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Geomorfologiya i Paleogeografiya

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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. Ivanov
ПИНРО
Russian Federation


I. E. Lomakin
ПИНРО
Russian Federation


A. L. Sorokin
ПИНРО
Russian Federation


V. R. Morozenko V. R.
ПИНРО
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.

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ISSN 2949-1789 (Print)
ISSN 2949-1797 (Online)