River processes produce distinctive landforms. Flashcards
(43 cards)
Define: Watershed.
The boundary of a river basin.
Define: Confluence.
The point where two rivers meet.
Define: Tributary.
A stream that joins a larger river.
Define: Source.
The start of a river.
Define: Mouth.
Where a river meets the sea.
Define: Hydraulic action.
This is the pressure of the water being pushed against the banks and bed of the river. It also includes the compression of air: as the water gets into cracks in the rock, it compresses the air; this puts even more pressure on the cracks and pieces of rock may break off.
Define: Corrasion.
Particles carried by the river are thrown against the river banks with considerable force.
Define: Corrosion.
This is the chemical reaction between certain rock types and the river water.
Define: Solution.
This is the chemical reaction between certain rock types and the river water.
Define: Attrition.
This is a process that involves the wearing away of the rocks that are in the river. In the upper course of a river, rocks continually roll around and knock into each other. They chip away at each other until smooth pebbles or sand are formed.
Define: Deposition.
This is the layering down of the load of the river.
Describe the 3 step process of physical weathering.
- Water gets into a crack in the rock.
- As the temperature decreases, pressure is created on the rock by a 9% increase in volume as the water freezes.
- When the temperature increases again, the crack will have increased in size.
Describe the 5 step process of biological weathering.
- A seed falls into a crack.
- Rain causes the seedling to grow.
- Roots force their way into cracks.
- As the roots grow they break up the rock.
- Burrowing animals also break up rock.
Describe the 3 step process of chemical weathering.
- Rainwater causes natural acids.
- Carbonates in limestone are dissolved by weak acids.
- The cracks in the rock expand.
Define: Mass movement.
When material moves down a slope, pulled by gravity.
Describe the 5 step process of soil creep.
- This is the slowest downhill movement.
- Gravity pulls the water in the soil down a slope.
- The soil particles will move downhill with the water.
- Heavy rainfall causes faster downhill movement.
- The slope appears to have ripples known as terracettes.
Describe the 9 step process of slumping.
- This is common on river banks.
- A large area of land moves down the slope.
- Due to the nature of the slip, it leaves behind a curved surface.
- This is common on clay river banks.
- During dry weather the clay contracts and cracks.
- When it rains the water runs into the cracks and is absorbed.
- The rock becomes saturated.
- This weakens the rock.
- Due to the pull of gravity, it slips down the slope on its slip plane.
What 8 characteristics are common in the lower course of a river?
- Mostly deposition.
- Gentle gradient.
- Very broad valley.
- Wider river channel.
- Deepest river channel.
- Fastest flowing.
- Large discharge.
- Silt and suspended material.
What 8 characteristics are common in the middle course of a river?
- Lateral erosion.
- Medium gradient.
- U-shaped valley.
- Wider river channel.
- Deeper river channel.
- Faster flowing.
- More discharge.
- Smaller material.
What 8 characteristics are common in the upper course of a river?
- Vertical erosion.
- Steep gradient.
- V-shaped valley.
- Narrow river channel.
- Shallow river.
- Slow flowing (because of friction).
- Small discharge.
- Large rocks.
Define: Interlocking spurs.
Barriers of hard resistant rock, which the river cannot easily erode.
Describe the 5 step process of the formation of interlocking spurs.
- Vertical erosion (in the form of abrasion, hydraulic action and solution) in the river channel results in the formation of a steep sided valley.
- Over time the sides of this valley are weakened by weathering processes and continued vertical erosion at the base of the valley.
- Gradually mass movement of materials occurs down the valley sides, gradually creating a v-shape.
- This material is then gradually transported away by the river when there is enough energy to do so.
- As the river flows through the valley it is forced to swing from side to side around more resistant rock spurs. As there is little energy for lateral erosion, the river continues to cut down vertically, flowing between spurs of higher land, creating interlocking spurs.
What are the 2 features of interlocking spurs?
- Spurs.
2. V-shaped valley.
Define: Waterfalls.
A waterfall is a river or other body of water’s steep fall over a rocky ledge into a plunge pool below.