Two different modes of the origin of Pleistocene pediments: an example from the Central Moravian Carpathians, Czech Republic

Czudek, Tadeáš

doi:10.7163/GPol.2011.S1.2

Pobierz

Tytuł: Two different modes of the origin of Pleistocene pediments: an example from the Central Moravian Carpathians, Czech Republic

Bibliografia:

1. Bubík, M. and Švábenická, L. (2000), Nové poznatky o ždánické jednotce na listu 34–221 Kyjov získané během sezony 1999 [New informations on the Ždánice Unit on the map sheet 34–221 Kyjov obtained during field season 1999], Zprávy o geologických výzkumech v roce 1999: 10–12.
2. Beck, N. (1994), Reliefentwicklung im nördlichen Rheinhessen unter besonderer Berücksichtigung der periglazialen Glacis- Pedimentbildung [Development of the relief in northern Rheinhessen with special regard to periglacial glacis and pediment development], Forschungen zur Deutschen Landeskunde, 237: 1–175.
3. Brunotte, E. and Garleff, K. (1989), Structural landforms and planation surfaces in southern Lower Saxony, Catena Suppl., 15: 151–164.
4. Büdel, J. (1977), Klima–Geomorphologie. Gebrüder Borntraeger.
5. Czudek, T. (1988), Kryopedimente – wichtige Reliefformen der rezenten und pleistozänen Permafrostgebiete [Cryopediments – important relief forms in contemporary and Pleistocene permafrost environments], Petermanns Geographische Mitteilungen, 132: 161–173.
6. Czudek, T. (2005), Vývoj reliéfu krajiny České republiky v kvartéru [Quaternary development of landscape relief of the Czech Republic], Moravské zemské muzeum.
7. Czudek, T. (2008), Kryopediment v údolí Litavy východně od Bučovic, Středomoravské Karpaty [Cryopediment in the Litava River valley east of Bučovice, Central Moravian Carpathians], Geologické výzkumy na Moravě a ve Slezsku, 15: 8–12.
8. Czudek, T. and Demek, J. (1970), Pleistocene cryopediments in Czechoslovakia, Acta Geographica Lodziensia, 24: 101–108.
9. Dylik, J. (1957), Próba porównania powierzchni zrównań w warunkach półsuchych klimatów gorących i zimnych [Tentative comparison of planation surfaces occuring under warm and under semi-arid climate conditions], Biuletyn Peryglacjalny, 5: 37–49.
10. French, H.M. (2007), The periglacial environment, 3rd Edition, John Wiley & Sons, Ltd.
http://dx.doi.org/10.1002/9781118684931 -
11. French, H.M. and Harry, D.G. (1992), Pediments and cold-climate conditions, Barn Mountains, unglaciated Northern Yukon, Canada, Geografiska Annaler, 74 A: 154–157.
12. Rotnicki, K. (1974), Slope development of Riss Glaciation end moraines during the Würm, its morphological and geological consequences, Quaestiones Geographicae, 1: 109–139.
13. Vandenberghe, J. and Czudek, T. (2008), Pleistocene cryopediments on variable terrain, Permafrost and Periglacial Processes, 19: 71–83.
http://dx.doi.org/10.1002/ppp.605 -
14. Zeman, A., Havlíček, P., Minaříková, D., Růžička, M. and Fejfar, O. (1980), Kvartérní sedimenty střední Moravy [Quaternary sediments in central Moravia], Anthropozoikum, 13: 37–91.