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12 Cards in this Set

  • Front
  • Back

Source

Where a river begins

Confluence point

Where two or more streams meet

Tributary

A stream or river that flows into a larger steam or river

Watershed

The boundary between two drainage basin

Mouth

Where a river meets the sea

Hydraulic action

The force of the river against the banks can cause air to be trapped in cracks .the pressure weakens this bank and gradually wears it away

Corrasion

Rocks carried along by the river wear down the river bed and banks

Attrition

Rocks being carried by the river smash together and break into smaller and smoother rocks

Corrosion

Where a chemical reaction happens between certain rock types and the river water.then it eats through the rock

V shaped valleys

Vertical erosion is most important near the source


The river cuts down into the bed through hydraulic action, attrition and corrosion


Due to vertical erosion the steep valley sides become unstable


Mass movement on the valley sides such as soil creep, leads to v shaped valley forming

Interlocking Spurs

Rivers erode vertically in the upper course and erode the softest rock fastest


If there is any hard rock the river will erode around it instead of through it to crest zig zag pattern


The ridges left behind are interlocking Spurs

Waterfalls

Hard rock and soft rocks are found together in layers, with the hard rock on top. Erosion of the soft rock is fasted. The hard rock is undercut over time to make an overhang. It is unsupported and will collapse. Over time the waterfall will move back upstream leaving a long gorge also it's leaves a plunge pool