Greater Caucasus

Hidden Ice of the Greater Caucasus

Levan Tielidze June 30, 2023

Figure 1 . The prominent rock glacier in the headwater of the Juta River valley, Kazbegi region, Georgian Caucasus, visited by thousands of tourists each year. [Credit: Levan Tielidze].

In this week’s blog, Levan Tielidze tells us about the first inventory of rock glaciers from the Greater Caucasus as an important basis for further research of geomorphology and palaeoglaciology in this region. What are Rock Glaciers? Rock glaciers are distinctive geomorphological landforms of frozen debris that are supersaturated with ice. The low ice velocity or certain speed of movement and per ...[Read More]

Massive melting of Caucasus glaciers

Levan Tielidze March 18, 2022

Ice-snow covered Mt. Kazbegi (5047 m above sea level), one of the tourist attractions of the Greater Caucasus region. Photo was taken from Village of Sno in Georgia. Photo Credit: Levan Tielidze

The Caucasus is one of the most studied glacierized regions in the world (see previous Cryoblogs on Caucasus glaciers here and here). In this week’s blog, Levan Tielidze tells us about the health of the Greater Caucasus glaciers. His first study published this year indicates that the rate of decline in glacier extent between 2000 and 2020 in the Greater Caucasus is four times higher than it was be ...[Read More]

Time & space of glaciers

Alexandra Rogozhina February 25, 2022

Ice fall in Azay glacier in the beginning of XX century [Credits: Alexandra Rogozhina & IGRAS/RGO]

People usually perceive space and time, comparing them to their own life Words such as “forever” and “until the end” appear in fiction But how can we imagine the space and time of the mountain glaciers whose existence goes beyond our usual perception? And why is it so important for us now? With this post, researcher Alexandra Rogozhina shares her thoughts on these suggestive topics. Mostly, ...[Read More]

Climate Change & Cryosphere – How the Chalaati Glacier (Georgian Caucasus) changed since the Little Ice Age

Levan Tielidze September 4, 2020

Chalaati Glacier is one of the largest glaciers in the Greater Caucasus and has undergone expansive mass loss. In this week’s blog post, Levan Tielidze tells us about Chalaati Glacier variations in the past centuries. His recent study was conducted based on surface exposure dating technique, dendrochronology (tree ring analysis), lichenometry, and satellite imagery. They found out that the Chalaat ...[Read More]

Does debris cover offset glacier retreat in the Greater Caucasus?

Levan Tielidze April 3, 2020

Figure 1: Supra-glacial debris cover (SDC) change on the Elbrus Massif from 1986 to 2014. A SPOT-7 image is used as the background. Blue shows retreat of clean-ice parts. Clean ice in 1986 consists of the clean ice in 2014 (grey, transparent) plus clean-ice area that retreated between 1986 and 2014 (dark blue). Credit: Tielidze et al., 2020

In this week’s blog, Levan Tielidze tells us about supra-glacial debris cover change for the Greater Caucasus. His recent study indicates more than a doubling in the area of supra-glacial debris cover for the Elbrus Massif‘s glaciers from 1986 to 2014, the largest glacierized massif in the whole region. Glaciers on the western slope of the Elbrus Massif are affected by avalanches and thus ar ...[Read More]

Climate Change & Cryosphere – Caucasus Glaciers Receding

Levan Tielidze June 7, 2019

Fig. 1: Tviberi Glacier in 1884 (left) and 2011 (right) [Credit: Fig. 2d and 2e in Tielidze, 2016]

The Tviberi Glacier valley is located in the Svaneti Region – a historic province of the Georgian Caucasus. Between 1884 and 2011, climate change has led to a dramatic retreat of the ice in this valley. Other glaciers in the Greater Caucasus evolved in a similar way in past decades. We investigated glaciers and their changes both in-situ and with remote sensing techniques in the 53 river bas ...[Read More]