A Text book of Geology

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Thence it continues on its rocky course down the valley.
5. Method of movement. The movement and condition of a glacier is almost wholly dependent on the facility with which ice breaks and unites again into solid ice when the broken surfaces are brought into contact. This quality, first noticed by Faraday and applied to Glaciers by Tyndall, is called regelation, the word meaning a freezing together again. It is easily tried by breaking a lump of ice and bringing the surfaces again into contact
...: if moist, as they are at the ordinary temperature, they at once become firmly united. A glacier moves on and accommodates itself to its uneven bed by breaking when necessary, and in its progress it may soon become as solid as before. Thus it breaks and mends itself as it goes.
Small portions of a glacier may slide along its bed, but the glacier never slides as a whole. In some places there may be an adaptation to an uneven surface by bending without breaking (which may take place if the force be ex- ceedingly slow in action) ; but this also is a means of motion of small importance, compared with the first mentioned.


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