A watershed is a channel that concentrates runoff to the main discharge point. Usually, the discharge point is at the lowest point in the watershed.
Headwaters are the beginning of a watershed. Watersheds are typically separated by ridges or mountains that form the highest part of the watershed. From here, runoff moves to lower elevations forming streams and rivers.
These streams and rivers can diverge and create subwatersheds, but all of the runoff discharges into one point, a lake or ocean.
Image Courtesy of Pixabay
Characteristics of Watershed
The characteristics of a watershed impact the runoff rate, erosion, and vegetation. These characteristics include area (size), length, slope, soil type, and vegetation.
The size (area) of a watershed can be a reflection of the amount of runoff and what is created by the runoff, i.e. river, stream, or creek. It could also reflect how the runoff is discharged, i.e. the ocean or lake. It also plays a role in how much runoff can be held in the watershed.
The length and slope of a watershed play a big factor in the runoff rate.
The slope of a watershed is the change in elevation between the headwaters and the discharge point. The greater the slope, the greater the runoff rate. Lesser slope, less runoff.
The length of a watershed is the distance between the headwaters and the discharge point. This mainly impacts how long it takes for runoff to reach the discharge point. Hence, the longer the watershed, the longer it would take for runoff to be discharged.
The type of soil found in watershed impacts the amount of runoff absorbed by soil as well as the vegetation. If the soil is very sandy or has large particles, the soil will take in more runoff water. In addition, if the soil is fertile, there will be more vegetation. Finally, soil can play a role in filtering water in a watershed.