Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya Tundra

Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya Tundra

The paper describes the methodology and presents the results of the calculation of the spectral characteristics of the terrain for the territory of the Bolshezemelskaya and Malozemelskaya Tundra (the north of the European part of Russia). There are nine terrain clusters, differing in the topographic...

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Main Authors: Kharchenko Sergey, Belyaev Yury
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/23/e3sconf_vc2020_04003.pdf
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spelling doaj-94cfb9f4e6c84784ae5d344dd6a181812021-04-02T13:22:42ZengEDP SciencesE3S Web of Conferences2267-12422020-01-011630400310.1051/e3sconf/202016304003e3sconf_vc2020_04003Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya TundraKharchenko SergeyBelyaev Yury0Lomonosov Moscow State UniversityThe paper describes the methodology and presents the results of the calculation of the spectral characteristics of the terrain for the territory of the Bolshezemelskaya and Malozemelskaya Tundra (the north of the European part of Russia). There are nine terrain clusters, differing in the topographic dissection pattern. Their geomorphological interpretation is given. Three clusters characterize mountainous and coarsely hilly terrain with the depth of dissection from 150 m and more. The others are low and elevated terrains with much lower depths of dissection (up to 50 m) and different patterns of interposition of landforms.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/23/e3sconf_vc2020_04003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Kharchenko Sergey
Belyaev Yury
spellingShingle Kharchenko Sergey
Belyaev Yury
Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya Tundra
E3S Web of Conferences
author_facet Kharchenko Sergey
Belyaev Yury
author_sort Kharchenko Sergey
title Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya Tundra
title_short Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya Tundra
title_full Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya Tundra
title_fullStr Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya Tundra
title_full_unstemmed Hydrographic and erosional dissection pattern as an indicator of landform type of the Malozemelskaya and Bolshezemelskaya Tundra
title_sort hydrographic and erosional dissection pattern as an indicator of landform type of the malozemelskaya and bolshezemelskaya tundra
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description The paper describes the methodology and presents the results of the calculation of the spectral characteristics of the terrain for the territory of the Bolshezemelskaya and Malozemelskaya Tundra (the north of the European part of Russia). There are nine terrain clusters, differing in the topographic dissection pattern. Their geomorphological interpretation is given. Three clusters characterize mountainous and coarsely hilly terrain with the depth of dissection from 150 m and more. The others are low and elevated terrains with much lower depths of dissection (up to 50 m) and different patterns of interposition of landforms.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/23/e3sconf_vc2020_04003.pdf
work_keys_str_mv AT kharchenkosergey hydrographicanderosionaldissectionpatternasanindicatoroflandformtypeofthemalozemelskayaandbolshezemelskayatundra
AT belyaevyury hydrographicanderosionaldissectionpatternasanindicatoroflandformtypeofthemalozemelskayaandbolshezemelskayatundra
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