Klamath Basin

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Klamath Basin Klamath Basin.jpg
Klamath Basin

The Klamath Basin is the region in the U.S. states of Oregon and California drained by the Klamath River. It contains most of Klamath County and parts of Lake and Jackson counties in Oregon, and parts of Del Norte, Humboldt, Modoc, Siskiyou, and Trinity counties in California. The 15,751-square-mile (40,790 km2) drainage basin is 35% in Oregon and 65% in California. In Oregon, the watershed typically lies east of the Cascade Range, while California contains most of the river's segment that passes through the mountains. In the Oregon-far northern California segment of the river, the watershed is semi-desert at lower elevations and dry alpine in the upper elevations. In the western part of the basin, in California, however, the climate is more of temperate rainforest, and the Trinity River watershed consists of a more typical alpine climate.

Contents

Geology and hydrology

The Upper Klamath Watershed lies between the Cascade Range and the Basin and Range Province in southern Oregon and northern California. Bedrock stratigraphy in the area includes volcanic deposits, volcanic ejecta, and fluviolacustrine deposits. [1] This creates three general hydrologic layers: 1) Highly permeable basalt with an older depositional age serving as the principle aquifer, 2) fluvial deposits made up of tuff, shale, agglomerate, sandstone, and volcanic ash that are collectively known as the Yonna Formation and act as a groundwater cap, and 3) more recent eruptive volcanic deposits that overlie the aquifer. [2] Little water is able to permeate through the upper volcanic deposit layers to the principle aquifers. Groundwater is able to move freely throughout the upper basin despite geologic structures that occur due to normal faulting which only confine groundwater on a local scale. [3] Artesian wells discharging into the Upper Klamath Lake are essential for recharge into the lake and Klamath River flow throughout the year. [4] Snowmelt is currently a large contributor of groundwater recharge in the Upper Klamath Basin. [5]

Distribution of subwatersheds

Map of Klamath River watershed showing subwatershed boundaries KlamathBasin-location.jpg
Map of Klamath River watershed showing subwatershed boundaries

The drainage basins of the Williamson and Sprague Rivers, in Oregon, are to the north and northeast of Upper Klamath Lake. Together, the two watersheds cover 3,069 square miles (7,950 km2), or 19.4% of the Klamath River watershed. [6] [7] [8] The basin of the Lost River, the largest subwatershed by area, lies to the southeast of Upper Klamath Lake and to the east of Lower Klamath Lake. This covers 3,009 square miles (7,790 km2) or 19.1% of the Klamath River watershed - nearly as much as the Williamson and Sprague. Proceeding west, the adjoining Butte Creek, Shasta, Scott and Salmon River watersheds have 603 square miles (1,560 km2), 795 square miles (2,060 km2), 813 square miles (2,110 km2), and 750 square miles (1,900 km2), respectively. These account for 4.3%, 5%, 5.2%. and 5% of the Klamath River watershed, respectively, or 19.5% of the watershed if put together. [6] [7] [8]

Further southwest, the watershed of the Trinity River, the second largest subwatershed of the Klamath, has 2,965 square miles (7,680 km2) or 19% of the watershed. The watershed of the South Fork Trinity River is 980 square miles (2,500 km2) - 33% of the Trinity watershed or 6% of the Klamath watershed. The primary tributaries of the Klamath together account for 77% of the total Klamath watershed - the remaining land area is drained by smaller tributaries such as Jenny Creek, Fall Creek and Blue Creek. [6] [7] [8]

Major bodies of water

The Upper Klamath Basin today, showing the remnants of the vast Lake Modoc Lower Klamath NWR marsh and mountains.JPG
The Upper Klamath Basin today, showing the remnants of the vast Lake Modoc

