8.3: Questions
- Page ID
- 53103
\( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)
\( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash {#1}}} \)
\( \newcommand{\dsum}{\displaystyle\sum\limits} \)
\( \newcommand{\dint}{\displaystyle\int\limits} \)
\( \newcommand{\dlim}{\displaystyle\lim\limits} \)
\( \newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\)
( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\)
\( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\)
\( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\)
\( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\)
\( \newcommand{\Span}{\mathrm{span}}\)
\( \newcommand{\id}{\mathrm{id}}\)
\( \newcommand{\Span}{\mathrm{span}}\)
\( \newcommand{\kernel}{\mathrm{null}\,}\)
\( \newcommand{\range}{\mathrm{range}\,}\)
\( \newcommand{\RealPart}{\mathrm{Re}}\)
\( \newcommand{\ImaginaryPart}{\mathrm{Im}}\)
\( \newcommand{\Argument}{\mathrm{Arg}}\)
\( \newcommand{\norm}[1]{\| #1 \|}\)
\( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\)
\( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\AA}{\unicode[.8,0]{x212B}}\)
\( \newcommand{\vectorA}[1]{\vec{#1}} % arrow\)
\( \newcommand{\vectorAt}[1]{\vec{\text{#1}}} % arrow\)
\( \newcommand{\vectorB}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)
\( \newcommand{\vectorC}[1]{\textbf{#1}} \)
\( \newcommand{\vectorD}[1]{\overrightarrow{#1}} \)
\( \newcommand{\vectorDt}[1]{\overrightarrow{\text{#1}}} \)
\( \newcommand{\vectE}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{\mathbf {#1}}}} \)
\( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)
\(\newcommand{\longvect}{\overrightarrow}\)
\( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash {#1}}} \)
\(\newcommand{\avec}{\mathbf a}\) \(\newcommand{\bvec}{\mathbf b}\) \(\newcommand{\cvec}{\mathbf c}\) \(\newcommand{\dvec}{\mathbf d}\) \(\newcommand{\dtil}{\widetilde{\mathbf d}}\) \(\newcommand{\evec}{\mathbf e}\) \(\newcommand{\fvec}{\mathbf f}\) \(\newcommand{\nvec}{\mathbf n}\) \(\newcommand{\pvec}{\mathbf p}\) \(\newcommand{\qvec}{\mathbf q}\) \(\newcommand{\svec}{\mathbf s}\) \(\newcommand{\tvec}{\mathbf t}\) \(\newcommand{\uvec}{\mathbf u}\) \(\newcommand{\vvec}{\mathbf v}\) \(\newcommand{\wvec}{\mathbf w}\) \(\newcommand{\xvec}{\mathbf x}\) \(\newcommand{\yvec}{\mathbf y}\) \(\newcommand{\zvec}{\mathbf z}\) \(\newcommand{\rvec}{\mathbf r}\) \(\newcommand{\mvec}{\mathbf m}\) \(\newcommand{\zerovec}{\mathbf 0}\) \(\newcommand{\onevec}{\mathbf 1}\) \(\newcommand{\real}{\mathbb R}\) \(\newcommand{\twovec}[2]{\left[\begin{array}{r}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\ctwovec}[2]{\left[\begin{array}{c}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\threevec}[3]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\cthreevec}[3]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\fourvec}[4]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\cfourvec}[4]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\fivevec}[5]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\cfivevec}[5]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\mattwo}[4]{\left[\begin{array}{rr}#1 \amp #2 \\ #3 \amp #4 \\ \end{array}\right]}\) \(\newcommand{\laspan}[1]{\text{Span}\{#1\}}\) \(\newcommand{\bcal}{\cal B}\) \(\newcommand{\ccal}{\cal C}\) \(\newcommand{\scal}{\cal S}\) \(\newcommand{\wcal}{\cal W}\) \(\newcommand{\ecal}{\cal