Glaciers Flashcards
Glacier:
- Mass movement of frozen ice on land
- Form at high latitude or high elevation
- Last extension of ice here began 20,000 years and receded about 10,000 years ago
- Today only covers 10% of land surface
Ice Flow:
Glaciers are not static, they are dynamic
Formation:
- A stead accumulation of snow piles up and compresses layers beneath,, these compressed layers turn into ice
- Force of gravity continuously pulls ice downward
- Firn
Movement:
- Fastest ice is found on the surface at the center of the valley
- Rate varies from a few cm to meters per day
Three categories of glaciers:
- Valley (alpine) glaciers
- Ice sheets (continental glaciers)
- Tidewater glacier
Valley (alpine):
- Found in mountainous regions
- High altitude
- Alps, Rockies
Ice Sheets (continental glaciers):
- Much larger
- Flow direction is form and area of thick ice to thin ice
- Greenland, Antarctica
Tidewater glacier:
- Flow far enough to reach out into ocean
- Create icebergs
Glacier accumulation:
Snow adds to weight of a glacier
Glacier wastage (ablation):
- Breaking of ice forming icebergs
- Melting and calving
Accumulation is greater than wastage:
Glacier advances
Accumulation is less than wastage:
Glacier retreats
Accumulation = wastage:
Glacier remains stationary
Glacial erosion & features:
- Plucking and abrasion
- U-shaped valleys, sharp ridges (Aretes), pyramid peaks (horns), water filled valleys (Fjords = hudson river) and bowl shaped valleys (cirques)
Deposition features:
- Drift
- Stratified Drift
- Till
Drift:
Any sediment deposited by moving ice
Stratified Drift (Fluvio):
Well-sorted sediments deposited by streams (meltwater)
Till:
Unsorted sediment, deposited by moving ice
Deposits of till:
- Lateral moraines
- Medial moraines
- End moraine
- Drumlin
- Glacial erractics
Lateral moraines:
Form along valley walls
Medial moraines:
Form where two later moraines meet
End moraine:
Left at terminus of glaciers where it retreats
Drumlin:
A tear-shaped ridge showing direction of ice flow
Glacial erratics:
Large boulder left behind a glacier
Deposits of stratified drift:
- Kame
- Esker
- Kettle
Kame:
A small hill forms where sorted sediments accumulate beneath ice
Esker:
- Winding path of stratified drift
- Forms under glacier streams
Kettle:
A depression caused by a block of ice that melts and can be water-filled