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The extent of Pleistocene glaciations in the western part of the Campo Imperatore (Gran Sasso Massif, Central Italy)

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Języki publikacji
EN
Abstrakty
EN
The Campo Imperatore is a virtually undrained tectonic depression located in the inner part of the Gran Sasso Massif, the highest relief within the Apennines (2,912 m a.s.l. at Corno Grande). This paper reports some major géomorphologie features of the western part of this depression, which   represents a specific and very fine example of glaciated mountain landscape, where landforms typical of glacial erosion are commonplace over l ,800 m a.s.l. Most of the glacial cirques are characterized by karstified bedrock topography, in places covered with thin drift deposits. Distinct recessional moraines are also present at various altitudes (i.e. around 2,250; 2,180; 2,000 and 1,740 m a.s.l). However, the most typical landforms on the floor of the main depression are those due to glacial deposition. There, at altitudes ranging around 1,640—1,590 m a.s.l., stagnant ice déglaciation patterns dominate in the form of a wide lobate moraine system which rises 25—30 m above an outwash plain covered by glaciofluvial, lacustrine and alluvial deposits. Within the latter, small (less than 10 m high) hills, comprising glacial drift, protrude from the flat valley floor. The remnants of these strongly degraded, transformed and laterally-eroded moraines denote the maximum extent of an older glaciation, some 1.5 km remote from the main system.
Czasopismo
Rocznik
Tom
Strony
37--43
Opis fizyczny
Bibliogr. 34 poz., rys.
Twórcy
autor
  • Department of Earth Sciences, University of Camerino,via Gentile III da Varano, Camerino 1-62032, Italy
autor
  • Department of Earth Sciences, University of Camerino,via Gentile III da Varano, Camerino 1-62032, Italy
autor
  • Department of Earth Sciences, University "La Sapienza", p. A. Mora, 1-001, Rome, Italy 
autor
  • Department of Geological Sciences, Third University of Rome, Largo San Leonardo Murialdo 1, 1-00146 Romejtaly
autor
  • Department of Geomorphology and Hydrology, Polish Academy of Sciences, ul. sw. Jana 22, P-31018 Krakow, Poland
Bibliografia
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-daf47d28-d014-489a-940c-35210b976616
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