Exam 4 Flashcards
rock flour
fine pulverized rock
till
unconsolidated sediment
abrasion
grinding by rock/ ice mixture
plucking
lifting of rocks and associated movement
moraine
debris of till at margins of the ice sheet (medial, terminal, recessional)
arete
knife-like ridge produced by parallel intersecting glacial trough walls
cirque
bowl shaped depression often near the glacial accumulation zone
horn
three or more adjacent cirques leaving pointed peek
col
gap or opening in the glacial trough wall
glacial trough
u-shaped valley carved by the glacier
hanging trough
where tributary glacier intersects primary alpine glacier
tarn
lake left in a cirque after glacial retreat
fiord
where a trough opens to the sea with glacial retreat
landslides
when failure steep sided trough walls
trough lake
elongated lakes left in glacial trough after glacial retreat
What are the two continental ice sheets today?
Antarctica and Greenland
Which continental ice sheet is the biggest?
Antarctica
Iceberg
90% volume below the sea level. Hazardous to shipping
Ice Shelf
A floating sheet of ice permanently attached to a landmass. These shelves are enormous and may be several hundred feet thick
Pleistocene glaciation
- Occurred from approximately 2.5 million to 22,700 years ago
- First noted by Louis Agassiz in mid-1800’s. He was a Swiss naturalist
- There were over 20 glacial events occurring during this time period with periods of glacial retreat
What are the impacts of Pleistocene Glaciation?
- Temperature change (5-10 degrees cooler)
- Isostatic adjustment (weight of ice forced continents down 300 meters; currently continents are rising at about 2 cm per year)
- Change in sea level (off Atlantic decreased 137 meters. Shoreline- 100 to 200 km from where it is today)
What causes these cycles of glaciation?
- Variations in the earth’s tilt
- Variations in the earth’s eccentricity in its orbit about the sun
- Precession (wobble)
- Variations in the arrangement of the continents through plate tectonics
- Variation in the ocean (air systems)
Drainage disruption
Soils that do not drain well in glaciated valleys. Gravelly with different size debris. ALSO POSSIBLY DERENGED DRANAGE SYSTEM where a drainage system has no coherent pattern. (tentative)
Pluvial lakes
a formerly large lake created by excessive rain paired with little evaporation