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: James L. Dickson, James W. Head, Joseph S. Levy, Gareth A. Morgan, David R. Marchant
Format: Dataset
Language:unknown
Published: 2017
Subjects:
Geology
gully
McMurdo Dry Valleys
source
pattern
sequence
deposition processes Flow advance
generation
erosion
vantage
importance
austral summer
South
Figure
sensor
signal
Site
formation
2010
Austral
South Fork
Antarc*
Antarctica
Online Access:https://doi.org/10.6084/m9.figshare.5621317.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/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).

Similar Items