Early in his career, Kamb studied the determination of the atomic structure of minerals, and how they related to different structures of ice. For his work in the field of minerals, Barclay Kamb was awarded the
Mineralogical Society of America award in 1968. He was awarded
Guggenheim Fellowships for the academic years 1959–1960 and 1961–1962. Professor Kamb concentrated on studying structures produced by rock flow and fracture in the earth. Kamb reported that if these streams were to increase in speed and become larger, this could potentially cause a collapse of the ice sheets. To explain the motion of these ice streams as well as
surging glaciers, he devised the theory that heat generated in the
till melts water that lubricates the glacier to make the flow of the ice stream more like a landslide than a normal glacier. In order to study these ice streams, Kamb and a team of 13 to 14 people made multiple expeditions to the Antarctic. In the October 2002 to January 2003 expedition, they installed video cameras and equipment to allow for remote data analysis, so teams would not have to venture out so often. Barclay Kamb and Hermann Engelhardt, both researchers at Caltech who led the teams, were honored by the American
Advisory Committee on Antarctic Names (ACAN) with the renaming of an ice stream and ice ridge into
Kamb Ice Stream and
Engelhardt Ice Ridge, respectively. In 1977 Barclay Kamb was awarded the
Seligman Crystal by the
International Glaciological Society. The Crystal is considered to be one of the highest awards in glaciology. ==References==