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Stratified Slope-Waste Deposits in the Esino River Basin, Umbria-Marche Apennines, Central Italy [PDF]
, 1983 Coltorti, M., Dramis, F., Pambianchi, G.
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A new approach for landform classification based on geomorphic entity objects: a case study on the Tibetan Plateau. [PDF]
Sci RepWei H +5 more
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Range Dynamics of the Moss <i>Pohlia cruda</i> in Italy Under Different Climate Change Scenarios. [PDF]
Plants (Basel)Bacilliere G +3 more
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Do periglacial landscapes evolve under periglacial conditions?
Geomorphology, 2003Polar and alpine periglacial areas are traditionally regarded as necessarily submitted to very efficient frost-driven processes that control the Holocene and ongoing geomorphic activity. During the last decade, the validity of this academic view has been increasingly questioned among the international scientific community.
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Philosophical Transactions of the Royal Society of London. B, Biological Sciences, 1977
During the colder parts of the Last Gold Stage at some times there were large ice masses, and at others there were periglacial conditions apparently without ice masses. It is a matter of doubt whether ice masses did form early in the Gold Stage, or whether periglacial conditions were dominant for the greater part of the stage, with ice only appearing ...
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During the colder parts of the Last Gold Stage at some times there were large ice masses, and at others there were periglacial conditions apparently without ice masses. It is a matter of doubt whether ice masses did form early in the Gold Stage, or whether periglacial conditions were dominant for the greater part of the stage, with ice only appearing ...
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2005
Many present landscape elements in western and central Europe are to a large extent the result of periglacial processes that prevailed during cold periods more than 10,000 years ago. As with the glacial chapter, this account of the periglacial geomorphology also needs to base itself upon processes that no longer or only to a limited extent take place ...
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Many present landscape elements in western and central Europe are to a large extent the result of periglacial processes that prevailed during cold periods more than 10,000 years ago. As with the glacial chapter, this account of the periglacial geomorphology also needs to base itself upon processes that no longer or only to a limited extent take place ...
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