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Palouse - Wikipedia. The Palouse (pə- LOOSS) is a region of the northwestern. United States, encompassing parts of southeastern. Washington, north central. Lost Wilderness Full Movie Part 1. Idaho and, by some definitions, parts of northeast Oregon. It is a major agricultural area, primarily producing wheat and legumes.

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Situated about 1. Watch Half Baked Online Gorillavid. Oregon Trail, the region experienced rapid growth in the late 1. Washington's most populous region, surpassing even the Puget Sound area.[1]The Palouse is home to two land grant universities, the University of Idaho in Moscow and Washington State University in Pullman. Just eight miles (1. Geography and history[edit]The origin of the name "Palouse" is unclear. One theory is that the name of the Palus tribe (spelled in early accounts variously as Palus, Palloatpallah, Pelusha, etc.) was converted by French- Canadian fur traders to the more familiar French word pelouse, meaning "land with short and thick grass" or "lawn." Over time, the spelling changed to Palouse.[2] Another theory is that the region's name came from the French word and was later applied to its indigenous inhabitants.

Traditionally, the Palouse region was defined as the fertile hills and prairies north of the Snake River, which separated it from Walla Walla County, and north of the Clearwater River, which separated it from the Camas Prairie, extending north along the Washington and Idaho border, south of Spokane, centered on the Palouse River. This region underwent a settlement and wheat- growing boom during the 1. Washington, originally pioneered in Walla Walla County south of the Snake River.[3]While this definition of the Palouse remains common today, the term is sometimes used to refer to the entire wheat- growing region, including Walla Walla County, the Camas Prairie of Idaho, the Big Bend region of the central Columbia River Plateau, and other smaller agricultural districts such as Asotin County, Washington, and Umatilla County, Oregon. This larger definition is used by organizations such as the World Wide Fund for Nature, who define the Palouse Grasslands ecoregion broadly.[4]The community of Palouse, Washington, is located in Whitman County, about 7 miles (1. Potlatch, Idaho. Nevertheless, the traditional definition of the Palouse region is distinct from the older Walla Walla region south of the Snake River, where dryland farming of wheat was first proved viable in the region in the 1.

During the 1. 87. Walla Walla region was rapidly converted to farmland, while the initial experiments in growing wheat began in the Palouse region, which previously had been the domain of cattle and sheep ranching. When those trials proved more than successful, a minor land rush quickly filled the Palouse region with farmers during the 1. The simultaneous proliferation of railroads only increased the rapid settlement of the Palouse. By 1. 89. 0 nearly all the Palouse lands had been taken up and converted to wheat farming.[5]Unlike the Walla Walla Country, which was solidly anchored on the city of Walla Walla, the Palouse region saw the rise of at least four centers, all within several miles of each other: Colfax (the oldest), Palouse, Pullman, and on the Idaho side, Moscow.

These four centers, along with at least ten lesser ones, resulted in a diffuse pattern of rural centers, relative to the centralized Walla Walla county.[6]Cities along the borders of the Palouse, and by some definitions included within it, include Lewiston, Idaho, serving the Camas Prairie farmlands; Ritzville, serving the eastern edge of the Big Bend Country; and Spokane, the region's major urban hub. So dominant was Spokane's position that it became known as the capital of the Inland Empire, including all the wheat- producing regions, the local mining districts, and lumber- producing forests. Spokane also served as the region's main railroad and transportation hub. By 1. 91. 0, although local terms like Palouse, Walla Walla Country, Big Bend, Umatilla Country, and Camas Prairie continued to be common, many people of the region began to regard themselves as living in the Inland Empire, the Wheat Belt, the Columbia Basin, or simply Eastern Washington, Oregon, or North Idaho.[7]Geology[edit]The peculiar and picturesque loess hills which characterize the Palouse Prairie are underlain by wind- blown sediments of the Palouse Loess that covers the surface of over 5. Columbia Plateau in southeastern Washington, western Idaho, and northeastern Oregon.

The Palouse Loess forms a fine- grained mantle of variable thickness that lies upon either the Miocene. Columbia River Basalt Group, non- glacial Pliocenefluvial sediments of the Ringold Formation, or Pleistocene glacial outburst flood sediments that are known informally as the Hanford formation. At its thickest, the Palouse Loess is up to 7.

It consists of multiple layers of loess separated by multiple well- defined calcretepaleosols and erosional unconformities. The degree of development of individual layers of calcrete together with thermoluminescence and optically stimulated luminescence dating of the loess indicate that each calcrete layer represents a period of thousands to tens of thousands of years of nondeposition, weathering, and soil development that occurred between episodic periods of loess deposition. A consistent sequence of normal- reverse- normal polarity signatures demonstrates that the older layers of loess accumulated between 2 and 1 million years ago. Detailed optically stimulated luminescence dating has shown that the uppermost layer of Palouse Loess accumulated between 1.

Regional trends in the distribution, thickness, texture, and overall composition of the Palouse Loess indicate that it largely consists of the wind- blown sediments eroded from fine- grained deposits of the Hanford formation that were periodically deposited by repeated Missoula Floods within the Eureka Flats area.[8][9][1. Showtime Full Love Bite Online Free more. Although superficially resembling sand or other types of dunes, the loess hills of the Palouse are of far different origin.

Internally, they lack any evidence of cross- bedding or erosion of interbedded layers of loess and calcrete that characterize dunes formed by moving currents. Instead, these hills consist of alternating layers of loess and calcrete that are more or less concordant with the modern surface of these hills. This layering demonstrates that the Palouse hills loess accumulated from the airfall of wind- silt from suspension. In addition, the ubiquitous homogenization of the loess by innumerable plant roots and insect burrows as it accumulated further supports the conclusion drawn from numerous thermoluminescence and optically stimulated luminescence dates that individual layers of loess accumulated over an extended period of time in terms of thousands of years.

Finally, the calcrete horzons are paleosols that represent the periodic cessation of loess accumulation for periods of thousands of years during which they formed within the surface of a loess layer.[1. Farming[edit]Early farming was extremely labor- intensive and relied heavily on human and horse- power.

An organized harvesting/threshing team in the 1. Teams moved from farm to farm as the crops ripened. By this point, the combine had been invented and was in use, but few farmers had enough horses to pull such a machine, which required a crew of 4. Because of this, use of combines on the Palouse lagged behind use in other farming communities in the United States. It was only when the Idaho Harvester Company in Moscow began to manufacture a smaller machine that combine harvesting became feasible.

By 1. 93. 0, 9. 0% of all Palouse wheat was harvested using combines.[1. The next step in mechanization was development of the tractor. As with the combines, the first steam engine and gasoline- powered tractors were too heavy and awkward for use on the steep Palouse hills. The smaller, general use tractors introduced in the 1.

As a result, by 1. Palouse farmers used tractors.[1. Today, the Palouse region is the most important lentil- growing region in the USA.[1.