Dr. Johannes Koch

   Department of Earth Sciences

   Simon Fraser University

 

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GLOSSARY OF GLACIAL FEATURES
 
 
 

ablation area
part of the glacier at lower
altitudes at which ablation exceeds accumulation; grey area of glacier tongue in photo

accumulation area
part of the glacier at
higher altitudes at which snow stays throughout melting season;

arête
sharp, narrow ridge formed as result of glacial erosion from two sides;

calving
detachment of blocks of ice from
a glacier into water;
cirque
armchair-shaped hollow with
steep sides and backwall due to glacial erosion high on a mountainside; flat basin containing often a lake (tarn); 

crevasse
deep V-shaped cleft formed in
the brittle part of a glacier; result of the fracture of ice undergoing extension;

dropstone
relatively large clast that falls
through the water column into soft sediment; released from icebergs; indicated by d in photo
drumlin
streamlined hillock, commonly
elongated parallel to former ice-flow direction; composed of glacial debris; gently inclined, smooth slope facing down-valley and a steep, rough slope  
facing up-valley 
erratic
boulder or large block of 
bedrock transported away from its source by a glacier; 
esker
long, commonly sinous ridge of sand
 & gravel; deposited by a stream in a subglacial tunnel; seen cutting through the lakes in the lower left of photo and in cross-section
fiord
long, narrow steep-sided arm of the
 sea; formed as a result of glacial erosion; 

glacier karst
debris-covered stagnant ice; typically with many lake-bearing caverns and tunnels; found at the snout of a retreating glacier;

glacier table
boulder sitting on a pedestal of ice; resulting from protective effect of the rock mass on ablation of the ice surface; still existing one in the lower right, previous one in the upper middle of the photo

glacial trough
U-shaped valley with steep sides and a flat bottom; formed by
glacial
erosion; 

groove
glacial abrasion form with striated (photo on right)
 and or polished sides and base; oriented parallel to the ice-flow direction, up to several meters wide and deep;
hanging glacier
glacier that spills out
from a high.level cirque od clings to a
steep mountain side; after retreating further up-valley building hanging valleys; 

horn
steep-sided, pyramid-shaped
peak; formed due to erosion on three or more sides; 

iceberg
piece of ice that has been shed by
 a glacier into a lake or the sea;
ice cliff
vertical face of ice; normally at
the terminus of an advancing glacier;
icefall
steep, heavily crevassed portion of 
a glacier;
jökulhlaup
sudden and catastrophic
outburst of water from a glacier; photo shows mega-ripples after flooding of Alsek River valley
kame
steep-sided mound of stratified sand & g
ravel deposited supra- or intraglacial by streams; 
not available

kame terrace
as kame, but deposited
along the margin of a glacier; flat or
gently sloping; 

kettle
bowl-shaped depression within an
area covered by glacial debris; forms as a result of the burial of a mass of glacier ice  
and subsequent melting;
loess
wind-blown sedimentof silt grade;
often the result of winnowing of fines from glacial outwash plains;
moraine
distinct ridges or mounds of
debris laid down directly by a glacier or pushed up by it; unsorted loose material
is till; subdivided into lateral, medial,
 ground, terminal
and push moraines; 
nunatak
rocky outcrops projecting above
the ice sheet surface; 
ogives
arcuate bands with the apex
 pointing down-glacier, which develop in icefalls; each band representing one year's movement through the icefall; seen in the right half of photo
portal
open archway through which a
meltwater stream emerges; 
roches moutonnée
rocky hillock with
gently inclined, smooth slope facing
up-valley resulting from glacial abrasion,
and a steep,
rough slope facing 
down-valley resulting from glacial plucking
rock flour
pulverized bedrock; carried in
suspension gives water the typical milky appearance; 
sandar
extensive flat plains of sand &
gravel with braided
streams of glacial
meltwater; 
sérac
tower of unstable ice; in regions of
fast glacier movement; 
surge
short phase of accelerated glacier
flow;
periodic; between surges often
stagnation; 
indicated by distorted medial moraine in photo
till
unsorted morainal
sediment; 
varve
sequence of laminae, deposited in
lakes;
representing a year's sedimentation; 
 
 
Recommended reading
Benn, Douglas I. & David J.A. Evans.(1998) Glaciers & Glaciation.Arnold Publishers:London.
Bennett, Matthew R. & Neil F. Glasser.(1996) Glacial Geology: Ice Sheets and Landforms. Wiley:New York.
Ferguson, Sue A.(1992) Glaciers of North America: a field guide.Fulcrum Publishers:Golden,CO.
Gadd, Ben.(1995) Handbook of the Canadian Rockies.Corax Press:Jasper, Alt.
Hambrey, Michael.(1994) Glacial Environments.UBC Press:Vancouver, B.C.
Prest, V.K.(1983) Canada’s Heritage of Glacial Features.Geological Survey of Canada:Ottawa. (Miscellaneous Report 28)
 

Last modified: 31.12.2003