Titlebook: Geomorphological Hazards in High Mountain Areas; Jan Kalvoda,Charles L. Rosenfeld Book 1998 Springer Science+Business Media Dordrecht 1998

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0924-5499 al and hazards are inferred from the development of landscape during the Quaternary. The history of glaciers can be seen as of central importance for this. The Ice Age glacial erosion created V-shaped valleys, which with their steep flanks - as a consequence of the interglacial formation of V -valle

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Samarendra Basu,James R. Millettetion on these processes from both the Nanga Parbat region as well as from Hunza where collateral data have been collected (Figure 1). In this paper we differentiate floods from within glaciers, floods from behind glacier dams, floods from behind slope failure dams, and debris-flow floods induced by torrential rains.

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Comparison with Other Spectroscopies,ts supplying the expanding middle class, has become a third agricultural pressure on the highlands of equatorial regions. Yet, although of such importance, farming in upland-steepland is said to be a neglected sector in Asian agriculture (.).

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https://doi.org/10.1007/978-3-030-39668-8ls from the surfaces covering the more resistant volcanics. The stream channels impacted by this debris quickly winnow away the fines, leaving behind gravels and large organic debris, the materials which form the gravel spawning beds and rearing pools for the region’s anadromous fish.

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Impact of Conversion of Upland Forest to Tourism and Agricultural Land Uses in the Gunung Kinabalu ts supplying the expanding middle class, has become a third agricultural pressure on the highlands of equatorial regions. Yet, although of such importance, farming in upland-steepland is said to be a neglected sector in Asian agriculture (.).

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https://doi.org/10.1007/b115596located on the eastern edge of the Belt (19°01′N(xiāo), 97°16′W) (Fig.1). They are the two highest strato-volcanoes in Mexico and the only ones that are active and have glaciers on their slopes. These characteristics make them a high risk area for lahar formation and other geomorphologie processes, so it is very important that the glaciers be monitored.