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The study was focused on the alluvial fans formed in the bottom of the Bystra river valley. A detailed analysis of four fans allowed to distinguish several phases of gully erosion related to human activity. The gullies started to develop in the Neolithis times, the subsequent phases of gully erosion could be dated to: Bronze Age, Middle Ages. In modern times, most of the sediments have been retained within the extensive gully systems.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
205--208
Opis fizyczny
Bibliogr. 5 poz., rys.
Twórcy
autor
autor
autor
autor
autor
- Faculty of Earth Sciences and Spatial Management, Maria Curie-Sklodowska University in Lublin, Poland, jozef.superson@poczta.umcs.lublin.pl
Bibliografia
- Ballantyne C.K., 1991. Late Holocene erosion in upland Britain: climatic deforestation or human influence? The Holocene 1: 81–85.
- Chiverrell R.C., Harvey A.M. & Foster G.C., 2007.Hillslope gullying in the Solway Firth —Morecambe Bay region, Great Britain: responses to human impact and/or climatic deterioration? Geomorphology 84: 317–343.
- Kadrow S. & Zakościelna A., 2000. An outline of the evolution of Danubian Cultures in Małopolska and Western Ukraine. Baltic-Pontic Studies 9: 187–255.
- Nogaj-Chachaj J., 1991. The stone-packed graves of Funnel Beaker culture in Karmanowice, site 35.Antiquity 65, 248: 628–639.
- Rozwałka A., 1999. Sieć osadnicza w archidiakonacie lubelskim w średniowieczu. Studium archeologiczno-historyczne. Maria Curie-Skłodowska University Press, Lublin.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ5-0052-0014