Rivers Flashcards
How does a river’s long profile change?
The river starts upland. The load is large as it hasn’t been broken down by erosion.
The lower course is a lot flatter. River’s load is fine sediment as erosion has broken down the rocks.
How does a river’s cross profile change?
Upper course - vertical erosion, shallow and narrow with steep sides in a v-shaped valley.
Middle course - less vertical erosion more lateral erosion so wider. It has a deeper channel and gently sloping sides
Lower course - Little erosion no vertical at all. Very wide and an almost flat valley with the channel at its deepest
What are the 4 main processes of erosion?
Hydraulic Action
Abrasion
Attrition
Solution
What is Hydraulic Action?
A form of erosion
The force of the river water colliding with rocks breaks particles away from the river channel
What is Abrasion?
A form of erosion
Eroded rocks are picked up by the river and they scrape and rub against the bottom of the channel. Wearing it away
What is Attrition?
A form of erosion
Eroded rocks are picked up by the river and crash into each other and break them into smaller pieces. This decreases their size and the rocks become more round as the river progresses from source to mouth.
What is solution?
River water dissolves some type of rock like chalk.
What is transportation?
Transportation is the movement of eroded material.
What are the 4 methods of transportation?
Traction
Saltation
Suspension
Solution
What is traction?
Large particles like boulders are rolled along the river bed by the force of the water.
What is Saltation?
Pebble-sized particles are bounced along the river bed by the force of the water.
What is Suspension?
Small particles like silt and clay are carried along by the water.
What is Solution?
Soluble materials dissolve in the water and are carried along
How are waterfalls and gorges formed?
Waterfalls form when a river flows over an area of hard rock followed by an area of soft rock.
The soft rock erodes (hydraulic action and abrasion) faster than the hard rock creating a step. As water flows over the step it erodes into a steep drop called a waterfall.
The hard rock is undercut by erosion and eventually collapses. This hard rock swirls around at the bottom where it erodes the softer rock by abrasion and creates a plunge pool.
Over time more undercutting causes more collapses and this leaves behind a STEEP SIDED GORGE.
How are interlocking spurs formed
Vertical erosion in the upper course of the river creates steep-sided V-shaped valleys.
The river lacks power so there is no lateral erosion so they wind around hillsides that stick out on either side.
They interlock with each other as the river winds around them. These are called interlocking spurs.
Why do rivers deposit sediment?
When a river loses velocity and energy.
Volume of water falls
Amount of eroded material increases
Water is shallower
River reaches its mouth
How are meanders formed?
As the current is faster on the outside of the bend it erodes faster due to the water being deeper so there is less friction these forms river cliffs.
On the inside of the bend, the water is slower so the eroded sediment is deposited here forming slip-off slopes