Glaciers, Deserts, and Wind (book only)

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gohard  on February 7, 2010

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Glaciers, Deserts, and Wind (book only)

Glacier
A thick ice mass that forms over hundreds or thousands of years
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Glacier A thick ice mass that forms over hundreds or thousands of years
Alluvial Fan Cone of debris at the mouth of a canyon
Playa lake Lakes lasting only a few days before drying
Playa Dry, flat bed left after Playa lake dries up
Blowouts Shallow depressions, noticeable results of depression
Desert Pavement Stony veneer, created as deflation lowers the surface, removing sand and silt
Abrasion Wind erodes by
Loess Topography mantled with windblown silt
Slip Face Leeward side of dune
Cross Beds Layers of sand formed on the slip face
Barchan Dunes Solitary sand dunes shaped like crescents, tips pointing downward
transverse Dunes Dunes formed in long ridges separated by troughs, at right angles
Sand Sea Extensive surface of wavy sand
Barchanoid Dunes Form scalloped rows of sand oriented at right angles
Longitudinal Dunes Long ridges of sand that form parallel to the prevailing wind where sand supplies are moderate
Parabolic Dunes form where vegitation partially covers sand
Star Dunes Isolated hills of sand that exhibit a complex form
Valley(Alpine) Glaciers Glaciers found in valleys moving a few centimeters per day
Ice Sheets Flow out in all directions from one or more centers, relatively huge
Ice Caps Glaciers covering some uplands and plateaus
Piedmont Glaciers Glaciers occupying broad lowlands at the bases of steep mountains
Flow The Movement of glacial ice
Plastic Flow Movement within the ice
Zone of Fracture The uppermost zone of a glacier and is very brittle
Crevasses Cracks in the zone of fracture do to tension
Zone of Accumulation Where snow accumulation and ice formation occur
Zone of wastage Where the snow from the previous winter melts
Calving Ice breaking off the front of glaciers
Ice Bergs Where glaciers meet the sea calving occurs
Budget Balance or lack of balance of accumulation and loss
Ablation Loss of snow from a glacier
Plucking Occurs when melt water penetrates cracks and joints along the rock floor of the glacier and freezes
Abrasion Ice and rock sliding over bed rock, act as sand paper to smooth and polish
Rock Flour Pulverized rock produced by the glacial gristmill
Glacial Striations Long scratches and grooves may be gouged into the bedrock
Glacial trough A once V-shaped valley widened, deepened, straightened into a U-shaped valley
Trunk Glaciers Main Glaciers
Hanging Valleys After ice has receded, valleys of tributary glaciers are left standing above the main glacial trough
Cirque Head of glacial valley associated with alpine glacier
Arêtes Sinuous, sharp, edged ridges
Horns Sharp pyramid like peaks
Fiords Deep spectacular inlets of the sea existing in high latitude areas
Glacial Drift Sediment of glacial origin
Till Deposited as glacial ice and drops its rock debris
Stratified Drift Sorted according to size and weight of fragments
Glacial Erratics Boulders found in till or lying freely
Moraines Layers or ridges of till
Lateral Moraines Wasted away materials left as ridges on the sides of valleys
Medial Moraines When two glaciers coalesce to form a single ice stream
End Moraine Ridge or till that forms at the terminus of a glacier
Ground Moraine Gently rolling layer of till deposited as the ice front recedes
Terminal End Moraine The first end moraine to form marks the farthest advance of the glacier
Recessional End Moraines Moraines that form as ice occasionally stabalizes
Outwash Plain Ramplike accumulation of stratified drift built adjacent to the down stream edge of most moraines
Valley Train Ramplike accumulation of stratified drift limited to a mountain valley
Kettles Morainses, outwash plains, and valley trains marked with basins or depressions
Drumlins Streamlined Assymettrical hills composed of till
Eskers Ridges composed largely of sand and gravel and are deposits made by streams
Drumlin Fields Cluster of drumlins
Kames Steep-sided hills composed of sand and gravel
Pluvial Lake Lakes forming in cool wet climates, when precipitation was moderate
Pluvia Means rain
Plate Tectonics Most attractive proposal for why glaciations have occurred only a few times
Ephermal Desert streams, carrying water only in response to period of rain
Wash/Arroyo Different names for Ephermal streams in the US
Wadi/Donga/Nullah Different names for ephermals around the world

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