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Glaciers & Coastal

glacial n coastal modifications to terrain

QuestionAnswer
Highland icefields? huge mountainous glaciers covering the high terrain
nunataks land protruding from mountainous glacier sheets
valley glaciers glaciers "tounges" that travel down to the valleys from the mountains
alpine glaciers glaciers that develop individually in the mountains rather than part of a broad icesheet
cirque glaciers glacier confined to the individual basin that it developed in
continental ice sheets glaciers of non mountainous origin
perglacial zone beyond the glacier never touched by ice but where influence was still felt
accumulation addition of ice to a glacier by incorporation of snow
ablation wastage of glacial ice due to melting and sublimation
neve or firn material formed by packed snow that is about half the density of water
accumulation zone upper portion of glacier where accumulation is morer than the ablation
ablation zone lower portion of glacier where ablation is more that accumulation
equilibrium line theoretical zone where accumulation and ablation is perfectly equal
glacial plucking glacial erosion where rock and land particles under a glacial are plucked out and dragged along as the glacier moves
glacial abrasion land is worn down by rock debris dragging along the floor
glacial flour finely ground rock material
moulins deep drainage shafts in glaciers
drift general term for material moved by a glacier
till rock debris directly deposited by a glacier with no meltwater repositioning
glacial erratics enormous fragments like boulders left by glaciers that are different form local bedrock
glaciofluvial deposition glacial deposition redeposited by meltwater
rouch moutonnee round and smooth characteristic made by glaciers moveing over a hill
stoss side side of mountain facing the direction where glacier came from
lee side side of mountain facing away from the direction that the glacier came from
moraine glacier deposited landform mostly made of till
termnial moraine ridge of till that marks the outermost limit of glacial advance
recessional moraine ridges that mark where glaciers were temporarily stablized dusring its final retreat
ground moraine when large quantities of till are laid downfrom underneath the glacier rather than the edges
drumlin hill smaller than a moraine that is parallel with movement of glacier
tarn depression from cirque that holds water
arete narrow jagged serrated spine of rock left by eroded side of a cirque
horn steep sided pyramid shaped mountain peak formed by quarrying of the headwalls where three or more cirques intersect
paternoster lakes shallow depressions that hold water along benches of glacial steps
lateral moraines large ridges along side of the glacier comnposed of unsorted debris
periglacial enviroment 20% of worlds land is periglacial and affected by glacial enviroment
patterned ground repeated patterns over large areas in the arctic
swells waves that escape the influence of generating wind
waves of oscillation waves that moveback and forth in the same place with little forward movement
wavelength horizontal distance from wavecrest to eavecrest or trough to trough
swash breaking wave rushing towards shore
wave refraction change of wave direction as it approaches shore
tsunami seismic sea waves caused by disruption along ocean floor. vertical displacement caused by reverse faulting
eustatuc sea level change sea level change from rise or fall of landmass/ rise or fall of amount of ocean water
longshore currents when water moves roughly parallel to the shore
beach drifitng zig zag movement of sediment that results in downwind displacement parallel to the coast
sediment budget for balance the removal of sand equals the addition ofsand
beach exposed body of deposit of loose sediment adjacent to a body of water
groin short wall or damn built to impede longshore current and force sand deposition on the upcurrent side of the structure
jetties built in pairs of either side of a river or harbor entrance to confine flow of water to a narrow zone to keep sand in motion
ria shoreline coastline with numerous estuaries
fjords deep shearwalled coastal indentations
marine terrace raised wavecut platform
fringing reefs reef built right onto a volcano
barrier reef ring of coral that seems to float but is attached to a sinking mountain
atoll reef surrounding a landless lagoon from sinking volcano
Created by: nicoruiz
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