E}\) \(\newcommand{\coords}[2]{\left\{#1\right\}_{#2}}\) \(\newcommand{\gray}[1]{\color{gray}{#1}}\) \(\newcommand{\lgray}[1]{\color{lightgray}{#1}}\) \(\newcommand{\rank}{\operatorname{rank}}\) \(\newcommand{\row}{\text{Row}}\) \(\newcommand{\col}{\text{Col}}\) \(\renewcommand{\row}{\text{Row}}\) \(\newcommand{\nul}{\text{Nul}}\) \(\newcommand{\var}{\text{Var}}\) \(\newcommand{\corr}{\text{corr}}\) \(\newcommand{\len}[1]{\left|#1\right|}\) \(\newcommand{\bbar}{\overline{\bvec}}\) \(\newcommand{\bhat}{\widehat{\bvec}}\) \(\newcommand{\bperp}{\bvec^\perp}\) \(\newcommand{\xhat}{\widehat{\xvec}}\) \(\newcommand{\vhat}{\widehat{\vvec}}\) \(\newcommand{\uhat}{\widehat{\uvec}}\) \(\newcommand{\what}{\widehat{\wvec}}\) \(\newcommand{\Sighat}{\widehat{\Sigma}}\) \(\newcommand{\lt}{<}\) \(\newcommand{\gt}{>}\) \(\newcommand{\amp}{&}\) \(\definecolor{fillinmathshade}{gray}{0.9}\)Question 1 An erosion agent is one that
Transport magma
Transport ices
Transport waters
Transport sediments
Question 2 Which of the following are erosion agents?
Magma
Glaciers
Running water
Wind
Question 3 Glaciers that have left observable landforms today are associated with which period of Earth's history?
Quaternary
Permian
Cambrian
Mississippian
Question 4 For how long can percipitation at high latitudes be stores as ice before making its way to the ocean?
Up to decades
Up to hundreds of years
Up to thousands of years
Up to millions of years
Question 5 Glaciers are considered as a part of
Both the rock cycle and the hydrologic cycle
The rock cycle only
The hydrologic cycle only
The carbon cycle
Question 6 The historical ice sheet that advanced across North America in the last ice age is called
Greenland ice sheet
Antarctica ice sheet
Laurentide ice sheet
Wisconsinan ice sheet
Question 7 Valley glaciers are most likely found at
High latitude, high altitude
Low latitude, low altitude
High latitude, low altitude
Low latitude, high altitude
Question 8 What is a notable example of a region where valley glaciers are nowadays common?
Coasts of Alaska
Rocky Mountain regions
Coasts of Australia
Appalachian Mountains
Question 9 What are the locations where continental ice sheets are found today?
Alaska and Iceland
Greenland and Antarctica
Greenland and Iceland
Antarctica and Arctic
Question 10 Ice sheets are of
Continental scale
Mountain scale
Valley scale
Scale of the summit of a volcano
Question 11 During which geologic period did continental ice sheets cover most of North America?
Quaternary
Cambrian
Permian
Jurassic
Question 12 The accumulation of ice at the summit of a volcanic mountain is an example of
Ice caps
Valley glaciers
Ice sheets
Piedmont glaciers
Question 13 How thick are continental ice sheets?
Up to thousands of meters
Up to tens of meters
Up to meters
Up to tens of thousands of meters
Question 14 What happens when a valley glacier exists the valley?
It advances forward
It spreads out and settles
It becomes a continental ice sheet
It becomes an ice cap
Question 15 Which is the glacier of the largest scale in comparison to others?
Alpine glacier
Valley glacier
Continental ice sheet
Ice cap
Question 16 The mechanism by which glaciers move is called
Plastic flow
Liquidation
Melting
Fracturing
Question 17 At what depth below the surface of a glacier does ice become soft or plastic?
50 meters
100 meters
200 meters
500 meters
Question 18 Plastic flow in ice is the equivalent of
Folding in rocks
Faulting in rocks
Dissolution in rocks
Exfoliation in rocks
Question 19 Above what depth is the zone of fracture (brittle zone) found in a glacier?
50 meters
100 meters
200 meters
500 meters
Question 20 The cracks in the zone of fracture of a glacier is called
Crevasses
Faults
Folds
Displacements
Question 21 Where was the famous 1948 measurement of valley glacier movement conducted?
