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WorksheetsGeomorphology Quiz
Total questions: 122
Worksheet time: 2hrs 1mins
Which type of weathering involves breakdown of rocks without chemical change?
Mechanical weathering
Chemical weathering
Biological weathering
Hydrolysis
Exfoliation domes are produced mainly by:
Hydration
Thermal expansion and contraction
Hydrolysis
Oxidation
Rusting of iron minerals is an example of:
Carbonation
Oxidation
Solution
Hydration
The chemical weathering process involving reaction with carbonic acid is:
Solution
Carbonation
Oxidation
Exfoliation
Which weathering dominates in humid tropics?
Mechanical
Chemical
Frost action
Salt weathering
Frost action is effective in:
Equatorial areas
Desert areas
Polar & high mountains
Coastal plains
Which mineral is most resistant to weathering?
Feldspar
Quartz
Pyroxene
Olivine
Laterite soil develops by:
Mechanical disintegration
Leaching of silica in humid tropics
Glacial till deposition
Aeolian deposition
Spheroidal weathering produces:
Honeycomb rocks
Rounded boulders
Talus cones
Loess
Biological weathering includes:
Plant root penetration
Animal burrowing
Lichen acid attack
All of the above
Salt weathering is most common in:
Arid regions & coasts
Humid tropics
Glacial valleys
River deltas
Which process turns feldspar into kaolinite clay?
Carbonation
Hydrolysis
Oxidation
Exfoliation
Chelation in weathering is caused by:
Acid rain
Organic acids from vegetation
Frost action
Insolation
Talus slopes result from:
Exfoliation
Rockfall due to frost weathering
Salt weathering
Hydrolysis
Onion-skin weathering is another name for:
Salt weathering
Exfoliation
Frost action
Oxidation
Which climatic condition favors both mechanical & chemical weathering?
Hot & dry
Cold & dry
Warm & moist
Hot & cold daily variation
Which of the following is in-situ decomposition of rocks?
Weathering
Erosion
Mass wasting
Transportation
Which factor does not influence the rate of weathering?
Climate
Rock type
Biological activity
Earth’s rotation speed
Which type of weathering is dominant in deserts?
Frost action
Salt weathering & insolation
Carbonation
Hydrolysis
Which process explains “honeycomb weathering” on coastal rocks?
Solution
Salt weathering
Frost shattering
Biological action
Erosion is different from weathering because it:
Breaks down rocks in situ
Involves removal and transportation of material
Is only mechanical
Happens only in deserts
Sheet erosion means:
Thin layers of topsoil washed away by water
Deep channel cutting
Wind removal of dust
Rockfall
Rill erosion differs from sheet erosion because:
It involves wind
It produces small channels
It is chemical
It is confined to coasts
Gully erosion represents:
Initial stage of sheet wash
Advanced stage of rill erosion
Chemical dissolution
Glacier action
The most powerful agent of erosion on Earth overall is:
Wind
Glaciers
Rivers
Groundwater
Abrasion in rivers refers to:
Solvent action of water
Grinding of river bed by sediments
Chemical attack by acids
Freeze–thaw
Attrition is:
Wearing down of load particles by collision
Freeze–thaw shattering
Glacier plucking
Wind deflation
Hydraulic action refers to:
Dissolving limestone
Pressure of water breaking rock joints
Sediment grinding
Wind erosion
Which erosion process rounds pebbles in a river?
Hydraulic action
Attrition
Plucking
Corrosion
Headward erosion leads to:
River capture (piracy)
Formation of deltas
Glacial moraines
Salt flats
Which landform results from vertical erosion in rivers?
V-shaped valleys
Deltas
Oxbow lakes
Loess deposits
Which erosion agent dominates in deserts?
Wind
River
Glacier
Ice
Which erosion agent is most effective in mountains?
Glaciers
Wind
Rivers
Groundwater
Corrasion is another word for:
Hydraulic pressure
Abrasion by sediment load
Oxidation
Wind deflation
Which process dominates in coastal cliff undercutting?
Solution
Hydraulic action & abrasion
Frost shattering
Aeolian action
Which factor increases erosive power of rivers?
Low slope
Vegetation cover
High velocity & discharge
Ice cover
Backwearing erosion creates:
Retreating slopes/cliffs
V-shaped valleys
Floodplains
Loess deposits
Which agent forms badlands by gully erosion?
Wind
Groundwater
Running water
Ice
Which is the main agent of erosion in karst regions?
Solution by groundwater
Wind abrasion
Frost shattering
Glaciers
Plucking in glaciers refers to:
Freezing of water at base tearing rocks away
Grinding of debris at glacier bottom
Wind polishing
Soil erosion by water
V-shaped valleys are most characteristic of which stage of a river?
