Open AccessIce gouging on the arctic shelf of Russia
Author(s) -
С. Л. Никифоров,
С. Л. Никифоров,
R. A. Ananiev,
R. A. Anan’ev,
N. V. Libina,
N. V. Libina,
N. N. Dmitrevskiy,
Н. Н. Дмитревский,
Л. И. Лобковский,
Л. И. Лобковский
Publication year - 2019
Publication title -
okeanologiâ
Language(s) - English
Resource type - Journals
ISSN - 0030-1574
DOI - 10.31857/s0030-1574593466-468
Subject(s) - geology , iceberg , oceanography , glacier , glacial period , continental shelf , arctic , seabed gouging by ice , ice shelf , archipelago , sea ice , geohazard , shelf ice , permafrost , arctic ice pack , antarctic sea ice , paleontology , geomorphology , cryosphere , landslide
The results of recent geological and geophysical expeditions indicate the activation of hazardous natural phenomena associated with ice gouging and represent geohazard for almost all activities, including operation of the Northern Sea Route. Within the Barents Sea and the western part of the Kara Sea, the modern ice gouging is mainly associated with icebergs which are formed as a result of the destruction of the glaciers of Novaya Zemlya, the Spitsbergen archipelago and Franz Josef Land, while on the eastern shelf it is caused by the destruction of seasonal or perennial ice fields. Fixed furrows can be divided into modern coastal gouges or deep water ploughmarks. All deep water gouges within the periglacial and glacial shelf are of paleogeographical origin, but with different mechanisms of action on the seabed. These furrows were formed by floating ice on the periglacial shelf. On the glacial shelf deep water ploughmarks were formed by large icebergs, which could carry out the gouging even on the continental slope and deep-sea ridges of the Arctic Ocean.