At Aletsch glacier
At Jungfrau glacier
At Northwestern glacier
At Bering glacier
Question 22 Which is the region where ice accumulates?
Zone of accumulation
Zone of melting (wastage)
Zone of fracture
Zone of continental divide
Question 23 Where in a glacier does the ice melt?
Zone of accumulation
Zone of melting (wastage)
Zone of fracture
Zone of continental divide
Question 24 The balance in the amount of ice in a glacier is called
Glacial balance
Glacial budget
Glacial account
Glacial equilibrium
Question 25 Glacial retreat occurs when the margin of a valley glacier
Moves in the direction of upstream
Moves in the direction of downstream
Remains unchanged over time
Does not have a correspondence with the glacial margin
Question 26 Glacial erosion refers to
The removal of rock materials by glaciers
The transport of water-borne materials by ice
The melting of ice into liquid water
The fracturing of rigid ice in the zoom of fracture
Question 27 What are the most common evidence of glacial erosion?
Rock debris released by melt water
Crevasses in the zoom of fracture
Horn of a mountain
The change of the margin in the zoom of melting
Question 28 Global warming is observable through the increased presence of
Glacial retreat
Glacial advancement
Glacial remaining stationary
Glacial equilibrium
Question 29 Abrasion is glacial erosion by
Scraping on rock surfaces
Frost wedging on of rocks
Breaking of rocks
Impedence of flow
Question 30 In what way is glacial erosion different from erosion by streams or wind?
Removed rock debris does not settle out
Fractures in ice stores rock debris
Melting dissolves rock debris
Removal of rock fragment occurs mostly in the zoom of fracture
Question 31 What types of sediments may be contained in a glacier as a result of erosion?
Silt, sand, gravel, boulder
Silt, sand, gravel
Silt, sand
Silt
Question 32 The rock fragments from glacial abrasion is called
Rock flour
Pigments
Horn
Exfoliation
Question 33 Plucking is equivalent to the mechanical weathering process of
Frost wedging
Exfoliation
Dissolving of minerals
Deposition of minerals
Question 34 What feature may be left on the basement rock by a moving glacier?
Fractures
Recrystallization
Metamorphism
Glacial polish
Question 35 Features of scratches and long grooves on the surface of glaciated basement rock are called
Glacial striations
Glacial deposits
Glacial moraines
Glacial valleys
Question 36 What factors affect the rate of glacial erosion?
Speed of glacial movement
Thickness of ice
Rock type
Volume of ice
Question 37 How are valleys eroded by streams differ from valleys eroded by glaciers?
Stream valleys are narrow and V-shaped; glacial valleys are wide and U-shaped
Stream valleys are narrow and U-shaped; glacial valleys are wide and V-shaped
Stream valleys are wide and V-shaped; glacial valleys are narrow and U-shaped
Stream valleys are wide and U-shaped; glacial valleys are narrow and V-shaped
Question 38 The sharp ridge between two glacial valleys is called
Arête
Hanging valley
Cirque
Horn
Question 39 The bowl-shaped depression at the end of a glacial valley is called
Cirque
Bowl
Dome
End
Question 40 What glacial erosion mechanism created the landform of a horn?
Abrasion
Plastic flow
Melting
Plucking
Question 41 Plastic flow in ice at the bottom of a glacier is equivalent to
Ductile deformation of rocks
Breaking of rocks
Elastic deformation of rocks
Fracturing of rocks
Question 42 The pyramod-shaped mountain peak shaped by glacial abrasion is called
Horn
Cirque
Deformation
Fracture
Question 43 How are erosions by continental ice sheets different from or similar to erosions by valley glaciers?
Ice sheets subdue landforms; valley glaciers sharpen landforms
Ice sheets sharpen landforms; valley glaciers subdue landforms
Ice sheets and valley glaciers both subdue landforms
Ice sheets and valley glaciers both sharpen landforms
Question 44 The difference in the amount of ice flows between the main valley and the side valleys results in the formation of
Hanging valleys
Horns
Glacial troughs
Cirques
Question 45 The linear inlets of sea is called
Fiords
Hanging valleys
Cirques
Horns
Question 46 Fiords formed as sea water submerged
Glacial troughs
Stream valleys
Cirques
Horns
Question 47 Where are fiords found?