Upper course
Middle course
Lower course
Delta
Meanders are produced mainly by:
Vertical erosion
Lateral erosion and deposition
Wind action
Glacial plucking
An oxbow lake forms due to:
Cut-off of a meander loop
Solution of limestone
Glacier melting
Aeolian deflation
A braided river is characterized by:
Multiple interlacing channels with islands
Only one deep channel
Underground flow
Radial drainage
An alluvial fan is formed where:
A river enters a standing body of water
A mountain stream enters a plain
Wind drops its load
Glacier melts
Deltas form when:
River enters a sea/lake and deposits load
River flows in mountains
Wind deposits silt
Glacier spreads debris
A river’s ultimate base level is:
Water table
Sea level
Lake level
Bedrock
River terraces are formed by:
Continuous lateral erosion
River rejuvenation and downcutting
Aeolian erosion
Glacial plucking
Natural levees are built by:
Wind action
River deposition during floods
Glacier deposition
Karst dissolution
Potholes in riverbeds are produced by:
Wind polishing
Pea-sized load swirling in eddies
Glacier abrasion
Solution
The largest delta in the world is:
Mississippi Delta
Amazon Delta
Ganga–Brahmaputra Delta
Nile Delta
The youthful stage of a river is dominated by:
Vertical erosion
Deposition
Lateral erosion
Braiding
Yazoo tributaries are:
Streams flowing parallel to main river within levees
Underground rivers in karst
Disappearing streams
Ephemeral desert streams
Dendritic drainage develops on:
Homogeneous rock structure
Dome-shaped uplands
Faulted terrain
Limestone
Radial drainage is common around:
Domes & volcanoes
Limestone plateaus
Karst basins
Coastal plains
Rectangular drainage indicates:
Uniform rock resistance
Faulted/jointed rocks
Volcanic landscape
Deltaic plains
River capture (piracy) happens due to:
Headward erosion of one stream diverting another
Glacier melting
Karst sinkholes
Wind erosion
Floodplains are mainly a result of:
River meandering and deposition
Glacial till deposition
Wind deflation
Chemical weathering
Point bars in rivers are formed on:
Outer banks of meanders
Inner banks of meanders
Delta mouth
Mid-channel islands
River rejuvenation is caused by:
Fall in sea level / uplift of land
Wind erosion
Glacier retreat
Levee building
The main erosional process of wind in deserts is:
Abrasion and deflation
Hydraulic action
Freeze–thaw
Plucking
Ventifacts are:
Stones polished and faceted by wind-blown sand
Glacial erratics
Rounded pebbles by rivers
Karst towers
Yardangs are:
Streamlined ridges carved by wind
Deposits of river load
Sand dunes
Glacial ridges
A deflation hollow is formed by:
Removal of loose sand by strong winds
Glacier plucking
River meander cutoff
Karst solution
Inselbergs in deserts are:
Isolated resistant rock hills
Sand dunes
River terraces
Moraine mounds
Mushroom rocks are formed by:
Differential wind abrasion near the base
Karst solution
Glacier erosion
Lava cooling
The slip face of a sand dune forms on the:
Windward side
Leeward side
Both sides equally
Flat desert floor
The most common sand dune type in deserts is:
Barchan dune
Parabolic dune
Longitudinal dune
Transverse dune
Seif dunes are characterized by:
Long narrow ridges parallel to wind
Crescent shape
Parabolic arms
Dome form
Loess deposits are:
Wind-blown silt accumulations
Marine clay
Glacial moraines
River floodplains
Deflation pavement is:
Surface covered with pebbles after wind removes fine material
Lava surface
Karst surface
Glacier-polished floor
Parabolic dunes differ from barchans in that:
Arms point upwind due to vegetation anchoring
They form in mountains
They form in loess
They are water-deposited
Erg refers to:
Sand sea in deserts
Rocky desert pavement
Loess plain
Glacier outwash
Reg is:
Desert surface of pebbles/gravel
Sand sea
Loess plateau
Karst depression
Aeolian deposition is most effective in:
Arid and semi-arid regions
Rainforest regions
Polar tundra
Coastal wetlands
Blowouts in sandy coasts/deserts are:
Depressions formed by wind erosion
Coastal lagoons
Karst caves
River oxbows
Which desert feature is depositional?
Yardang
Deflation hollow
Barchan dune
Inselberg
Loess is highly fertile because:
High mineral content and porous texture
Presence of organic matter
Volcanic ash origin
Calcium carbonate only
Which of the following is NOT an aeolian landform?
