Pleistocenní permafrost na území Československa

Rok, strany: 1986, 245 - 252

The paper discusses indicators for the presence of Pleistocene permafrost in Czechoslovakia, Permafrost existed as early as the Early Pleistocene prior to the Brunhes-Matuyama boundary. An attempt has been made to calculate its thickness at the basis of Computer technique In the Upper Pleniglacial. This thickness varied from approximately 50 m to app. 250 m and, in some places, up to 400 m (Tatra Mts.). In some summit parts of the Tatra Mts. permafrost can be assumed to exist even in the present time.

ISO 690:

Czudek, T. 1986. Pleistocenní permafrost na území Československa. In Geografický časopis, vol. 38, no.2-3, pp. 245-252. 0016-7193.

APA:

Czudek, T. (1986). Pleistocenní permafrost na území Československa. Geografický časopis, 38(2-3), 245-252. 0016-7193.

Vydavateľ: Geografický ústav SAV/Institute of Geography of the Slovak Academy of Sciences