Lesson 1.1.2.4
1.1.2.4 How does human activity cause change within glaciated and periglacial landscape systems? Quiz: OCR Geography, Unit 1
20 questions
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Lesson 1.1.2.4, How does human activity cause change within glaciated and periglacial landscape systems?: 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 human activity is the primary driver of landscape change in periglacial North Slope, Alaska?
- Oil extraction
- Wind farming
- Forestry logging
- Bauxite mining
-
What process is directly accelerated by thermal radiation from uninsulated buildings on permafrost?
- Frost heave
- Glacial plucking
- Permafrost thawing
- Solifluction stopping
-
Which landscape feature forms when widespread thawing of permafrost causes uneven ground collapse?
- Roche moutonnée
- Thermokarst
- Arête network
- Drumlin field
-
Why are sections of the Trans-Alaska Pipeline elevated above the ground surface?
- Avoid glacier advancement
- Prevent permafrost thawing
- Prevent wind erosion
- Stop river flooding
-
What effect does gravel extraction from periglacial river beds have on sediment flow?
- Depletes sediment supply
- Prevents river scour
- Stops channel erosion
- Increases bedload supply
-
What primary landform modification occurs when permafrost beneath a pingo melts completely?
- Striation pattern
- Esker ridge construction
- Ground collapse crater
- Roche moutonnée formation
-
What is the main reason for constructing large dams in high alpine glaciated valleys?
- Tidal energy capture
- Hydroelectric power generation
- Arable crop irrigation
- Geothermal steam production
-
How do dam reservoirs in glaciated valleys impact the downstream transport of sediment?
- Increasing downstream bedload
- Accelerating moraine formation
- Eliminating channel scour
- Trapping sediment upstream
-
What process increases directly downstream of a dam due to sediment-starved clear water?
- Channel scour
- Glacial deposition
- Frost shattering
- Sediment deposition
-
How does dam regulation typically alter seasonal meltwater discharge downstream in glaciated valleys?
- Increases summer floods
- Reduces peak flows
- Doubles annual discharge
- Stops winter flow
-
What happens to a glacier when total annual accumulation exceeds total annual ablation?
- Zero mass balance
- Negative mass balance
- Dynamic equilibrium loss
- Positive mass balance
-
What term describes the line on a glacier where annual accumulation equals annual ablation?
- Equilibrium line
- Solifluction boundary
- Trim line
- Terminus line
-
What is the net mass balance of a glacier gaining 5 metres and losing 7 metres annually?
- -2 metres
- -12 metres
- +2 metres
- +12 metres
-
What is the effect of artificial snowmaking on local hydrological inputs in alpine ski resorts?
- Reduces groundwater storage
- Increases water abstraction
- Eliminates winter snowpack
- Decreases river runoff
-
What happens to glacier surface albedo when dark soot and dust accumulate on the ice?
- Albedo remains constant
- Albedo increases
- Albedo decreases
- Albedo doubles
-
How does permafrost degradation affect the stability of active solifluction slopes?
- Eliminates surface water
- Increases slope instability
- Prevents mass movement
- Stabilises soil layers
-
What calculation measures the difference between total sediment inputs and sediment outputs in a glacial valley?
- Hydraulic radius
- Sediment budget
- Mass balance
- Cross-sectional area
-
How does building urban infrastructure on permafrost alter the ground surface energy balance?
- Increases ground albedo
- Increases heat absorption
- Reduces geothermal heat
- Decreases thermal conductivity
-
What valley floor change is commonly observed downstream of major alpine dam developments?
- Glacier advance
- Valley aggradation
- River bed lowering
- Moraine accumulation
-
What happens to the periglacial active layer thickness when surface tundra vegetation is cleared?
- It freezes permanently
- It decreases
- It increases
- It remains unchanged
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