Mind map
Rivers

Mind map: Rivers
Map content
Rivers
Water Cycle
- Stores
- Channel Storage
- Groundwater Storage
- Surface runoff
- Interception Storage
- Surface Storage
- Flows & Transfers
- Infiltration
- Percolation
- Throughflow
- Groundwater flow
- Surface runoff
- Channel flow
- Stores
Drainage Basins
- Watershed
- Source
- Confluence
- Tributary
- Channel
- Mouth
Weathering
- Mechanical
- Freeze-thaw
- Chemical
- Carbonation
- Biological
- Living things
- Mechanical
Course
- Upper
- Steep
- V-shaped valley
- Narrow, shallow channel
- Middle
- Medium
- Gently sloping valley
- Wider, deeper channel
- Lower
- Gentle
- Very wide, flat valley
- Wide, deep channel
- Upper
Erosion
- Hydraulic Action
- Abrasion
- Attrition
- Solution
Transportation
- Traction
- Saltation
- Suspension
- Solution
Deposition
Landforms
- Erosional and depositional river landforms
- Meanders
- Large bends in a river. The current is faster on the outside of the bend. More erosion happens on the outside of the bend. The current is slower on the inside of the bend. Eroded material is deposited on the inside of the bend.
- Ox bow lakes
- They start off as meanders. Erosion causes the outside bends to get closer until there's only a small bit of land left between the bends. The river breaks through this to take the fastest route. Deposition eventually cuts off the meander.
- Flood Plains
- Levees
- Deltas
Hydrographs
- Peak discharge
- The highest discharge in the period of time you're looking at
- Peak rainfall
- Lag Time
- The delay between peak rainfall and peak discharge
- Rising Limb
- The increase in river discharge as rainwater flows into the river
- Falling Limb
- The decrease in river discharge as the river returns to the normal level
- Impermeable rock
- More runoff Shorter lag time
- Dry or freezing conditions
- Shorter lag time More runoff
- Previously wet conditions
- Shorter lag time More runoff
- Steep slopes
- Shorter lag time More runoff
- Peak discharge
Information
- Description
- Mind Map on Rivers, created by Sasha Curtis on 26/10/2015.
- Created by
- Sasha Curtis
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