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glacier
The current climatic, average glacier snow-line in the research area runs about 5500 m asl.
      
Preliminary results on hydrological and hydrochemical features of Kartamak Glacier area in Mt.
      
The variations of the meltwater runoff draining from Kartamak Glacier in Mt.
      
Critical approach to methods of glacier reconstruction in high Asia and discussion of the probability of a Qinghai-Xizang (Tibet
      
This overview discusses old and new results as to the controversy on the past glacier extension in High Asia, which has been debated for 35 years now.
      
The Kvíárj?kull, a southern outlet glacier of the Vatnaj?kull, is confined in the mountain foreland by lateral moraines measuring a height of up to 150 m.
      
A historic-genetic model of the formation of the lateral moraines is presented considering the breaches in the lateral moraines as result from glacier bifurcations and therefore as former tributary tongue basins.
      
Such breaches in the lateral moraines are also common landscape features at glaciers outside of Iceland and are from wider importance for the paleoreconstruction of former glacier stages.
      
In 2005, an automatic weather station was operated at the East Rongbuk glacier Col of Mt.
      
A GIS-based glacier inventory for the Antarctic Peninsula and the South Shetland Islands -A first case study on King George Isla
      
The aim of the international project "Global Land Ice Measurements from Space (GLIMS)" headed by the US Geological Survey is to establish a world wide glacier inventory based on satellite imagery.
      
This data set will form a first digital baseline study for future glacier monitoring.
      
The presented GIS-based glacier inventory for King George Island is a case study for the area of the Antarctic Peninsula.
      
In the database of the glacier inventory topographic information, specific glaciological parameters as well as metadata will be included.
      
Glaciological data sets should comprise information on glacier retreat in different periods, glacier velocities, ice thickness and bedrock topography as well as derived parameters.
      
Finally, better access to historic aerial photography would enable a continuous record of glacier retreat from the beginning of the 1950's onward.
      
Sympatric Anadromous-Resident Pairs of Threespine Stickleback Species in Young Lakes and Streams at Bering Glacier, Alaska
      
We discovered such pairs in four lakes and four streams, including recently deglaciated terrain, near the Bering Glacier, Alaska.
      
Bering Glacier surges are accompanied and ended by massive glacial outburst floods, which create unmatched dynamics in the surrounding lakes and streams.
      
The glacier takes centuries to reach the sea and the lightning stroke zig-zags to earth faster than the eye can see.
      
 

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