Upper Klamath Lake is the largest present-day body of water in the Klamath River watershed, covering 96 square miles (250 km2) on average, with a shoreline of 87 miles (140 km). It is also the largest freshwater lake in the state of Oregon. [9] Historically, Lower Klamath Lake and Tule Lake were one interconnected freshwater marsh that totaled 195 square miles (510 km2) - more than twice the present-day dimensions of Upper Klamath Lake, and larger than Lake Tahoe in central California. This interconnected wetland still supports up to 3.7 million migrating birds per year. [10] In wet years, the two lakes would connect to Upper Klamath Lake, forming one huge body of water. These lakes occupy the basin that was prehistorically occupied by Lake Modoc, a 1,100-square-mile (2,800 km2) freshwater lake that covered the entire Upper Klamath Basin, or 7% of the watershed - an area three times larger than the massive Salton Sea in southern California. This lake existed up to 11,000 years ago at the end of the most recent ice age. [11] Today, Upper Klamath Lake encompasses just 0.6% of the Klamath watershed.

There are also several artificial bodies of water in the watershed - including Lake Ewauna, J.C. Boyle Reservoir, Copco Lake, and Iron Gate Reservoir on the main Klamath. [12] Lake Ewauna, also called Keno Reservoir, is 3.8 square miles (9.8 km2) in size, and is about 20 miles (30 km) long. [13] The J.C. Boyle Reservoir is much smaller, with a surface area of 0.65 square miles (1.7 km2). [14] Copco Reservoir is about 5.4 miles (8.7 km) long and is 1 square mile (2.6 km2) in area. [15] Iron Gate Reservoir covers 1.4 square miles (3.6 km2) and is about 6.8 miles (10.9 km) long. [16] Together, the four lower mainstem reservoirs total just 6.85 square miles (17.7 km2), or 0.04% of the Klamath River watershed.

Trinity Lake, on the mainstem of the Trinity River, is the largest tributary reservoir in the Klamath River watershed. At 25 square miles (65 km2) in size, it is larger than all four mainstem Klamath reservoirs combined (excluding Upper Klamath Lake). [17]

Landscape of the basin Klamath Basin landscape.jpg
Landscape of the basin

Watershed

According to the USGS watershed classification system, the Klamath Watershed is a 6-digit, level 3 Accounting Unit within Region 18, known as the California watershed region. [18] The accounting unit of the Klamath Watershed is 180102 and includes twelve 8-digit Hydrologic Units (HUCs) covering 9.4 million acres. [19] In the 2000 census, about 114,000 people were estimated to be living within the Klamath Watershed. The largest population centers include Klamath Falls, Oregon (19,462) and Yreka, California (7,290). [20] Land ownership within the basin breaks down into the following: about 90,000 acres are controlled by tribal reservations, 6.2 million acres are managed by public agencies (including the Bureau of Land Management, National Forests, National Wildlife Refuges, and National Park Service), and 3.7 million is privately owned. [21] Of the privately owned land, 557,000 acres are used for farming 80% of which is irrigated farmland. Nearly half of irrigated land utilizes water from the Bureau of Land Management’s Klamath Project. The vast majority of privately owned agriculture and rangeland occurs in the Lost River and Shasta River sub-basins. [22]

The Klamath Basin watershed includes:

These three rivers are located above (north) of the Klamath Lake basin:

These features are inside or near the Klamath Lake basin:

These are the major downstream tributaries of the Klamath River:

Communities

Communities in the Klamath Basin include:

See also

Related Research Articles

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Williamson River (Oregon)

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The Klamath River is a river in southern Oregon and northern California in the United States. This article describes its course.

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The Klamath River Hydroelectric Project is a series of hydroelectric dams and other facilities on the mainstem of the Klamath River, in a watershed on both sides of the California/Oregon border.

Klamath River (Hydroelectric Project)

The Klamath river begins below Upper Klamath Lake in Southern Oregon and flows about 300 miles through Northern California until draining into the Pacific ocean. Upper Klamath Lake is the largest freshwater lake in Oregon and was established by the late Pliocene period. The lake fills a graben that is thousands of meters deep. The Klamath Basin lies on the edge of the Basin and Range province and is adjacent to the High Cascades of Southern Oregon.

