The King Salmon Fault is a northwest-trending thrust fault in the Northern Interior of British Columbia, Canada. [1] It takes its name from King Salmon Lake which lies at the headwaters of King Salmon Creek. [1] [2]
Lake Sammamish is a freshwater lake 8 miles (13 km) east of Seattle in King County, Washington, United States. The lake is 7 miles (11 km) long and 1.5 miles (2 km) wide, with a maximum depth of 105 feet (32 m) and a surface area of 8 sq mi (21 km2). It lies east of Lake Washington and west of the Sammamish Plateau, and stretches from Issaquah in the south to Redmond in the north. At Issaquah it is fed by Issaquah Creek, and at Redmond it drains to Lake Washington via the Sammamish River, named after the native people who once lived along its entire length.
The Stikine River is a major river in northern British Columbia (BC), Canada and southeastern Alaska in the United States. It drains a large, remote upland area known as the Stikine Country east of the Coast Mountains. Flowing west and south for 610 kilometres (379 mi), it empties into various straits of the Inside Passage near Wrangell, Alaska. About 90 percent of the river's length and 95 percent of its drainage basin are in Canada. Considered one of the last truly wild large rivers in BC, the Stikine flows through a variety of landscapes including boreal forest, steep canyons and wide glacial valleys.
The Skeena River is the second-longest river entirely within British Columbia, Canada. Since ancient times, the Skeena has been an important transportation artery, particularly for the Tsimshian and the Gitxsan—whose names mean "inside the Skeena River" ,and "people of the Skeena River," respectively. The river and its basin sustain a wide variety of fish, wildlife, and vegetation, and communities native to the area depend on the health of the river. The Tsimshian migrated to the Lower Skeena River, and the Gitxsan occupy territory of the Upper Skeena.
Houston is a forestry, mining and tourism town in the Bulkley Valley of the Northern Interior of British Columbia, Canada. Its population as of 2021 was 3,052, with approximately 2,000 in the surrounding rural area. It is known as the "steelhead capital" and it has the world's largest fly fishing rod. Houston's tourism industry is largely based on ecotourism and Steelhead Park, situated along Highway 16. Houston is named in honour of the pioneer newspaperman John Houston.
Diana Lake Provincial Park is a 233 hectares provincial park located 16 kilometres east of the city of Prince Rupert in the North Coast Regional District of British Columbia, Canada. The park was established by BC Parks in 1980.
Juniper Beach Provincial Park is a provincial park in the Thompson Country region of south central British Columbia, Canada. The facility is on the north side of the Thompson River, west of the town of Savona, and downstream from the Kamloops Lake outflow. On BC Highway 1, the locality is by road about 20 kilometres (12 mi) east of Cache Creek and 65 kilometres (40 mi) west of Kamloops.
The Sheslay River is a tributary of the Inklin River in northwest part of the province of British Columbia, Canada. It joins the Nahlin River to form the Inklin River, one of the main tributaries of the Taku River. The lower Sheslay River marks the boundary between the Taku Plateau and the Nahlin Plateau. Its mouth at the Nahlin River marks the junction of the Taku, Nahlin, and Kawdy Plateaus. All three of these are part of the larger Stikine Plateau region.
The Mount Edziza volcanic complex is a large group of volcanoes and associated lava flows in northwestern British Columbia, Canada. It is located 40 kilometres southeast of Telegraph Creek and 85 kilometres southwest of Dease Lake on the Tahltan Highland. The complex encompasses a broad, steep-sided lava plateau that extends over an area of 1,000 square kilometres. Its highest summit reaches an altitude of 2,786 metres above sea level, making the MEVC the highest of four large complexes in an extensive north–south trending volcanic region. An ice cap obscures the highest summit which is characterized by several outlet glaciers stretching out to lower altitudes.
The Tahltan River is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada. It flows generally east and southeast about 95 km (59 mi) to join the Stikine River at Tahltan, British Columbia. The lower Tahltan River marks the boundary between the Tahltan Highland and the Nahlin Plateau, both of which are part of the larger Stikine Plateau region.
The Iskut River, located in the northwest part of the province of British Columbia is the largest tributary of the Stikine River, entering it about 11 km (6.8 mi) above its entry into Alaska.
The Southgate River is a river in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, entering the head of Bute Inlet, on that province's South Coast, just east of the mouth of the Homathko River at Waddington Harbour. The lower reaches of the river's course are flat-bottomed and are named Pigeon Valley.
