Watersheds (College Board AP® Environmental Science): Revision Note
Characteristics of watersheds
What is a watershed?
A watershed is an area of land where all precipitation and surface water drains into a common body of water, such as a river, lake, or ocean
Also known as a drainage basin
A watershed collects and channels water through a network of connected streams that all drain to the same outlet
Watersheds vary in size, from small creeks to massive river basins like the Mississippi River Watershed
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Image caption: A watershed is the entire area of land where all rainfall and surface water drains to a common outlet. Its boundary follows the high ridges that separate one drainage area from another.
Key characteristics of a watershed
Area
The total land surface area that drains into a water body
Larger watersheds collect more water
This influences regional water flow
Example: The Amazon River Basin is the largest watershed in the world, covering about 7 million km²
Length
The distance from the watershed’s highest point to its outlet (where water drains into a larger body)
Longer watersheds typically have a more complex drainage network with more streams feeding the main river
Slope
The gradient or steepness of the land within the watershed
Affects water speed, erosion, and sediment transport
Steep slopes cause rapid runoff and higher erosion potential
Gentle slopes allow more infiltration and slower runoff
Example: Mountainous watersheds have steep slopes, leading to flash flooding
Soil type
Determines water infiltration, soil water retention, and erosion potential
Sandy soils: High permeability, low water retention, higher erosion risk
Clay soils: Low permeability, high water retention, more prone to surface runoff
Loamy soils are an ideal mixture of sand, silt and clay, so are ideal for plant growth and water absorption
Example: Watersheds with clay-heavy soil may experience more surface runoff and erosion
Vegetation
The type and density of plants affect water retention, erosion control, and infiltration
Dense vegetation slows runoff, improves groundwater recharge, and reduces erosion
Deforested or barren areas have higher erosion and reduced water retention
Watershed divides
The boundaries separating one watershed from another
Typically found along ridges or high elevations where water flows in different directions
Example: The Continental Divide in North America determines whether water flows to the Atlantic or Pacific Ocean
Human activities and water quality
Whatever happens on the land within a watershed eventually affects the water quality at its outlet
Pollutants, sediments, and excess nutrients are washed by rainfall into the stream network and carried downstream
This is why watersheds are often used as management units when protecting water quality
Major land-use impacts covered elsewhere in the course:
Clearcutting removes the trees that anchor the soil, raising sedimentation and stream temperatures (see The Effect of Clearcutting on Forests)
Mining of ores releases heavy metals, acid mine drainage, and tailings into local waters (see Mining of Ores)
Agricultural practices such as tilling and fertiliser use cause nutrient runoff and eutrophication downstream (see Environmental Impacts of Agricultural Practices)
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