A moraine is any accumulation of unconsolidated debris ( regolith and rock ), sometimes referred to as glacial till , that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour . Lateral moraines are those formed at the side of the ice flow, and terminal moraines are those formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines ( till -covered areas forming sheets on flat or irregular topography ) and medial moraines (moraines formed where two glaciers meet).
93-508: Wapusk National Park ( / w ə ˈ p ʌ s k / ) is Canada's 37th national park , established in 1996. The name comes from the Cree word for polar bear ( wâpask ). Located on the shores of Hudson Bay in the Hudson Plains ecozone 45 kilometres (28 mi) south of Churchill , its accessibility is limited due to its remote location and an effort to preserve the park. The park
186-684: A country dependent on natural resources, Canada's national parks represent a compromise between the demand for profit from the land's resources and tourism and the need for preservation and sustainable development . While conservationist ideas and a Canadian desire towards getting back to nature were evident in the early development of national parks in Canada, a greater role was played by chambers of commerce, local governments, promoters of tourism, and recreational groups who advocated for profit-driven commercial development, while incorporating wildlife preservation when possible. Canada's national parks allowed
279-624: A faster rate. As a tactic to increase the number of people travelling to and through national parks, members of each constituency surrounding national parks began to advocate for the construction of well-built roads, including the development of the Trans-Canada Highway . As the main highway travelling through the Canadian Rockies, the Trans-Canada Highway has provided accessible visitation and commerce to
372-407: A glacier or former glacier, or by shape. The first approach is suitable for moraines associated with contemporary glaciers—but more difficult to apply to old moraines , which are defined by their particular morphology, since their origin is debated. Some moraine types are known only from ancient glaciers, while medial moraines of valley glaciers are poorly preserved and difficult to distinguish after
465-404: A healthy ecosystem exists. Ecosystems in national parks have often been damaged due to the exploitation of resources, the expansion of tourism, and external land use practices outside national parks. Through Parks Canada realizing the necessity of managing national parks by human hands to maintain biotic and abiotic components, Parks Canada placed an emphasis on ecological integrity within
558-457: A lack of communication from stakeholders. The Wapusk National Park 2017 Management plan aims to foster greater participation between policy makers and local indigenous communities and incorporate valuable traditional ecological knowledge into management strategies to ensure prosperity for all. Wapusk National Park is home to a number of species, including animals and plants. The park shelters polar bears, birds, wolves, caribou, and many more. During
651-579: A large part of the Hudson Bay Lowlands , a subarctic region bordering Hudson Bay that is mostly muskeg and wet peatlands . Wapusk National Park lies on the traditional territories of many Indigenous communities such as the Cree of York Factory, Fox Lake, Sayisi-Dene, and Inuit. Native species like caribou and polar bears are being heavily affected by climate change through warmer temperatures, ice and permafrost melting, and changing vegetation in
744-591: A minor shift towards preservationist attitudes over Canada's parks as recreational use and development was still permitted. The initial ideal of national parks was to create uninhabited wilderness. Creating this required the displacement of Indigenous and non-Indigenous residents who lived within the intended park boundaries, and restrictions on how these residents had previously used the land and resources within parks for subsistence. Jasper National Park , established in 1907, restricted income-generating activities such as hunting, along with culturally valuable practices of
837-535: A prairie restoration. The bison grazing patterns help to maintain a variety of prairie biodiversity. In Gwaii Haanas National Park Reserve and Haida Heritage Site , removing Norway rats which were accidentally introduced to the area, is conducted because they eat eggs, as well as juvenile and adult seabirds, and reduce the seabird population. Staff monitor for the return of rats by trapping and poison baits for recovering native seabird populations. Through parks policies and operation practices, Parks Canada has recognized
930-452: A series of transverse ridges running across a valley behind a terminal moraine. They form perpendicular to the lateral moraines that they reside between and are composed of unconsolidated debris deposited by the glacier. They are created during temporary halts in a glacier's retreat. In permafrost areas an advancing glacier may push up thick layers of frozen sediments at its front. An arctic push moraine will then be formed. A medial moraine
