part 5
PART 1: EFFECTS OF GLACIERS
Why do we care?
Source of freshwater
Seasonal regulation
Contribution to sea level rise
Vulnerability to cliamte change
Climate change proxies
Feedback loop
Habitat for unique species
Influence on river systsems
Tourism
Natural hazards
global indicator of enviornmental health
Alters thermohaline circulation (blue and red chart)
Sea level change
Melt all glaciers = sea lebel rise about 65m or 200 ft
Glaciers trap huge amounts of water
Isostatic depression
E antarctic ice sheet has caused up to 2.5 km of isostatic depression
Glacier --> crust subsidence --> moves horizontally outward
Isostatic rebound
Moves horizontally inwards --> crust rebound moving up vertically
Drinking water and irrigation
Ex- washington get 470 billion gallons/year
PART 2: GLACIER BASICS
GLACIER- large mass of ice that forms from the accumulation, compaction, and recrystallization of snow over many years.
Forming a glacier
Granular snow
Firn (denser)
Glacial ice
Requires time, cold, and precipitation
Types of glaciers
Valley glacier aka mountain, alpine
Ex- mt kilimanjaro- africa ca 20k feet
Continental glacier
Aka ice sheets
Glacial movements
Accumulation- process by which snow and ice build up in a glacier or snowpack over time
Ablation- processes through which a glacier loses mass, primarily through melting, sublimation, and calving.
Both accumulation and ablation need each other
Firn line- critical boundary on a glacier that separates the accumulation zone from the ablation zone
Speed varies in different parts of a glacier
Upslope v downslope
Things stuck in the ice get moved
Plastic flow- > 50 m thick
Basal slip- process by which glaciers move over their bed (the ground beneath the glacier) due to the presence of water and the gravitational force acting on the ice
Glacial feature
Crevasse- deep, vertical fracture or crack that forms in a glacier or ice sheet
PART 3: GLACIAL EROSION
Abrasion- involves the wearing away and smoothing of a surface through friction and erosion caused by the movement of particles
Plucking- occurs in glacial environments, where a glacier picks up and removes pieces of rock and sediment from the underlying bedrock as it moves
Erosive features
Striations
U shaped valleys
Cirque
Tarns
Horn
Arete
Roche moutonnée
PART 4: GLACIAL SEDIMENT DEPOSITS
Erratics
Till
Outwash
Loess
DEPOSITIONAL FEATURES AND EROSIONAL FEATURES ARE DIFFERENT
Depositional features
Moraines
Eskers
Drumlin
Kames
Kettle lakes (kettles)