<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Grosse, Guido</style></author><author><style face="normal" font="default" size="100%">Schirrmeister, L.</style></author><author><style face="normal" font="default" size="100%">Kunitsky, V.V.</style></author><author><style face="normal" font="default" size="100%">H.-W. Hubberten</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The use of CORONA images in remote sensing of periglacial geomorphology: an illustration from the NE Siberian coast</style></title><secondary-title><style face="normal" font="default" size="100%">Permafrost &amp; Periglacial Processes</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Remote sensing, thermokarst, GIS, Siberia, corona, dem, Bykovsky peninsula, Laptev Sea, permafrost, periglacial, geomorphology, patterned ground</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><urls><related-urls><url><style face="normal" font="default" size="100%">http://permafrost.gi.alaska.edu/sites/default/files/Grosse et al 2005 PPP.pdf</style></url></related-urls></urls><number><style face="normal" font="default" size="100%">2</style></number><volume><style face="normal" font="default" size="100%">16</style></volume><pages><style face="normal" font="default" size="100%">163-172</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">CORONA images have been used for the mapping of periglacial features on the Bykovsky Peninsula and adjacent Khorogor Valley in NE Siberia. Features, mapped and analyzed within a geographical information system include thermokarst depressions, thermo-erosional valleys, thermo-erosional cirques, thermokarst lakes, thermokarst lagoons and pingos. More than 50% of the area is strongly influenced by thermally-induced subsidence. Thermokarst in the area is probably less active today than in the early-middle Holocene.</style></abstract></record></records></xml>