Lawson, Wendy, 1989

Publication Details

  • Title:

    The structural evolution of Variegated Glacier, Alaska
  • Authors:

    Lawson, Wendy
  • Publication Date:

    1989
  • Publisher:

    University of Cambridge, United Kingdom 
  • Ordering Info:

    Not available
  • Quadrangle(s):

    Mount Saint Elias; Yakutat

Bibliographic Reference

Lawson, Wendy, 1989, The structural evolution of Variegated Glacier, Alaska: University of Cambridge, United Kingdom, Ph.D. dissertation.

Abstract

Photographic database, comprising 12 sets of vertical aerial photogaphs taken between 1948 and 1983; has enabled the structural glaciology of surge-type Variegated Glacier, Alaska,to be analyzed for a period that spans two surge cycles and includes the effects of three surges. The glacier-wide patterns of crevasse development at the end of each of these surges, which occurred in 1947-48, 1964-65, and 1982-83, were remarkably similar, despite differences in surge intensities and extents. At the end of each surge a three-fold longitudinal zonation of crevasse orientation characterised that part of the glacier that had been affected by surge activity. This zonation comprises: (i) transverse crevasses in a narrow upper zone, (ii) superimposed longitudinal and transverse crevasses in an extensive middle zone, and (iii) longitudinal crevasses in a narrow lower zone. The main difference between patterns produced by successive surges was small variations in the extent of the three zones. During quiescence, the most intense crevasse development occurs in the upper glacier in the latter part of quiescence, and is a function of increasingly steep down-glacier velocity gradients developing in the build-up to the impending surge. Some crevassing also develops in the central part of the glacier in mid-quiescence that is not related to the surge nature of the glacier, but to normal flow processes over bedrock. There is no structural evidence to indicate that any of the tributaries of Variegated Glacier surge. This observation suggests that the bulb-like loops in the medial moraines at Variegated Glacier form during quiescence as a result of the steady flow of the tributaries into the stagnant trunk glacier, rather than as a result of tributary surges.

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