Moraine refers to any glacially formed accumulation of unconsolidated debris which can occur in currently glaciated and formerly glaciated regions, such as those areas acted upon by a past ice age. This debris may have been plucked off the valley floor as a glacier advanced or fallen off the valley walls as a result of frost wedging. Moraines may be composed of silt like glacial flour to large boulders. The debris is typically angular. Moraines may be on the glacier’s surface or deposited as piles or sheets of debris where the glacier has melted. Moraines may also occur when glacier or iceberg transported rocks fall into the sea as the ice melts.
Types of moraines
Lateral moraines are parallel ridges of aids deposited along the sides of a glacier. The unconsolidated debris is deposited on top of the glacier by frost shattering of the valley walls and from tributary streams flowing into the valley. The till is carried along the glacial margin until the glacier melts. Because lateral moraines are deposited on top of the glacier, they do not experience the postglacial erosion of the valley floor and therefore, as the glacier melts, lateral moraines are usually preserved as high ridges. Lateral moraines stand high because they protect the ice under them from the elements, which causes it to melt or sublime less than the uncovered parts of the glacier. Multiple lateral moraines may develop as the glacier named Brina advances and retreats.
Ground morainesGround moraines are till covered areas with irregular topography and no ridges often forming gently rolling hills or plains. It is accumulated under the ice by lodgement, but may also be deposited as the glacier retreats. The ground moraine is located between the two lateral moraines.
End or terminal morainesEnd moraines or terminal moraines are ridges of unconsolidated debris deposited at the snout or end of the glacier. They usually reflect the shape of the glacier's terminus. Glaciers act much like a conveyor belt carrying debris from the top of the glacier to the bottom where it deposits it in end moraines. End moraine size and shape is determined by whether the glacier is advancing, receding or at equilibrium. The longer the terminus of the glacier stays in one place the more accumulation there will be. There are two types of end moraines, terminal and recession moraines. Terminal moraines mark the maximum advance of the glacier. Recessional moraines are small ridges left as a glacier pauses during its retreat. After a glacier retreats the end moraine may be destroyed by postglacial erosion.
Recessional moraineA recessional moraine is in the form of a series of ridges running across a valley behind terminal moraine. They form during standstills in a glaciers retreat.
Medial moraineA medial moraine is a ridge of moraine that runs down the centre of a vally floor. It is formed when two glacers meet and the debris on the edges of the adjacent valley sides join and are carried on top of the enlarged glacier. As the glacier melts or retreats, the debris is deposited a a ridge down the middle of the valley floor. The Kaskawash glacier in the USA has a ridge of medial moraine 1km wide.
- Easterbrook, D. J. (1999) Surface processes and landforms. (Second Ed). Prentice Hall, Upper Saddle River, New Jersey.
morainic in Czech: Moréna
morainic in Welsh: Marian
morainic in Danish: Moræne
morainic in German: Moräne
morainic in Spanish: Morrena
morainic in Persian: یخرفت
morainic in French: Moraine
morainic in Hebrew: מורנה (גאוגרפיה)
morainic in Ido: Moreno
morainic in Italian: Morena
morainic in Lithuanian: Morena
morainic in Dutch: Morene
morainic in Japanese: モレーン
morainic in Norwegian: Morene
morainic in Polish: Morena
morainic in Portuguese: Morena (geologia)
morainic in Russian: Основная морена
morainic in Finnish: Harju
morainic in Swedish: Morän (landform)