Home Valley, Washington

Wyeth is an unincorporated locale in Hood River County, Oregon, United States. It is the site of a campground area in the Columbia River Gorge National Scenic Area off Interstate 84 (I-84). It was a railway station and had a post office between 1901 and 1936. It was named after explorer Nathaniel J. Wyeth, builder of Fort Hall (today's Pocatello, Idaho) and the Fort William trading post on Sauvie Island. The area is now home to the Wyeth State Recreation Area.Wyeth is located 51 miles east of Portland at exit #51 of I-84, and 1/4 mile west on Herman Creek Road. It is a trailhead for Wyeth Trail #411, the Gorge Trail #400, and Gorton Creek Falls.

The Columbia River Gorge is a canyon of the Columbia River in the Pacific Northwest of the United States. Up to 4,000 feet (1,200 m) deep, the canyon stretches for over eighty miles (130 km) as the river winds westward through the Cascade Range, forming the boundary between the state of Washington to the north and Oregon to the south. Extending roughly from the confluence of the Columbia with the Deschutes River (and the towns of Roosevelt, Washington, and Arlington, Oregon) in the east down to the eastern reaches of the Portland metropolitan area, the water gap furnishes the only navigable route through the Cascades and the only water connection between the Columbia Plateau and the Pacific Ocean. It is thus that the routes of Interstate 84, U.S. Route 30, Washington State Route 14, and railroad tracks on both sides run through the gorge. A popular recreational destination, the gorge holds federally protected status as the Columbia River Gorge National Scenic Area and is managed by the Columbia River Gorge Commission and the U.S. Forest Service.

The Wind River is a tributary of the Columbia River, in the U.S. state of Washington. Its entire course of 30 miles (48 km) lies within Skamania County. Crusattes River is an old variant name.When Lewis and Clark passed by the river in October 29, 1805, they called it the ‘New Timbered River’ after the Oregon Ash trees in the area.

Wind Mountain is a 1,907-foot-elevation (581-meter) summit located in Skamania County of Washington state.

Lake Bonneville is a reservoir on the Columbia River in the U.S. states of Oregon and Washington. It was created in 1937 with the construction of Bonneville Dam. The reservoir stretches between it and The Dalles Dam, upstream. It lies in parts of three counties in Oregon (Multnomah, Hood River, Wasco) and two in Washington (Skamania, Klickitat).

The Stevenson-Carson School District is located in Skamania County, Washington, with the district office in Stevenson, Washington It consists of Carson Elementary School in Carson, Washington, Stevenson Elementary School in Stevenson, Washington. Columbia George School in Carson, Washington Wind River Middle School in Stevenson, Washington. Stevenson High School in Stevenson, WashingtonAs of 2021, there were 842 students in the district.

Camp Benson Falls is a 90-foot waterfall on Summit Creek in Lindsey Creek State Park, Hood River County, Oregon, United States. Its elevation is 369 feet (112 m). Summit Creek is a tributary of the Columbia River and enters it about 11 miles (18 km) west of the city of Hood River. The falls are located about 600 metres (2,000 ft) from the terminus of Summit Creek.

Carson is a small census-designated place in the Columbia River Gorge National Scenic Area, north of the Columbia River in Skamania County, in the southwestern part of Washington, United States. Carson is located north of Washington State Route 14 and the town lies south of Stabler and between Stevenson to the west and Underwood and the neighboring cities of Bingen and White Salmon to the east.

The Cascade Locks Work Center, in Mount Hood National Forest near the town of Cascade Locks, Oregon, was built by the Civilian Conservation Corps in 1936. It was listed on the National Register of Historic Places in 1986 for its architecture. The Rustic style structures were designed by the architects of the United States Forest Service. The listing includes three contributing buildings on a 1.9-acre (0.77 ha) parcel. Historically the Work Center has been used as a single dwelling and a warehouse.

Mount Defiance is a peak near the Columbia River Gorge in the US state of Oregon. It rises to an elevation of 5,010 feet (1,527 m) in the Mount Hood National Forest in Hood River County, Oregon. The northern and western flanks of the mountain are in the Mark O. Hatfield Wilderness. The route up the mountain is often considered one of the hardest climbs in the Gorge; the trail gains 5,000 feet (1,500 m) in 6 miles (9.7 km) from the Starvation Creek Trailhead. Mount Defiance is composed chiefly of lava flows. The base is basalt from an old shield volcano, and it is capped by andesite. The mountain was named by Dr. P.G. Barrett, an early resident of the Hood River Valley, as he believed it retained its winter snow late into the spring in defiance of the warming weather.

Hole-in-the-Wall Falls, also known as Warren Falls, is a 96-foot man-made waterfall on Warren Creek in Starvation Creek State Park, Hood River County, Oregon, United States. Its main drop is 60 feet. It was created in 1938 when Warren Creek was diverted through a tunnel (hence its name) to prevent washouts of the Columbia River Highway. The creation of the falls shut off a natural cascade known as Warren Creek Falls named after the creek that formed it.

Warren Creek Falls was a waterfall located in Starvation Creek State Park at the north skirt of the Columbia River Gorge, in Hood River County in the U.S. state of Oregon. It was located in a privileged area along the Historic Columbia River Highway, where several waterfalls are located in Starvation Creek State Park, including Cabin Creek Falls, Lancaster Falls, and Starvation Creek Falls—all within 2 miles (3 km) of each other. It is frequently referred to as the name for Hole-in-the-Wall Falls, a few yards downstream of Warren Creek. The remaining bedrock and its river trail are surrounded by forests in the heart of the Columbia Plateau, off the western skirt of Viento Ridge. When water levels of the diversion tunnel reach over the crest, the overflowing waters run the old natural course of Warren Creek and a stream falls down the old site of the diverted cascade.