References

  1. ↑ Upper Klamath Basin Groundwater Study (2013). In United States Geological Survey: Oregon Water Projects. Retrieved from http://or.water.usgs.gov/projs_dir/or180/background.html
  2. ↑ Leonard, A. R. and Harris, A. B. (1974). Ground water in selected areas in the Klamath Basin, Oregon. Salem: Oregon State Engineer.
  3. ↑ Sherrod, D. R. and Pickthorn L. B. G. (1992). Geologic Map of the Klamath Falls: 1° by 2° quadrangle, south-central, Oregon.
  4. ↑ Snyder D. T. and Morace J. L. (1997). Nitrogen and phosphorus loading from drained wetlands adjacent to Upper Klamath and Agency Lakes, Oregon. Portland, Oregon: U.S. Department of the Interior, U.S. Geological Survey.
  5. ↑ Klamath River Basin (n.d.). In United States Department of Agriculture: Natural Resources Conservation Service. Retrieved from https://www.nrcs.usda.gov/wps/portal/nrcs/detail/national/home/?cid=nrcs143_023523
  6. 1 2 3 Hydrology, Ecology and Fishes of the Klamath River Basin, p.27
  7. 1 2 3 BEST and WSTB, p. 26
  8. 1 2 3 "Klamath River Basin - Overview". United States Department of Agriculture Natural Resources Conservation Service . www.nrcs.usda.gov. Retrieved 2009-08-21.
  9. ↑ "Klamath Lake". Oregon Lakes Association. www.oregonlakes.org. Archived from the original on 2009-06-27. Retrieved 2009-08-21.
  10. ↑ Blake, Blake and Kittredge, p. 1
  11. ↑ Delong, Jay. "Walking in 100-Year-Old Footsteps in Southern Oregon". North American Native Fishes Association. www.nanfa.org. Retrieved 2009-08-21.
  12. ↑ "Klamath River Dam and Sediment Investigation" (PDF). Yurok Tribe of California. www.yuroktribe.org. November 2006. Retrieved 2009-08-21.
  13. ↑ "Lake Ewauna/Keno Reservoir Reach Location and Characteristics" (PDF). PacifiCorp Klamath Hydroelectric Project. PacifiCorp. Archived from the original (PDF) on 2004-02-22. Retrieved 2009-08-21.
  14. ↑ "J.C. Boyle Reservoir - Reservoir Location and Characteristics" (PDF). PacifiCorp Klamath Hydroelectric Project. PacifiCorp. Archived from the original (PDF) on 2004-02-22. Retrieved 2009-08-21.
  15. ↑ "Project Description". Klamath Basin Tribal Water Quality Work Group. www.klamathwaterquality.com. Retrieved 2009-08-21.
  16. ↑ "Iron Gate Reservoir: Reservoir Location and Characteristics" (PDF). PacifiCorp Klamath Hydroelectric Project. www.pacificorp.com. Archived from the original (PDF) on 2003-08-24. Retrieved 2009-08-21.
  17. ↑ "Shasta/Trinity River Division Project". U.S. Bureau of Reclamation . www.usbr.gov. Archived from the original on 2013-02-22. Retrieved 2009-08-21.
  18. ↑ United States Geological Survey (2014). Water Resources of the United States: Boundary descriptions and names of regions, subregions, accounting units, and cataloging units. Retrieved from http://water.usgs.gov/GIS/huc_name.html#Region18
  19. ↑ United States Geological Survey (2014). Water Resources of the United States: Boundary descriptions and names of regions, subregions, accounting units, and cataloging units. Retrieved from http://water.usgs.gov/GIS/huc_name.html#Region18
  20. ↑ Population and Land Ownership (2009). In Klamath Basin Water Crisis. Retrieved from http://www.klamathbasincrisis.org/tmdl/populationandlandownership082809.htm
  21. ↑ Klamath Basin (n.d.). In Center for Science and Technology Policy Research. Retrieved from http://cstpr.colorado.edu/klamathbasin/background/physical.html
  22. ↑ United States Department of Agriculture: Natural Resources Conservation Service (2002). Klamath River Basin: Land Use/Land Cover Map. Retrieved from https://www.nrcs.usda.gov/Internet/FSE_MEDIA/nrcs143_022731.jpg

Coordinates: 42°N122°W / 42°N 122°W / 42; -122

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