Lake Roosevelt National Recreation Area
The Mighty Columbia…The river
now becomes deeply encañoned….the bluffs are many-colored….To this
must be added the green of the trees….the old gold of the
bunch-grass shining in the sunlight….forming one of the grandest,
most beautiful sights in the universe. Lt. Thomas W. Symons,
Columbia River Navigation Survey, 1881.
Columbia River
For thousands
of years the Columbia River flowed wild and free. The untamed
waters made their way to the Pacific – changing channels, skirting
glaciers, suddenly flooding – controlled only by what nature
dictated. Nomadic Indians moved with the seasons and followed their
sources of food. Various Salishan tribes in the north whose lived
centered around the Columbia River called it Swah-netk-qhu – Big
Water. Indians knew the river for its rich salmon runs and, in the
1800s, traders and settlers knew it as a transportation route that
brought supplies upriver and delivered furs and crops downriver. In
the mid-1900s the building of dams harnessed the river as never
before. People now experienced the river in new ways. Dams provided
electricity and irrigation water and protected homes from flooding.
Construction of Grand Coulee Dam led to the creation of Lake
Roosevelt. In 1946 the area was federally designated a national
recreation area.
Today sagebrush and golden bunchgrass
adorn the shores along the southern half of the lake. Lichens
on basalt cliffs add splashes of yellow, red, and green. The
northern half of the park reveals cooler mountains forested
with ponderosa pine, Douglas fir, and western larch. As
Lieutenant Symons did in 1881, you can marvel at the landscape
– it is still a grand and most beautiful sight.Reading the
Rocks
During the ice age a massive glacial lobe moved down from
Canada, creating an ice dam that blocked the natural courses of
rivers. Rivers backed up. Huge lakes formed, including Lake
Missoula. The increasing level of the water behind the ice dam
caused it to float and burst. Sudden, massive walls of water – some
thought to be 400 feet high with speeds approaching 65 miles per
hour – flushed across central Washington. This cycle, glaciers
advancing and retreating, floods caused by ice dams forming and
bursting, repeated many times. The water carried gravel and debris,
icebergs and boulders, scouring bedrock into the bizarre landscape
we call channeled scablands and gouging steep-walled gorges called
coulees.
Fort Spokane and the Indians
Fort
Spokane, established in 1880, was one of the last frontier
forts built in the West. Ownership of land became a problem as
the area filled with entrepreneurs seeking the agricultural
opportunities promoted by the Northern Pacific Railroad.
Keeping the semi-nomadic Spokane and Colville tribes within
reservation boundaries – and keeping land-hungry settlers out
– was potentially a difficult job. The fort’s strategic
location at the confluence of the Columbia and Spokane rivers
allowed a small peace-keeping force to keep an eye on the
Indians and the settlers. Fortunately, this was a time of
relative peace. The troops at Fort Spokane saw little action
aside from routine drills, parades, and patrol duty.
In 1898 most troops left for duty in Cuba after the outbreak of
the Spanish-American War. The post was decommissioned and
transferred to the Bureau of Indian Affairs. The fort opened as an
Indian boarding school in 1900, but declining enrollments closed
the school in 1908. The fort served on and off as a tuberculosis
sanitorium and Indian hospital until its final closure in 1929.
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