Geomorphology of the Corner High seamounts (North Atlantic)
Abstract
New data on the Corner High (SE Newfoundland) seamounts relief are presented. Main detections of lineaments are determined. The structure proved to indergo a considerable descent (about 1700 m). It is also shown that the seamounts had not been turned into guyots because of short duration of the subaerial stage of their development.
About the Authors
V. E. IvanovRussian Federation
I. E. Lomakin
Russian Federation
A. L. Sorokin
Russian Federation
V. R. Morozenko V. R.
Russian Federation
Review
For citations:
Ivanov V.E., Lomakin I.E., Sorokin A.L., Morozenko V. R. V.R. Geomorphology of the Corner High seamounts (North Atlantic). Geomorfologiya. 1989;(3):60-64.