Unit 2 Flashcards
What is an Ice Sheet?
Completely submerged rock/land, forming a gently sloping dome of ice.
• Several Km thick
• 50,000km^2 in size
• Unconstrained
eg Greenland ice sheet
What is an ice cap?
Smaller version of ice sheet. Occupies upland areas.
• Smaller than 50,000km^2
• Unconstrained
eg Devon Ice Cap (Canada)
What is an Ice field?
Ice covering an upland area, but not thick enough to bury topography.
• 10-10,000km^2
• Constrained
eg Colombia Ice field (Canada)
What is an ‘Unconstrained ice mass’?
These masses have a morphology and flow pattern that is the most part independent of underlying topography.
What is a ‘Constrained ice mass’?
These masses have a morphology and flow pattern that is strongly dependent on underlying topography.
What is ‘topography’
Natural shape of the land.
What is morphology?
The form, shape, structure of an ice mass.
What is a Valley glacier?
A glacier confined between valley walls and terminating in a narrow tongue.
• Forms ice caps, sheets or cirques.
• May terminate in sea as a tidewater glacier
• 3-1,500km^2
• Constrained
eg The Alps
What is a Piedmont glacier?
A valley glacier that extends beyond the end of a mountain valley into a flatter area and spreads out as a fan.
• 3-1000km^2
• Constrained
eg Malaspina Glacier, USA
What is a Cirque glacier
Smaller glacier occupying a hollow on the mountain side - carving out a cirque
• 0.5-8km^2
• Constrained
eg Lower Curtis Glacier
What is an Ice shelf?
Large area of floating glacier ice from the coast where several glaciers have reached the sea and coalesce.
• 10-100,000km^2
• Constrained
eg Ward Hunt (Canada)
What is thermal regime?
Temperature of ice.
What is a Cold Based (polar) Glacier?
• Found at high LATITUDES
• Average ice temp. is well below 0°C
• May be up to 500m thick
• Glacier is permanently frozen to bedrock
What is a Warm Based (temperate) Glacier?
• Found at high ALTITUDE areas
• Temp. fluctuates above and below melting point (seasonal)
• Water exists as a liquid below 0°C due to pressure
• Not permanently frozen to bedrock
What is pressure melting?
Pressure melting is where ice will melt at temperatures below 0°C due to the pressure from the weight of the overlaying glacial ice.
Warm based glaciers experience pressure melting at their base.