Glaciers of Avacha group of volcanoes in Neoholocene

• Published in: Ice and Snow
• Main Authors: T. Manevich M., S. Samoilenko B., Т. Маневич М., С. Самойленко Б.
• Format: Article in Journal/Newspaper
• Language: Russian
• Published: IGRAS 2016
• Subjects: Avacha group volcanoes;glacier dynamics;lichenometry;Little Ice Age;moraine; Авачинская группа вулканов;динамика ледников;лихенометрия;малый ледниковый период;морена; Avacha; Arctic; Arctic and Alpine Research; КАМЧАТК*
• Online Access: https://ice-snow.igras.ru/jour/article/view/327; https://doi.org/10.15356/2076-6734-2016-3-399-412

The study of moraines at the Avacha volcano group revealed that glaciers changes at all volcanoes within the group happened almost synchronously. Glacial deposits could be grouped into three generations, corresponding to three periods of glacier fluctuations in Neoholocene. The largest glaciation within the group occurred ~2000 years ago. Fragments of moraine, corresponding to that period were found only in the moraine complex of the Ditmar Glacier which was 15% larger then today at that time. The most of moraines at the Avacha volcano group were formed during the Little Ice Age, which in the studied region continued up to the first decades of XX centuries. The maximal advance of glaciers probably happened in XVII century. The moraine corresponding to that period was found at the Kozelsky Glacier valley. At present time the total area of glaciers which moraines were described and dated approaches 21.46 km2. The area of reconstructed moraines corresponding to the Little Ice Age is estimated to be 2.79 km2, therefore at that period the total glaciation area reaches 24,25 км2 exceeding the present area by 13%. It could be claimed that in general during the time past the Little Ice Age the glaciation nature and glacier types did not change sufficiently. The rate of glacier degradation at various parts of the group is different and depends mainly on exposition. At the valleys of four glaciers we found moraines formed in the middle of XX century. They may appear in 1941–1952 when the unfavorable weather conditions leaded to stable negative anomalies in accumulation have happened. Представлена реконструкция колебаний ледников Авачинской группы вулканов в позднем голоцене по результатам изучения моренных комплексов. Выделены и описаны три генерации морен, формирование которых произо- шло около 2000 л.н., в эпоху малого ледникового периода – с середины XVII до начала XX в. и в середине XX в.