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The Keya Paha River is a river flowing 127 miles (204 km) through the U.S. states of South Dakota and Nebraska.
The Walker River is a river in west-central Nevada in the United States, approximately 62 miles (100 km) long. Fed principally by snowmelt from the Sierra Nevada mountains of California, it drains an arid portion of the Great Basin southeast of Reno and flows into the endorheic basin of Walker Lake. The river is an important source of water for irrigation in its course through Nevada; water diversions have reduced its flow such that the level of Walker Lake has fallen 160 feet (49 m) between 1882 and 2010. The river was named for explorer Joseph Reddeford Walker.
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Schoharie Creek is a river in New York that flows north 93 miles (150 km) from the foot of Indian Head Mountain in the Catskills through the Schoharie Valley to the Mohawk River. It is twice impounded north of Prattsville to create New York City's Schoharie Reservoir and the Blenheim-Gilboa Power Project.
Streamflow, or channel runoff, is the flow of water in streams, rivers, and other channels, and is a major element of the water cycle. It is one component of the runoff of water from the land to waterbodies, the other component being surface runoff. Water flowing in channels comes from surface runoff from adjacent hillslopes, from groundwater flow out of the ground, and from water discharged from pipes. The discharge of water flowing in a channel is measured using stream gauges or can be estimated by the Manning equation. The record of flow over time is called a hydrograph. Flooding occurs when the volume of water exceeds the capacity of the channel.
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The Beaver River is an intermittent river, 280 miles (450 km) long, in western Oklahoma and northern Texas in the United States. It is a tributary of the North Canadian River, draining an area of 11,690 square miles (30,300 km2) in a watershed that extends to northeastern New Mexico and includes most of the Oklahoma Panhandle.
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Toby Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 10.5 miles (16.9 km) long and flows through Dallas Township, Dallas, Kingston Township, Courtdale, Luzerne, Pringle, Kingston, Edwardsville, and Larksville. The watershed of the creek has an area of 36.5 square miles (95 km2). The entire drainage basin is designated as a Migratory Fishery and parts are designated as either a Coldwater Fishery, a Warmwater Fishery, or a Trout Stocking Fishery. The creek has two named tributaries: Huntsville Creek and Trout Brook. It is said to show "some degraded conditions", but does not experience severe pollution and is not considered to be impaired. The creek is piped underground in Pringle, but resurfaces in Edwardsville.
Climate change in Nebraska encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Nebraska.
References
- ↑ U.S. Geological Survey Geographic Names Information System: Pumpkin Creek (Nebraska)
- 1 2 3 Shumway, Grant Lee (1921). History of Western Nebraska and Its People. Western publishing & engraving Company. p. 40.
- 1 2 3 4 5 6 7 8 9 Network, University of Nebraska-Lincoln | Web Developer. "Pumpkin Creek History | Nebraska Extension". extension.unl.edu. Retrieved 2018-09-23.
- 1 2 3 "USGS Surface Water data for USA: USGS Surface-Water Annual Statistics". waterdata.usgs.gov. Retrieved 2018-09-23.
- 1 2 3 Network, University of Nebraska-Lincoln | Web Developer. "Pumpkin Creek Project | Nebraska Extension". extension.unl.edu. Retrieved 2018-09-23.
- ↑ Network, University of Nebraska-Lincoln | Web Developer. "Regulations & Policies | UNL Water". water.unl.edu. Retrieved 2018-09-23.
Coordinates: 41°38′01″N103°01′29″W / 41.6335853°N 103.0246517°W