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Chapter 6
Concept 3 Quiz
Concept 3 Quiz
Describe the features produced by glacial erosion and deposition.
This activity contains 10 questions.
A broad, ramp-like surface of stratified drift built adjacent to the downstream edge of most end moraines of continental glaciers is called a(n)
outwash plain
fiord
valley train
kettle
moraine
Glacial troughs that have become deep, steep-sided inlets of the sea are called
cirques
hanging valleys
washes
kames
fiords
Identify each of the indicated alpine glacial features by selecting the correct response.
(Alpine glacial features diagram, Copyright © Prentice Hall, Inc.)
This question presents 6 items numbered 3.1 through 3.6. Each item is presented with a pulldown menu containing the letters A through F.
For each item below, use the pull-down menu to select the letter that labels the correct part of the image.
3.1 pater noster lakes
[hint]
A
B
C
D
E
F
3.2 hanging valley
[hint]
A
B
C
D
E
F
3.3 horn
[hint]
A
B
C
D
E
F
3.4 glacial trough
[hint]
A
B
C
D
E
F
3.5 arête
[hint]
A
B
C
D
E
F
3.6 cirque
[hint]
A
B
C
D
E
F
Medial moraines form along the sides of valley glaciers.
True
False
Glaciated valleys typically exhibit a V-shaped appearance.
True
False
Medial moraines are bowl-shaped erosional features found at the heads of glacial valleys.
True
False
Materials deposited directly by the glacier as it melts are known as till.
True
False
Sharp pyramid-like peaks carved and sculptured by alpine glaciers are called
cirques
kames
horns
hanging valleys
arêtes
The rate of glacial erosion is variable because it depends on
the rate of glacial movement
how resistant the surface beneath the glacier is
the bed load characteristics at the base of the glacier
the thickness of the ice
all of the above
Streamlined asymmetrical hills composed of till are best known as
striations
outwash
tarns
eskers
drumlims
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