Ventifact
Yardang
Drumlin
Barchan
The main controlling factor of dune type is:
Wind direction and strength
Soil fertility
Temperature
Vegetation alone
The process by which glaciers pick up rocks is called:
Abrasion
Plucking
Deflation
Corrosion
Striations on bedrock indicate:
Wind erosion
Glacial abrasion
River polishing
Karst corrosion
A U-shaped valley is formed by:
River erosion
Glacial erosion
Wind deflation
Chemical weathering
Hanging valleys are produced when:
Tributary glaciers join main glaciers
Wind erodes ridges
Karst solution deepens sinkholes
Rivers capture tributaries
Cirques (or corries) are:
Bowl-shaped depressions at valley heads
Wind hollows
Karst dolines
River meanders
An arête is:
A sharp ridge between two cirques
A glacial lake
A sand dune
A karst pillar
A pyramidal peak (horn) forms when:
Several cirques erode a mountain from all sides
River erosion steepens valley sides
Loess accumulates
Karst solution hollows hills
A fjord is:
Submerged glacial valley
Karst depression
Loess plain
River terrace
Moraines are:
Deposits of glacial debris
Wind-blown dust
Lava ridges
River levees
Lateral moraines are found:
Along valley sides
At glacier snout
Underneath glacier
Middle of glacier
Terminal moraines mark:
Furthest advance of a glacier
Glacial birthplaces
River base level
Wind deposition zone
Eskers are:
Long sinuous ridges of sand and gravel
Glacial scratches on rocks
Karst ridges
Loess plateaus
Drumlins are:
Streamlined hills of till
Volcanic cones
Desert dunes
Karst towers
Kames are:
Irregular mounds of stratified sand & gravel
Glacial scratches
Cirques
Loess mounds
Outwash plains (sandurs) are:
Glacial meltwater deposits beyond moraines
Wind-blown sand seas
Karst plateaus
River levees
Tarn is:
A small lake in a cirque
A desert hollow
A dune slip face
A loess plain
Roche moutonnée is:
Asymmetrical rock shaped by ice movement
Wind-eroded rock pedestal
Karst limestone hill
Sand dune
Till plain is formed by:
Direct deposition of glacial load after retreat
Wind deposition of loess
River floodplain
Lava outpouring
Erratics are:
Large boulders transported by glaciers
River pebbles
Wind faceted stones
Karst blocks
Karst topography develops primarily in:
Granite
Basalt
Limestone
Sandstone
The chief agent of karst landform development is:
Wind erosion
Glacial erosion
Chemical solution by water & carbonic acid
River meandering
Sinkholes (dolines) are:
Depressions formed by solution/collapse in limestone
Wind-blown hollows
Glacial troughs
River meanders
A chain of merged dolines is called:
Uvala
Polje
Cirque
Tarn
A polje in karst refers to:
Very large flat-floored depression
Small sinkhole
Karst cave
Isolated tower
Karst valleys often lack surface streams because:
Water disappears underground through swallow holes
Climate is arid
Rocks are impermeable
All rivers are glacial
Stalactites grow:
From cave roof downward
From cave floor upward
Horizontally from cave walls
Only in deserts
Stalagmites grow:
From cave floor upward
From cave roof downward
As ridges
As sheets
When stalactite and stalagmite join, they form:
Pillar (or column)
Uvala
Drumlin
Mushroom rock
Travertine terraces are formed by:
Deposition of calcium carbonate from spring water
Wind accumulation
Lava cooling
Glacial till
Karst towers (mogotes) are:
Isolated steep limestone hills
Sand dunes
Volcanic plugs
Inselbergs
Speleothems are:
Cave mineral deposits (stalactites, stalagmites, etc.)
Wind-blown sands
Glacial moraines
Loess mounds
Which is NOT a karst landform?
Dolines
Cirques
Stalactites
Poljes
Swallow holes are also known as:
Poners
Drumlins
Yardangs
Eskers
The term “Karst” was first used in:
Slovenia (Dinaric Alps)
Himalayas
Rockies
Sahara
Lapies are:
Grooved limestone surfaces formed by solution
Loess deposits
Glacial grooves
Wind ripples
Karst springs usually emerge:
At valley bottoms where underground rivers resurface
From volcanic cones
At glacier snouts
From sand dunes
Cockpit karst is characterized by:
Star-shaped depressions separated by conical hills
Parallel ridges and valleys
Circular drumlins
Flat outwash plains
Tower karst (fengcong/fenglin) is best developed in:
Tropical humid regions (e.g., China, Vietnam)
Polar glaciated areas
Arid deserts
Volcanic plateaus
Which of the following is depositional in karst?
Stalactite
Doline
Uvala
Polje
What is the primary cause of river meandering?
Increased sediment load
Human intervention
Variations in water velocity
Glacial activity
Which type of erosion is characterized by the removal of soil in thin layers?
Rill erosion
Gully erosion
Sheet erosion
Bank erosion
Which process is responsible for the formation of karst landscapes?
Volcanic activity
Chemical weathering of limestone
Glacial erosion
Wind erosion
