Glacial landforms

thumb|right|250px|The snow-free debris hills around the lagoon are lateral and terminal moraines of a valley glacier in [[Manang, Nepal.]] thumb|right|250px|Moraine of the Nanga Parbat North Face Glacier as seen from [[Fairy Meadows, Pakistan.]] thumb|Aerial view of the moraine of the Nanga Parbat North Face Glacier.

thumb|Two cirques with semi-permanent snowpatches near Abisko National Park, Sweden thumb|Upper Thornton Lake Cirque in North Cascades National Park, U.S.

lake formed by a melted glacier

thumb|Drumlins around Horicon Marsh, Wisconsin, in an area with one of the highest concentration of drumlins in the world. The curved path of the [[Laurentide Ice Sheet is evident in the orientation of the various mounds.|380px]] thumb|Elongate and Magellanic subpolar forests|forested drumlins south of [[Puerto Williams, Chile. Flow direction here was at time of formation from west to east (left to right on picture).]]

thumb|right|upright=1.3|Transverse crevasses, Chugach State Park, Alaska A crevasse is a deep crack that forms in a glacier or ice sheet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces.

plain formed from glacier sediment that was transported by water.

shallow depression formed by a retreating glacier

U-shaped valley originally cut by water under the glacial ice near the margin of continental ice sheets

mountain range in the southwestern Caucasus Mountains, Georgia

Orø is a small island in Denmark located in the Isefjord within Holbæk Municipality. The island covers and has a population of 1020 (). There are four villages on Orø: Bybjerg, the largest village on the island with a population of 276 (1 January 2025), Brønde, Gamløse and Næsby.

well-like shaft within a glacier

landforms created by the action of glaciers

large precariously balanced stones

thumb|The fjard of Somes Sound, [[Maine, USA.]]

floods dating from the end of the last ice age, in the USA

An urstromtal (plural: Urstromtäler) is a type of broad glacial valley, for example, in northern Central Europe, that appeared during the ice ages, or individual glacial periods of an ice age, at the edge of the Scandinavian ice sheet and was formed by meltwaters that flowed more or less parallel to the ice margin. Urstromtäler are an element of the glacial series. The term is German and means "ancient stream valley". Although often translated as "glacial valley", it should not be confused with a valley carved out by a glacier. More accurately some sources call them "meltwater valleys" or "ice

cave formed within the ice of a glacier

The Tüttensee (Lake Tütten) is a small lake in the Chiemgau region, the Bavarian Alpine foothills of the Traunstein district, within the municipalities of Grabenstätt and Vachendorf. With an area of and a maximum depth of , it is one of many Kettle-Lakes in the alpine foothills, that resulted from remnants of dead ice after a glacier retreated.

Body of liquid water that flows down a channel formed by a glacier

type of rock formation

depositional glacial feature of ice or snow with an insulating layer of dirt

thumb|The Tollensesee, a glacial finger lake thumb|150px|Map of the Ammersee showing its elongated shape

fan-shaped body of sediments deposited by braided streams from a melting glacier

geographic feature created by glaciation

national park in Turkey