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    Economy[ edit ] Aberdeen Centreone of the many Asian-themed shopping malls in Richmond. Richmond supports aboutjobs in various areas including services, retailing, tourism, light manufacturing, airport services and aviation, agriculture, fishing, and government. Before its dissolution, Canadian Airlines operated an office in Richmond.

    Of this area, 3, hectares are farmed by farms; the rest is either vacant or occupied by non-farm uses.

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    Cranberries and blueberries are the dominant crops grown. Other crops grown include strawberriescornand potatoes. Success from these malls has created significant economical growth in Richmond. Richmond Centre has become Canada's 12th most profitable mall. The strip malls located on Alexandra Road are famous for their restaurants and the area is more commonly known as "food street". Development[ edit ] City Centre development plan[ edit ] This article's tone or style may not reflect the encyclopedic tone used on Wikipedia.

    See Wikipedia's guide to writing better articles for suggestions. August Learn how and when to remove this template message East-facing aerial view of Westminster Highway and Canada Line Richmond city planners are one year into their update of its official plan for the city centre. The plan is anchored by the Canada Line and includes the development of nine transit-oriented village centres. The population of the area is expected to grow from about 40, toresidents. According to a senior planner for the city, the goal of the plan is to "turn the middle arm of the Fraser River into a focus instead of an edge.

    Now, they want people to face the river and embrace the waterfront. The property owner, Vanprop Investment Inc.

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    Aspac's plans are for "probably the highest-end development Richmond has seen to date" said Mayor Brodie. Some construction will not begin until afterand will take up to 12 years to complete. The warehouses and commercial parks near the development are also slated for redevelopment.

    Lecky Boathouse[ edit ] The University of British Columbia recently constructed a new boathouse along the river. The popular John M. Lecky boathouse [33] draws crowds from rowing regattas and Dragon Boat Races. Cambie Road Pedestrian Bridge[ edit ] A possible pedestrian bridge where Cambie Road reaches the river is also being included in a future vision of the area.

    It would link nature trails on the north and south banks, and make Aberdeen Centre within walking distance for BCIT's aerospace campus students. The mixed use development would include over 2, residential units, various commercial uses, and a hotel. The Canada Line is considered critical to the project. A fifth Richmond station at Capstan Way No. Also included will be affordable housing units, a space daycare, and a 0. Live-work dwellings are also being proposed by the developers, where shop owners would live above their ground level operations.

    Aberdeen Centre[ edit ] Fairchild Developments is building a six floor expansion to its Chinese-oriented shopping centre. The plan includes an office building, and a link to the Canada Line's Aberdeen Station. The mall is also considering purchasing transit coupons for staff and customers to encourage them to use the new line.


    The new complex was completed in The casino is currently in the process of adding an addition above the newly added six story car park and skytrain Bridgeport Station. The City of RichmondCanada Lands Companyand the Musqueam Indian Band entered a agreement with the federal government that included the intent to remove the land from the ALR for the purposes of high-density development.

    The application was rejected on 10 February The lawsuit remains dormant and it is the understanding of Coun. Harold Steves that the lawsuit will remain dormant unless the city wants to develop the lands into anything that is not related to ALR use". This event includes a parade, and a huge barbecued salmon sale in front of the Steveston Community Centre.

    It is a family event that celebrates the region's maritime heritage with live entertainment, ships, exhibits and demonstrations. InRichmond hosted a tall ships festival which attracted an estimatedpeople to Steveston.

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    The success of this event surpassed many expectations and caused traffic congestion in the usually quiet area. Toys, clothes, cell phones, and food are available along with live entertainment.

    It is very popular and is usually crowded.

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    This marked the first time the ceremony had taken place on the West Coast, as it traditionally takes place in Toronto.
    Etymology[ edit ] The name of the mountains is a translation of an Amerindian name that is closely related to Algonquian ; the Cree name as-sin-wati is given as, "When seen from across the prairies, they looked like a rocky mass". The first mention of their present name by a European was in the journal of Jacques Legardeur de Saint-Pierre inwhere they were called "Montagnes de Roche".

