Anomalous Erosional Topography in Victoria Land, Antarctica.
An area of some 18 square kilometers at the head of Wright Dry Valley displays an erosional terrain of unique characteristics-a labyrinthine complex of erratic, interconnecting channels cut to depths of more than 100 meters in bedrock. It is interpreted as a result of catastrophic fluvial erosion, probably analogous to that which produced the Channeled Scabland of eastern Washington, though on a greatly reduced areal scale.
Smith
H T
HT