Silcott, Washington | |
---|---|
Coordinates: 46°24′54.6″N117°11′51.6″W / 46.415167°N 117.197667°W | |
Country | United States |
State | Washington |
County | Asotin |
Elevation | 738 ft (225 m) |
Time zone | UTC-8 (Pacific (PST)) |
• Summer (DST) | UTC-7 (PDT) |
ZIP Code | 99403 |
Area code | 509 |
GNIS feature ID | 1533427 [1] |
Silcott is an unincorporated community and ghost town in Asotin County, in the U.S. state of Washington. [2] It is located on the south bank of the Snake River and U.S. Route 12 passes through the community. [3] Much of the townsite was inundated when Lower Granite Lake filled on the Snake River behind Lower Granite Dam in 1975. [4]
The area that became Silcott was inhabited by the Nez Perce since before recorded history. Lewis and Clark camped in the area during their expedition in 1805 and interacted with the native peoples. In 1837 the first orchard in the Snake River valley was planted in Silcott. The community was initially settled by white people in the mid-1800s and served as a river crossing with a mill and warehouses. In the late 1800s the community was badly damaged in a fire. [5]
A post office called Silcott was established in 1883, and remained in operation until 1931. [6] The community was named after John Silcott, an early settler. [7]
Much of the former townsite was flooded when Lower Granite Lake filled behind Lower Granite Dam in the 1970s. [4]
The Snake River is a major river in the interior Pacific Northwest region of the United States. About 1,080 miles (1,740 km) long, it is the largest tributary of the Columbia River, which is the largest North American river that empties into the Pacific Ocean. Beginning in Yellowstone National Park, western Wyoming, it flows across the arid Snake River Plain of southern Idaho, the rugged Hells Canyon on the borders of Idaho, Oregon and Washington, and finally the rolling Palouse Hills of southeast Washington. It joins the Columbia River just downstream from the Tri-Cities, Washington, in the southern Columbia Basin.
The Grande Ronde River is a 210-mile (340 km) long tributary of the Snake River, flowing through northeast Oregon and southeast Washington in the United States. Its watershed is situated in the eastern Columbia Plateau, bounded by the Blue Mountains and Wallowa Mountains to the west of Hells Canyon. The river flows generally northeast from its forested headwaters west of La Grande, Oregon, through the agricultural Grande Ronde Valley in its middle course, and through rugged canyons cut from ancient basalt lava flows in its lower course. While it joins the Snake River upstream of Asotin, Washington, more than 90 percent of the river's watershed is in Oregon.
The Palouse River is a tributary of the Snake River in Washington and Idaho, in the northwest United States. It flows for 167 miles (269 km) southwestwards, primarily through the Palouse region of southeastern Washington. It is part of the Columbia River Basin, as the Snake River is a tributary of the Columbia River.
Lower Granite Lock and Dam is a concrete gravity run-of-the-river dam in southeastern Washington in the United States. On the lower Snake River, it bridges Whitman and Garfield counties. Opened 49 years ago in 1975, the dam is located 22 miles (35 km) south of Colfax and 35 miles (56 km) north of Pomeroy.
Chengwatana is an abandoned village site in Pine County, Minnesota, United States.
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Salmon Falls Creek is a tributary of the Snake River, flowing from northern Nevada into Idaho in the United States. Formed in high mountains at the northern edge of the Great Basin, Salmon Falls Creek flows northwards 121 miles (195 km), draining an arid and mountainous basin of 2,103 square miles (5,450 km2). The Salmon Falls Creek valley served as a trade route between the Native American groups of the Snake River Plain and Great Basin. Today, most of its water is used for irrigation.
Pactola, also known as Camp Crook, (1875–1950s) is a ghost town in Pennington County, South Dakota, United States. It was an early placer mining town and existed into the early 1950s, when it was submerged under Pactola Lake.
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Gould City is an unincorporated community in Garfield County, in the U.S. state of Washington. It is located at the confluence of North Deadman Creek and South Deadman Creek where the two form Deadman Creek. The townsite, as of 2023 largely a ghost town is located in the thin and deep valley cut by the creeks.
Rogersburg is an unincorporated community in Asotin County, in the U.S. state of Washington. The community is situated across from the state line with Idaho on the southern bank at the confluence of the Grande Ronde and Snake rivers.
Wawawai is a former town in the south central part of Whitman County, Washington in the United States. It got its name from a Nez Perce word said to mean "council ground." The town was platted in 1878 and served a community of orchards along the Snake River. The river would ultimately lead to Wawawai's demise as water rose behind Lower Granite Dam, which was completed in 1975, and submerged what was once Wawawai under 80 feet of water. Wawawai County Park is located along the banks of the river immediately above the former town site.
Asotin Creek is a tributary of the Snake River in Asotin County, southeastern Washington. The creek's main stem is 15.5 miles (24.9 km) long, and measured to the head of its longest tributary its length is 33.7 miles (54.2 km). It flows into the Snake River at the town of Asotin, about 5 miles (8.0 km) south of Lewiston–Clarkston. Asotin Creek drains about 325 square miles (840 km2) of mostly semi-arid plateau country on the northeastern flank of the Blue Mountains.
Alpowa Creek is a stream in Garfield and Asotin Counties, southeastern Washington. It starts near Peola, about 10 miles (16 km) south of Pomeroy, in the foothills of the northern Blue Mountains just outside the Umatilla National Forest. It initially flows north through farmland before descending northeast into a canyon, flanked to the north by Alpowa Ridge and to the south by Knotgrass Ridge. It receives Stember Creek from the left; downstream of there, U.S. Highway 12 runs parallel to it. It empties into the Snake River at Lower Granite Lake, the impoundment formed by Lower Granite Dam, about 8 miles (13 km) to the west of Clarkston.