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    Other mountain ranges continue beyond those two rivers, including the Selwyn Mountains in Yukonthe Brooks Range in Alaskaand the Sierra Madre in Mexicobut those are not part of the Rockies, though they are part of the American Cordillera.

    Their counterparts north of the Kootenai Riverthe Columbia Mountainsare considered a separate system in Canada, lying to the west of the huge Rocky Mountain Trench. This runs the length of British Columbia from its beginnings in the middle Flathead River valley in western Montana to the south bank of the Liard River.

    In Canada, geographers define three main groups of ranges: The Muskwa and Hart Ranges together comprise what is known as the Northern Rockies the Mackenzie Mountains north of the Liard River are sometimes referred to as being part of the Rocky Mountains, but this is an unofficial designation. The Tetons are a rugged subrange in Wyoming. The Rocky Mountains are notable for containing the highest peaks in central North America. Farther north in Alberta, the Athabasca and other rivers feed the basin of the Mackenzie Riverwhich has its outlet on the Beaufort Sea of the Arctic Ocean.

    See Rivers of the Rocky Mountains for a list of rivers. Human population is not very dense in the Rocky Mountains, with an average of four people per square kilometer and few cities with over 50, people. However, the human population grew rapidly in the Rocky Mountain states between and The populations of several mountain towns and communities have doubled in the last forty years. Geology of the Rocky Mountains The rocks in the Rocky Mountains were formed before the mountains were raised by tectonic forces.

    The oldest rock is Precambrian metamorphic rock that forms the core of the North American continent. There is also Precambrian sedimentary argillitedating back to 1. During the Paleozoicwestern North America lay underneath a shallow sea, which deposited many kilometers of limestone and dolomite.

    This mountain-building produced the Ancestral Rocky Mountains. They consisted largely of Precambrian metamorphic rock forced upward through layers of the limestone laid down in the shallow sea. Terranes began colliding with the western edge of North America in the Mississippian approximately million years agocausing the Antler orogeny.

    In Canada, the terranes and subduction are the foot pushing the rug, the ancestral rocks are the rug, and the Canadian Shield in the middle of the continent is the hardwood floor. Scientists hypothesize that the shallow angle of the subducting plate increased the friction and other interactions with the thick continental mass above it. Tremendous thrusts piled sheets of crust on top of each other, building the broad, high Rocky Mountain range.

    Just after the Laramide orogeny, the Rockies were like Tibet: In the last sixty million years, erosion stripped away the high rocks, revealing the ancestral rocks beneath, and forming the current landscape of the Rockies. Periods of glaciation occurred from the Pleistocene Epoch 1. These ice ages left their mark on the Rockies, forming extensive glacial landforms, such as U-shaped valleys and cirques.

    Recent glacial episodes included the Bull Lake Glaciationwhich began aboutyears ago, and the Pinedale Glaciationwhich perhaps remained at full glaciation until 15,—20, years ago. For example, volcanic rock from the Paleogene and Neogene periods 66 million — 2.

    Millennia of severe erosion in the Wyoming Basin transformed intermountain basins into a relatively flat terrain. The Tetons and other north-central ranges contain folded and faulted rocks of Paleozoic and Mesozoic age draped above cores of Proterozoic and Archean igneous and metamorphic rocks ranging in age from 1. Ecology of the Rocky Mountains There are a wide range of environmental factors in the Rocky Mountains. Tundra in the Rocky Mountains of Colorado Instead, ecologists divide the Rocky Mountain into a number of biotic zones.

    Each zone is defined by whether it can support trees and the presence of one or more indicator species.

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    Two zones that do not support trees are the Plains and the Alpine tundra. Near treeline, zones can consist of white pines such as whitebark pine or bristlecone pine ; or a mixture of white pine, fir, and spruce that appear as shrub-like krummholz. Finally, rivers and canyons can create a unique forest zone in more arid parts of the mountain range.

    The Rocky Mountains are an important habitat for a great deal of well-known wildlife, such as elkmoosemule and white-tailed deerpronghornmountain goatsbighorn sheepbadgersblack bearsgrizzly bearscoyoteslynxesand wolverines.

