Touchet Formation

The Touchet Formation (also referred to as Touchet beds) consists of large quantities of gravel and fine sediment which overlays several thousand feet of volcanic basalt of the Columbia River Basalt Group. These Touchet beds are often covered by windblown loess soils which was deposited later. [ [http://www.wallawallawatershed.org/_acrobat/WRIA32Level1/S2%20Regional%20Overview.pdf#search=%22Touchet%20Formation%22 Walla Walla Level 1 Watershed Assessment.] ] cite book|author=Bjornstad, Bruce|title=On the Trail of the Ice Age Floods: A Geological Guide to the Mid-Columbia Basin |publisher=Keokee Books; San Point, Idaho |year=2006|id=ISBN 978-1-879628-27-4]

Naming of the Touchet Formation

The type locality for the Touchet Formation was originally observed at the confluence of the Touchet River with the Walla Walla River by Flint in 1938. Once the phenomena was correctly identified, numerous other examples were also found through the basin of the former Lake Lewis.cite book|author=Carson, Robert J. and Pogue, Kevin R.|title=Flood Basalts and Glacier Floods:Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington |publisher=Washington State Department of Natural Resources (Washington Division of Geology and Earth Resources Information Circular 90)|year=1996|id=ISBN none ]

Creation of the Touchet Formation

The Touchet beds were deposited during the various flood events (e.g., Missoula Floods) that occurred around 16,000 years ago. During the floods, flow through the Wallula Gap was slow enough such that water pooled in a temporary lake, Lake Lewis. Lake Lewis backflooded up the Yakima, Walla Walla, Touchet and Tucannon River Valleys. In these relatively calm arms of the lake, the slack waters were thick with suspended materials eroded from the scablands above. Some of the suspended materials settled out, creating thick Touchet Formation layers or rhythmites which are found throughout these valleys. Typically the heaviest materials settled out first, followed by finer materials, providing a layer with a graduated particle composition.

The side valleys were protected from the violent currents of the main channel; as a result the flood strata laid down by earlier floods was not eroded away by subsequent floods, but was buried and preserved. Other sediments and materials such as volcanic ash from eruptions of Mount St. Helens are interspersed between layers. They serve to date the various Missoula Floods; in 1980, R. B. Waitt studied the Touchet Formation in the wall of the Burlingame Canyon west of Walla Walla, Washington, where he counted at least 41 flood deposit layers. These floods could only occur when glacial Lake Missoula existed, which estimates at 15,300 to 12,700 years ago. Mt. St. Helens "S" ash fell in eastern Washington about 13,000 years B.C.E. and is ten rhythmites below the top of the Touchet beds. [cite book|author=Waitt, R.B.|title=About Forty Last-glacial Lake Missoula Jökulhlaups through Southern Washington |publisher=Jour. Geology, v. 88, p. 653-679 |year=1980|id=ISBN none] [cite book|author=Waitt, R.B.|title=Case for Periodic, Colossal Jökulhlaups from Pleistocene Glacial Lake Missoula|publisher=Geol. Soc. America Bull., v. 96, p. 1271-1286.|year=1985|id=ISBN none] More recent studies have used carbon dating to establish the ages of deposition for the various layers.

Locations where Touchet beds are evident

Touchet river valley

The Touchet Formation was originally identified at the confluence of the Touchet River with the Walla Walla River. These formations are found at some distance up the Touchet River Valley.

Walla Walla river valley

The Walla Walla River Valley is a closed basin with the river entering a broad open area about 8 miles above the confluence with the Columbia. West of the city of Walla Walla, Touchet Beds are common. The Gardena Terrace rhythmites can be found most of the way to Walla Walla, Washington. They are extensively exposed at Burlingame Canyon, just southwest of the town of Touchet near the confluence ot the Touchet and Walla Walla Rivers. cite book|author=J.E.Allen and M. Burns with S.C. Sargent |title=Cataclysms on the Columbia |publisher=Timber Press, Portland, Oregon |year=1986 (reprinted 2005) |id=ISBN 0-88192-215-3]

Yakima river valley

Lake Lewis extended up the Yakima Valley, flooding an area of about 600 mi² of the valley and covering the area of the present day Yakima, Washington by about 200 feet. The valley extends for 80 miles, widening westwards above the Chandler Narrows and then narrowing again at Union Gap just below the town of Yakima. The Toppenish Basin and Benton Basin of the lower Yakima river both have extensive Touchet beds. Rhythmites are extensively exposed 1 mile north of Mabton and at Zillah. Ice rafted erratics are also commonly found in these beds. [ [http://pubs.usgs.gov/sir/2006/5116/section7.html USGS publication ] ]

Tucannon river valley

The Tucannon River and its tributary, the Pataha Creek have valleys partially filled with alluvial deposits. Flood plain deposits consist of the Touchet Beds, loess silt and fine sand. These alluvial deposits narrow as they approach the basalt valley walls, and thicken into the central valley, with a maximum alluvial thickness of between 20 & 100 feet.

References

ee also

*Varve