Alaska's coasts
Montana's Glacial National Park
The Rocky Mountains
The Grand Teton Mountains
Question 48 The formation of Fiords is attributed to
Rising sea levels after ice ages end
Global temperature increases today
Erosion by ice at the coastal regions
Erosion by ice anywhere valley glaciers are present
Question 49 Fiords are an evidence that
Glaciers are able to erode beds deeper than the surface of the sea
Rivers are able to erode beds deeper than the surface of the sea
Both rivers and glaciers are able to erode beds deeper than the surface of the sea
Neither rivers nor glaciers are able to erode beds deeper than the surface of the sea
Question 50 Glacial drift represents the fact that deposits of glacial origin
May come from a distant place
Are always of local origin
Are created by floods
Are the result of dike formation
Question 51 Unlike streams, glaciers does not
Sort rock particles by size
Transport rock particles
Erode rocks
Move
Question 52 Deposits of stratified drift are
Rock particles sorted by size
Rock particles unsorted by size
Glacier erratics
Boulders of a uniform size
Question 53 Stratified drift is sorted by
Stream of meltwater of the glacier
Ice of the glacier
Wind
Deformation of the crustal rock
Question 54 Accumulation of stratified drift usually include
Sand, gravel
Silt, sand, gravel
Sand, gravel, glacial erratic
Silt, sand, gravel, glacial erratic
Question 55 Moraines are
Layers or ridges of glacier deposits
Subdued mountains peaks
Sharpened mountain peaks
Carved valleys
Question 56 What are the most common glacial deposition landforms?
Moraines
Outwash plains
Kettles
Kettle lakes
Question 57 Rock debris removed from valley walls and accumulated as ridges at the bases of the walls are called
Ground moraines
Medial moraines
End moraines
Lateral moraines
Question 58 When valleys join and glacial ice streams merge, lateral moraines also merge to become
Lateral moraines
End moraines
Medial moraines
Ground moraines
Question 59 Ridges of sediments that accumulate at the terminus of glaciers are called
Ground moraines
Lateral moraines
Medial moraines
End moraines
Question 60 As the glacial front recedes and ice melts, a layer of sediments is deposited from the dropped debris, called
End moraines
Lateral moraines
Medial moraines
Ground moraines
Question 61 The last end moraine, marking the final margin of the glacial advance, is called
Lateral moraine
Recessional end moraine
Ground moraine
Terminal end moraine
Question 62 End moraines that form during temporary climate stabilization during the overall glacial retreat are called
Recessional end moraines
Ground moraines
Lateral moraines
Terminal end moraines
Question 63 A flat accumulation of stratified drift formed near the edges of end moraines is called
Outwash plain
Esker
Kettle lake
Recessional end moraine
Question 64 Asymmetrical, elongated hills of till with the gentle side aligned with the direction of glacial advance are called
Kames
Lateral moraines
Drumlins
End moraines
Question 65 Twisting-shaped ridges of till deposits from streams in channeled flows beneath the ice are called
Drumlins
End moraines
Eskers
Kames
Question 66 Round-shaped, steep-sided hills associated with the retreat of ice sheets are called
End moraines
Kames
Eskers
Drumlins
Question 67 Lakes that formed during glacial retreat when meltwater was trapped between the glacial fronts and the sloped land barriers are called
Glacial lakes
Pluvial lakes
Great Lakes
Proglacial lakes
Question 68 The largest proglacial lake in North America during the retreat from the last glacial maximum was
Lake Superior
Lake Bonneville
Lake Michigan
Lake Agassiz
Question 69 Which of the following is the largest pluvial lake in North America during the last ice age?
Lake Michigan
Lake Bonneville
Lake Superior
Lake Agassiz
Question 70 Lakes that formed during the ice ages due to lower evaporation rates are called
Proglacial lakes
Pluvial lakes
The Great Lakes
Alluvial lakes

