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Mount Waddington, once known as Mystery Mountain, is the highest peak in the Coast Mountains of British Columbia, Canada. Although it is lower than Mount Fairweather and Mount Quincy Adams, which straddle the United States border between Alaska and British Columbia, Mount Waddington is the highest peak that lies entirely within British Columbia. It and the subrange which surround it, known as the Waddington Range, stand at the heart of the Pacific Ranges, a remote and extremely rugged set of mountains and river valleys.
Hotham Inlet, also known as Kobuk Lake, is an arm of Kotzebue Sound on the northwestern coast of the U.S. state of Alaska. It is 50 miles (80 km) long and 5–20 miles (8–32 km) wide. The inlet is the outlet of the Kobuk and Selawik Rivers and it is bounded on the southwest by the Baldwin Peninsula.
The Waddington Range is a subrange of the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is only about 4,000 km2 in area, relatively small in area within the expanse of the range, but it is the highest area of the Pacific Ranges and of the Coast Mountains, being crowned by its namesake Mount Waddington 4,019 m (13,186 ft). The Waddington Range is also extremely rugged and more a complex of peaks than a single icefield, in contrast to the other huge icefield-massifs of the southern Coast Mountains, which are not so peak-studded and tend to have more contiguous icemasses.
Mount Raleigh, elevation 3,132 m (10,276 ft), is one of the principal summits of the Pacific Ranges of the Coast Mountains of southern British Columbia in Canada. It is located just southeast of the confluence of the Southgate and Bishop Rivers, northeast of the head of Bute Inlet, and is the highest summit south of the Bishop River's divide with the Lillooet River at Ring Pass, which is at the southeastern edge of the Lillooet Icefield and just north of the Pemberton Icecap. It is also the highest peak south of the pass between the upper basins of Chilko Lake and the Taseko Lakes, just north of which is Monmouth Mountain at 3,182 m (10,440 ft).
Bute Inlet is one of the principal inlets of the British Columbia Coast. It is 80 km (50 mi) long from the estuaries of the Homathko and Southgate Rivers at the head of the inlet, to the mouth, where it is nearly blocked by Stuart Island, and it averages about 4 km (2.5 mi) in width. Bute Inlet is in a spectacular wilderness setting and is one of the most scenic waterways in the world. In the upper reaches of the inlet mountains rise 2,700 m (9,000 ft) feet above sea level. Bute Inlet is a spectacular wilderness that is visited by very few people. In more recent years tourists are travelling from around the world to view grizzly bears in a natural setting and explore the wilderness of Bute Inlet.
Jervis Inlet is one of the principal inlets of the British Columbia Coast, about 95 km (59 mi) northwest of Vancouver, and the third of such inlets north of the 49th parallel, the first of which is Burrard Inlet, Vancouver's harbour.
Knight Inlet is one of the principal inlets of the British Columbia Coast, and the largest of the major inlets in the southern part of the Coast. It is fifth in sequence of the great saltwater inlets north from the 49th parallel near Vancouver, but it is the first whose outflow points away from the Strait of Georgia, opening into Queen Charlotte Strait at the Kwakwakaʼwakw community of Memkumlis on Village Island.
Seymour Inlet is one of the lesser travelled of the principal inlets of the British Columbia Coast. Unlike larger inlets such as Knight or Bute, it is not flanked by mountains but by relatively low, but still rugged, coastal hill-country and forms a maze of complex, narrow waterways and tidal pools and lagoons. It is located within a corresponding maze of peninsulas on the mainland on the northwest side of the Queen Charlotte Strait region.
Loughborough Inlet is one of the lesser principal inlets of the British Columbia Coast. It penetrates the Coast Mountains on the north side of the Discovery Islands archipelago, running about 35 km (22 mi) from its head at the mouth of the Stafford River to Chancellor Channel and Cordero Channel, which are on the north side of West Thurlow Island. A further 14 km (8.7 mi) west along Chancellor Channel is Johnstone Strait.
Holberg is a former ferry terminal about 35 kilometres (22 mi) from the northwest tip of Vancouver Island, British Columbia. This unincorporated community is at the head of Holberg Inlet, which forms the western arm of Quatsino Sound.