The Hackett River is a tributary of the Sheslay River in northwest part of the province of British Columbia, Canada. It flows generally northwest about 33 km (21 mi), through two lakes, a wetland, and a gorge, to join the Sheslay River, which in turn is a tributary of the Inklin River, the main southeast fork of the Taku River.
The Tuya River is a major tributary of the Stikine River in northwest part of the province of British Columbia, Canada. From its source at High Tuya Lake in Tuya Mountains Provincial Park just south of Ash Mountain, the highest peak of the Tuya Range, the Tuya River flows south about 200 km (120 mi) to meet the Stikine River in the Grand Canyon of the Stikine. The Tuya River's main tributary is the Little Tuya River. The Tuya River divides the Tanzilla Plateau on the east from the Kawdy Plateau, to the northwest, and the Nahlin Plateau, to the southwest. All three are considered sub-plateaus of the Stikine Plateau. The Tuya River's watershed covers 3,575 km2 (1,380 sq mi), and its mean annual discharge is estimated at 36.9 m3/s (1,300 cu ft/s). The mouth of the Tuya River is located about 24 km (15 mi) northeast of Telegraph Creek, British Columbia, about 67 km (42 mi) southwest of Dease Lake, British Columbia, and about 210 km (130 mi) east of Juneau, Alaska. The Tuya River's watershed's land cover is classified as 35.7% shrubland, 31.4% conifer forest, 14.0% mixed forest, 7.2% herbaceous, and small amounts of other cover.
Oregana Creek Provincial Park is a provincial park in British Columbia, Canada, located 150 kilometres northwest of Salmon Arm, British Columbia, near Adams River. The park, which is 286 ha. in size, was established in 2010.
King Salmon Creek is a creek in the Atlin District of British Columbia, Canada. The creek begins at King Salmon Lake and flows generally eastward to join the Taku River. Southeast of that confluence is King Salmon Mountain.
Taku River/T'aḵú Téiú' Conservancy is a conservancy located in the Stikine Region of British Columbia, Canada. It was established on June 22, 2012, as a result of the Wóoshtin Wudidaa Atlin Taku Land Use Plan and Taku River Tlingit First Nation Strategic Engagement Agreement. The conservancy protects a large region of pristine wilderness along the Taku River from its confluence with the Nakina and Inklin Rivers to the Alaska-British Columbia border.
The Ecstall River is a tributary of the Skeena River in the province of British Columbia, Canada. It originates in the Kitimat Ranges, and flows about 110 km (68 mi) to the lower tidal reach of the Skeena River at Port Essington, about 30 km (19 mi) southeast of Prince Rupert, 95 km (59 mi) southwest of Terrace, and 85 km (53 mi) northwest of Kitimat. Its drainage basin covers about 1,485 km2 (573 sq mi) and contains the largest blocks of unlogged land on the north coast of British Columbia, although large-scale industrial logging operations, both active and proposed, have been occurring in the watershed since the 1980s.
The McNeil River is a tributary of the Skeena River in the North Coast Regional District of the province of British Columbia, Canada. It originates at Minerva Lake in the Kitimat Ranges of the Coast Mountains, and flows south about 13 km (8.1 mi) to the lower tidal reach of the Skeena River at Tyee Bank, across the Skeena from Port Essington, about 25 km (16 mi) southeast of Prince Rupert, 95 km (59 mi) southwest of Terrace, and 88 km (55 mi) northwest of Kitimat. Its watershed covers 41.4 km2 (16.0 sq mi), and its mean annual discharge is 4.07 m3/s (144 cu ft/s).
The Dudidontu River is a tributary of the Nahlin River in northwest part of the province of British Columbia, Canada. It joins the Nahlin River, which forms the Inklin River, one of the main tributaries of the Taku River. The Dudidontu River's watershed covers 964 km2 (372 sq mi), and its mean annual discharge is 15.4 m3/s (540 cu ft/s). Almost half of the Dudidontu's flow comes from its main tributary, Kakuchuya Creek, and Kakuchuya Creek's main tributary, Matsatu Creek. The mouth of the Dudidontu River is located about 150 km (93 mi) northeast of Juneau, Alaska and about 110 km (68 mi) northwest of Telegraph Creek, British Columbia.
The Little Iskut River is a tributary of the Iskut River in the northwest part of the province of British Columbia, Canada, in Cassiar Land District. From its source at Little Ball Lake in Mount Edziza Provincial Park, the Little Iskut River flows about 45 km (28 mi), generally north to the vicinity of Mowdale Lake, then southeast and south to the Iskut River just below Cascade Falls. The Little Iskut River is part of the Stikine River drainage basin, as the Iskut River is a major tributary of the Stikine.