Cold Flashcards
(29 cards)
Katabatic winds
cold mountain winds- the dense air flows down from the mountains to the lowland, chilling the ground as it passes over
insolation
incoming solar radiation, that is, heat received from the sun
orographic rainfall
rain that is produced as air is forced to rise over high ground such as a mountain barrier, it subsequently cools, condensation occurs and precipitation is produced
striations
scratch marks on a rock caused by abrasion
chatter marks
discontinuous scratch marks on a rock caused by abrasion
roche montonnee
rock that has been plucked and made smooth by glaciers. upstream side = smooth due to abrasion. downstream slope = steeper and rougher due to plucking
divergent flow
ice flow which is around an object rather than over it
carbonation
weathering in which calcium carbonate reacts with an acid water to form calcium bicarbonate which is soluble and removed in solution
hydrolysis
chemical weathering process where water reacts with minerals such as feldspars to produce clay minerals
Till
sediment deposited by glaciers- unsorted deposits with a range of size. also called boulder clay
neve
transitional stage between snow and ice. has survived at least one summers melting, and has been compressed by following winters snowfall
extrusion flow
the movement of ice as a result of becoming too deep/heavy and therefore unstable. it ‘collapses’ and begins to flow outwards as a result of its own weight and pressure
bergschrund
a large crack or crevasse
randkluft
a gap between the rock face and ice in the hollow, caused when heat from the rock melts the ice
pressure release
weathering in which a rock is able to expand outwards as a result of the ‘unloading’ of pressure and as a result, cracks appear in the rock
spur
a projection of land from a ridge or mountain. interlocking spurs in upper valley. truncated spurs are those which have been eroded in their lower parts by glaciers
ribbon lake
long, linear lakes which fill a glaciated trough. e.g. lake windermere
hanging valley
a small U shaped valley formed by a small glacier that joins and hangs above a large U shaped valley formed by a larger glacier
scree
angular sediment that collects at the foot of a mountain range or cliff. usually broken off by freeze thaw weathering
moraine
glacial deposits consisting of poorly sorted, often angular, loose rock fragments
col/spillway
a low point in a ridge or high ground, often formed as a result of back-to-back cirques. some may be formed by the movement of glacier ice from one valley into another
unstratified material
glacially deposited material which is unsorted, variable i size and has no distinct layers
ablation
the removal of material from a glacier such as by melting, evaporation, sublimation
moulins
circular sink hole or portals into glaciers. may be caused by meltwater entering a crevasse