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  • Článek nabízí základní informace o vývoji a reliéfu pramenné oblasti mazonky v peruánském pohoří Cordillera Chila. Z analýzy tvarů reliéfu vyplývá, že oblast se vyvíjí pod vlidvem intenzívních geomorfologických procesů, které odrážejí dynamiku orogenních procesů a klimatických podmínek. Pleistocénní klimatické změny jsopu zaznamenány v podobě glaciálních tvarů reliéfu, které byly ve studované oblasti přednostně zkoumány. Výsledky nasvědčují rozsáhlému zalednění, které v minulosti postoupilo za hranice studované oblasti. Na základě interpretace terénních a distančních dokladů lze usuzovat na velmi rychlý ústup ledovců ve druhé polovině 20. století. (cs)
  • Paper provides the initial insight into the development and specific features of the Amazon catchment area in the Cordillera Chila, Peru. The analysis suggests that the catchment area has undergone very intensive relief development, that continues presently. Numerous morphological processes that reflect orogenic dynamics as well as climatic conditions affect the relief development of this area. Pleistocene climatic variations are recorded in the glacial landforms, which were examined throughout the landscape. According to observations, the glaciation was much more extensive during the past time extending far beyond the catchment area. Interpretations suggest that glaciers in the catchment area experienced very rapid retreat in the second half of the 20th century.
  • Paper provides the initial insight into the development and specific features of the Amazon catchment area in the Cordillera Chila, Peru. The analysis suggests that the catchment area has undergone very intensive relief development, that continues presently. Numerous morphological processes that reflect orogenic dynamics as well as climatic conditions affect the relief development of this area. Pleistocene climatic variations are recorded in the glacial landforms, which were examined throughout the landscape. According to observations, the glaciation was much more extensive during the past time extending far beyond the catchment area. Interpretations suggest that glaciers in the catchment area experienced very rapid retreat in the second half of the 20th century. (en)
Title
  • Geomorfologie pramenné oblasti Amazonky v pohoří Cordillera Chila (cs)
  • Geomorphology of the Amazon source area in the Cordillera Chila
  • Geomorphology of the Amazon source area in the Cordillera Chila (en)
skos:prefLabel
  • Geomorfologie pramenné oblasti Amazonky v pohoří Cordillera Chila (cs)
  • Geomorphology of the Amazon source area in the Cordillera Chila
  • Geomorphology of the Amazon source area in the Cordillera Chila (en)
skos:notation
  • RIV/ENGEL___:_____/02:00012340!RIV/2005/MSM/700215/N
http://linked.open.../vavai/riv/strany
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  • RIV/ENGEL___:_____/02:00012340
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  • geomorphology;Amazon sources;Cordillera Chila;Peru (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [899F7B610BC0]
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  • 123
http://linked.open...iv/tvurceVysledku
  • Engel, Zbyněk
issn
  • 1211-1910
number of pages
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