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
Scabland
rough, barren, volcanic topography with thin soils and little vegetation
Loess
Wind transported sediment from glaciated areas or deserts
striations
abrasion marks- trend in direction of ice movement- see rocks in central park, NY
glacial erratics
rock derived from poleward locations but carried south by glacial ice
kettle
when block of stagnate ice melts leaving a pitted area (small depression)
drumlin
smooth elongated hills- inverted spoon
eskers
winding ridges composed of sand and gravel; remnants of streams beneath glacial ice
kame
steep sided hill; where sand and gravel accumulated in ice crack or fissure (small hill)
marginal glacial lakes
where elongated valleys were carved and lakes were left as remnants
Stratified drift/ till
glacially sorted debris at edge of glacier
What are landforms made by?
Waves and currents
__% of population live within 93 miles of coastline
44%
What is the primary source of wave energy?
Wind
What are “swells”?
large waves when there is stronger wind
What is wave structure?
wave length, height, period, trough
What is a breaker
collapse of wave crest as wave approaches a shoreline
What kind of pattern do waves have?
Oscillartory
Swash
waves that wash up on the beach after an incoming wave has broken (at an angle)
Backwash
waves that wash back into the body of water
Beach Drift
movement along the coast based off swash and backwash
Longshore Drift
the movement of material along the shore by wave action
Jetties
a landing stage or small pier at which boats can dock or be moored
Groins
smaller version of jetties along coastline to help slowdown beach drift and longshore drift
Artificial nourishment
dumping in sand on coastline to reduce erosion
Wave cut terraces
a narrow water ridge inclining gradually away from the bottom of an eroded sea cliff.
sea caves
a type of cave formed primarily by the wave action of the sea
Sea arches
natural opening in the shape of a cliff, it is developed when the waves collide with the rock
sea stack
rock formation made up of a steep or upright column or columns of rock in the sea near a coast.
beach
a landform alongside a body of water which consists of loose particles
spit
A spit is a coastal landform connected to mainland
boymouth bar
a sandbank that partially or completely closes access to a bay.
tombolo
a bar of sand or shingle joining an island to the mainland.