Rock glaciers in the Western and High Tatra Mountains, Western Carpathians

被引:15
|
作者
Uxa, Tomas [1 ,2 ]
Mida, Peter [1 ]
机构
[1] Charles Univ Prague, Dept Phys Geog & Geoecol, Fac Sci, Albertov 6, Prague 12843 2, Czech Republic
[2] Acad Sci Czech Republ, Inst Geophys, Dept Geotherm, Bocni 2 1401, Prague 14131 4, Czech Republic
来源
JOURNAL OF MAPS | 2017年 / 13卷 / 02期
关键词
Rock glaciers; inventory; Western and High Tatra Mts; Carpathians; Slovakia; Poland; PRONIVAL RAMPARTS; REGIONAL INVENTORY; PROTALUS RAMPARTS; EASTERN; PALEOCLIMATE; PERMAFROST; CLIMATE; VALLEY; ENVIRONMENT; CHRONOLOGY;
D O I
10.1080/17445647.2017.1378136
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
A detailed map of rock glaciers at a scale of 1 : 40 000 is produced for the Western and High Tatra Mts., Western Carpathians, based on remotely sensed mapping. We inventoried a total of 383 rock glaciers, covering a total area of 13.84km(2). Most rock glaciers (85%) are considered relict (without permafrost). These landforms have an average lower limit of 1684 m asl and occupy a total area of 12.50km(2). In contrast, intact rock glaciers (containing permafrost) cover a total area of 1.34km(2) and their average lower limit is located at 1986m asl, which is 56 m above the previously suggested lower limit of discontinuous permafrost. The inventory adds new information about rock-glacier occurrence in the European high-mountain areas and improves the understanding of present and past environmental conditions in the region.
引用
收藏
页码:844 / 857
页数:14
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