is a hill
in the south part of Augen Bluffs
, Miller Range
. The hill rises 100-200 m above the west side of Marsh Glacier
and is connected to Augen Bluffs by a col 10-20 m lower than the height of the hill. So named by the Ohio State University Geological Party
, 1967-68, because an isoclinal fold is well exposed on the side of the hill.