1023-696: A variety of landscapes that mark Canada's natural heritage. On July 20, 1871, the Crown Colony of British Columbia committed to Confederation with Canada. Under the union's terms, Canada was to begin construction of a transcontinental railway to connect the Pacific Coast to the eastern provinces. As the Canadian Pacific Railway surveyors began to study the land in 1875, the location of the country's natural resources sprouted further interest. Evidence of minerals quickly introduced
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#17327651735771116-615: A wide range of protected areas, encompassing National Historic Sites , National Marine Conservation Areas (NMCA), and National Park Reserves. Canada established its first national park in Banff in 1885, and has since expanded its national park system to include 37 national parks and 11 national park reserves. Canada's first national park , located in Banff , was established in 1885. Tourism and commercialization dominated early park development, followed closely by resource extraction. Commodifying
1209-560: A worldview of ecology and abundance to one where the environment acted as a limited resource. Created in 1909, the Commission of Conservation became the Canadian forum for conservation issues, acting as an advisory and consultative body used to answer questions related to conservation and better utilization of Canada's natural and human resources. The Commission focused on a concept that maximized future profits through good management in
1302-538: Is 11,475 square kilometres (4,430 sq mi) of protected diverse and remote wilderness, located in Northeast Manitoba along the coast of Hudson Bay. Wapusk derives from the Cree word for "white bear" , and as the meaning indicates, is a significant maternity denning area for the polar bear, Ursus maritimus . The park is also characterized by being part of a large transitional zone between the three biomes of arctic tundra, marine, and boreal forest. It includes
1395-640: Is a ridge of moraine that runs down the center of a valley floor. It forms when two glaciers meet and the debris on the edges of the adjacent valley sides join and are carried on top of the enlarged glacier. As the glacier melts or retreats, the debris is deposited and a ridge down the middle of the valley floor is created. The Kaskawulsh Glacier in the Kluane National Park , Yukon , has a ridge of medial moraine 1 km wide. Supraglacial moraines are created by debris accumulated on top of glacial ice. This debris can accumulate due to ice flow toward
1488-430: Is also affecting the vegetation structure of subarctic ecosystems, which impacts the wildlife that depends on these ecosystems. Flooding and raising of bogs impact the polar bear habitat and the reductions in the space of arctic tundra due to permafrost melting has impacts on caribou. The Lesser Snow Geese, a keystone species , are rapidly increasing population wise and are destroying vegetation and soil conditions which
1581-960: Is concern as tundra ecosystems are extremely sensitive to impacts, specifically, human trampling of tundra vegetation. Lichens are the primary food of caribou in winter, are very sensitive to impact and can all die in an area after only low levels of trampling. Increased tourism can create problems for the species living in Wapusk National Park that are already struggling from climate change and habitat loss . National Parks of Canada National parks of Canada Parcs Nationaux du Canada ( French ) [REDACTED] Herbert Lake in Banff National Park , Alberta [REDACTED] Distribution and location of national parks in Canada National parks of Canada are vast natural spaces located throughout
1674-582: Is currently one NMCA Reserve: Two areas are under consideration as a National Marine Conservation Area or NMCA Reserve: In addition to national parks, a National Landmarks program was foreseen in the 1970s and 1980s, but has not been established beyond a single property. Landmarks were intended to protect specific natural features considered "outstanding, exceptional, unique, or rare to this country. These natural features would typically be isolated entities and of scientific interest." To date, only one Landmark has been established— Pingo National Landmark —in
1767-482: Is expected that park reserves will become national parks under the National Parks Act when the land claims are resolved. These include: The following areas have been proposed as Parks or Reserves, studied, and discussed among stakeholders: In addition, Parks Canada is considering other areas for future national parks: National Marine Conservation Areas (NMCAs) are a relatively new creation within
1860-401: Is home to Cape Churchill, which is renowned as the best location in the world to view and photograph wild polar bears. Cape Churchill is only accessible by helicopter or Tundra Buggy. The park was the subject of a short film in 2011's National Parks Project , directed by Hubert Davis and scored by Kathleen Edwards , Matt Mays and Sam Roberts . Established in 1996, Wapusk National Park
