Podrobnosti záznamu

Název
    The Sudetic tributaries of Upper Odra transformation during the Holocene period
Údaj o odpovědnosti
    Kazimierz Klimek
Další názvy
    Landform Evolution in European Mountains (Variant.)
    Tranformacja sudeckich doplywów górnej Odry w holocenie
Autor
    Klimek, Kazimierz
Jazyk
    anglicky
Zdrojový dokument - seriál
    Studia geomorphologica carpatho-balcanica
Svazek/č.
    Vol. 34
Strany
    p. 27-45
Rok
    2000
Poznámky
    8 obr., 8 fot., 21 bibl.
    il.
    res. pol.
    Zkr. název ser.: Stud. geomorphol. carpatho-balcanica
Předmětová skupina
    holocén
    hydrologie
    koryto
    kvartér oblastí kontinentálního zalednění Českého masivu
    lidské aktivity
    morfologie fluviální
    paleolimnologie
    periglaciální jevy
    povodeň
    řeka
    spád řeky
Geografické jméno
    ČR-Morava
    Krnov (Bruntál)
    Opava
    Osoblaha (Bruntál)
    Polsko - jihozápad
Klíčové slovo
    During
    Holocene
    Odra
    Period
    Sudetic
    Transformation
    Tributaries
    Upper
Abstrakt (anglicky)
   In the border zone of the Eastern Sudety Mts. (800-1,400 m a.s.l.)and their northeasters foreland (200-300 m a.s.l.), there is a clear change in relief of the alluvial plains as well as a change ins tructure and grain size of their associated sediments. Within the Eastern Sudety Mts, Holocene transformation of valley was predominantly influenced by climate changes. It was mainly associated with valley floor widening which were inherited from past climatic events. In the mountains foreland, Holocene transformation of valleys caused by climatic changes started at the end of Vistulian. The development of agriculture and progress in settlement, which started in the older Bronze Age, has considerably influenced the valley floors transformation during the last two millenniums.
   This caused large sedimentation of fine-grained alluvia (mainly overbank deposits)which originated from washing-out of slope mantles in the mountain part of the drainage basins and from the soils erosion in the foreland of the mountainsIn the border zone of the Eastern Sudety Mts. (800-1,400 m a.s.l.)and their northeasters foreland (200-300 m a.s.l.), there is a clear change in relief of the alluvial plains as well as a change ins tructure and grain size of their associated sediments. Within the Eastern Sudety Mts, Holocene transformation of valley was predominantly influenced by climate changes. It was mainly associated with valley floor widening which were inherited from past climatic events. In the mountains foreland, Holocene transformation of valleys caused by climatic changes started at the end of Vistulian.
   The development of agriculture and progress in settlement, which started in the older Bronze Age, has considerably influenced the valley floors transformation during the last two millenniums. This caused large sedimentation of fine-grained alluvia (mainly overbank deposits)which originated from washing-out of slope mantles in the mountain part of the drainage basins and from the soils erosion in the foreland of the mountainsIn the border zone of the Eastern Sudety Mts. (800-1,400 m a.s.l.)and their northeasters foreland (200-300 m a.s.l.), there is a clear change in relief of the alluvial plains as well as a change ins tructure and grain size of their associated sediments. Within the Eastern Sudety Mts, Holocene transformation of valley was predominantly influenced by climate changes. It was mainly associated with valley floor widening which were inherited from past climatic events.
   In the mountains foreland, Holocene transformation of valleys caused by climatic changes started at the end of Vistulian. The development of agriculture and progress in settlement, which started in the older Bronze Age, has considerably influenced the valley floors transformation during the last two millenniums. This caused large sedimentation of fine-grained alluvia (mainly overbank deposits)which originated from washing-out of slope mantles in the mountain part of the dra
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    20. 8. 2007
Datum importu
    8. 8. 2012