作者: Gianna Ayala , Charly French
DOI: 10.1002/GEA.20041
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摘要: The chronology and pattern of Holocene landscape development in the Nebrodi Mountains north-central Sicily, seen valley alluviation pedological record, has been investigated Fiume di Sotto Troina valley. Intensive geomorphological survey revealed three phases alluvial aggradation reflecting increased hillslope disturbance during late Pleistocene Holocene. results sediment analyses, archaeological survey, literary evidence were combined a Geographical Information System (GIS) order to model potential erosion caused by different land-use practices throughout history. This paper presents used investigate possible Roman their effects on change as documented catchment basin. support correlation between intensive pastoralism erosional sedimentary record. © 2005 Wiley Periodicals, Inc.