Water In Deserts Flashcards
What are the sources of water in hot deserts?
- Exogenous rivers
- Endoreic rivers
- Empemeral rivers
- Episodic flash floods
- Fog (Atacama)
Exogenous rivers
Are rivers that have their source in mountains, outside desert regions
- They have sufficient water to flow continuously despite the high rates of evaporation
- E.g. The Nile, the Colorado
Episodic flash floods
Are infrequent rainfall events that tend to involve torrential, conventional storms unleashing large amounts of water in a very short period of time
- The sunbaked soil results in large amounts of overland flow that is capable of carrying out significant erosion, particularly in mountains where steep gradients increase the rates of flow.
- During such high magnitude events, huge amounts of sediment can be washed out of the mountains to be deposited as vast alluvial plains on the lowlands below.
Episodic flash floods - Types of flooding
Sheet flooding - water flows as a sheet over the landscape
Channel flash flooding - when water makes its way into channels in the landscape
Endoreic rivers
Are rivers that flow into deserts but terminate usually in a lake or inland (dead) sea
- such as the River Jordan, which drains into the dead sea
Ephemeral rivers
Are rivers or streams that flow intermittently (on and off) in desert regions.
- They might flow after storm events or they might be fed my snowmelt in the spring adjacent from the mountains
- Flow rates can vary dramatically and in times of flood ephemeral river can be powerful forces of erosion
Alluvial fan
This is a depositional feature formed by water flowing out of a mountain range onto the flat desert plane.
- The sediment has been eroded form the mountains then transported along a river channel before being deposited on the edge of a desert plain.
Water action (sheet wash/ flooding) processes
- Splash erosion
- Sheet erosion
- Rill erosion
- Gully erosion
- Bank erosion
Water action (river) processes
- Erosion
- Transportation
- Deposition
Erosion
- Hydraulic action
- Abrasion
- Corrasion
- Solution
Transportation
- Traction
- Saltation
- Suspension
- Solution
Splash erosion
The force of falling water displacing soil particles
Sheet erosion
Water running as a sheet over impermeable surfaces or compacted soil washing away disturbed particles
Rill erosion
Sheet wash wears down the soil to form a definite path to form rivulets in the soil called rills
Gully erosion
Over time, rills become wider and deeper to form gullies
Bank erosion
Fast water flow wears away the stream sides, causing the banks to collapse and the channel to widen
Hydraulic action
The sheer force of water
Abrasion
Sandpaper effect of loose rocks being ground over bedrock
Corrasion
Fragments of rock carries by water gouging or sculpting bedrock
Solution
Dissolving of soluble rocks such as limestone
Traction
Rolling sediment along the surface or channel bed
Saltation
Bouncing or leaping motion of particles
Suspension
Sediment carried within the body of water
Solution
Dissolved sediment
Deposition
Takes place where velocity drops, such as on the inside of meander bends or where streams flow out of a mountain onto flat desert plains (alluvial fan)