NECESSITY OF SOIL CONSERVATION IN THE FAR NORTH
The carrying-out of conservation laws is ofter complicated, not only by organizational factors concerning which much has been written, but also by insufficient ability to foresee the consequences of human activity, which may variously affect different geographic topographical zones. This may be easi...
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ftdtic:AD0690797 2023-05-15T15:04:40+02:00 NECESSITY OF SOIL CONSERVATION IN THE FAR NORTH Kryuchkov,V. V. DEFENCE SCIENTIFIC INFORMATION SERVICE OTTAWA (ONTARIO) 1969-06 text/html http://www.dtic.mil/docs/citations/AD0690797 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0690797 en eng http://www.dtic.mil/docs/citations/AD0690797 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Geology Geochemistry and Mineralogy (*EROSION SOILS) (*SOILS SIBERIA) PROTECTION DAMAGE PERMAFROST FREEZING MELTING ICE FOREST FIRES GRASSES ARCTIC REGIONS USSR SOIL CONSERVATION TRANSLATIONS TUNDRA Text 1969 ftdtic 2016-02-18T22:12:17Z The carrying-out of conservation laws is ofter complicated, not only by organizational factors concerning which much has been written, but also by insufficient ability to foresee the consequences of human activity, which may variously affect different geographic topographical zones. This may be easily seen in the example of Northeast Siberia. The Maritime (Pacific Coastal) Plain from the Omoloi to the Kolyma, an extent of 1000-1100 km, is built up mainly of lacustrine-alluvial sediments containing an enormous amount of subterranean vein-ice, forming 50-60% of the volume of the top 50-100 m layer of the ground. Indeed the very existence of the plain is possible only thanks to the ground's remaining frozen. Its thawing can cause large sections of the earth's surface to sink below sea level. (Author) Trans. of Priroda (USSR) n12 p72-74 1968, by E. R. Hope. Text Arctic Ice permafrost Tundra Siberia Defense Technical Information Center: DTIC Technical Reports database Arctic Kolyma ENVELOPE(161.000,161.000,69.500,69.500) Pacific |
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Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Geology Geochemistry and Mineralogy (*EROSION SOILS) (*SOILS SIBERIA) PROTECTION DAMAGE PERMAFROST FREEZING MELTING ICE FOREST FIRES GRASSES ARCTIC REGIONS USSR SOIL CONSERVATION TRANSLATIONS TUNDRA |
spellingShingle |
Geology Geochemistry and Mineralogy (*EROSION SOILS) (*SOILS SIBERIA) PROTECTION DAMAGE PERMAFROST FREEZING MELTING ICE FOREST FIRES GRASSES ARCTIC REGIONS USSR SOIL CONSERVATION TRANSLATIONS TUNDRA Kryuchkov,V. V. NECESSITY OF SOIL CONSERVATION IN THE FAR NORTH |
topic_facet |
Geology Geochemistry and Mineralogy (*EROSION SOILS) (*SOILS SIBERIA) PROTECTION DAMAGE PERMAFROST FREEZING MELTING ICE FOREST FIRES GRASSES ARCTIC REGIONS USSR SOIL CONSERVATION TRANSLATIONS TUNDRA |
description |
The carrying-out of conservation laws is ofter complicated, not only by organizational factors concerning which much has been written, but also by insufficient ability to foresee the consequences of human activity, which may variously affect different geographic topographical zones. This may be easily seen in the example of Northeast Siberia. The Maritime (Pacific Coastal) Plain from the Omoloi to the Kolyma, an extent of 1000-1100 km, is built up mainly of lacustrine-alluvial sediments containing an enormous amount of subterranean vein-ice, forming 50-60% of the volume of the top 50-100 m layer of the ground. Indeed the very existence of the plain is possible only thanks to the ground's remaining frozen. Its thawing can cause large sections of the earth's surface to sink below sea level. (Author) Trans. of Priroda (USSR) n12 p72-74 1968, by E. R. Hope. |
author2 |
DEFENCE SCIENTIFIC INFORMATION SERVICE OTTAWA (ONTARIO) |
format |
Text |
author |
Kryuchkov,V. V. |
author_facet |
Kryuchkov,V. V. |
author_sort |
Kryuchkov,V. V. |
title |
NECESSITY OF SOIL CONSERVATION IN THE FAR NORTH |
title_short |
NECESSITY OF SOIL CONSERVATION IN THE FAR NORTH |
title_full |
NECESSITY OF SOIL CONSERVATION IN THE FAR NORTH |
title_fullStr |
NECESSITY OF SOIL CONSERVATION IN THE FAR NORTH |
title_full_unstemmed |
NECESSITY OF SOIL CONSERVATION IN THE FAR NORTH |
title_sort |
necessity of soil conservation in the far north |
publishDate |
1969 |
url |
http://www.dtic.mil/docs/citations/AD0690797 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0690797 |
long_lat |
ENVELOPE(161.000,161.000,69.500,69.500) |
geographic |
Arctic Kolyma Pacific |
geographic_facet |
Arctic Kolyma Pacific |
genre |
Arctic Ice permafrost Tundra Siberia |
genre_facet |
Arctic Ice permafrost Tundra Siberia |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0690797 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766336404264058880 |