1953-417: Is increasing the salinity of nearby bodies of water. This not only affects the aquatic community, but again, polar bears and caribou. Steps are currently being taken by Wapusk National Park to reduce the population and fix the damages done by the geese. Wapusk National Park does not receive many visitors as the only way to access the park is through helicopter overflights or over snow into the denning area in
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#17327651735772046-419: Is leading to a decline in the conditions of polar bears who are having to come ashore earlier with less fat resources built up. This has negative impacts on reproduction in terms of litter size, cub mass, survival of dependent young, etc., and affects the overall abundance of polar bears. Tracking the numbers of polar bears is currently very important in these subarctic regions. Caribou are also being affected by
2139-594: Is proven from the data collected in 1994 that noted 500, 000 caribou compared to 2017 where only 288, 000 where reported. This data is based on the Qamanirjuaq herd which covers areas in Manitoba, Nunavut, Saskatchewan, and the Northwest Territories. There are a number of active threats against the population of caribou, the first being climate change. The rising hot temperatures are only threatening
2232-655: The American Museum of Natural History and City College of the City University of New York published a report in Canadian Field-Naturalist offering the first documented evidence that the temperamental grizzly bears are migrating into polar bear territory . Researchers found that seven grizzlies have been spotted in Wapusk National Park south of Churchill, between 2003 and 2008. Wapusk National Park shares its southwestern border with
2325-449: The National Parks Act was established. Under this act, mineral exploration and development were banned and only limited use of timber was permitted within the parks. For Canada to continue its economic success through resource development, the boundaries of Canada's national parks were altered prior to the 1930 Act in order to exclude resource rich land from park areas. The exclusion of resource development in Canada's national parks marked
2418-529: The Northwest Territories . Another was proposed at the same time (1984)— Nelson Head National Landmark —on the southern tip of Banks Island , also in the Northwest Territories. It was to include some 180 km (70 sq mi), 40 km (25 mi) of coastline, and protect the sea cliffs at Nelson Head and Cape Lambton. Durham Heights were to be included, which reach an elevation of 747 m (2,450 ft). The legislation providing for
2511-425: The 1600’s. First Nations shared their ecological knowledge with settlers, and the fur trade began. The Hudson Bay Company established roots in the area because the location was effective for shipping and transportation. 1910 was when Treaty 5 was signed, an agreement with Canada that interfered with traditional resource management defined by the distribution of harvesting and allowing time for resources to recover before
2604-561: The Aboriginal groups who had used the region. Jasper is a large park in the southern, frequently visited portion of Canada, and one of many parks geared towards tourism more than preservation. Most parks are designed to have the appeal of uninhabited wilderness while also having amenities and roads to facilitate visitors. Human activity within the park was allowed, but primarily only those activities that generated revenue, such as snowboarding and lodging for tourists. Some have claimed that
2697-521: The Acadians who comprised approximately 85 percent of the over 1,500 people who were displaced to create the park. Many inhabits dispossessed of their land by Parks Canada resisted, and the Acadian residents' resistance of eviction was extensive enough to delay the official opening of the park until 1979. Through protest and civil disobedience, they won greater compensation from the government to address
2790-636: The Banff, Jasper, Yoho and Kootenay National Parks have been officially designated land as wilderness in national parks. The boundaries of all communities in national parks are changed and the developments of commerce in their communities are restricted. Profit no longer became priority and initiative for preservation through ecological integrity increased. To maintain or restore ecological integrity, ecosystem restorations are implemented in many parks, attempting to bring back damaged ecosystems to their original healthy state and making them sustainable. For example, Grasslands National Park brought back Bison bison for
2883-499: The Churchill Wildlife Management Area (WMA) which was established in 1978. Wapusk National Park itself was established to protect the area which is a unique transitional zone between three biomes and the existing strong biodiversity among plant and animal species. These three biomes include tundra , marine, and boreal . Wapusk National Park was created with future generations in mind, so they can enjoy
