The Taku River is a river running from British Columbia, Canada, to the northwestern coast of North America, at Juneau, Alaska. The river basin spreads across 27,500 square kilometres (10,600 sq mi). The Taku is a very productive salmon river and its drainage basin is primarily wilderness.
Heart Peaks, originally known as the Heart Mountains, is a mountain massif in the Northern Interior of British Columbia, Canada. It is 90 km (56 mi) northwest of the small community of Telegraph Creek and just southwest of Callison Ranch. With a maximum elevation of 2,012 m (6,601 ft), it rises above the surrounding landscape on the Nahlin Plateau, which is part of the western Stikine Plateau. Heart Peaks has been an area of prospecting since the 1980s with the discovery of precious metals.
Level Mountain is a large volcanic complex in the Northern Interior of British Columbia, Canada. It is located 50 kilometres north-northwest of Telegraph Creek and 60 kilometres west of Dease Lake on the Nahlin Plateau. With a maximum elevation of 2,164 metres , it is the second-highest of four large complexes in an extensive north–south trending volcanic region. Much of the mountain is gently-sloping; when measured from its base, Level Mountain is about 1,100 metres tall, slightly taller than its neighbour to the northwest, Heart Peaks. The lower, broader half of Level Mountain consists of a shield-like structure while its upper half has a more steep, jagged profile. Its broad summit is dominated by the Level Mountain Range, a small mountain range with prominent peaks cut by deep valleys. These valleys serve as a radial drainage for several small streams that flow from the mountain. Meszah Peak is the only named peak in the Level Mountain Range.
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 Inklin River is a tributary of the Taku River in the northwest part of the province of British Columbia, Canada. It originates at the confluence of its two main tributaries, the Nahlin River and the Sheslay River and flows generally west and northwest about 83 km (52 mi) to join the Nakina River. The confluence of the Inklin and Nakina Rivers, at the uninhabited locality of Inklin, marks the beginning of the Taku River. The mouth of the Inklin River is located about 100 km (62 mi) northeast of Juneau, Alaska and about 160 km (99 mi) northwest of Telegraph Creek, British Columbia.
The Stikine Plateau is a plateau in northern British Columbia, Canada. It lies between the Boundary Ranges of the Coast Mountains on the west and southwest and the Cassiar Mountains along its northeast, and between the Skeena Mountains on its south and southeast and the Jennings and Nakina Rivers on the north.
The Nahlin Plateau is a plateau in northwestern British Columbia, Canada, located between the Sheslay River and Tuya River on the west and east and the Nahlin River and the Stikine River to the north and south. It is a subplateau of the Stikine Plateau; adjoining parts of the same larger plateau are the Taku Plateau to the northwest, the Tahltan Highland to the southwest and south, the Kawdy Plateau to the north, and the Spatsizi Plateau to the southeast. The Nahlin Plateau is the location of the Level Mountain Range and Heart Peaks, two small mountain ranges forming parts of large shield volcanoes.
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 Nahlin River is a river in far northwestern British Columbia, Canada, flowing northwest to meet the Sheslay River, forming there the commencement of the Inklin River, the main southeast fork of the Taku.
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.
The Little Tuya River is a tributary of the Tuya River in northwest part of the province of British Columbia, Canada. It flows generally south and east about 71 km (44 mi) to join the Tuya River near Cariboo Meadows. The Little Tuya River's watershed covers 569 km2 (220 sq mi), and its mean annual discharge is an estimated 6.69 m3/s (236 cu ft/s).
The Yukon Telegraph Trail, also known simply as the Telegraph Trail, is a historic pathway in the Canadian province of British Columbia that extends from the village of Ashcroft in the south to the community of Atlin in the north. It was used for servicing the Yukon Telegraph Line which extended from Ashcroft in the south to Dawson City, Yukon in the north. The telegraph line was constructed by the Dominion Government Telegraph Service from 1898 to 1901. It was abandoned in 1936 with the advent of radio communication. Along the length of the trail are remains of telegraph cabins, telegraph cable and other artifacts that were used during the construction of the telegraph line.
