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within the tested area. The inventory was not an exhaustive list of all the slope instabilities in<br />

the area, but an inventory of all areas showing any kind of signal on ERS-SAR interferograms,<br />

that can be interpreted as a possible slope movement.<br />

The resulting inventory of ERS-InSAR-detected instabilities can be seen as a preliminary<br />

tool compiled at regional scale which can be useful for further investigations to be carried out<br />

(if required) at local scale. It appears to be an attractive perspective both for early natural hazard<br />

management and process understanding of slope movement in permafrost areas.<br />

Keywords: SAR interferometry, permafrost, slope instabilities, rock glacier<br />

106<br />

Active Lag Block Streams in the Chinese Tian Shan<br />

Stuart A. Harris, Guodong Cheng, Cui Zhijiu<br />

(1.Department of Geography, University of Calgary, T2N 1E4, Canada;<br />

2.Cold and Arid Regions Environmental and Engineering Research Institute, Lahnzou, China,<br />

730000; 3. Department of Geography, Peking University, Beijing, China.)<br />

Abstract: Active lag block streams are forming today in the mountains of the Chinese Tian<br />

Shan above treeline near cold-based glaciers. Mean annual air temperatures are below –5.4°C<br />

while the mean annual precipitation exceeds 420mm. This paper describes the three main<br />

types of situation in which they occur (drainage from a hanging valley, gullies on a steeply<br />

sloping valley wall, and in front of an end moraine), together with their characteristics.<br />

Conditions favoring their formation include continuous permafrost, sediments with abundant<br />

large blocks, incipient sorted patterned ground, a discontinuous vegetation cover, steep slopes,<br />

high precipitation and a fairly thick winter snow cover. Once started, washing out of the finer<br />

interstitial material leaving behind the blocks will occur with every spring snow melt and heavy<br />

precipitation event. These results are important since they appear to provide the first<br />

description of active lag block streams being formed. Lag block streams are rather common in<br />

many parts of the world, but their conditions of formation have been the subject of considerable<br />

debate in the absence of any known modern analogues.<br />

Key words: Active lag block streams, Tian Shan, continuous permafrost, sorted patterned<br />

ground, end moraines, permafrost hydrology.<br />

Exposed glacial and debris-covered ice in the Hindu Kush, Afghanistan.<br />

Umesh Haritashya, John Shroder, Michael Bishop, Henry Bulley, Jeffrey Olsenholler<br />

GLIMS (Global Land Ice Measurements from Space) Regional Center for Southwest Asia (Afghanistan and<br />

Pakistan), Department of Geography and Geology, University of Nebraska at Omaha, Omaha, NE 68182<br />

USA<br />

Abstract:Snow, glacier ice, and debris-covered glacial and ground ice in Afghanistan are

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