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VARIATION IN SURFACE ELEVATION OF THE NISQUALLY GLACIER MT. RAINIER, WASHINGTON

 

作者: Arthur JOHNSON,  

 

期刊: International Association of Scientific Hydrology. Bulletin  (Taylor Available online 1960)
卷期: Volume 5, issue 3  

页码: 54-60

 

ISSN:0020-6024

 

年代: 1960

 

DOI:10.1080/02626666009493180

 

出版商: Taylor & Francis Group

 

数据来源: Taylor

 

摘要:

Variation in surface elevations of the Nisqually Glacier has been recorded since 1942 by the annual measurement of three profiles across the glacier, designated as nos. 1, 2, and 3, located 0.5, 1.0, and 1.7 miles respectively from the terminus, at approximate mean elevations of 5,250,6,000, and 6,800 feet. A fourth profile, 2-A, located 1.4 miles from the terminus at an approximate mean elevation of 6,450 was measured from 1948 to 1954. These profiles cross the glacier approximately normal to the direction of flow. Additional data are available from measurements made at profiles no. 1 and no. 2 in 1931, 1932 and 1941. The results of these measurements show that a wave or surge has been moving down the glacier.

 

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