Geology 12
Presents
Outline:
• Chp 14
• Chp 15
• Chp 16
• Chp 17
• Chp 18
Mass Wasting (Landslides)
Running Water
Groundwater
Glaciers and Glaciation
Wind and Deserts
Glaciers and
Glaciation
A: Introduction
B: Glacial Erosion and Transport
C: Glacial Deposits
Glaciers
A: Introduction/Glaciers
•
Glacier: mass of ice composed of
compacted snow and recrystallized snow
flowing under its own weight under the
force of gravity.
• Move via:
1. plastic deformation below 40m just from the
shear weight of ice.
2. basal slip: sometimes with the presence of
melt water the glacier may slide.
Glacier Movement
Glacier Movement
•Copy diagram
Crevasse
Total surface movement
40m
Plastic deformation
Basal slip
Types of Glaciers
1. Valley/Alpine Glaciers: confined to mountain
valleys (yoodle leh)
• Flow down hill
• Few km wide by 10’s of km long by several
100 m thick
• Ex: Alaskan Alpine Glaciers
2 km wide x 120 km long x 400 m thick
ice
1. Valley/Alpine Glaciers
Types of Glaciers
2. Ice Sheets: BIG
• Flow out horizontally in every direction from
where the snow accumulates the most
a) Continental Glaciers:
• Largest: 100s of km long/wide by 3-5 km
thick
• Ex: Greenland, Antarctica (now) and N.
Amer’ during the last ice age 25,000 yrs
ago (most of Canada)
Ice Sheets: Continental Glaciers
Types of Glaciers
2. Ice Sheets:
b) Ice Caps
• <50,000 km2
• Ex: Penny Ice Cap (Baffin Isld), Iceland,
Spitsberg Isld.
ice
crust
isostacy
Ice Sheets: Ice Caps
Isostasy
• Glacial Movement
Zone of accumulation
Firn limit
snow
ice
Zone of
wastage
Ice front
Firn: pebbles of ice; intermediate stage
between snow and ice
Glacial Movement
Firn: Pebbles of ice
•Intermediate stage between
snow and ice
Firn
Glacial Movement
Glacial advance: when accumulation > wastage
Glacial Retreat: when accumulation < wastage
Glacial Movement
Glacial advance: when accumulation > wastage
Glacial Retreat: when accumulation < wastage
• Calving: process of
producing icebergs.
gla
ci
er
ocean
• Calving: process of
producing icebergs.
Icebergs