deposit of sand and gravel carried by running water from the melting ice of a glacier and laid down in stratified deposits. An outwash may attain a thickness of 100 m (328 feet) at the edge of a glacier, although the thickness is usually much less; it may also extend many kilometres in length. For example, outwash deposits from the Wisconsin (Wisconsin Glacial Stage) Glaciation can be traced to the mouth of the Mississippi River, 1,120 km (700 miles) from the nearest glacial terminus.

The sheet of outwash may be pitted with undrained kettles or dissected by postglacial streams. Outwash plains are commonly cross-bedded with units of alternating grain size. The ordinarily gentle slope causes the larger material to be dropped nearest the glacier, while the smaller grain sizes are spread over greater distances. Striated pebbles are uncommon because the striations are worn away during transport. Outwashes are the largest of the fluvioglacial deposits and provide a considerable source of windblown material. When confined within valley walls, the outwash deposit is known as a valley train.