Matsatu Creek, historically called the Matsatu River, is a stream in the Northern Interior of British Columbia, Canada. It is located 40 km (25 mi) north of the abandoned settlement of Sheslay in Cassiar Land District. From its head at Level Mountain, where it has cut a large gorge into its western escarpment, Matsatu Creek flows northwest into Kakuchuya Creek, the main tributary of the Dudidontu River.
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 Koshin River is a tributary of the Nahlin River in northwest part of the province of British Columbia, Canada. It flows generally north about 58 km (36 mi) to join the Nahlin River, which forms the Inklin River, one of the main tributaries of the Taku River. The Koshin River flows through the Nahlin Plateau. It joins the Nahlin River at the boundary between the Nahlin and Kawdy Plateaus. Both plateaus are part of the larger Stikine Plateau region.
Beatty Creek is a tributary of the Tahltan River in northwest part of the province of British Columbia, Canada. It flows generally south about 62 km (39 mi) to join the Tahltan River a few kilometres downstream from the Little Tahltan River confluence. The Tahltan River is one of the main tributaries of the Stikine River.
Kaha Creek is a tributary of the Koshin River in northwest part of the province of British Columbia, Canada. It flows generally northwest for roughly 30 km (19 mi) to join the Koshin River about 3.8 km (2.4 mi) north of Hatin Lake, and about 6 km (3.7 mi) north of Callison Ranch. Kaha Creek's watershed covers 95.1 km2 (36.7 sq mi), and its mean annual discharge is estimated at 1.19 m3/s (42 cu ft/s). The mouth of Kaha Creek is located about 93 km (58 mi) north of Telegraph Creek, British Columbia, about 165 km (103 mi) east of Juneau, Alaska, and about 103 km (64 mi) west of Dease Lake, British Columbia. Kaha Creek's watershed's land cover is classified as 41.1% conifer forest, 40.2% shrubland, 12.3% barren, and small amounts of other cover.
Lost Creek is a tributary of the Koshin River in northwest part of the province of British Columbia, Canada. It flows generally northwest for roughly 26 km (16 mi) to join the Koshin River just north of Hatin Lake, and about 4 km (2.5 mi) north of Callison Ranch. Lost Creek's watershed covers 70.0 km2 (27.0 sq mi), and its mean annual discharge is estimated at 1.07 m3/s (38 cu ft/s). The mouth of Lost Creek is located about 90 km (56 mi) north of Telegraph Creek, British Columbia, about 102 km (63 mi) west of Dease Lake, British Columbia, and about 163 km (101 mi) east of Juneau, Alaska. Lost Creek's watershed's land cover is classified as 46.3% shrubland, 31.5% conifer forest, 12.2% barren, and small amounts of other cover.
Megatushon Creek is a tributary of the Nahlin River, part of the Taku River watershed in northwest part of the province of British Columbia, Canada. It flows generally northeast and east for roughly 22 km (14 mi) to join the Nahlin River not far from the Nahlin's source south of Tachilta Lakes. Megatushon Creek's watershed covers 52.7 km2 (20.3 sq mi), and its mean annual discharge is estimated at 1.03 m3/s (36 cu ft/s). The mouth of Megatushon Creek is located about 65 km (40 mi) west of Dease Lake, British Columbia, about 78 km (48 mi) north of Telegraph Creek, British Columbia, and about 120 km (75 mi) east of Juneau, Alaska. Megatushon Creek's watershed's land cover is classified as 34.8% barren, 32.3% shrubland, 24.8% conifer forest, and small amounts of other cover.
Granite Lake is a lake on the Kawdy Plateau of the Northern Interior of British Columbia, Canada. It is located northwest of the junction of the Nahlin and Tuya rivers in Cassiar Land District.
