Mount Matheson
   HOME
*





Mount Matheson
Mount Matheson, at , is the highest point in East Sooke East Sooke is an unincorporated community south and east of Sooke, British Columbia, Canada. It consists of over 500 houses (and one volunteer fire department) along with the headquarters of the Royal Canadian Marine Search and Rescue (RCMSAR) ..., British Columbia. From the top there are panoramic views from Cape Flattery to Mount Baker. The bedrock is Eocene-era basalt.http://ftp.maps.canada.ca/pub/nrcan_rncan/publications/ess_sst/119/119507/gscmap-a_1553a_e_1983_mn01.pdf Geology, Victoria, west of sixth meridian. J.E. Muller, 1983 References Mountains of British Columbia under 1000 metres Greater Victoria Juan de Fuca region {{BritishColumbia-geo-stub ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Vancouver Island Ranges
The Vancouver Island Ranges, formerly called the Vancouver Island Mountains, are a series of mountain ranges extending along the length of Vancouver Island which has an area of . The Vancouver Island Ranges comprise the central and largest part of the island. The Geological Survey of Canada refers to Vancouver Island, Haida Gwaii, and the Alaska Panhandle as the Insular Belt including the sea floor out to 100 km (62 mi) west of Vancouver Island. The Vancouver Island Ranges are a sub-range of the Insular Mountains. Explorations The first European sighting of these ranges was likely Sir Francis Drake. A sighting of land on June 5, 1579 was recorded by his crew aboard the vessel ''Golden Hind'' at a latitude of 48 degrees north but not finding safe harbour, they moved on southward. The highest peak of the Vancouver Island Ranges, the Golden Hinde, is named for his vessel. The first European explorer likely to have observed any of the mountains of the Vancouver Island ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


List Of Mountains Of British Columbia
List of mountains of British Columbia is a list of mountains in the Canadian province of British Columbia. List of Mountains See also *Geography of British Columbia *List of mountains of Canada *Mountain peaks of Canada *List of mountain peaks of North America *List of mountain peaks of the Rocky Mountains Notes {{reflist British Columbia Mountains A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher th ...
...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6million people in Metro Vancouver. The first known human inhabitants of the area settled in British Columbia at least 10,000 years ago. Such groups include the Coast Salish, Tsilhqotʼin, and Haida peoples, among many others. One of the earliest British settlements in the area was Fort Victoria, established ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

National Topographic System
The National Topographic System or NTS is the system used by Natural Resources Canada for providing general purpose topographic maps of the country. NTS maps are available in a variety of scales, the standard being 1:50,000 and 1:250,000 scales. The maps provide details on landforms and terrain, lakes and rivers, forested areas, administrative zones, populated areas, roads and railways, as well as other man-made features. These maps are currently used by all levels of government and industry for forest fire and flood control (as well as other environmental issues), depiction of crop areas, right-of-way, real estate planning, development of natural resources and highway planning. To add context, land area outside Canada is depicted on the 1:250,000 maps, but not on the 1:50,000 maps. History Topographic mapping in Canada was originally undertaken by many different agencies, with the Canadian Army’s Intelligence Branch forming a survey division to create a more standardized mappi ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

East Sooke
East Sooke is an unincorporated community south and east of Sooke, British Columbia, Canada. It consists of over 500 houses (and one volunteer fire department) along with the headquarters of the Royal Canadian Marine Search and Rescue (RCMSAR) organization on the south side of the Sooke Basin. East Sooke borders on East Sooke Regional Park, an area of , with views south to Olympic National Park in the United States. East Sooke does not have a town council. Instead it is governed by a regional director who is also responsible for other unincorporated areas in the Capital Regional District (the regional district of Greater Victoria). East Sooke's general character is rural, although it is a bedroom community of Victoria, British Columbia. Its close proximity to Victoria, its character as a bedroom community, and its large tracts of undeveloped land have made it an attractive location for recreation and retirement developments. Political scuffles over the development of the com ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Cape Flattery (Washington)
Cape Flattery () is the northwesternmost point of the contiguous United States. It is in Clallam County, Washington on the Olympic Peninsula, where the Strait of Juan de Fuca joins the Pacific Ocean. It is also part of the Makah Reservation, and is the northern boundary of the Olympic Coast National Marine Sanctuary. Cape Flattery can be reached from a short hike, most of which is boardwalked. Cape Flattery Trail, with photographs. The westernmost point in the contiguous United States is at Cape Alava, south of Cape Flattery in Olympic National Park. However, the westernmost tip of Cape Flattery is almost exactly as far west as Cape Alava, the difference being approximately 5 seconds of longitude, about , at high tide and somewhat more at low tide. The Cape Flattery Lighthouse is on Tatoosh Island, just off the cape. Makah Bay and Neah Bay are on either side of the cape. Neah Bay, Washington is the closest town to the cape. History James Cook Cape Flattery is the oldest per ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Mount Baker
Mount Baker (Lummi: '; nok, Kw’eq Smaenit or '), also known as Koma Kulshan or simply Kulshan, is a active glacier-covered andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount St. Helens. About due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field. While volcanism has persisted here for some 1.5 million years, the current volcanic cone is likely no more than 140,000 years old, and possibly no older than 80–90,000 years. Older volcanic edifices have mostly eroded away due to glaciation. After Mount Rainier, Mount Baker has the heaviest glacier cover of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, is greater than that of all the other Cascades volcanoes (except Rainier) combined. It is also one of the snowiest places in the world; ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Mountains Of British Columbia Under 1000 Metres
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Greater Victoria
Greater Victoria (also known as the Greater Victoria Region) is located in British Columbia, Canada, on the southern tip of Vancouver Island. It is usually defined as the thirteen municipalities of the Capital Regional District (CRD) on Vancouver Island as well as some adjacent areas and nearby islands. The Capital Regional District administers some aspects of public administration for the whole metro region; other aspects are administered by the individual member municipalities of Greater Victoria. Roughly, Greater Victoria consists of all land and nearby islands east of a line drawn from the southern end of Finlayson Arm to the eastern shore of Sooke Harbour, along with some lands on the northern shore of Sooke Harbour. Many places, buildings, and institutions associated with Victoria such as the University of Victoria, Victoria International Airport, and the Swartz Bay Ferry Terminal, are outside the City of Victoria itself, which has an area of just on the sout ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]