- jökulhlaup lake drainage
- дренаж из озера в виде ледникового паводка
Glacial hydrology dictionary. Б.Р.Мавлюдов.
Glacial hydrology dictionary. Б.Р.Мавлюдов.
Glacial lake outburst flood — A glacial lake outburst flood (GLOF) can occur when a lake contained by a glacier (called Jökulhlaup if it was a subglacial lake, marginal lake drainage if it was dammed between ice and the ground) or a terminal moraine dam fails. This can happen … Wikipedia
Overdeepening — Sognefjord in Norway, the second longest fjord in the world, shows characteristic overdeepening. Overdeepening is a characteristic of basins and valleys eroded by glaciers. An overdeepened valley profile is often eroded to depths which are… … Wikipedia
Sandur — For other uses, see Sandur (disambiguation). Skeiðarársandur in Iceland, viewed from its eastern margin at the terminus of Svínafellsjökull glacier A sandur (plural sandar) is a glacial outwash plain formed of sediments deposited by meltwater at… … Wikipedia
Outflow channels — Kasei Valles, seen in MOLA elevation data. Flow was from bottom left to right. North is up. Image is approx. 1600 km across. The channel system extends another 1200 km south of this image to Hebes Chasma. Outflow channels is the term used to… … Wikipedia
Driftless Area — Relief map showing primarily the Minnesota part of the Driftless Area. The wide diagonal river is the Upper Mississippi River. In this area, it forms the boundary between Minnesota and Wisconsin. The rivers entering the Mississippi from the west… … Wikipedia
Kettle (landform) — A kettle (or kettle hole) is a shallow, sediment filled body of water formed by retreating glaciers or draining floodwaters. Overview. [Tarbuck, E and Lutgens, F:Earth, page 351. Prentice Hall, 2002] Kettle holes can also form as the result of… … Wikipedia
Grímsvötn — mit Berg Grímsfjall 1972 Höhe 1.725 … Deutsch Wikipedia