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2976-622: The Hudson Bay melts entirely, waiting on the tundra until the water freezes again in November. Pregnant females remain ashore, sheltered in maternity dens within the peatlands in Wapusk, giving birth in peat dens, emerging each year in March. Numerous birds are found in Wapusk National Park and it is a likely breeding area of the short-billed dowitcher . In 2010, biologists affiliated with
3069-540: The Labrador Inuit Park Impacts and Benefits Agreement with Inuit Association. As with the Ivvavik agreement, it ensures that Inuit can continue to use land and resources as their traditional activities and keep their exclusive relationship with the land and ecosystems. In addition, they agreed to manage the park cooperatively. A seven-member co-operative management board will be established to advise
3162-660: The Landmark required a formal request be made by the Minister of the Environment within 10 years (until 1994). None was ever made. [REDACTED] Canada portal [REDACTED] Geography portal Moraine The word moraine is borrowed from French moraine [mɔ.ʁɛn] , which in turn is derived from the Savoyard Italian morena ('mound of earth'). Morena in this case
3255-691: The Northwest Territories. Qausuittuq, Quttinirpaaq, Sirmilik and Ukkusiksalik, in Nunvut. Akami-Uapishkᵁ-KakKasuak-Mealy Mountains and Torngat Mountains in Newfoundland and Labrador. Sable Island, Nova Scotia. The Bruce Peninsula and Rouge in Ontario. Wapusk, Manitoba, and Gwaii Haanas and Gulf Islands in British Columbia. A national park reserve is an area administered and protected like a national park but subject to Indigenous land claims . It
3348-522: The Rocky Mountains Park Bill was proposed, it elicited various criticisms at the time, one being the implicit contradiction between the exploitation of resources within this national reservation. However, the overarching nineteenth century ideology that lumbering and mining would contribute to the usefulness of the reserve as opposed to depreciating the park overshadowed the concerns of resource exploitation. The natural resources within
3441-589: The Rogen moraines look like tigerstripes on aerial photographs . Rogen moraines are named after Lake Rogen in Härjedalen , Sweden , the landform's type locality. Closely related to Rogen moraines, de Geer moraines are till ridges up to 5m high and 10–50m wide running perpendicular to the ice flow. They occur in large groups in low-lying areas. Named for Gerard De Geer , who first described them in 1889, these moraines may have developed from crevasses underneath
3534-491: The accumulation of sand and gravel deposits from glacial streams emanating from the ice margin. These fan deposits may coalesce to form a long moraine bank marking the ice margin. Several processes may combine to form and rework a single moraine, and most moraines record a continuum of processes. Reworking of moraines may lead to the formation of placer deposits of gold as is the case of southernmost Chile . Moraines can be classified either by origin, location with respect to
3627-510: The area the national park covers overlaps the indigenous communities of the Cree and Chipewyan indigenous communities. European settlements also occupied the area as early as 1619 and onwards. The location of the protected park was between two large trade centres, the York Factory and Prince of Wales Fort in 1684 and 1731. Trade relied on the fur found in those parts of Manitoba and lasted for 250 years. In later years,1940's and 1980's,
3720-610: The area. The highway is designed to provide a heavy flow of traffic, while also including many accessible pull-offs and picnic areas. With a high frequency of travelers and many destinations to stop, tourism boomed after the Trans-Canada Highway was established. As the highway travels through Banff and the Bow Valley area, it includes scenic views of most of the mountains, and an environment rich with wildlife. With an increase in tourism to Rocky Mountain Park, growth and prosperity came to
3813-408: The base of the ice as lodgment till with a thin and discontinuous upper layer of supraglacial till deposited as the glacier retreats. It typically is found in the areas between end moraines. Rogen moraines or ribbed moraines are a type of basal moraines that form a series of ribs perpendicular to the ice flow in an ice sheet . The depressions between the ribs are sometimes filled with water, making
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3906-484: The bird sanctuary in Point Pelee, began developing. In order to push their views further, this movement, headed by James B. Harkin and Arthur Oliver Wheeler , was forced to argue that divine scenery was itself a source of profit – tourism – in order to push aside what they saw as a far greater avenue of exploitation: resource extraction. By 1930, even the conservation movements within Canada came to understand that
3999-438: The cold has an effect on the appearance of the park. Not only do the leaves on the trees change colour but the rest of the plants shift shades as well. Other species of plants that bloom at Wapusk are alpine azalea, common yarrow, wild rosemary, roundleaf orchis, cutleaf anemone, field wormwood, and fireweed. Caribou are one of the most noticeable species at Wapusk National Park that have been steadily declining in population. This
