- Yakama Nation Treaty of 1855
- Tecumseh, Shawnee Chief
- Chief Bluejacket, Shawnee
- Augustine Indian Reservation
- Alturas Indian Reservation
- Treaty With The Cheyenne And Arapaho, 1865
- Treaty With The Apache, Cheyenne, And Arapaho, 1865
- Assiniboine (Nakoda) Treaties
- Arikara Treaties
- Shasta (Chasta) Treaties
- Arapaho Treaties
- Anadarko Treaties
- Aionai Treaties
- Appalachicola Treaties
- Apache Treaties
Plateau Region Tribes
Columbia Plateau and the Tribes who lived in this region
Location: Washington | Oregon | Idaho | Part of Montana | Part of CaliforniaThe Plateau Region has three sub-regions: the Sierra and Cascade Mountains, the Rocky Mountains, and the Columbia Plateau, which are further divided into 14 ecoregions. At least forty-seven tribes called this area home.
The Columbia Plateau is bordered by the Northern Rocky Mountains to the east and in the west by the Sierra Nevada and Cascade Mountain ranges. The plateau covers an area of about 100,000 square miles (260,000 square km) in British Columbia, Canada, and Washington, Oregon, and a small part of Idaho that is mostly covered with basaltic lava flows. The mountainous regions extend into northern California, parts of Washington and northwestern Montana.
The elevation ranages from 500 feet to 5,000 feet (60 to 1,500 m) above sea level on the plateau, and over 14,000 feet in the mountains.
The climate is semi-arid highland desert, and vegetation is limited mostly to sagebrush shrubs and grasses on the plateau.
It includes nearly 500 miles (800 km) of the Columbia River, as well as the lower reaches of major tributaries such as the Snake and Yakima rivers and their associated drainage basins.
The Columbia and Snake Rivers are the major water systems in the region. Other rivers include the Deschutes, John Day, Umatilla, and Walla Walla rivers.
The extensive Columbia River system drains the Rocky Mountains on its way to the Pacific Ocean. As it flows to the Columbia River, the Snake River passes through a broad plain in southern Idaho—the Snake River plain.
The ancient Columbia River was forced into its present course by the northwesterly advancing lava. The lava, as it flowed over the area, first filled the stream valleys, forming dams that in turn caused numerous lakes to form.
A porous, volcanic bedrock lies underneath the plain, so Snake River tributaries often disappear underground, thus creating a need for irrigation. After coursing through this plain, the Snake River flows through Hell's Canyon—a 6,000-foot-deep gorge—before reaching the Columbia River.
This main river also carves its way through a relatively open area, the Palouse hills of Washington, another irrigated farm region. Aside from the Palouse hills and the Snake River plain, much of the Columbia Plateau consists of mountains, such as the Blue Mountains, that lie in the rain shadow of the Cascade Mountains.
The average precipitation in this area is only 12 inches per year, with most moisture falling in the form of winter snows in the mountains.
There are five volcanoes in the Columbia Plateau region, which were visited by Lewis and Clark on their epic journey. They are Mount Adams, Mount Hood, Mount Jefferson, Mount Rainier, and Mount St. Helens. Mount St. Helens had a massive eruption as recently as 1980, which blew out the side of the mountain and deposited significant ash hundreds of miles away. All together, there are 27 active volcanic areas in the Plateau Region today, with ten volcanoes having a high probability of eruption in this century.
Also known as the Columbia Basin, and originally carved by glaciers and slowly eroded over time by the Columbia River, the basin was further sculpted about 12,000 years ago by a series of violent flows known as the Spokane Floods. The floods left behind strange basaltic rock formations known as the Channeled Scablands.
The basin is characterized by native shrub-steppe vegetation and thousands of acres of ponds and marshes created by irrigation water from the Columbia Basin Project. Southwest Washington includes the vast wheat fields of the Palouse Hills and the rugged Blue Mountains which straddle the border between Washington and Oregon.
During the early stages of the Columbia Basin formation, granite rock was slowly created by heat and pressure deep in the crust of the earth. Then the crust was uplifted, exposing the granite, creating mountains similar to the Okanogan Highlands north of Grand Coulee Dam. Forty to sixty million years ago the formation of the outline of the Columbia Basin was complete. The land had subsided below sea level, and a large inland sea had formed. The land was again uplifted and then, 10-15 million years ago, was flooded with volcanic lava. The boundaries of the flood lava were located in almost the same position as the former seashore. Many layers of lava were needed to build up to a 5,000 feet (1500 meter) thickness and form the smooth surfaced Columbia Plateau.
