OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Hazardous Earth
Subduction at oceanic-continental and oceanic-oceanic boundaries
- 2 things to know
- Component 03
Overview
Recall questions on subduction, ocean trenches and the Challenger Deep, Benioff zones, how magma forms above a subducting slab and why it is silica-rich, accretionary prisms, the Andes, island arcs such as the Marianas and Aleutians, back-arc basins, great and deep-focus earthquakes, and violent eruptions.
What you need to know
Answer each one before you reveal it.
At an oceanic-continental boundary, which plate is subducted, and why?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is subduction?
Model answer
The sinking of a dense oceanic plate beneath a less dense plate at a convergent boundary, carrying it back into the mantle.
- 2
At an oceanic-continental boundary, which plate is subducted, and why?
Model answer
The oceanic plate, because it is denser than continental crust and so sinks beneath it.
- 3
What is an ocean trench, and how does it form?
Model answer
A long, narrow, very deep depression in the ocean floor, formed where the subducting plate bends sharply downwards and drags the sea floor down with it.
- 4
Name the deepest point on the ocean floor and the trench in which it lies.
Model answer
The Challenger Deep, in the Mariana Trench, at almost 11,000 m below sea level.
- 5
What is a Benioff zone?
Model answer
The inclined plane of earthquake foci that marks the descending slab, becoming progressively deeper with distance from the trench.
- 6
Explain why magma is generated above a subducting slab.
Model answer
Water driven out of the hydrated minerals in the sinking slab rises into the overlying mantle wedge and lowers its melting point, so it melts without being heated any further.
Other ways to work this
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