Glaciation 2 Flashcards
Striations?
As a glacier moves across and area of exposed rock, larger fragments of angular debris embedded in the ice tend to leave a series of parallel scratches and grooves called straitions
Rock drumlin
Smooth elongated mounds of till that run parallel to ice flow movement
Till
An unsorted mixture or rocks Clays and sands
Moraine?
Type of landform that develops when the debris carried by a glacier is deposited
Lateral moraine
Formed from debris from frost shattering of valley sides and is carried along edges of glacier . When the glacier melts, it leaves an embankment of material along the valley side
Medial moraine
Found in the centre of the valley and results from the merging of two lateral moraines where two glaciers joined
Terminal moraine
High mound of material extending across a valley or lowland area, at right angles to and marking the maximum advance of the glacier or ice sheet
Recessional moraine
Marks areas where glacier stopped retreating and remained stationary long enough for a mound to build up, which usually are parallel to terminal moraine
Push moraine
Temporary changes in climate allowed ice to advance again
Outwash plains
Is a plain formed by glacial sediments and are deposited by meltwater past maximum extent of ice
Kame?
Well sorted, undulating mounds made of sand and gravel deposited by melt water
Esker
Long narrow ridges made of sorted sand and gravel
Formed during times of deglaciation
Fossilized courses of sub glacial melt water streams
Bed of meltwater channel builds up because no flood plain exists under high pressure below glacier
Kettle
Blocks of ice detach from glacier as it retreats
Ice is partially buried by glacifluvial deposits fro meltwater
When ice melts, it leaves an enclosed depression which fills with water
Eustatic adjustment
World wide fall or rise in sea level due to changes in hydrological cycle, caused by water being held in storage on land in ice sheets or released following the melting of ice sheets
Isostatic adjustment
Local change in sea level resulting from depression or uplift of the earths crust by increased or decreased weight imposed upon it by the ice sheets.