Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica
Abstract An extensive system of mirabilite (Na 2 SO 4 · 10H 2 O) beds has been mapped on the Ross Ice Shelf near Black Island. The salt beds are normally underlain by a thin layer of mud and their surface is covered by a non-marine algal mat and boulder lag. These authors suggest the salt has been f...
Published in: | Journal of Glaciology |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1981
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000011187 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011187 |
id |
crcambridgeupr:10.1017/s0022143000011187 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/s0022143000011187 2024-03-03T08:38:48+00:00 Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica Brady, Howard Thomas Batts, Barry 1981 http://dx.doi.org/10.1017/s0022143000011187 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011187 en eng Cambridge University Press (CUP) Journal of Glaciology volume 27, issue 95, page 11-18 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1981 crcambridgeupr https://doi.org/10.1017/s0022143000011187 2024-02-08T08:37:11Z Abstract An extensive system of mirabilite (Na 2 SO 4 · 10H 2 O) beds has been mapped on the Ross Ice Shelf near Black Island. The salt beds are normally underlain by a thin layer of mud and their surface is covered by a non-marine algal mat and boulder lag. These authors suggest the salt has been formed by the displacement of sub-ice-shelf brines to the ice-shelf surface. Evidence also suggests that other terrestrial mirabilite beds in the McMurdo Sound area were formed in the same manner and deposited by the Ross Ice Shelf during its Wisconsin retreat from McMurdo Sound. Mirabilite salt in the dry valleys, southern Victoria Land, may have also originated from melt waters which dissolved ice-shelf mirabilite beds. Article in Journal/Newspaper Antarc* Antarctica Ice Shelf Journal of Glaciology McMurdo Sound Ross Ice Shelf Victoria Land Black Island Cambridge University Press Victoria Land McMurdo Sound Ross Ice Shelf Black Island ENVELOPE(70.100,70.100,-49.440,-49.440) Journal of Glaciology 27 95 11 18 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Brady, Howard Thomas Batts, Barry Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica |
topic_facet |
Earth-Surface Processes |
description |
Abstract An extensive system of mirabilite (Na 2 SO 4 · 10H 2 O) beds has been mapped on the Ross Ice Shelf near Black Island. The salt beds are normally underlain by a thin layer of mud and their surface is covered by a non-marine algal mat and boulder lag. These authors suggest the salt has been formed by the displacement of sub-ice-shelf brines to the ice-shelf surface. Evidence also suggests that other terrestrial mirabilite beds in the McMurdo Sound area were formed in the same manner and deposited by the Ross Ice Shelf during its Wisconsin retreat from McMurdo Sound. Mirabilite salt in the dry valleys, southern Victoria Land, may have also originated from melt waters which dissolved ice-shelf mirabilite beds. |
format |
Article in Journal/Newspaper |
author |
Brady, Howard Thomas Batts, Barry |
author_facet |
Brady, Howard Thomas Batts, Barry |
author_sort |
Brady, Howard Thomas |
title |
Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica |
title_short |
Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica |
title_full |
Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica |
title_fullStr |
Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica |
title_full_unstemmed |
Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica |
title_sort |
large salt beds on the surface of the ross ice shelf near black island, antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
1981 |
url |
http://dx.doi.org/10.1017/s0022143000011187 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011187 |
long_lat |
ENVELOPE(70.100,70.100,-49.440,-49.440) |
geographic |
Victoria Land McMurdo Sound Ross Ice Shelf Black Island |
geographic_facet |
Victoria Land McMurdo Sound Ross Ice Shelf Black Island |
genre |
Antarc* Antarctica Ice Shelf Journal of Glaciology McMurdo Sound Ross Ice Shelf Victoria Land Black Island |
genre_facet |
Antarc* Antarctica Ice Shelf Journal of Glaciology McMurdo Sound Ross Ice Shelf Victoria Land Black Island |
op_source |
Journal of Glaciology volume 27, issue 95, page 11-18 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000011187 |
container_title |
Journal of Glaciology |
container_volume |
27 |
container_issue |
95 |
container_start_page |
11 |
op_container_end_page |
18 |
_version_ |
1792507258923384832 |