Characteristics and Origins of the Debris and Ice, Matanuska Glacier, Alaska

• Published in: Journal of Glaciology
• Main Author: Lawson, D.E.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 1979
• Subjects: Earth-Surface Processes; glacier; Journal of Glaciology; Alaska
• Online Access: http://dx.doi.org/10.1017/s0022143000030252; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030252

Abstract The physical characteristics of the ice and debris of the Matanuska Glacier, Alaska (lat. 61 ° 47 ’ , long. 147 ° 45 ’ ) and their consistent variation in a vertical stratigraphic column of the glacier indicate multiple origins for both. The two zones of ice recognized in the glacier are the upper englacial zone, which comprises the bulk of the glacier (est. 300 m thick), and the thin (3 to 15 m thick) basal zone, which contains an estimated 97% of the sediment transported in the glacier. The physical characteristics of the ice and the quantity and mode of distribution of debris in it define two ice facies in each zone. The englacial zone consists mainly of the debris-poor (0.002 volume per cent) diffused facies. White coarse-bubbly ice and blue coarse-clear ice (2 to 10 cm diameter) comprise most of this facies. The bubble-rich banded facies (debris bands) contains abundant debris (25 to 50 volume per cent), varies in lateral and vertical extent, and occurs randomly in the diffused facies.