Components of the natural environment

Western Sørkapp Land geological structure is very varied.Pre-Quaternary bedrock consists of three complexes: (1) the most extensive rocksfrom the Middle Proterozoic to the Silurian, folded in the Caledonian Orogeny:dolomites, phyllites, schists, quartzites, limestones, sandstones, breccias, and othe...

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Main Authors: Ziaja, Wiesław, Węgrzyn, Michał, Lisowska, Maja, Olech, Maria, Osyczka, Piotr
Format: Book Part
Language:English
Published: Springer 2016
Subjects:
Online Access:http://ruj.uj.edu.pl/xmlui/handle/item/19417
https://doi.org/10.1007/978-3-319-26574-2_3
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spelling ftjagiellonuniir:oai:ruj.uj.edu.pl:item/19417 2024-06-23T07:49:55+00:00 Components of the natural environment Ziaja, Wiesław Węgrzyn, Michał Lisowska, Maja Olech, Maria Osyczka, Piotr 2016 http://ruj.uj.edu.pl/xmlui/handle/item/19417 https://doi.org/10.1007/978-3-319-26574-2_3 eng eng Springer Transformation of the natural environment in Western Sørkapp Land (Spitsbergen) since the 1980s, Ziaja Wiesław, s. 19-33 978-3-319-26572-8 978-3-319-26574-2 doi:10.1007/978-3-319-26574-2_3 http://ruj.uj.edu.pl/xmlui/handle/item/19417 bedrock climate glaciation landforms waters vegetation artykuł (rozdział w książce) 2016 ftjagiellonuniir https://doi.org/10.1007/978-3-319-26574-2_3 2024-06-12T23:50:31Z Western Sørkapp Land geological structure is very varied.Pre-Quaternary bedrock consists of three complexes: (1) the most extensive rocksfrom the Middle Proterozoic to the Silurian, folded in the Caledonian Orogeny:dolomites, phyllites, schists, quartzites, limestones, sandstones, breccias, and others;(2) Early Carboniferous clastic sediments: sandstones, including quartzitic sand-stones, siltstones, and shales; and (3) Triassic sedimentary rocks: sandstones andconglomerates. None of these complexes lies horizontally. Loose Quaternarydeposits (marine, glacial,fluvial, organic, frost-weathering, slope, including talusand solifluction) are not continuous. The climate is Arctic and marine-type. Averageannual temperatures vary from−9to−3°C there. Average annual precipitationtotals reach 300–500 mm. The mountains in northwest Sørkapp Land remain free ofglaciers due to their exposure to relatively warm and dry eastern foehn winds. All thelowlands are unglaciated too. Sørkapp Land glaciation is clearly Arctic-type for tworeasons: the common presence of permafrost, and the very weak influence of altitudeon the distribution and extent of glaciers. The principal landform types in westernSørkapp Land are coastal lowlands, mountains, and mountain valleys. Nonglacialrivers and lakes (supplied directly by atmospheric precipitation and an active layer ofpermafrost) play an important part. There are also karst springs and glacial rivers andlakes in the northeast and southeast of the study area. Typically for the High Arctic,theflora of western Sørkapp Land is dominated by cryptogams, mainly lichens—about 170 species—whereas vascular plantflora includes 82 species. Differentvegetation types often create complex mosaics, following diverse habitat conditions(bedrock, terrain relief, hydrology, etc.). In a few places the presence of seabirdcolonies has a local but strong impact on the vegetation. Book Part Arctic permafrost Sørkapp Land Jagiellonian University Repository Arctic Sørkapp Land ENVELOPE(16.523,16.523,76.801,76.801) 19 33
institution Open Polar
collection Jagiellonian University Repository
op_collection_id ftjagiellonuniir
language English
topic bedrock
climate
glaciation
landforms
waters
vegetation
spellingShingle bedrock
climate
glaciation
landforms
waters
vegetation
Ziaja, Wiesław
Węgrzyn, Michał
Lisowska, Maja
Olech, Maria
Osyczka, Piotr
Components of the natural environment
topic_facet bedrock
climate
glaciation
landforms
waters
vegetation
description Western Sørkapp Land geological structure is very varied.Pre-Quaternary bedrock consists of three complexes: (1) the most extensive rocksfrom the Middle Proterozoic to the Silurian, folded in the Caledonian Orogeny:dolomites, phyllites, schists, quartzites, limestones, sandstones, breccias, and others;(2) Early Carboniferous clastic sediments: sandstones, including quartzitic sand-stones, siltstones, and shales; and (3) Triassic sedimentary rocks: sandstones andconglomerates. None of these complexes lies horizontally. Loose Quaternarydeposits (marine, glacial,fluvial, organic, frost-weathering, slope, including talusand solifluction) are not continuous. The climate is Arctic and marine-type. Averageannual temperatures vary from−9to−3°C there. Average annual precipitationtotals reach 300–500 mm. The mountains in northwest Sørkapp Land remain free ofglaciers due to their exposure to relatively warm and dry eastern foehn winds. All thelowlands are unglaciated too. Sørkapp Land glaciation is clearly Arctic-type for tworeasons: the common presence of permafrost, and the very weak influence of altitudeon the distribution and extent of glaciers. The principal landform types in westernSørkapp Land are coastal lowlands, mountains, and mountain valleys. Nonglacialrivers and lakes (supplied directly by atmospheric precipitation and an active layer ofpermafrost) play an important part. There are also karst springs and glacial rivers andlakes in the northeast and southeast of the study area. Typically for the High Arctic,theflora of western Sørkapp Land is dominated by cryptogams, mainly lichens—about 170 species—whereas vascular plantflora includes 82 species. Differentvegetation types often create complex mosaics, following diverse habitat conditions(bedrock, terrain relief, hydrology, etc.). In a few places the presence of seabirdcolonies has a local but strong impact on the vegetation.
format Book Part
author Ziaja, Wiesław
Węgrzyn, Michał
Lisowska, Maja
Olech, Maria
Osyczka, Piotr
author_facet Ziaja, Wiesław
Węgrzyn, Michał
Lisowska, Maja
Olech, Maria
Osyczka, Piotr
author_sort Ziaja, Wiesław
title Components of the natural environment
title_short Components of the natural environment
title_full Components of the natural environment
title_fullStr Components of the natural environment
title_full_unstemmed Components of the natural environment
title_sort components of the natural environment
publisher Springer
publishDate 2016
url http://ruj.uj.edu.pl/xmlui/handle/item/19417
https://doi.org/10.1007/978-3-319-26574-2_3
long_lat ENVELOPE(16.523,16.523,76.801,76.801)
geographic Arctic
Sørkapp Land
geographic_facet Arctic
Sørkapp Land
genre Arctic
permafrost
Sørkapp Land
genre_facet Arctic
permafrost
Sørkapp Land
op_relation Transformation of the natural environment in Western Sørkapp Land (Spitsbergen) since the 1980s, Ziaja Wiesław, s. 19-33
978-3-319-26572-8
978-3-319-26574-2
doi:10.1007/978-3-319-26574-2_3
http://ruj.uj.edu.pl/xmlui/handle/item/19417
op_doi https://doi.org/10.1007/978-3-319-26574-2_3
container_start_page 19
op_container_end_page 33
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