Multnomah Falls is a waterfall located on Multnomah Creek in the Columbia River Gorge, east of Troutdale, between Corbett and Dodson, Oregon, United States. The waterfall is accessible from the Historic Columbia River Highway and Interstate 84. Spanning two tiers on basalt cliffs, it is the tallest waterfall in the state of Oregon at 620 ft (189 m) in height. The Multnomah Creek Bridge, built in 1914, crosses below the falls, and is listed on the National Register of Historic Places.
The Squamish-Lillooet Regional District is a quasi-municipal administrative area in British Columbia, Canada. It stretches from Britannia Beach in the south to Pavilion in the north. Lillooet, Pemberton, Whistler and Squamish are the four municipalities in the regional district. Its administrative offices are in the Village of Pemberton, although the district municipalities of Squamish and Whistler are larger population centres. The district covers 16,353.68 km² of land area.
Bridal Veil Falls Provincial Park is a BC Park located on the Trans-Canada Highway just east of Rosedale, British Columbia, Canada, part of the City of Chilliwack. The community of Bridal Falls is located adjacent to the falls and park as well as the interchange between the Trans-Canada and BC Highway 9 and has a variety of highway-based tourism services. Access to the falls requires a short hike from the parking lot and well groomed trails, taking most groups 15-25 minutes.
Oneonta Gorge is a scenic gorge located in the Columbia River Gorge area of the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. Exposed walls of 25-million-year-old basalt are home to a wide variety of ferns, mosses, hepatics, and lichens, many of which grow only in the Columbia River Gorge. Oneonta Gorge with its 50 species of wildflowers, flowering shrubs and trees has been described as "one of the true dramatic chasms in the state." The Oneonta Gorge Creek Bridge is listed on the National Register of Historic Places.
The Cheakamus River is a tributary of the Squamish River, beginning on the west slopes of Outlier Peak in Garibaldi Provincial Park upstream from Cheakamus Lake on the southeastern outskirts of the resort area of Whistler. The river flows into Cheakamus Lake before exiting it and flowing northwest until it turns south and enters Daisy Lake. Between the outlet of Daisy Lake and its mouth, much of its length is spent going through Cheakamus Canyon, where the river flows through swift rapids and even one good sized waterfall. The river flows south from the lake and through the canyon before joining the Squamish River at Cheekye, a few miles north of the town of Squamish. The river's name is an anglicization of the name of Chiyakmesh, a village of the Squamish people and a reserve of the Squamish Nation.
Nairn Falls Provincial Park is a provincial park in British Columbia, Canada located on the Green River adjacent to British Columbia Highway 99 and the Canadian National Railway line just south of Pemberton and less than twenty minutes north of the resort town of Whistler. The 170 hectare park was established in 1966, shortly after the highway's opening, to protect and enhance visitor access to Nairn Falls.
Pyramid Creek Falls Provincial Park is a provincial park in British Columbia, Canada, located on the east side of the North Thompson River between the towns of Blue River (S) and Valemount (N).
Keyhole Falls is the unofficial name for the largest waterfall along the Lillooet River in British Columbia, Canada. The falls are 115 feet (35 m) high and are a punchbowl type of waterfall.
The Sea-to-Sky Corridor, often referred to as the Corridor or the Sea to Sky Country, is a region in British Columbia spreading from Horseshoe Bay through Whistler to the Pemberton Valley and sometimes beyond to include Birken and D'Arcy. From Whistler on up, the region overlaps with the older and more historic Lillooet Country, of which Squamish, at the region's centre, was once the southward extension in the days when it was the rail-port terminus from the Interior, via Lillooet, and accessible from the Lower Mainland only by sea. Most of the region is in the Squamish-Lillooet Regional District, although south of Britannia Beach a small part of the region is in the Greater Vancouver Regional District.
The Callaghan Valley is located in the Sea to Sky Country of southwestern, British Columbia, in the Pacific Ranges of the Coast Mountains 90 km north of Vancouver. It was the home of the 2010 Winter Olympics's Whistler Olympic Park, the venue for the Nordic events of the Olympics, and adventure tourism operations including Canadian Wilderness Adventures.
The Whistler Olympic and Paralympic Village was a 2010 Winter Olympics facility in the resort town of Whistler, British Columbia. The Olympic Village is considered one of Whistler's legacy projects, in that it is being used after the Olympics to help house and train Canadian athletes. Whistler is one of the two host communities for the Games. The site of this athletes' village is in the Cheakamus Valley approximately 20 minutes south of the Whistler Mountain competition venues, and 6 km from the highway cutoff for the Whistler Olympic Park sliding events venue in the Callaghan Valley.
The Powder Mountain Icefield, also called the Powder Mountain Icecap and the Cayley Icefield, is a glacial field in the Pacific Ranges of southwestern British Columbia, Canada, about 20 kilometres (12 mi) west of Whistler and about 90 kilometres (56 mi) north of Vancouver. On the west side of the icefield is the valley of the Squamish River, while on its east is the Callaghan Valley, which is the setting for the Nordic facilities for the 2010 Winter Olympics.
The Whistler Olympic Park is the location of the Nordic events facilities for the 2010 Winter Olympics and is located in the Madeley Creek basin in the Callaghan Valley, west of Whistler, British Columbia, Canada. The facility hosted the biathlon, cross-country skiing, Nordic combined, and ski jumping. After the Olympics the park remains a public facility, complementing the extensive wilderness trails and alpine routes already in use. Three temporary stadiums were built with a capacity for 12,000 spectators each. The location is approximately 8 km from the junction of its access road with Highway 99 and 14 km from the Whistler Olympic Village.
Brandywine Creek, also formerly known as the Long John River after a local prospector and trapper, is a tributary of the Cheakamus River in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, entering that stream via Daisy Lake, just below Brandywine Falls. The creek is about 14 km in length and originates on the south slope of Brandywine Mountain in Brandywine Meadows, at the southern end of the Powder Mountain Icefield and is the next basin immediately southwest of that of the Callaghan Valley, the site of the Nordic events facility for the 2010 Olympics. The creek's valley has been partially logged. An unnamed hot spring lies in its upper reaches, near Mount Fee.
Eagle Creek is a tributary of the Columbia River in Multnomah and Hood River counties in the U.S. state of Oregon. It cuts through a narrow canyon in its 3,200 feet (980 m) descent to the Columbia River Gorge and is known for its concentration of 13 waterfalls in about 5 miles (8.0 km) distance. Eight major falls are on Eagle Creek and the East Fork Eagle Creek itself, while five are on its tributaries.
There are multiple waterfalls in the basin of the North Fork Cascade River, a river in the North Cascades of Washington that drains to the Cascade River. Many of these are taller than the more famous waterfalls in North America, but do not receive much attention due to their remoteness.
The Paradise River in Washington state, United States, is known for having a total of eight major waterfalls.
Ashlu Falls is a short but significant waterfall along lower Ashlu Creek. The falls are located about 6 km above the mouth of Ashlu Creek and mark the head of Ashlu Canyon. The creek is actually crossed by a logging road bridge between the two tiers.
Cascade Falls Regional Park is a regional park under the administration of the Fraser Valley Regional District in the Hatzic Valley of the Lower Mainland region of British Columbia, Canada. The park was originally 9.5 hectares in area but was expanded to a current 22 hectares. It has picnic tables and pit toilets, with various hiking trails and a walkway leading to a viewing platform over a large waterfall, which is 15 minutes walk from the park's parking lot.
