Spring Creek | |
---|---|
Location | |
Country | United States |
Physical characteristics | |
Source | |
• location | north of Kansas, Oklahoma |
• coordinates | 36°13′31″N94°47′31″W / 36.22518°N 94.79195°W |
Mouth | Fort Gibson Lake |
• location | south of Murphy, Oklahoma |
• coordinates | 36°06′44″N95°15′30″W / 36.11232°N 95.25830°W Coordinates: 36°06′44″N95°15′30″W / 36.11232°N 95.25830°W |
Spring Creek originates in Eastern Oklahoma near the town of Kansas, and flows generally southwest about 34 miles through Delaware, Cherokee, and Mayes counties before emptying into Fort Gibson Lake on the Grand (Neosho) River. [1] [2] [3] Throughout its roughly 117,000 acre watershed, the creek is fed by small springs which contribute most of the estimated 15 million gallons of water that flow through it per day. [2] Spring Creek is listed as having high quality water, being one of only five bodies of water in the state having this rating. [3]
This creek is not to be confused with the Spring Creek in Roger Mills County in Western Oklahoma, which feeds Spring Creek Lake [4] [5] before becoming a tributary of the Washita River, [6] nor with the Spring Creek that fills Lake Chickasha in Caddo County, Oklahoma, near Chickasha in Central Oklahoma, [7] nor with any of the other watercourses in Oklahoma with the Spring Creek name, [8] nor with numerous other watercourses named Spring Creek in other states and countries.
Tulsa County is located in the U.S. state of Oklahoma. As of the 2010 census, the population was 603,403, making it the second-most populous county in Oklahoma, behind only Oklahoma County. Its county seat and largest city is Tulsa, the second-largest city in the state. Founded at statehood, in 1907, it was named after the previously established city of Tulsa. Before statehood, the area was part of both the Creek Nation and the Cooweescoowee District of Cherokee Nation in Indian Territory.
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U.S. Route 412 is a U.S. highway in the south-central portion of the United States, connecting Springer, New Mexico to Columbia, Tennessee. A 504.11-mile (811.29 km) section of the highway crosses the state of Oklahoma, traversing the state from west to east. Entering the state southwest of Boise City, US-412 runs the length of the Oklahoma Panhandle and serves the northern portion of the state's main body, before leaving the state at West Siloam Springs. Along the way, the route serves many notable cities and towns, including Boise City, Guymon, Woodward, Enid, and the state's second-largest city, Tulsa.
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The combination of topographic and climatic factors in the Tulsa, Oklahoma area have frequently caused major flash flooding, especially near streams that normally drain the area. The city was founded atop a bluff on the Arkansas River. Thus, elevation protected most of the inhabitants and their possessions from damage when the river flooded. However, by the turn of the 20th Century the population growth had moved closer to the river, and the flatlands west of the Arkansas had begun to develop as well. The floods typically caused widespread property damage and sometimes death. By the 1920s, seasonal floods of the Arkansas began to cause serious damage and loss of life. Since its founding, city leaders had responded to such events by simply rebuilding and replacing the property that had been destroyed in situ. Not until 1970 did the city government begin developing strategies to mitigate floods or at least minimize property damage and prevent loss of life. This article describes some of the more notable floods in Tulsa, then the mitigation and control strategies that evolved from them.
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