Lesson 1.1.2.3
1.1.2.3 How do glacial landforms evolve over time as climate changes? Quiz: OCR Geography, Unit 1
20 questions
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Lesson 1.1.2.3, How do glacial landforms evolve over time as climate changes?: 20 multiple choice questions for the OCR Geography (H481), Unit 1: Landscape Systems, written with Revision Ninja.
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The 20 questions
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Which long, winding ridge of stratified sand and gravel is deposited by meltwater streams beneath glaciers?
- Kame
- Esker
- Moraine
- Drumlin
-
Which glacio-fluvial landform is a mound of sorted sediment deposited in depressions on stagnant ice?
- Esker
- Kame
- Erratic
- Corrie
-
What extensive, flat landform is created by sorted sediments deposited by meltwater beyond a glacier?
- Outwash plain
- Roche moutonnée
- Ribbon lake
- Till plain
-
How are glacio-fluvial landforms like eskers modified as post-glacial vegetation establishes on them?
- Gelifluction
- Sublimation
- Gleying
- Stabilisation
-
Which process sorts sediment in glacio-fluvial landforms, separating fine material from coarse gravel?
- Glacial abrasion
- Frost shattering
- Ice plucking
- Fluvial deposition
-
Which ice-cored periglacial mound relies on hydrostatic pressure from a trapped water body to form?
- Thermokarst depression
- Solifluction lobe
- Open-system pingo
- Closed-system pingo
-
Which pingo type forms in discontinuous permafrost where artesian groundwater rises and freezes near the surface?
- Open-system pingo
- Closed-system pingo
- Patterned ground
- Thermokarst lake
-
Which periglacial process sorts coarse stones into geometric shapes on gently sloped terrain?
- Abrasion
- Gelifluction
- Frost heaving
- Nivation
-
What landform remains after the central ice core of a pingo completely thaws?
- Ruptured pingo remnant
- Roche moutonnée
- Drumlin field
- Arête
-
Which mass movement process involves saturated surface soil sliding over impermeable permafrost in summer?
- Rotational slump
- Soil creep
- Rockfall
- Solifluction
-
What irregular landscape of marshy hollows forms when permafrost thaws due to climate warming?
- Patterned ground
- Outwash plain
- Thermokarst
- Erratic field
-
Why are elevated pile foundations used for buildings constructed in periglacial settlements?
- Prevent permafrost thawing
- Promote frost heaving
- Stop surface flooding
- Increase wind exposure
-
How does removing natural vegetation cover in periglacial areas impact the active soil layer?
- Prevents solifluction
- Freezes groundwater permanently
- Increases thawing depth
- Decreases thawing depth
-
What immediate change occurs to river sediment supply downstream when a valley dam is constructed?
- Increased turbidity
- Sediment surging
- Sediment trapping
- Enhanced deposition
-
Which process increases directly below glacial river dams due to clear, sediment-starved discharge?
- Channel scour
- Braid formation
- Delta growth
- Aggradation
-
How do gravel extraction activities in glacio-fluvial landscapes alter original post-glacial landforms?
- Accelerates freeze-thaw
- Increases glaciation
- Destroys stratification
- Forms pingos
-
What effect does active layer warming have on slope stability in high-latitude periglacial regions?
- Stabilises soil matrices
- Increases slope failure
- Prevents mass movement
- Eliminates solifluction
-
How does post-glacial stream incision modify outwash plains over extended geological timescales?
- Forms terraces
- Builds moraines
- Creates eskers
- Generates pingos
-
What thermal impact do heated oil pipelines have when laid directly across permafrost landscapes?
- Builds pingos
- Freezes active layers
- Melts ground ice
- Prevents solifluction
-
How does modern climate change affect the rate of physical weathering on post-glacial landforms?
- Stops river incision
- Reduces freeze-thaw frequency
- Eliminates oxidation
- Increases plucking
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