Klemtu is an unincorporated community on Swindle Island in the coastal fjords of British Columbia, Canada. It is located on Kitasoo Indian Reserve No. 1.
Kitasu Hill is a young, basaltic cinder cone on southwestern Swindle Island on the coast of the Canadian province of British Columbia. It is located 17 km (11 mi) southwest of Klemtu and south of Kitasu Bay. Kitasu Hill produced lava flows that extend to the north. It is the most prominent volcano of the Milbanke Sound Group.
Helmet Peak is a monogenetic cinder cone of the Milbanke Sound Group in British Columbia, Canada. The basaltic tuff breccias on Lake Island and Lady Douglas Island originated from Helmet Peak on Lady Island.
The Milbanke Sound Group, also called the Milbanke Sound Cones, is an enigmatic group of five small basaltic volcanoes in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada. Named for Milbanke Sound, this volcanic group straddles on at least four small islands, including Swindle, Price, Lady Douglas and Lake Island. Not much is known about this group of volcanoes and they remain undated. However, they all likely formed in the past 10,000 years after the last glacial period as evidenced by a small amount of erosion. The age of the most recent volcanic activity is also unknown. Most of the Milbanke Sound Cones are covered by mature forest. Kitasu Hill and Helmet Peak are the only two cones that are officially named.
Milbanke Sound is a sound on the coast of the Canadian province of British Columbia.
Calvert Island is an island on the coast of the Canadian province of British Columbia. It is east of Queen Charlotte Sound in the Central Coast region, about 100 kilometres (62 mi) north of the town of Port Hardy, which is at the north end of Vancouver Island.
Price Island is an island on the coast of the Canadian province of British Columbia. It is located at the southeastern end of Hecate Strait and the northeastern end of Queen Charlotte Sound. The southernmost point of Price Island, called Day Point, is used to delineate the boundary between Hecate Strait and Queen Charlotte Sound. Milbanke Sound is just to the south of Price Island. Laredo Sound is just north. Swindle Island lies just north of Price Island. The main Inside Passage route crosses Milbanke Sound and enters Finlayson Channel just east of Price Island. Price Island is located within the Kitimat-Stikine Regional District.
Campbell Island is an island in the Canadian province of British Columbia, located west of Denny Island and north of Hunter Island, near Milbanke Sound. The Inside Passage waterways of Lama Passage and Seaforth Channel meet at its northern end.
Wakeman Sound is a sound on the South Coast of British Columbia, Canada, located in the area north of the Broughton Archipelago, which lies on the north side of Queen Charlotte Strait, on the northeast side of Broughton Island. It is a sidewater opening of and opening north off Kingcome Inlet.
Dufferin Island is an island on the Central Coast of British Columbia, Canada, on the south side of Seaforth Channel just northwest of Bella Bella. It was named in 1876 by Captain Chatfield and the officers of HMS Amethyst after Frederick Hamilton-Temple-Blackwood.
Lake Island is an island on the coast of the Canadian province of British Columbia. It is located between Mathieson Channel and Lady Trutch Passage, and is flanked by Dowager Island, Lady Douglas Island, and a long finger shaped peninsula of the Canadian mainland to the east. Lake Island is not a lake island, as it is in an inlet of the Pacific Ocean, and lies only some 6 kilometres from the open sea.
Lady Douglas Island is an island in the North Coast region of the Canadian province of British Columbia. It is located off the south coast of Dowager Island.
Finngal Island is a small island on the central coast of British Columbia, Canada, south of Dufferin Island. Composed of columnar basalt lava flows, it is part of a volcanic group called the Milbanke Sound Group.
Snippaker Creek Cone is a cinder cone of the Iskut-Unuk River Cones group in northwestern British Columbia, Canada, located near the western flank of Cinder Mountain. It last erupted during the Holocene epoch.
Kitsumkalum First Nation is a band government of the Tsimshian people based at Kitsumkalum, British Columbia in the Skeena River valley in the North Coast region near Terrace, British Columbia, Canada. They are a member government of the Tsimshian First Nations treaty council.
The Don Peninsula is a peninsula in British Columbia, Canada. It extends southwest between the Mathieson and Spiller Channels in the Milbanke Sound area. Later discovered to be a peninsula, it was first charted as an island.
The Canadian Cascade Arc, also called the Canadian Cascades, is the Canadian segment of the North American Cascade Volcanic Arc. Located entirely within the Canadian province of British Columbia, it extends from the Cascade Mountains in the south to the Coast Mountains in the north. Specifically, the southern end of the Canadian Cascades begin at the Canada–United States border. However, the specific boundaries of the northern end are not precisely known and the geology in this part of the volcanic arc is poorly understood. It is widely accepted by geologists that the Canadian Cascade Arc extends through the Pacific Ranges of the Coast Mountains. However, others have expressed concern that the volcanic arc possibly extends further north into the Kitimat Ranges, another subdivision of the Coast Mountains, and even as far north as Haida Gwaii.
Finlayson Channel is a channel of the British Columbia Coast, Canada. It is a northern extension of Milbanke Sound. To its west are Swindle and Sarah Islands, to its east Roderick, Susan and Dowager Islands. It was first charted in 1793 by James Johnstone, one of George Vancouver's lieutenants during his 1791-95 expedition.
Mathieson Channel is a channel of the British Columbia Coast. It is a northern extension of Milbanke Sound. To its west are Pooley, Roderick, Susan and Dowager Islands, to its east the Don Peninsula. It was first charted in 1793 by James Johnstone, one of George Vancouver's lieutenants during his 1791-95 expedition.
Seaforth Channel is a channel in the Central Coast region of the Canadian province of British Columbia which is part of the Inside Passage - the 950 miles (1,530 km) passage between Seattle, Washington and Juneau, Alaska. The marine highway goes through Seaforth Channel on the way to Milbanke Sound, one of the open sea portions of the Inland Passage. Seaforth Channel which is part of the Prince Rupert/Port Hardy BC ferry route, extends in a westerly direction from Denny Island to Milbanke Sound between Denny Island, Campbell Island and the Wright group of islands on the south. In October 2016, a Texas-owned tug/barge transiting the Canadian waters of the Inside Passage without a local pilot was hard grounded on a reef at the entrance to Seaforth Channel in October 2016. More than 100,000 L of fuel contaminated the coast, coves and shores 20 km (12 mi) west of Bella Bella, the core community of the Heiltsuk Nation as well as the environmentally sensitive Great Bear Rainforest - Canada's contribution to the Queen's Commonwealth Canopy (QCC), a network of forest conservation programs. Clean up response and salvage was criticized by the Heiltsuk, B.C. Premier Christy Clark and Prime Minister Justin Trudeau. In November in Vancouver the Prime Minister announced a $1.5B ocean protection plan to "create a marine safety system, restore marine ecosystems and undertake research into oil spill cleanup methods."
