The Township of Esquimalt is a municipality at the southern tip of Vancouver Island, in British Columbia, Canada. It is bordered to the east by the provincial capital, Victoria, to the south by the Strait of Juan de Fuca, to the west by Esquimalt Harbour and Royal Roads, to the northwest by the New Songhees 1A Indian reserve and the town of View Royal, and to the north by a narrow inlet of water called the Gorge, across which is the district municipality of Saanich. It is almost tangential to Esquimalt 1 Indian Reserve near Admirals Road. It is one of the 13 municipalities of Greater Victoria and part of the Capital Regional District.
Ladysmith, originally Oyster Harbour, is a town located on the 49th parallel north on the east coast of Vancouver Island, British Columbia, Canada. The local economy is based on forestry, tourism, and agriculture. A hillside location adjacent to a sheltered harbour forms the natural geography of the community.
Central Saanich is a district municipality in Greater Victoria, British Columbia, Canada, and a member municipality of the Capital Regional District. It is located on the Saanich Peninsula, in the far south-east of Vancouver Island. It is the traditional territory of the W̱SÁNEĆ people. The district began as a farming community, and many hobby farms, along working farms and vineyards, still exist. In recent decades, the area has seen increasing residential, commercial, and industrial development, especially around the neighbourhoods of Brentwood Bay and Saanichton, which are occasionally referred to as separate communities.
The Mount Meager massif is a group of volcanic peaks in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Part of the Cascade Volcanic Arc of western North America, it is located 150 km (93 mi) north of Vancouver at the northern end of the Pemberton Valley and reaches a maximum elevation of 2,680 m (8,790 ft). The massif is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits including Mount Meager which is the second highest of the massif.
Mount Fee is a volcanic peak in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located 13 km (8.1 mi) south of Callaghan Lake and 21 km (13 mi) west of the resort town of Whistler. With a summit elevation of 2,162 m (7,093 ft) and a topographic prominence of 312 m (1,024 ft), it rises above the surrounding rugged landscape on an alpine mountain ridge. This mountain ridge represents the base of a north-south trending volcanic field which Mount Fee occupies.
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.
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.
The Tseax Cone, also called the Tseax River Cone or the Aiyansh Volcano, is a young and active cinder cone and adjacent lava flows associated with the Nass Ranges and the Northern Cordilleran Volcanic Province. It is located east of Crater Creek at outlet of Melita Lake, southeast of Gitlakdamix and 60 kilometres (37 mi) north of Terrace, British Columbia, Canada.
Armadillo Peak is a 7.5-million-year-old caldera, located about 3 km north of Bourgeaux Creek and northeast of Raspberry Pass, British Columbia, Canada. It is south of Mount Edziza and is overlapped by the Ice Peak central volcano, which was formed during the early Pleistocene. Its caldera is largely destroyed by glaciers. It is part of the Mount Edziza volcanic complex, which is made of basaltic lava flows.
Mount MacKenzie is a volcanic peak, located 40 km (25 mi) northeast of Hagensborg, British Columbia, Canada. It is one of the volcanic peaks of the Rainbow Range, which is one of the three major shield volcanoes that form the Anahim Volcanic Belt. Mount MacKenzie was formed when the North American Plate moved over a hotspot, similar to the one feeding the Hawaiian Islands, known as the Anahim hotspot.
Ice Peak is a stratovolcano, located 39 km (24 mi) west of Tatogga and 3 km (2 mi) south of Mount Edziza, British Columbia, Canada. It overlaps the 7.5-million-year-old Armadillo Peak. It lies on a large volcanic plateau, which is made of basaltic lava flows from the massive Mount Edziza volcanic complex. Ice Peak last erupted during the Holocene.
The Silverthrone Caldera is a potentially active caldera complex in southwestern British Columbia, Canada, located over 350 kilometres (220 mi) northwest of the city of Vancouver and about 50 kilometres (31 mi) west of Mount Waddington in the Pacific Ranges of the Coast Mountains. The caldera is one of the largest of the few calderas in western Canada, measuring about 30 kilometres (19 mi) long (north-south) and 20 kilometres (12 mi) wide (east-west). Mount Silverthrone, an eroded lava dome on the caldera's northern flank that is 2,864 metres (9,396 ft) high, may be the highest volcano in Canada.
Mount Somolenko is a volcanic peak in southwestern British Columbia, Canada, located 83 km (52 mi) east of Rivers Inlet and 7 km (4 mi) south of Mount Silverthrone. It is the highest peak south of Mount Silverthrone in the Ha-Iltzuk Icefield.
Mount Fitzgerald is a volcanic peak in southwestern British Columbia, Canada, located 84 km (52 mi) east of Rivers Inlet and 4 km (2 mi) east of Mount Silverthrone.
The Mount Edziza volcanic complex is a large and potentially active north-south trending complex volcano in Stikine Country, northwestern British Columbia, Canada, located 38 kilometres (24 mi) southeast of the small community of Telegraph Creek. It occupies the southeastern portion of the Tahltan Highland, an upland area of plateau and lower mountain ranges, lying east of the Boundary Ranges and south of the Inklin River, which is the east fork of the Taku River. As a volcanic complex, it consists of many types of volcanoes, including shield volcanoes, calderas, lava domes, stratovolcanoes, and cinder cones.
Meszah Peak is a volcanic cone located 66 km (41 mi) north of Telegraph Creek and 136 km (85 mi) southwest of Zus Mountain in British Columbia, Canada. It is the highest peak of the Level Mountain Range, a cluster of bare peaks on the summit of the massive Level Mountain shield volcano, which forms the most voluminous and most persistent eruptive centre in the Northern Cordilleran Volcanic Province.
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.
Range 3 Coast Land District is one of the 59 land districts of British Columbia, Canada, which are part of the cadastral divisions of British Columbia.
Whitetop Mountain is a forested hill in the West-Central Interior of British Columbia, Canada. It is on the northwest side of junction of the Chilcotin River and Downton Creek. Whitetop is a volcanic cone of the Chilcotin Plateau and Anahim Volcanic Belt.
