Glacial Boulders on the Arctic Coast of Alaska

Reports incidental observations made in the Barrow-Cape Simpson area 1949-50. Pleistocene glaciers of Alaska did not extend north beyond the northern foothills of the Brooks Range, yet glacial boulders have been reported near and along the coast. Altogether 56 such erratic boulders from sheltered sp...

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Published in:ARCTIC
Main Author: McCarthy, Gerald R.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1958
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66784
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/66784 2023-05-15T14:19:21+02:00 Glacial Boulders on the Arctic Coast of Alaska McCarthy, Gerald R. 1958-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66784 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66784/50697 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66784 ARCTIC; Vol. 11 No. 2 (1958): June: 69–132; 70-85 1923-1245 0004-0843 Animal distribution Animal migration Animal physiology Atlantic salmon Biological sampling Brook trout Costs Diurnal variations Employment Fish spawning Fisheries Measurement Metabolism Oxygen Salmoninae Temperature Tides Koksoak Rivière Québec Caniapiscau Mélèzes Rivière aux Kuujjuaq info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1958 ftunivcalgaryojs 2022-03-22T21:23:36Z Reports incidental observations made in the Barrow-Cape Simpson area 1949-50. Pleistocene glaciers of Alaska did not extend north beyond the northern foothills of the Brooks Range, yet glacial boulders have been reported near and along the coast. Altogether 56 such erratic boulders from sheltered spots on the shore, as far as 8-9 mi inland on the tundra and a few from the present sea floor were examined. Their location and size, rock type with field description and petrographic analysis are tabulated. Of granite (16), diabase (17), quartzite (10), etc., they range in weight from 2-3 lbs. to 4-5 tons. They are thought to represent morainic material left by melting icebergs, and the bergs to have been produced from glaciers in widely separated areas. Article in Journal/Newspaper Arctic Arctic Atlantic salmon Barrow Brooks Range glaciers Iceberg* Kuujjuaq Tundra Alaska University of Calgary Journal Hosting Arctic Barrow Cape ENVELOPE(-61.704,-61.704,-63.716,-63.716) Cape Simpson ENVELOPE(-87.066,-87.066,67.351,67.351) Kuujjuaq ENVELOPE(-68.398,-68.398,58.100,58.100) Northern Foothills ENVELOPE(163.917,163.917,-74.733,-74.733) ARCTIC 11 2 70
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Animal distribution
Animal migration
Animal physiology
Atlantic salmon
Biological sampling
Brook trout
Costs
Diurnal variations
Employment
Fish spawning
Fisheries
Measurement
Metabolism
Oxygen
Salmoninae
Temperature
Tides
Koksoak
Rivière
Québec
Caniapiscau
Mélèzes
Rivière aux
Kuujjuaq
spellingShingle Animal distribution
Animal migration
Animal physiology
Atlantic salmon
Biological sampling
Brook trout
Costs
Diurnal variations
Employment
Fish spawning
Fisheries
Measurement
Metabolism
Oxygen
Salmoninae
Temperature
Tides
Koksoak
Rivière
Québec
Caniapiscau
Mélèzes
Rivière aux
Kuujjuaq
McCarthy, Gerald R.
Glacial Boulders on the Arctic Coast of Alaska
topic_facet Animal distribution
Animal migration
Animal physiology
Atlantic salmon
Biological sampling
Brook trout
Costs
Diurnal variations
Employment
Fish spawning
Fisheries
Measurement
Metabolism
Oxygen
Salmoninae
Temperature
Tides
Koksoak
Rivière
Québec
Caniapiscau
Mélèzes
Rivière aux
Kuujjuaq
description Reports incidental observations made in the Barrow-Cape Simpson area 1949-50. Pleistocene glaciers of Alaska did not extend north beyond the northern foothills of the Brooks Range, yet glacial boulders have been reported near and along the coast. Altogether 56 such erratic boulders from sheltered spots on the shore, as far as 8-9 mi inland on the tundra and a few from the present sea floor were examined. Their location and size, rock type with field description and petrographic analysis are tabulated. Of granite (16), diabase (17), quartzite (10), etc., they range in weight from 2-3 lbs. to 4-5 tons. They are thought to represent morainic material left by melting icebergs, and the bergs to have been produced from glaciers in widely separated areas.
format Article in Journal/Newspaper
author McCarthy, Gerald R.
author_facet McCarthy, Gerald R.
author_sort McCarthy, Gerald R.
title Glacial Boulders on the Arctic Coast of Alaska
title_short Glacial Boulders on the Arctic Coast of Alaska
title_full Glacial Boulders on the Arctic Coast of Alaska
title_fullStr Glacial Boulders on the Arctic Coast of Alaska
title_full_unstemmed Glacial Boulders on the Arctic Coast of Alaska
title_sort glacial boulders on the arctic coast of alaska
publisher The Arctic Institute of North America
publishDate 1958
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66784
long_lat ENVELOPE(-61.704,-61.704,-63.716,-63.716)
ENVELOPE(-87.066,-87.066,67.351,67.351)
ENVELOPE(-68.398,-68.398,58.100,58.100)
ENVELOPE(163.917,163.917,-74.733,-74.733)
geographic Arctic
Barrow Cape
Cape Simpson
Kuujjuaq
Northern Foothills
geographic_facet Arctic
Barrow Cape
Cape Simpson
Kuujjuaq
Northern Foothills
genre Arctic
Arctic
Atlantic salmon
Barrow
Brooks Range
glaciers
Iceberg*
Kuujjuaq
Tundra
Alaska
genre_facet Arctic
Arctic
Atlantic salmon
Barrow
Brooks Range
glaciers
Iceberg*
Kuujjuaq
Tundra
Alaska
op_source ARCTIC; Vol. 11 No. 2 (1958): June: 69–132; 70-85
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66784/50697
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66784
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