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Watershed delineation is the process of identifying the boundary of a watershed, also referred to as a catchment, drainage basin, or river basin.It is an important step in many areas of environmental science, engineering, and management, for example to study flooding, aquatic habitat, or water pollution.
Groundwater sapping is a geomorphic erosion process that results in the headward migration of channels in response to near constant fluid discharge at a fixed point. The consistent flow of water displaces fine sediments which physically and chemically weathers rocks. [1]
The confluence of Monument Creek (right) with Fountain Creek (center) in Colorado Springs, Colorado. Monument Creek is an El Paso County, Colorado, stream on the Arkansas River water basin. It flows south from Mount Deception through Pikeview and Monument, and into Colorado Springs, where it meets up with Fountain Creek. [1]
The surrounding topography of a catchment zone influences the flow vectors and direction that the water flows. [1] Water flows from areas of high potential energy to low potential energy under the influence of gravity. The geometry of the slope leading to the catchment area influences the amount of water the catchment will contain. [1]
Water balance. Groundwater recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table ...
The process of finding a drainage boundary is referred to as watershed delineation. Finding the area and extent of a drainage basin is an important step in many areas of science and engineering. Most of the water that discharges from the basin outlet originated as precipitation falling on the basin. [11]
Water from Pikes Peak's south slope was the first major water source for the city of Colorado Springs. [4] [b] After water that has flowed through Ruxton Creek has been processed by the hydroelectric plants, it flows to the Mesa water treatment plant. [4] [5] Water left in or diverted to Ruxton Creek flows to Fountain Creek. [4]
The spring water of Manitou Springs originates from two sources. "Deep-seated waters" of Rampart Range and Ute Pass provide one source of mineral water. Water below the surface is run through cavernous drainage systems called karst aquifers. Limestone in the water dissolves and resulting carbonic acid, or carbon dioxide, make the water ...