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КАМЕННЫЕ ГЛЕТЧЕРЫ КОЛЫМСКОГО НАГОРЬЯ
https://doi.org/10.15356/2076-6734-2012-2-106-114
Аннотация
На основе дистанционного картографирования и полевых исследований в хребтах Больших Порогов, Туманском, Хасынском, Дел-Урэчэн, а также в Дукчинском и Килганском горных массивах установлено около 1160 образований, морфологически сходных с каменными глетчерами или развивающихся в тесной ассоциации с ними. Кроме каровых каменных глетчеров абляционного происхождения обнаружено большое число присклоновых лопастевидных образований, формирующихся в пределах контрастного неотектонического рельефа в зонах тектонического бедленда и в ассоциации с сейсмогенерирующими разломами. Использование комплекса региональных данных по тефрахронологии, лихенометрии, пыльцевым спектрам и радиоуглеродным датировкам позволяет предварительно отнести большинство активных каменных глетчеров к позднему голоцену.
Список литературы
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Дополнительные файлы
Для цитирования: Галанин А.А. КАМЕННЫЕ ГЛЕТЧЕРЫ КОЛЫМСКОГО НАГОРЬЯ. Лёд и Снег. 2012;52(2):106-114. https://doi.org/10.15356/2076-6734-2012-2-106-114
For citation: Galanin A.A. ROCK GLACIERS IN THE KOLYMA HIGHLAND. Ice and Snow. 2012;52(2):106-114. https://doi.org/10.15356/2076-6734-2012-2-106-114
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ISSN 2076-6734 (Print)
ISSN 2412-3765 (Online)