1 In geomorphology a sand wedge polygon is a micro-relief landform, 7–14 m in diameter, ‘devoid of vegetation and…outlined by textural changes in the soil’ (Péwé (1959) Am. J. Sci. 257). Ice-wedge polygons are formed after a temperature drop so extreme that ‘the ground contracts and cracks, forming a narrow void. During the winter, snow blowing across the tundra surface fills in the crack and freezes to form a thin ice vein. The following spring the ice vein thaws, but it refreezes the following winter and the ground preferentially cracks again along the same ice vein. New snow blows into the crack and freezes, gradually “wedging” the ground open’ (Morgan (1972) Canad. J. Earth Scis 9, 6).
2 In GIS, a closed area bounded by a connected sequence of paired x and y coordinates, the first and last coordinate pairs being the same, and all other pairs being unique. More commonly known as an area.