Refer to the diagram illustrating plate movement at a convergent margin.
Identify the plate that descends beneath the other plate.
State the direction of movement indicated by the yellow arrows along the descending slab.
Outline one reason why oceanic lithosphere can descend into the mantle at this type of plate margin.
Explain how rifting can lead to the formation of new oceanic crust.
Explain how an earthquake can generate a tsunami.
Refer to the diagram illustrating the relationship between subduction and magma beneath a volcanic arc.
Describe the position of the magma bodies relative to the descending slab.
Outline one reason why magma is generated above a subducting slab.
Explain two ways in which human activities can trigger earthquakes.
Refer to the diagram illustrating pathways through which magma reaches the surface.
State the position of the large underground magma reservoir relative to the volcanic cone.
Identify one visible difference between the eruptions at the summit outlet and the flank outlet.
Outline one reason why a composite volcano may erupt explosively.
Explain how volcanic activity can generate two different secondary hazards.
Refer to the diagram illustrating the construction of a volcanic cone by successive deposits.
State two characteristics of the arrangement of the layers forming the volcanic cone.
Outline one reason why magma may reach the surface through an outlet on the flank of a volcano.
Explain two physical factors, other than volcanic activity, that can cause mass movements.
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To what extent do contrasting eruption styles account for differences between shield, composite and cinder volcanoes?
To what extent does depth of focus determine the severity of earthquake ground shaking?
To what extent can plate movement be explained by mantle convection currents alone?
Examine why earthquakes of similar magnitude can generate different secondary hazards.
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Evaluate the usefulness of liquidity and speed of onset for classifying mass movement events.
Examine why mass movement events of the same type can differ in duration, extent and frequency.