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• W3217102510 abstract "The timing of glaciation in the Balkans during the Late Pleistocene has only recently been established using terrestrial cosmogenic nuclide exposure dating. Previously, the evidence for the timing of these glacier advances and retreats came from indirect evidence, especially from downstream fluvial records. However, it was established more than 15 years ago that Late Pleistocene glaciers in Greece were much smaller than those of the Middle Pleistocene and similar observations followed a decade ago in Montenegro. Nevertheless, Late Pleistocene glaciers were important in shaping the landscape, especially in the highest mountains. Glaciers were most extensive during the early part of the Last Glacial Maximum (LGM) period (29–25 ka) and were retreating in the later part of this interval (25–19 ka). This shift was caused by increasing aridity and resulted in rock glacier formation in some mountain areas." @default.
• W3217102510 created "2021-12-06" @default.
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• W3217102510 date "2022-01-01" @default.
• W3217102510 modified "2023-10-16" @default.
• W3217102510 title "The Balkans: glacial landforms from the Last Glacial Maximum" @default.
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• W3217102510 doi "https://doi.org/10.1016/b978-0-12-823498-3.00058-3" @default.
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