    The status of most species in the Rocky Mountains is unknown, due to incomplete information. European-American settlement of the mountains has adversely impacted native species. Examples of some species that have declined include western toadsgreenback cutthroat troutwhite sturgeonwhite-tailed ptarmigantrumpeter swanand bighorn sheep.

    In the United States portion of the mountain range, apex predators such as grizzly bears and gray wolves had been extirpated from their original ranges, but have partially recovered due to conservation measures and reintroduction. Other recovering species include the bald eagle and the peregrine falcon. Like the modern tribes that followed them, Paleo-Indians probably migrated to the plains in fall and winter for bison and to the mountains in spring and summer for fish, deer, elk, roots, and berries.

    In Colorado, along with the crest of the Continental Divide, rock walls that Native Americans built for driving game date back 5,—5, years. A growing body of scientific evidence indicates that indigenous people had significant effects on mammal populations by hunting and on vegetation patterns through deliberate burning.


    Native American populations were extirpated from most of their historical ranges by disease, warfare, habitat loss eradication of the bisonand continued assaults on their culture. The Lewis and Clark Expedition — was the first scientific reconnaissance of the Rocky Mountains. The expedition was said to have paved the way to and through the Rocky Mountains for European-Americans from the East, although Lewis and Clark met at least 11 European-American mountain men during their travels.

    Among the most notable are the expeditions of David Thompson explorerwho followed the Columbia River to the Pacific Ocean. Resolution of the territorial and treaty issues, the Oregon disputewas deferred until a later time. InSpain ceded their rights north of the 42nd Parallel to the United States, though these rights did not include possession and also included obligations to Britain and Russia concerning their claims in the same region.

    Settlement[ edit ] AfterAmerican fur traders and explorers ushered in the first widespread Caucasian presence in the Rockies south of the 49th parallel. Negotiations between the United Kingdom and the United States over the next few decades failed to settle upon a compromise boundary and the Oregon Dispute became important in geopolitical diplomacy between the British Empire and the new American Republic.

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    Despite such efforts, inBritain ceded all claim to Columbia District lands south of the 49th parallel to the United States; as resolution to the Oregon boundary dispute by the Oregon Treaty.

    The Idaho gold rush alone produced more gold than the California and Alaska gold rushes combined and was important in the financing of the Union Army during the American Civil War. The transcontinental railroad was completed in[28] and Yellowstone National Park was established as the world's first national park in Though political complications pushed its completion tothe Canadian Pacific Railway eventually followed the Kicking Horse and Rogers Passes to the Pacific Ocean.

    President Harrison established several forest reserves in the Rocky Mountains in — Economic development began to center on miningforestryagricultureand recreationas well as on the service industries that support them. Tents and camps became ranches and farms, forts and train stations became towns, and some towns became cities.

    Minerals found in the Rocky Mountains include significant deposits of coppergold, leadmolybdenumsilvertungstenand zinc. The Wyoming Basin and several smaller areas contain significant reserves of coalnatural gasoil shaleand petroleum. For example, the Climax mine, located near LeadvilleColorado, was the largest producer of molybdenum in the world. Molybdenum is used in heat-resistant steel in such things as cars and planes. The Climax mine employed over 3, workers.

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    The Coeur d'Alene mine of northern Idaho produces silver, lead, and zinc. In one major example, eighty years of zinc mining profoundly polluted the river and bank near Eagle River in north-central Colorado. High concentrations of the metal carried by spring runoff harmed algaemossand trout populations. An economic analysis of mining effects at this site revealed declining property values, degraded water quality, and the loss of recreational opportunities. The Rocky Mountains contain several sedimentary basins that are rich in coalbed methane.

    Coalbed methane is natural gas that arises from coal, either through bacterial action or through exposure to high temperature. Coalbed methane supplies 7 percent of the natural gas used in the United States. These two basins are estimated to contain 38 trillion cubic feet of gas. Coalbed methane can be recovered by dewatering the coal bed, and separating the gas from the water; or injecting water to fracture the coal to release the gas so-called hydraulic fracturing.

    Agriculture includes dryland and irrigated farming and livestock grazing. Livestock are frequently moved between high-elevation summer pastures and low-elevation winter pastures, a practice known as transhumance.

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