AQA A-Level Geography 7037
Water and Carbon Cycles
Hot Desert Systems and LandscapesLandscape
Coastal Systems and LandscapesLandscape
Glacial Systems and LandscapesLandscape
HazardsHazards or ecosystems
Ecosystems Under StressHazards or ecosystems
Global Systems and Global Governance
Changing Places
Contemporary Urban EnvironmentsHuman option
Population and the EnvironmentHuman option
Resource SecurityHuman option
Hot Desert Systems and Landscapes
Playas, Inselbergs and Landscape Development
- 3 things to know
- Component 1
Overview
Recall questions on playas in endorheic basins with their temporary lakes and salts, on inselbergs and parallel slope retreat, and on how weathering, aeolian and fluvial processes, time and relict landforms shape desert landscapes.
What you need to know
Answer each one before you reveal it.
What processes maintain the steep sides of an inselberg?
Under what conditions do aeolian processes dominate in desert environments?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is a playa?
Model answer
A flat, dry lake bed in an enclosed desert basin where ephemeral lakes evaporate, leaving deposits of salt and fine sediment.
- 2
Where does water collect in an endorheic basin to form a playa?
Model answer
Water drains to the lowest point in the closed basin.
- 3
What forms temporarily in an endorheic basin after rainfall?
Model answer
A temporary lake forms.
- 4
Why does the temporary lake in a playa disappear?
Model answer
High evaporation rates exceed inflow, causing the lake to dry up.
- 5
What happens to dissolved salts as playa water evaporates?
Model answer
Dissolved salts precipitate as the water evaporates.
- 6
What is an inselberg?
Model answer
An isolated, steep-sided residual hill rising abruptly from surrounding pediments or plains, formed from resistant rock.
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