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WatershedsWatersheds Watersheds are nature's way of dividing up the landscape. Rivers, lakes, Watersheds estuaries, wetlands, streams, even the oceans can serve as catch basins
for the land adjacent to them. Ground water aquifers serve the same
purpose for the land above them. The actions of people who live within a
watershed affect the health of the waters that drain into it.
John Wesley Powell -- scientist, geographer, and leader of the first
expedition through the Grand Canyon in 1869-- perhaps described it best
when he said that a watershed is:
" that area of land, a bounded hydrologic system, within which all living
things are inextricably linked by their common water course and where, as
humans settled, simple logic demanded that they become part of the
community."
Spring Creek, a tributary to Rowlett Creek and the East Fork of the Trinity
River June 21, 2003
STATION 08061540 ROWLETT CREEK NR SACHSE, TX Spring Creek is a tributary to Rowlett Creek. This web site by the U.S. Geological Survey Water Resources Division provides water quality and streamflow information for streams in Texas, including this monitoring site closest to Spring Creek Preserve: Rowlett Creek near the town of Sachse (STATION 08061540). The station is maintained in cooperation with the City of Dallas, Water Utilities Department. By clicking on this site, you can plot gage height (measurement of surface water elevation) or discharge (measurement of streamflow in cubic feet per second). Other information includes water quality parameters such as alkalinity, nitrates, dissolved oxygen, and pH. Since Spring Creek is a tributary to Rowlett Creek, hydrologic conditions are similar, but with a lower discharge rate since the further up a tributary you travel, the smaller the contributing watershed area for surface runoff and shallow groundwater discharge. The drainage area for Rowlett Creek is 120 square miles. Rowlett Creek is a tributary to the East Fork of the Trinity River, which eventually flows into the Gulf of Mexico.
land clearing and coversion to industrial and residential development along with acres and acres of paved roads. Flashier storm peaks increase the erosion potential along stream banks and causes fluvial geomorphologic changes in the river system such as headcutting and meander widening. The mean annual flow has generally increased over the 29 years of record, as evidenced in the graph. A watershed needs to have about 15-20 percent of its landscape free of roads and development (pervious versus impervious) in order to function properly....this includes groundwater recharge, stream equilibrium (balance of aggradation and degradation), near normal aquatic biological communities, normal surface temperatures, flood attenuation, and for functions that remain undiscovered. Impervious surfaces can be generally defined as any material of natural or anthropogenic source that prevents the infiltration of water into soil, thereby changing the flow dynamics, sedimentation load, and pollution profile of storm water runoff. The growth of impervious surfaces is directly related to human activity and habitation through the construction of buildings, roads, parking lots, sidewalks, and so on. As precipitation is diverted from possible soil infiltration, the unfiltered flow over the impervious surface allows significant increases in water runoff, as well as a rise in the acquisition and retention rate of chemical contaminants and sediments from anthropogenic sources. The subsequent surge in the in flow rate and volume in the receiving stream brings about an enlargement of bank-full and stream scour events and significantly influences the morphological structure. The in-stream and riparian ecology is thus altered owing to changes in structural habitat and the related increases in sedimentation and pollution loadings (Arnold and Gibbons, 1996). What can you do to protect your streams and watersheds? Form a homeowners association, or urge your city council to implement plans to leave open space as well as riparian areas along streams, use best management practices or BMPs to reduce erosion and protect stream health, and preserve wildlife habitat in your watershed. Also refer to the smart growth links on this website. Below is a one-year plot of streamflow from March, 2000 to mid-February, 2001. Discharge, measured in cubic feet per second (cfs), was very low from June 21, 2000 until October 14, 2000. Winter rains returned with a recent flood peak of over 7,000 cfs in February, 2001. (Graph modified from original USGS graph for educational purposes).
"To encourage stewardship of the nation's water resources and to celebrate more than 25 years of progress under the Clean Water Act, the Environmental Protection Agency (EPA) is leading an "Adopt Your Watershed" campaign. Through this effort, EPA challenges citizens and organizations to join us and others who are working to protect and restore our valuable rivers, streams, wetlands, lakes, ground water, and estuaries." See the EPA Adopt Your Watershed web site
http://cfpub1.epa.gov/surf/huc.cfm?huc_code=12030106
Water Resources Information WATERS new website maps water quality River Network - River Network has announced the recent launch of its new database information on Clean Water Act contacts by State West Gulf River Forecast Center - National Weather Service National Atlas of the United States - you can produce your own map to view your watershed. click to enlarge Trinity River Basin - National Water Quality Assessment (NAWQA) Animation of Daily Streamflows Maps - USGS Water Quality in the Trinity River Basin - USGS data 1992-1995 Quality of Ground Water in Aquifer Outcrops - Trinity River Basin; USGS U.S. Geological Survey Water Resources Division Dallas/Ft. Worth Climatology - National Weather Service Forecast Office |
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