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They described an area of great biodiversity and ecological importance. In 1980, the rocks and surrounding areas were protected as an ecological reserve under joint BC Parks-Pearson College UWC management. [3] In 2006 and 2007, the Race Rocks Tidal Power Demonstration Project was installed. After a six-year period for experimental research, the ...
The Pacific Undersea Gardens was a 150-foot (45 m) vessel that was towed from the Oak Bay Marina to the waters of the Inner Harbour. Visitors descended 15 feet (4.5 m) beneath the ocean surface to look through the many viewing windows of the aquariums that surrounded the vessel and see the various marine life of coastal British Columbia, in their natural and protected environment.
The Shaw Centre for the Salish Sea (formerly known as the Shaw Ocean Discovery Centre) is a not-for-profit community aquarium and cultural learning centre dedicated to the ecosystem of the Salish Sea. It is located on the waterfront in the town of Sidney on Vancouver Island in British Columbia, Canada. Since its grand opening on June 20, 2009 ...
Geologic belts of Western Canada. The geology of British Columbia is a function of its location on the leading edge of the North American continent.The mountainous physiography and the diversity of the different types and ages of rock hint at the complex geology, which is still undergoing revision despite a century of exploration and mapping.
The Chuckanut Formation in northwestern Washington (named after the Chuckanut Mountains, near Bellingham), its extension in southwestern British Columbia (the Huntingdon Formation), and various related formations in central Washington (including the Swauk, Roslyn, Manastash, and Chumstick) are fluvial sedimentary formations of Eocene age ...
Siwash Rock in 2006. Siwash Rock is a rock outcropping in Vancouver, British Columbia, Canada's Stanley Park. A legend among the Indigenous Squamish people surrounds the rock. It is between 15 and 18 metres (49 and 59 ft) tall. It became known to mariners as Nine Pin Rock for its resemblance to a bowling pin.
Loss Creek begins at an unnamed confluence at a point north of the settlement of Jordan River at an elevation of 507 metres (1,663 ft). [3] It flows west for 14 kilometres (8.7 mi), taking in the right tributaries Gain Creek and Noyse Creek, passing under Highway 14, and taking in the right tributary Jack Elliott Creek.
Queen Elizabeth Park is a 130-acre [1] municipal park located in Vancouver, British Columbia, Canada. It is located on top of Little Mountain approximately 125 metres (410 ft) above sea level [ 2 ] and is the location of former basalt quarries dug in the beginning of the twentieth century to provide materials for roads in the city.
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