork during the end of austral summer (February/March), 2010. Noise/static patterns are due to low signal reaching the sensor during night-time conditions late in austral summer. 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:
Geology
FOS Earth and related environmental sciences
Austral
McMurdo Dry Valleys
South Fork
Antarc*
Antarctica
Online Access:https://dx.doi.org/10.6084/m9.figshare.5621317
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/5621317
Description
Summary:Flow advance in Gully A and pond generation on the floor of South Fork during the end of austral summer (February/March), 2010. Noise/static patterns are due to low signal reaching the sensor during night-time conditions late in austral summer. Vantage point shown in Figure 4a (Site 1).

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