A Geographical Study of the Morphogenesis of Northern Lapland
The research area, which is rectangular in shape and stretches from the 69th parallel to the Arctic Ocean, is divided into multi-stage square units. Morphometric analyses have been made of the certain components of the landforms within these units. On the basis of the distribution of these component...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1969
|
Subjects: | |
Online Access: | http://www.dtic.mil/docs/citations/AD0722133 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0722133 |
id |
ftdtic:AD0722133 |
---|---|
record_format |
openpolar |
spelling |
ftdtic:AD0722133 2023-05-15T14:58:45+02:00 A Geographical Study of the Morphogenesis of Northern Lapland Kaitanen,Veijo TURKU UNIV (FINLAND) INSTITUTUM GEOGRAPHICUM 1969-03 text/html http://www.dtic.mil/docs/citations/AD0722133 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0722133 en eng http://www.dtic.mil/docs/citations/AD0722133 Availability: Pub. in Fennia, v99 n5 p1-30 1970. No copies furnished by DDC or NTIS. DTIC AND NTIS Geology Geochemistry and Mineralogy (*TERRAIN EROSION) (*FINLAND GEOGRAPHY) SEDIMENTARY ROCK STRATIGRAPHY SURFACES RIVERS STATISTICAL DATA OROGENY ROCK GEOLOGIC AGE DETERMINATION NORWAY SWEDEN ARCTIC OCEAN ISLANDS USSR GEOMORPHOLOGY LANDFORMS Text 1969 ftdtic 2016-02-19T00:42:21Z The research area, which is rectangular in shape and stretches from the 69th parallel to the Arctic Ocean, is divided into multi-stage square units. Morphometric analyses have been made of the certain components of the landforms within these units. On the basis of the distribution of these components it has been possible to draw some conclusions concerning the morphogenesis of Northern Lapland which do not fully correspond to those made earlier. The bipartite division which is distinguished in the relief is the result of different erosional processes caused by climatic changes rather than a consequence of different stages of evolution caused by similar erosional processes. In the same way it seems that the theory of superposition and inheritance explains more convincingly the interrelations between the elements of relief than the theory of local accelerations of fluvial incision caused by very late block movements. On the basis of the arguments used in the paper, the glacial transformation of earlier landforms in the Finnish part of the research area may be regarded in general as having been slight and in places almost nonexistent. Thus also the tor-like forms belonging to the minor relief have been able to a certain extent to escape ultimate destruction during the latest glaciation. (Author) Text Arctic Arctic Ocean Lapland Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Norway |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Geology Geochemistry and Mineralogy (*TERRAIN EROSION) (*FINLAND GEOGRAPHY) SEDIMENTARY ROCK STRATIGRAPHY SURFACES RIVERS STATISTICAL DATA OROGENY ROCK GEOLOGIC AGE DETERMINATION NORWAY SWEDEN ARCTIC OCEAN ISLANDS USSR GEOMORPHOLOGY LANDFORMS |
spellingShingle |
Geology Geochemistry and Mineralogy (*TERRAIN EROSION) (*FINLAND GEOGRAPHY) SEDIMENTARY ROCK STRATIGRAPHY SURFACES RIVERS STATISTICAL DATA OROGENY ROCK GEOLOGIC AGE DETERMINATION NORWAY SWEDEN ARCTIC OCEAN ISLANDS USSR GEOMORPHOLOGY LANDFORMS Kaitanen,Veijo A Geographical Study of the Morphogenesis of Northern Lapland |
topic_facet |
Geology Geochemistry and Mineralogy (*TERRAIN EROSION) (*FINLAND GEOGRAPHY) SEDIMENTARY ROCK STRATIGRAPHY SURFACES RIVERS STATISTICAL DATA OROGENY ROCK GEOLOGIC AGE DETERMINATION NORWAY SWEDEN ARCTIC OCEAN ISLANDS USSR GEOMORPHOLOGY LANDFORMS |
description |
The research area, which is rectangular in shape and stretches from the 69th parallel to the Arctic Ocean, is divided into multi-stage square units. Morphometric analyses have been made of the certain components of the landforms within these units. On the basis of the distribution of these components it has been possible to draw some conclusions concerning the morphogenesis of Northern Lapland which do not fully correspond to those made earlier. The bipartite division which is distinguished in the relief is the result of different erosional processes caused by climatic changes rather than a consequence of different stages of evolution caused by similar erosional processes. In the same way it seems that the theory of superposition and inheritance explains more convincingly the interrelations between the elements of relief than the theory of local accelerations of fluvial incision caused by very late block movements. On the basis of the arguments used in the paper, the glacial transformation of earlier landforms in the Finnish part of the research area may be regarded in general as having been slight and in places almost nonexistent. Thus also the tor-like forms belonging to the minor relief have been able to a certain extent to escape ultimate destruction during the latest glaciation. (Author) |
author2 |
TURKU UNIV (FINLAND) INSTITUTUM GEOGRAPHICUM |
format |
Text |
author |
Kaitanen,Veijo |
author_facet |
Kaitanen,Veijo |
author_sort |
Kaitanen,Veijo |
title |
A Geographical Study of the Morphogenesis of Northern Lapland |
title_short |
A Geographical Study of the Morphogenesis of Northern Lapland |
title_full |
A Geographical Study of the Morphogenesis of Northern Lapland |
title_fullStr |
A Geographical Study of the Morphogenesis of Northern Lapland |
title_full_unstemmed |
A Geographical Study of the Morphogenesis of Northern Lapland |
title_sort |
geographical study of the morphogenesis of northern lapland |
publishDate |
1969 |
url |
http://www.dtic.mil/docs/citations/AD0722133 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0722133 |
geographic |
Arctic Arctic Ocean Norway |
geographic_facet |
Arctic Arctic Ocean Norway |
genre |
Arctic Arctic Ocean Lapland |
genre_facet |
Arctic Arctic Ocean Lapland |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0722133 |
op_rights |
Availability: Pub. in Fennia, v99 n5 p1-30 1970. No copies furnished by DDC or NTIS. |
_version_ |
1766330871696064512 |