Movement Directions in Late Paleozoic Glacial Rocks of the Horlick and Pensacola Mountains, Antarctica
Striae and associated structures beneath and within the Buckeye Tillite in the Ohio Range of the Horlick Mountains show that Permian(?) glaciers moved toward the west-southwest. Striae in the Wisconsin Range of the Horlicks display similar orientation, but the sense of movement could not be determin...
Published in: | Science |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science (AAAS)
1966
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1126/science.153.3737.746 https://www.science.org/doi/pdf/10.1126/science.153.3737.746 |
id |
craaas:10.1126/science.153.3737.746 |
---|---|
record_format |
openpolar |
spelling |
craaas:10.1126/science.153.3737.746 2024-06-09T07:38:57+00:00 Movement Directions in Late Paleozoic Glacial Rocks of the Horlick and Pensacola Mountains, Antarctica Frakes, L. A. Matthews, J. L. Neder, I. R. Crowell, J. C. 1966 http://dx.doi.org/10.1126/science.153.3737.746 https://www.science.org/doi/pdf/10.1126/science.153.3737.746 en eng American Association for the Advancement of Science (AAAS) Science volume 153, issue 3737, page 746-749 ISSN 0036-8075 1095-9203 journal-article 1966 craaas https://doi.org/10.1126/science.153.3737.746 2024-05-16T12:54:28Z Striae and associated structures beneath and within the Buckeye Tillite in the Ohio Range of the Horlick Mountains show that Permian(?) glaciers moved toward the west-southwest. Striae in the Wisconsin Range of the Horlicks display similar orientation, but the sense of movement could not be determined. Paleoglaciers in the Neptune Range and the Cordiner Peaks of the Pensacola Mountains moved toward the south-southwest with some dispersion. Paleocurrents flowed parallel to ice motion in the Ohio Range and in the Pensacolas, but they also flowed toward the north-northeast in the Pensacolas. Article in Journal/Newspaper Antarc* Antarctica AAAS Resource Center (American Association for the Advancement of Science) Pensacola Mountains ENVELOPE(-58.000,-58.000,-83.500,-83.500) Ohio Range ENVELOPE(-114.000,-114.000,-84.750,-84.750) Neptune Range ENVELOPE(-53.000,-53.000,-84.000,-84.000) Horlick Mountains ENVELOPE(-120.000,-120.000,-85.000,-85.000) Wisconsin Range ENVELOPE(-125.000,-125.000,-85.500,-85.500) Cordiner Peaks ENVELOPE(-53.517,-53.517,-82.804,-82.804) Science 153 3737 746 749 |
institution |
Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
Striae and associated structures beneath and within the Buckeye Tillite in the Ohio Range of the Horlick Mountains show that Permian(?) glaciers moved toward the west-southwest. Striae in the Wisconsin Range of the Horlicks display similar orientation, but the sense of movement could not be determined. Paleoglaciers in the Neptune Range and the Cordiner Peaks of the Pensacola Mountains moved toward the south-southwest with some dispersion. Paleocurrents flowed parallel to ice motion in the Ohio Range and in the Pensacolas, but they also flowed toward the north-northeast in the Pensacolas. |
format |
Article in Journal/Newspaper |
author |
Frakes, L. A. Matthews, J. L. Neder, I. R. Crowell, J. C. |
spellingShingle |
Frakes, L. A. Matthews, J. L. Neder, I. R. Crowell, J. C. Movement Directions in Late Paleozoic Glacial Rocks of the Horlick and Pensacola Mountains, Antarctica |
author_facet |
Frakes, L. A. Matthews, J. L. Neder, I. R. Crowell, J. C. |
author_sort |
Frakes, L. A. |
title |
Movement Directions in Late Paleozoic Glacial Rocks of the Horlick and Pensacola Mountains, Antarctica |
title_short |
Movement Directions in Late Paleozoic Glacial Rocks of the Horlick and Pensacola Mountains, Antarctica |
title_full |
Movement Directions in Late Paleozoic Glacial Rocks of the Horlick and Pensacola Mountains, Antarctica |
title_fullStr |
Movement Directions in Late Paleozoic Glacial Rocks of the Horlick and Pensacola Mountains, Antarctica |
title_full_unstemmed |
Movement Directions in Late Paleozoic Glacial Rocks of the Horlick and Pensacola Mountains, Antarctica |
title_sort |
movement directions in late paleozoic glacial rocks of the horlick and pensacola mountains, antarctica |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1966 |
url |
http://dx.doi.org/10.1126/science.153.3737.746 https://www.science.org/doi/pdf/10.1126/science.153.3737.746 |
long_lat |
ENVELOPE(-58.000,-58.000,-83.500,-83.500) ENVELOPE(-114.000,-114.000,-84.750,-84.750) ENVELOPE(-53.000,-53.000,-84.000,-84.000) ENVELOPE(-120.000,-120.000,-85.000,-85.000) ENVELOPE(-125.000,-125.000,-85.500,-85.500) ENVELOPE(-53.517,-53.517,-82.804,-82.804) |
geographic |
Pensacola Mountains Ohio Range Neptune Range Horlick Mountains Wisconsin Range Cordiner Peaks |
geographic_facet |
Pensacola Mountains Ohio Range Neptune Range Horlick Mountains Wisconsin Range Cordiner Peaks |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Science volume 153, issue 3737, page 746-749 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.153.3737.746 |
container_title |
Science |
container_volume |
153 |
container_issue |
3737 |
container_start_page |
746 |
op_container_end_page |
749 |
_version_ |
1801376433572937728 |