The start of the river - Usually in high areas, very shallow and thin as they have a large gradient and not enough discharge to grow
Drainage basin
The area of land drained by a river and its tributaries - no water in ground as it all flows down the valley and into the river
Confluence
Where a tributary joins a larger river - increase of discharge
Mouth
The end of a river (Usually where it joins the sea) - Where estuaries occur, tidal areas
Water shed
The edge of a river basin
Tributary
A small stream that joins a larger river
Upper course
Thin and shallow river as the gradient is large so water cannot build up, Straight river as not enough force for erosion, interlocking spurs occur here.
Middle course
Meanders and oxbow lakes occur here as gradient is lower so the water build up and erodes the sides of the river. Wider and a bit deeper than the upper course
Lower course
Very wide and deep, flood plains and levees occur here as it is so flat. Lots of deposition occurs here as it has little energy
Attrition
Rocks collide with each other in the river and breaks them down into smaller pieces
Hydraulic action
Water compresses air into the cracks of a river bank and increases pressure so the cracks grow bigger.
Solution
Water is slightly acidic and dissolves some types of rock on the bed and banks
Abrasion
Rocks carried by the river scrape and rub along the banks and bed which wears them down
Interlocking spurs
Step 1: Very steep V-shaped valley takes up valley floor
Step 2: Freeze thaw weathering widens valley
What types of rock are involved in the formation of waterfalls?