During the Ice Age, the old Cascade Mountains were also formed. Their outline still remains on the western slopes of the Cascades. The uplifting mountains were not able to block the flow of the Columbia River completely, and a deep Columbia River gorge was formed. Near the end of the Ice Age the volcanoes of the high Cascades rose to elevations of 14,000-15,000 feet (4000-4500 meters). Older volcanoes, such as Mt. Hood and Mt. Rainier, were sculpted by glaciers of the Ice Age; others such as Mt. St. Helens remained unsculpted, retaining their original volcanic form.
Eighteen thousand years ago the Columbia Basin was nearly covered by floodwaters when an ice dam at Lake Missoula in western Montana broke. Large boulders were strewn near the outlet of the Lower Coulee (Lake Lenore). Other boulders were carried in icebergs as far as western Oregon.
The floodwaters were 800 feet (250 meters) deep near Pasco and 400 feet (125 meters) deep at Portland. After the Ice Age, the Columbia River returned to its former channel. The channeled scab lands and large coulees that had been formed were left stranded 500-1600 feet (150-500 meters) above the present river floor and serve as a constant reminder of some of the most unusual episodes in geologic history.
- Cayuse, Oregon
- Celilo (Wayampam)
- Upper Chinookan (Dialects: Clackamas, Cascades, Hood River Wasco, Wishram Kathlamet, Wishram, Cathlamet, Multnomah)
- Columbian (Dialects: Wenatchee, Sinkayuse, Chelan) Washington, Oregon
- Coeur d'Alene, Idaho
- Colville, Washington
- Upper Cowlitz
- Flathead (Selisch or Salish), Idaho and Montana
- John Day
- Kalispel Washington
- Klamath, Oregon
- Klikitat, Washington
- Kootenai/Ktunaxa, British Columbia, Montana, Idaho
- Lower Snake (Chamnapam, Wauyukma, Naxiyampam)
- Modoc, California, Oregon
- Molala (Molale) Oregon
- Nez Perce, Idaho and Washington
- Nicola Athapaskans (extinct)
- Nlaka'pamux aka the Thompson people, British Columbia
- Okanagan (Siylx), British Columbia & Washington (Dialects: Northern and Southern)
- Palus (Palouse), Washington
- Pend'Oreilles (Kalispel), Washington
- Rock Creek
- Secwepemc (Shuswap), British Columbia
- Sinixt (Lakes Indians), British Columbia, Washington, Idaho
- Spokane, Washington
- St'at'imc (Lillooet)
- Tygh Valley
- Umatilla Oregon
- Upper Nisqually (Mishalpan)
- Walla Walla, Oregon and Washington
- Wasco, Oregon
- Yakama (Yakima), Washington
The Confederated Tribes of the Umatilla Indian Reservation is a combination of the Umatilla (Natítayt, meaning The People) , Walla Walla, and Cayuse tribes of Oregon.
Salish nations inhabited the upper Columbia River and middle Fraser River regions of the Cordillera, and were separated from the coastal region by the Cascade and Coast Mountains, through which the Columbia and Fraser Rivers flow. They include the Flathead and Pend d’Oreille nations of present-day Montana; the Coeur d’Alene of Idaho; the Kalispel, Colville, Spokan, Sanpoil, Nespelem, Methow Penskwaus, Wenatchee, Okanogan-Similkameen, and Sintaiekt of Washington; and the Lakes Sinixt, Okanagan-Similkameen, Secwepemc, Nlakapmx, and St’at’imc of British Columbia.
The Colville Confederated Tribes are comprised of 12 plateau bands which include the Moses-Columbia, Sanpoil, Nespelem, Methow, Entiat, Colville, Lakes, Wenatchee (Wenatchi), Chief Joseph’s Band of Nez Perce, Palus, Southern Okanogan, and Chelan. Their ancestral lands incorporated approximately thirty nine million acres in Central Washington and Southern British Columbia.
Coeur d’Alene Indian villages were numerous and permanent, each village and the people there had a distinct name in their ancestral language. Collectively, members today call themselves, "Schitsu'umsh," meaning "Those Who Are Found Here."
The Spokane Tribe (sqeliz – meaning The People) is comprised of five bands: sntu/t/uliz, snzmeme/, scqesciOni, sl/otewsi, hu, and sDmqeni. Their traditional homelands spanned most of present day Eastern Washington: north to Canada, east to Idaho, south to the Columbia River, and as far west as the Cascades.
The Yakamas have lived in Central and South Central Washington since time immemorial. The lands of the Yakama extended in all directions along the Cascade Mountain Range to the Columbia River and beyond. Tribal elders say their distance of travel sometimes took them as far north as Canada and as far south as California. The Yakama Nation includes these bands: Kah-miltpah, Klickitat, Klinquit, Kow-was-say-ee, Li-ay-was, Oche-Cotes, Palouse, Pesquose, See-ap-Cat, Sk'in-pah, Shyiks, Wisham, Wenachapam, and Yakama.
Battle of Steptoe Butte