An ice field (also spelled icefield) is an area less than 50,000 kmĀ² (19,305 mileĀ²) of ice often found in the colder climates and higher altitudes of the world where there is sufficient precipitation. It is an extensive area of interconnected valley glaciers from which the higher peaks rise as nunataks. Ice fields are larger than alpine glaciers, smaller than ice sheets and similar in area to ice caps. The topography of ice fields is determined by the shape of the surrounding land forms, while ice caps have their own forms overriding underlying shapes.
Read more about Ice Field: Formation
Famous quotes containing the words ice and/or field:
“In vain produced, all rays return;
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