title: Anomalous Erosional Topography in Victoria Land, Antarctica.
abstract: 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.
authors.forename: H T
authors.initials: HT
authors.lastname: Smith