Abstract
The Altai Mountains occupy the northwestern part of the Central Asian collision belt. The late-Holocene behavior of glaciers in the Altai Mountains was reconstructed for the Khaidun river valley in the western part of the Russian Altai. We report here 17 new radiocarbon datings from wood remains buried by moraines, from peat layers and lacustrine sediments. The glaciers’ advance took place in 2500–2200
Get full access to this article
View all access options for this article.