4092-529: The construction of mines and resource exploitation in Canada's previously untouched wilderness. Exploration led to the discovery of hot springs near Banff, Alberta , and in November 1885, the Canadian Government made the springs public property, protecting them from possible private ownership and exploitation. This event brought about the beginning of Canada's movement towards preserving land and setting it aside for public usage as national parks. By
4185-428: The cooler environment that they are built to live in. The act of wildfires have also played a role in the caribou decline. Habitat loss has been an important contributor as the human activities of mining, logging, and oil development have impacted caribou habitats. As for conservation efforts, Wapusk National Park is a protected area with limited human disruptions. They take matters in migration routes, calving grounds, and
4278-605: The country that are protected by Parks Canada , a government agency. Parks Canada manages the National Parks and Reserves in order to protect and preserve the Canadian wildlife and habitat that fall within the ecosystems of the park, keep them safe, educate visitors, and ensure public enjoyment in ways that do not compromise the area for future generations. The areas that fall within Parks Canada's governance include
4371-456: The country's national parks had an entrenched system of profit-based motives. The Parks Canada Agency Act came into action in 1998 to ensure the protection of parks for further generations' use and national interest as places of cultural and historical importance. According to Parks Canada, ecological integrity is a state with three elements: non-living elements, living elements, and a series of ecological functions. By having all three elements,
4464-533: The creation of the first administrative body, the Dominion Parks Branch, now known as Parks Canada , to administer national parks in Canada. With the Branch in place, the parks system expanded from Banff eastward, combining both use and protection as the foundation to national park management. The major motives behind the creation of national parks in Canada were profit and preservation. Inspired by
4557-462: The development of a campground, trailer park, and other attractions. Cave and Basin Springs were forced to rebuild their bathing pools in 1904 and then again in 1912, because of growing public interest in the hot springs. By 1927, campground accommodations at Tunnel Mountain were adapting to include room for trailers as well as tents. Due to increased demand, the campground was extended, and by 1969 it
4650-564: The establishment and success of Yellowstone National Park in the United States, Canada blended the conflicting ideas of preservation and commercialism in order to satisfy its natural resource needs, conservationist views of modern management, a growing public interest in the outdoors and the new popularity of getting back to nature. This growing interest to escape the hustle and bustle of the city brought about ideas of conserving Canada's unspoiled wildernesses by creating public parks. As
4743-436: The federal minister of Environment for the matters of parks eco-management. Parks Canada recognized Indigenous knowledge and their unique historical and cultural relationship with the lands, and thus, Parks Canada started to cooperate with Indigenous people for park management. Following 1985, began the creation of new national parks or national park reserves, including Aulavik, Nááts’ihch’oh, Tuktut Nogait and Thaidene Nëné, in
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#17327651735774836-493: The glacier is advancing, receding or at equilibrium. The longer the terminus of the glacier stays in one place, the more debris accumulate in the moraine. There are two types of end moraines: terminal and recessional. Terminal moraines mark the maximum advance of the glacier. Recessional moraines are small ridges left as a glacier pauses during its retreat. After a glacier retreats, the end moraine may be destroyed by postglacial erosion. Recessional moraines are often observed as
4929-442: The glacier's surface or deposited as piles or sheets of debris where the glacier has melted. Moraines may form through a number of processes, depending on the characteristics of sediment, the dynamics on the ice, and the location on the glacier in which the moraine is formed. Moraine forming processes may be loosely divided into passive and active . Passive processes involve the placing of chaotic supraglacial sediments onto
5022-515: The governmental, academic, and public level. Canada's national parks were no longer places of unlimited natural resources, but were now considered a place where resources needed to be conserved through regulation to ensure future and continued use. J.B. Harkin , the Parks Commissioner in 1911, advocated the complete eradication of coal and mineral extraction in the parks. However, Harkin's vision did not come to fruition until 1930 when
