rivers Flashcards
upper course gradient, valley and channel shape
steep gradient, v-shaped valley, narrow and shallow channel
middle course gradient, valley and channel shape
medium gradient, gently sloping valley side, deeper channel
lower course gradient, valley and channel shape
gentle gradient, almost flat valley, wide and deep channel
vertical erosions
deepens the river valley and channel making v-shaped
lateral erosion
widen the river valley and channel
4 processes of erosion
-hydraulic action
-abrasion
-attrition
-solution
hydraulic action
force of the river water colliding with rocks breaks rock away from the river channel
abrasion
eroded rocks picked up by the river scrape and rub along the channel, wearing it away
attrition
eroded rocks picked up by the river crash into each other and break into smaller fragments
solution
river water dissolved some types of rock
4 processes of transportation
-traction
-suspension
-saltation
-solution
traction
large particles are pushed along the river bed by the force of the water
suspension
small particles like silt and clay are carried along by the water
saltation
pebble-sized particles are bounced along the river bed by the force of the water
solution
soluble materials dissolve in the water and are carried along
what is deposition
when a river drops the material it’s transporting
why does deposition occur
when the river loses velocity and energy
how does particle size affect deposition
smaller particles are transported further and are deposited closer to the river’s mouth
formation of waterfalls
-softer rock is eroded more than the hard rock, creating a step
-a steep drop is eventually created, a waterfall
formation of gorges
-hard rock is eventually undercut by erosion, it becomes unsupported and collapses
-the collapsed rock erodes the softer rock by abrasion creating a deep plunge pool
-more undercutting causes more to collapse. The waterfall retreats leaving behind a steep sided gorge
interlocking spurs
-in the upper course of a river most of the erosion is vertical, creating v-shaped valleys.
-the river doesn’t have enough power to erode laterally so they have to wind around the hillsides
landforms formed by erosion
waterfalls, gorges and interlocking spurs
landforms formed by erosion and deposition
meanders and oxbow lakes
how are meanders formed
-the current is faster on the outside of the bend because the river channel is deeper
-more erosion takes place on the outside of the bend forming river cliffs
-the current is slower on the inside of the bend because the river channel is shallower, so eroded material is deposited on the inside of the bend, forming slip-off slopes
oxbow lake formation
-meanders get larger over time, erosion causes the outside bends to get closer
-the river breaks through the small bit of land in between and the river follows the shortest course
-deposition eventually cuts off the meander forming an oxbow lake