کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
1044172 1484284 2008 11 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Pleistocene glacial relief of the central part of Mt. Prokletije (Albanian Alps)
کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات زمین شناسی
پیش نمایش صفحه اول مقاله
Pleistocene glacial relief of the central part of Mt. Prokletije (Albanian Alps)
چکیده انگلیسی

The central and highest area of Mt. Prokletije (Albanian Alps) is situated in northern Albania and eastern Montenegro (at 42°30′N). The highest peak is Maja e Jezerces (2694 m). Detailed geomorphological mapping was used to reconstruct the positions of former glaciers. The longest Ropojana glacier had a length of 12.5 km and surface of 20 km2; others include Valbona Glacier (9.5 km, 10.5 km2), Grbaja Glacier (5 km, 6.7 km2) and Bogićevica Glacier (6 km, 6.9 km2). Three series of moraines can be distinguished: the lowest at an average altitude of 990 m (average ELA 1750 m), the middle series at 1350 m (ELA 1942 m), and the highest at 1900 m (ELA 2123 m). As no advanced dating methods have yet been used to provide a numerical chronological framework for these features, hypotheses are made based on the comparison with the advanced studies of other similar mountains in the Mediterranean region. The moraines of the first stage (lowest series) correspond to one of pre-LGM glaciations (Middle or even Early Würmian), the second stage moraines probably correspond to LGM, and the third stage could be attributed to Younger Dryas. The mapping included a number of inactive and active rock glaciers, as well as three small active glaciers (surface 5 ha and less), at 1980–2100 m altitude, in the area close to Maja e Jezerces.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Quaternary International - Volume 190, Issue 1, 1 November 2008, Pages 112–122
نویسندگان
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