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Landforms

Water carving rock

Rivers from source to mouth, then coasts, ice, karst, and folds. Landforms you can orbit.

Ice-cut mountains, not a river poster.
Process, then shape.Wikimedia Commons, CC BY
A meander belt on a floodplain.
Landforms

River long profile

A Lake District beck in spate and the Mississippi in flood are the same machine at different stations: steep and narrow, then lazy and wide.

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A collision range: process written as relief.
Landforms

Landform types

A mountain is not a hill with ambition. Height, slope, and a flat top are different machines.

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A steep valley cut by water, not ice.
Landforms

River erosion

A waterfall is a nick point walking upstream.

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A delta from orbit: load dumped into still water.
Landforms

River deposition

When the water slows, the load sits down: slip-off slope, levée, floodplain, delta, estuary.

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A wind gap or elbow of capture.
Landforms

River capture

A more aggressive neighbour can steal a headwater. The elbow is the scar.

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A spit built by longshore drift.
Landforms

Coasts

Constructive waves build. Destructive waves take. Longshore drift is the conveyor. Cave–arch–stack–stump is the headland’s life.

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A valley glacier in a U-trough.
Landforms

Glacial landforms

Ice is a river that can be a kilometre thick. It leaves a cirque, an arête, a horn, a U, and a pile of till.

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Tower karst or a cave in carbonate rock.
Landforms

Karst

Limestone does not just break. It dissolves along joints: pavement, swallow hole, cave.

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Barchan dunes: horns downwind.
Landforms

Wind landforms

Yardangs are carved. Barchans are built. Wind is a sculptor where vegetation is thin.

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A landslide scar and a hummocky toe.
Landforms

Mass movement

Holderness till does not wait for a wave. After rain the cliff rotates on a curved shear and the toe shoves the beach.

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Patterned ground: polygons from freeze–thaw.
Landforms

Periglacial landforms

The Cairngorms still carry freeze–thaw scars. Alaska still has ice wedges growing. Cold without a glacier is its own factory.

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