5115-623: The habitats there. The climate here is subarctic and wet, having many rivers and bogs called " Muskeg " by the indigenous Cree people native to that area. In terms of ecology, Wapusk's location is part of the Hudson Plains ecozone. The historical geology of the Wapusk National Park shows sequences of Palaeozoic aged rocks running northwest to southeast of the map. There are three formations that cover this area: The Severn River formation, Ewkan river formation and Attawapiskat formation . These are all limestone and Dolomite formations. Records of human occupation and resource extractions from Wapusk show
5208-449: The ice sheet. The Kvarken has a very high density of de Geer moraines. End moraines, or terminal moraines , are ridges of unconsolidated debris deposited at the snout or end of the glacier. They usually reflect the shape of the glacier's terminus . Glaciers act much like a conveyor belt, carrying debris from the top of the glacier to the bottom where it deposits it in end moraines. End moraine size and shape are determined by whether
5301-781: The importance of community involvement in order to sustain a healthy ecosystem. The transition towards developing parks as a place of preservation began with the National Parks Act of 1930. This event marked a shift in park management practices. Revised in 1979 under the National Parks Policy, the Act placed greater emphasis on preserving the natural areas in an unimpaired state through ecological integrity and restoration, moving away from development based heavily on profit. Acting as national symbols, Canada's national parks exist in every province and territory representing
5394-527: The importance of working together with Indigenous peoples and other communities to manage parks' healthy ecosystem within and around national parks. In 1984, Ivvavik National Park was established as a result of an Aboriginal land claim agreement. Now, Ivvavik is managed co-operatively by Parks Canada and the Inuvialuit. Their mutual goals are to protect wild life , keep the ecosystem healthy and protect their cultural resources. In addition, they ensure
5487-628: The land was exploited by the military for rocket launch testing by the Churchill Research Range. One of the known historical events to have happened here was the Battle of Hudson's Bay . Indigenous communities have a strong history and a lasting relationship with the land that is now Wapusk National Park. Wapusk National Park is the traditional territory of the Cree of York Factory First Nation, Fox Lake First Nation, Sayisi-Dene First Nation, and Inuit. The Cree from York Factory relied on
5580-417: The landscape with limited reworking, typically forming hummocky moraines. These moraines are composed of supraglacial sediments from the ice surface. Active processes form or rework moraine sediment directly by the movement of ice, known as glaciotectonism. These form push moraines and thrust-block moraines, which are often composed of till and reworked proglacial sediment. Moraine may also form by
5673-594: The late 1880s, Thomas White , Canada's Minister of the Interior, responsible for federal land management, Indian affairs, and natural resources extraction, began establishing a legislative motion towards establishing Canada's first national park in Banff. May 1911 marked one of the most significant events in the administration and development of national parks in Canada as the Dominion Forest Reserves and Parks Act received royal assent. This law saw
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#17327651735775766-610: The loss of fishing within the park that had previously been their main source of income. The resistance of the Acadians impacted future park creation, as in 1979 Parks Canada announced that it would no longer use forced relocation in new parks. An advisory committee was created by Parks Canada in 2008 to reflect on the Kouchibouguac process and address outstanding grievances. In the late 19th century, Canadians changed their view of nature and resources as opinions started to focus on conservationist ideas. They were transitioning from
5859-410: The national parks that marked a shift from profit to preservation. The change in values is derived from the establishment of 1930 National Parks Act that limited use of resource for park management, and in 1979, under revised National Parks Policy, the maintenance of ecological integrity was prioritized for the preservation of national parks of Canada. In 1988, the National Parks Act was amended and
5952-787: The next exploitation. In 2008, "Voices from the Margins: The Muskekowuck Athinuwick/Cree People of Northern Ontario and the Management of Wabusk/Polar Bear" was published accounting stories of Indigenous involvement in the decision-making process about the management of polar bears in Wapusk National Park. The Inuit critiqued various proposed management strategies and changes to the national park, for it impacted their traditional practices. Other challenges for Indigenous participation in decision making processes for Wapusk National Park have included geographic isolation from decision-making facilities, and
