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Sharp accordingly had the training to look at glaciers quantitatively and build a conceptual model of glacier behavior based in mathematics, and in the years following his expedition with Walter Wood he shifted his attention to glaciers. Using the knowledge he had gained at Harvard (and as an undergraduate at the California Institute of Technology) and techniques then in use by his European contemporaries, Sharp returned to the St. Elias Mountains in the early 1950s, where he made significant advances in quantitative glaciology, including the use of seismic measurements to determine glacier thickness and the analysis of the transformation of snow to ice from heat and mass transfer principles.

During the International Hydrological Decade (19661975), the South Cascade Glacier measurement protocols, in combination with European methods, were adopted as international standards of observation. The South Cascade Glacier project evolved into a long-term program of observations of a transect of glaciers from Gulkana Glacier in the Alaska Range to Maclure Glacier in California’s Sierra Nevada Mountains. At this time glaciers were increasingly becoming recognized as critical components in hydrology, and glacier interactions with climate as a vital part of hydrological changes, both on short-term, local scales and long-term, global scales.

Meier, and A. Post, Calving speed of Alaskan tidewater glaciers, with application to Columbia Glacier. USGS Professional Paper 1258-C, US Government Printing Office, Washington DC, 1982. The Opening of a New Landscape: Columbia Glacier at Mid-Retreat 10/22/2007 11:44:02 AM Figure 25. Main Branch, view to the West, toward the terminus, June 2004. The medial moraines coming from the Main Branch’s tributaries converge on the terminus in the background. The moraines jog sideways in their path down glacier, partly in response to a bedrock step beneath the glacier, and partly due to changes in the speed of flow in the different tributaries.

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La filosofia futura by Emanuele Severino

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