Podrobnosti záznamu

Název
    Reconstruction of continental glaciation in the Oldřichov Highland: co-operation of geomorphology and other research methods
Další názvy
    Rekonstrukce kontinentálního zalednění Oldřichovské vrchoviny: spolupráce geomorfologie a jiných výzkumných metod
Autor
    Nývlt, Daniel
Jazyk
    anglicky
Typ dokumentu
    článek ve sborníku
Zdrojový dokument - monografie
    Geomorfologický sborník 2
Poznámky
    Akce: 2003 ; Nečtiny
Výraz tezauru
    glaciation, sedimentary petrology, glaciofluvial sediments, middle Pleistocene, Oldřichov Highland, northern Bohemia
Klíčové slovo
    Co-operation
    Continental
    Geomorphology
    Glaciation
    Highland
    Methods
    Oldřichov
    Other
    Reconstruction
    Research
Abstrakt (česky)
   The Elsterian continental glacier was checked in the course of its southern advance through the Frýdland Hilly Land by the barrier of the Jizera Mts. The ice sheet reached up to ~420-430 m a.s.l. in the northern foothills of the mountains. The only possibility for further penetration to the south was the upward movement through narrow valleys and crossing over the lowermost transfluence pass of the Oldřichov Col. The northern valley was filled to the altitude 430-460 m a.s.l. by the ice and due to the subsequent pushing of the advancing ice mass stood the ice sheet front up to the Oldřichov Col (478 m). The glacier lobe penetrated ~1800-2000 m beyond the col to the southern valley during its maximum advance, this corresponds approximately to the beginning of the accumulation of the sedimentary body of the Mníšek glaciofluvial sand and gravel. The maximum thickness of the ice in the northern valley did not exceed ~50-60 m, near the Oldřichov Col the ice thickness remained <10 m.
Abstrakt (anglicky)
   The Elsterian continental glacier was checked in the course of its southern advance through the Frýdland Hilly Land by the barrier of the Jizera Mts. The ice sheet reached up to ~420-430 m a.s.l. in the northern foothills of the mountains. The only possibility for further penetration to the south was the upward movement through narrow valleys and crossing over the lowermost transfluence pass of the Oldřichov Col. The northern valley was filled to the altitude 430-460 m a.s.l. by the ice and due to the subsequent pushing of the advancing ice mass stood the ice sheet front up to the Oldřichov Col (478 m). The glacier lobe penetrated ~1800-2000 m beyond the col to the southern valley during its maximum advance, this corresponds approximately to the beginning of the accumulation of the sedimentary body of the Mníšek glaciofluvial sand and gravel. The maximum thickness of the ice in the northern valley did not exceed ~50-60 m, near the Oldřichov Col the ice thickness remained <10 m.
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (RIV)
Zdrojový formát
    R
Datum importu
    15. 10. 2014