Wahluke Slope

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Looking north across Wahluke Slope towards Sentinel Gap Middle-saddle-mountains-sentinel-gap-looking-northwesterly-P4140091.JPG
Looking north across Wahluke Slope towards Sentinel Gap

Wahluke Slope is a geographic feature in Grant, Benton and Adams Counties of Eastern Washington. It is a broad, south-facing slope with a grade of about 8%, [1] situated between the Saddle Mountains and the Columbia River's Hanford Reach. It has been described as "basically a 13-mile-wide gravel bar" created by the Glacial Lake Missoula floods at the end of the last ice age about 15,000 years ago. [2] Much of the Slope, part of the Hanford Nuclear Reservation, was added to the Saddle Mountain National Wildlife Refuge in 1999. [3] Much of the remainder is used for viniculture.

Contents

Human use

Washington State Route 24 extends from Mattawa, Washington on the western edge of the Slope nearly due east–west. Mattawa is the only population center on the Slope. There was once a town of Wahluke and a Wahluke ferry that crossed the Columbia to the north of White Bluffs. [4] [5] The land was acquired by the U.S. government for the Hanford Nuclear Reservation and the residents, including Wanapum people, ordered to leave in 1943. [6] In two actions in 1953 and 1958 the Atomic Energy Commission returned almost 200,000 acres (810 km2) to public use, mostly for agriculture with irrigation recently provided by Columbia Basin Project sources. [7] Settlement on the Slope by non-Native Americans has been termed as troubled, initially due to lack of water, then later by the Federal Government's land policies, resulting in "sporadic" growth of the town of Mattawa. [8]

Nuclear concerns

The potential for release of nuclear contaminants into the Slope in the event of a nuclear accident, and the historical atmospheric releases in the ranges of many Curies per month, are of concern to modern authors on Hanford. [9] [10] [11]

Viniculture

Viniculture is a major agricultural activity on the Slope, with nearly 10,000 acres (40 km2) of vineyards. [2]

Related Research Articles

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<span class="mw-page-title-main">Wahluke Slope AVA</span>

Wahluke Slope is an American Viticultural Area (AVA) located within Grant County, Washington established on January 6. 2006 by the Alcohol and Tobacco Tax and Trade Bureau {TTB), Treasury after reviewing the petition submitted by the Wahluke Slope Wine Grape Growers Association (WSWGGA), represented by Alan J. Busacca, Ph.D., proposing the establishment of the viticultural area named "Wahluke Slope."

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<span class="mw-page-title-main">Savage Island (Washington)</span>

Savage Island lies on the last free flowing stretch of the Columbia River known as the Hanford Reach in Washington, United States; other interesting geological features of the area include the White Bluffs, as well across the river the Hanford Dunes. The island is within the boundaries of the Wahluke Wildlife Unit, a natural preserve managed by the US Fish and Wildlife Service as part of the Hanford Reach National Monument. Historically, Savage Island has supported small farms and settlements ranging from prior to the Manhattan Project buyout of the lands in 1943; The Wanapum tribe were known to inhabit this particular region. The wildlife of the island include mule deer, coyote, burrowing owl, and western diamondback rattlesnake; the island is primarily arid shrub steppe, with some wetland habitat by the shore of the river.

<span class="mw-page-title-main">Rattlesnake Hills</span>

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The Yakima Fold Belt of south-central Washington, also called the Yakima fold-and-thrust belt, is an area of topographical folds raised by tectonic compression. It is a 14,000 km2 (5,400 sq mi) structural-tectonic sub province of the western Columbia Plateau Province resulting from complex and poorly understood regional tectonics. The folds are associated with geological faults whose seismic risk is of particular concern to the nuclear facilities at the Hanford Nuclear Reservation and major dams on the Columbia and Snake Rivers.

<span class="mw-page-title-main">Sentinel Gap</span>

Sentinel Gap is a water gap formed by the Columbia River in the Saddle Mountains, near Mattawa in Washington state. The gap is "a water gap where erosion by the Columbia River was able to keep pace with folding, faulting and uplifting across the Saddle Mountain anticline". During Ice Age floods in which waters from the Channeled Scablands found passage to the Pacific Ocean here and at Wallula Gap, this opening was "repeatedly reamed out, which probably widened and steepened the walls of the gap". Strandlines from the floods can be seen on the basalt walls of the gap.

<span class="mw-page-title-main">Hanford Engineer Works</span> Former American nuclear production complex

The Hanford Engineer Works (HEW) was a nuclear production complex in Benton County, Washington, established by the United States federal government in 1943 as part of the Manhattan Project during World War II. It built and operated the B Reactor, the first full-scale plutonium production reactor. Plutonium manufactured at the HEW was used in the atomic bomb detonated in the Trinity test in July 1945, and in the Fat Man bomb used in the atomic bombing of Nagasaki in August 1945. The HEW was commanded by Colonel Franklin T. Matthias until January 1946, and then by Colonel Frederick J. Clarke.

References

  1. Wahluke Slope characteristics, Washington State Wine Commission
  2. 1 2 "Wahluke Slope is one of Washington wine country's hidden gems", Northwest wine blog, Seattle Post-Intelligencer, July 28, 2010
  3. Ken Olsen (December 20, 1999), "Hanford leaves a surprising Cold War legacy", High Country News
  4. Saddle Mountain Unit (PDF) (Fact sheet), U.S. Fish and Wildlife Service, August 2002
  5. Metsker's Map of Grant County, Washington
  6. Sanger 1995, pp. 16–18.
  7. Brown 2013, p. 187.
  8. Kirk & Alexander 1995, p. 116.
  9. Brown 2013.
  10. Gerber & Findlay 2007.
  11. PSR 2010.

Sources

46°45′N119°30′W / 46.750°N 119.500°W / 46.750; -119.500