Template southern-alps

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Southern Alps

Key surface features:

• High mountain ranges (1 st )

• V-shaped valleys and jagged ridges

(2 nd )

Internal processes:

• Convection currents move the plates

• Both plates colliding (destructive plate boundary) leading to uplift

External processes:

• Weathering by ice, water, wind, bio

• Erosion of sediment and deposition on the plains

• Three processes must be linked to the surface features for E. At least one internal and one external process is needed (last one can be either).

• One of each must be linked for M.

• All info must be in the context

Step one

Find/draw a diagram (cross section) to show the three ideas:

• Surface features

• Internal processes

• External processes

Annotate this diagram (around the diagram or refer to in the report).

Step two

• A description of the surface features:

• Mountain ranges

• V-shaped valleys and ridges

• Canterbury plains

Step three

Explain the first internal process that has caused the mountain ranges to form.

• Convection currents (explain how they occur)

• Name the two plates that the sounds are found on

• Link the direction of the current to how the plates are moving

• What type of plate boundaries has this caused?

• When was this happening? (most recently)

Step four

Explain the second internal process that has caused the mountain ranges to form.

• What type of plate boundary has this caused?

• When was this happening? (most recently)

• Where has uplift occurred (why did subduction not occur?)

• What type of rocks were being exposed (age type?)

• CONTEXT, CONTEXT – LINK TO THE SURFACE

FEATURES

Step 5

Explain the first external process that reduced the height of the southern alps

• Weathering and erosion

• The cold winters and frost cracking

• Weathering due to melting snow/water

• Erosion of rock due to wind and water

• Change in the appearance of the mountains over time, due to the above.

Step 6

Explain the second external process that has impacted the appearance of the South Island.

• Erosion of weathered rock

• Transportation by rivers that flow down the valleys

• Deposition of sediment forming the

Canterbury plains

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