River landform: A feature that is made naturally that shapes the earth’s surface.
Upper course landform:
V-shaped valleys
River Landforms:
Upper course
Potholes: Hollows in the river bed, formed by vertical erosion.
River landforms
• Upper course
Rapids:
Areas of shallow, fast flowing water in a stream.
Alternating bands of soft and hard rock, the softer bands get eroded quicker.
River landforms
Upper course
Waterfalls:
A river or other body of water’s steep fall over a rocky ledge into a plunge pool below
Forms when A band of softer rock comes after a band of harder rock and the softer rock gets eroded faster, undercutting rocks.
Overhead hard rock forms an overhang and usually collapses that forms a plunge pool.
This creates a gorge because the water is retreating upwards.
River landforms
Upper course
Gorges:
A narrow valley with steep, rocky walls located between hills or mountains
Caused by the waterfall’s water undercutting the soft rock underneath the hard rock and causing the water to retreat upstream.
River landforms
Upper course
Interlocking spurs: Spurs of land in either side of the valley face in the river to wind around them.
River landforms
Middle and Lower course
Meander:
A bend in the river
Caused by outwards erosion and inwards deposition (Slip off slope)
River landforms
Middle and Lower course
Ox bow lake:
Forms when meanders continue to erode.
Because of the outwards erosion and inner bend deposition, the two ends of the meander and forms into a straight line leaving behind an abandoned meander.
River landforms:
Lower course
Floodplain:
A wide, flat area caused by meanders shifting along the valley.
Forms both due to erosion and deposition
Erosion removes interlocking spurs
Deposition because of the material being deposited during a flood on each side of the river.
River landform:
Middle and lower course
Levee:
Formed by deposition in times of a river flood.
Made of sand and silt, sides of the river bank rises when floods occur.
River landform
Lower course
Delta:
Formed at the end of the river.
Deposition of material at the mouth of the river, load builds up and cause the river channels to narrow, causing distributaries for the water to go to the sea, making a delta.