The Homathko Icefield is an icefield in British Columbia, Canada. Officially named the Homathko Snowfield from 1950 until the current name was adopted in 1976, it is one of the largest icefields in the southern half of the Coast Mountains, with an area of over 2,000 km2 (770 sq mi). It is located between Chilko Lake and the Homathko River, and lies across the Great Canyon of that river to the east of the Waddington Range. Although adjacent to Mount Queen Bess, the Homathko Icefield is largely an expanse of ice, about 30 km (19 mi) across, ringed by relatively minor peaks and distinguished, relative to the other Coast Mountains icefields, by lack of any major ones. The Lillooet Icecap and the Compton Névé, both similar in size to the Homathko Icefield but much more peak-studded, lie to the Homathko Icefield's southeast across the Southgate River which bends around the icefield-massif's southern flank to reach the head of Bute Inlet adjacent to the mouth of the Homathko River. The icefield is essentially one large ice-girt montane plateau between these two rivers.
Forward Harbour was a cannery town in the Johnstone Strait region of the Central Coast of British Columbia, Canada, located on the inlet of the same name, which is on the mainland side of Wellbore Channel, to the east of Hardwicke Island. Nearby on the same vicinity on the Mainland, though fronting on other bodies of water, are Jackson Bay to the immediate north, off Sunderland Channel, and Heydon Bay, British Columbia to the east on Loughborough Inlet.
HMS San Josef was a 114-gun first-rate ship of the line of the Royal Navy. Originally built at Ferrol in Galicia for the Spanish Navy in 1782–83, she was captured from the Spanish Navy at the Battle of Cape St Vincent on 14 February 1797. In 1809 she served as the flagship of Admiral John Thomas Duckworth.
Frederick Sound is a sound in the Central Coast of British Columbia, Canada. It is the largest branch of Seymour Inlet and along with that inlet was named in honour of Frederick Seymour, second governor of the Colony of British Columbia. Frederick Sound has two inlets, one named Salmon Arm and the other unnamed. The complex maze of hidden waterways forming Seymour Inlet is in the region of Queen Charlotte Strait.
Actaeon Sound is a sound in the Queen Charlotte Strait region of the Central Coast of British Columbia, branching off northeasterly from the north side of Drury Inlet near its head on the mainland of British Columbia to the north of the town of Port McNeill, on the opposite side of Queen Charlotte Strait. On the south side of the sound is the Bond Peninsula at 50°56′50″N127°06′55″W, which is formed by a sidewater, Bond Lagoon at 50°56′34″N127°06′34″W, both presumably named in 1865 by Captain Pender, in association with other Admiralty and HMS Actaeon-related names.
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 Broughton Peaks are a group of low mountain summits west of the south end of Effingham Inlet, to the north of Bamfield in the Barkley Sound region of the west coast of Vancouver Island, British Columbia, Canada.
Drury inlet is an inlet in the Queen Charlotte Strait region of the Central Coast of British Columbia, Canada, extending west from Wells Passage to the northwest of North Broughton Island, northwest of the town of Port Hardy. Branching off to the northeast from the north side of the head of the inlet is Actaeon Sound.
Waddington Harbour is a harbour at the head of Bute Inlet in the Central Coast region of British Columbia, Canada. Also issuing into the head of Bute Inlet and Waddington Harbour, just east of the mouth of the Homathko, is the Teaquahan River. Issuing directly into the inlet a few miles south on the harbour's southeast is the Southgate River, one of the major rivers of the central Pacific Ranges, which begins on the west side of the Lillooet Icecap. Its lower valley adjacent to the inlet's shores is called Pigeon Valley.
Mount Bute, also known as Bute Mountain, is a 2,810-metre (9,220-foot) mountain located in the Coast Mountains of British Columbia, Canada. Situated at the southern extreme of the Homathko Icefield, Mount Bute has an impressive 800-metre sheer granite west face, and Bute Glacier dominates the north aspect. This imposing mountain is visible from Waddington Harbour at the head of Bute Inlet, in a remote wilderness area that few visit. Its nearest higher peak is Mount Grenville, 13.0 km (8.1 mi) to the east-northeast. Mount Grenville is the highest summit of the icefield. Mount Bute is 63.0 km (39.1 mi) southeast of Mount Waddington, the highest peak of the entire Coast Mountains range.
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50°29′N125°16′W / 50.483°N 125.267°W
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