6045-529: The park and all its diversity. To ensure this goal is met the Ecological Integrity Monitoring Program (EIMP) builds baseline data to monitor climate change impacts, and the restoration of ecosystems. They work with a variety of external organizations including researchers, provincial governments, and indigenous communities to monitor human and natural change to strengthen resiliency and persistence within ecosystems. The park
6138-626: The park system. There are currently three NMCAs: Fathom Five National Marine Park and Saguenay–St. Lawrence Marine Park were created prior to the NMCA concept, and subsequently classified as an NMCA without changing their legal names. NMCAs have a different mandate than their terrestrial counterparts. They are designed for sustainable use, although they usually also contain areas designed to protect ecological integrity . Similar to national park reserves, National Marine Conservation Area Reserves are intended to become full NMCAs once claims are resolved. There
6231-589: The park, as did Ivvavik National Park in the Northern Yukon. Through grassroots organizations and political lobbying, Indigenous residents of these areas were able to have greater influence over the process of park creation. For both Kluane and Ivvavik parks, Indigenous organizations protested and testified to Parliamentary Committees, describing how these restrictions infringed on their ability to provide for themselves through traditional fishing, hunting, and trapping. Ivvavik National Park, established in 1984,
6324-407: The park. Tourism in this park is not very high but there is concern for the negative impacts increased tourism may cause. The geology of the area has many underlying limestone formations, and a past in fur trade. Glacial processes shape many of the habitats seen today. It is one of Canada's wildest and most remote landscapes. In summer, the polar bears of Wapusk National Park come ashore as the ice on
6417-476: The parks to profit Canada's national economy as well as conserving the natural areas for public and future use became an integrated method of park creation. The process of establishing national parks has often forced the displacement of Indigenous and non-Indigenous residents of areas within the proposed park boundaries. Conflicts between the creation of parks and the residents of the area have been negotiated through co-management practices, as Parks Canada acknowledged
6510-623: The parks were seen as being unlimited and therefore should be used as it was economically beneficial for the nation. By 1911, as Canadians became aware of the depletion occurring within America's natural resources, a debate focused on the extent of resource exploitation in Canada's national parks erupted. This debate began as early as 1906 at the Forestry Convention in Ottawa as it stimulated a new interest in conservation which spoke to
6603-473: The present. Rather than preserving through non-use, the commission was concerned with managing resources for long-term gain. Other conservation-minded organizations, like the Alpine Club , had different ideas that focused on the preservation of natural wilderness and opposed any type of development or construction. This movement was successful as the creation of parks solely for preservation purposes, like
6696-558: The preservation of the Inuvialuit traditional way of living, including trapping, hunting and fishing. Another example is Torngat Mountains National Park . In 2005, it was established as a result of the Labrador Inuit Land Claims Agreement. It preserves the aboriginal rights of the Labrador Inuit in Canada, which are land, resources and self-government rights. The federal government also signed
6789-405: The public an avenue into nature, while also integrating ideas of preserving Canada's scenic landscape and wildlife populations in an era of development and major resource extraction. The integration of public visitation for national parks in Canada heavily contributed to the beginnings of public constituencies for certain parks. The parks who mobilized with a public constituency tended to prosper at
6882-427: The rabbit, geese, bear, and caribou populations as their food sources. No parts of the animals were wasted as they used techniques like smoking, drying, or using the fat for cooking oil. When the caribou moved inland in the winter they would follow. Before industrialization, canoes were modes of transportation on the nearby network of rivers. European traders arrived to the traditional lands of York Factory First Nation in
6975-500: The regulation of ecological integrity was embodied. However, due to the conflicting interests of profit and preservation, the maintenance of ecological integrity has progressed slowly. The big movement on maintenance of ecological integrity has happened since 2001. Canada National Parks Act of 2001 reinforced the necessity of maintenance and restorations of ecological integrity by saving natural resources and ecosystem. It sets new principles for park management plans. Wilderness areas in
7068-471: The retreat or melting of the glacier. Lateral moraines are parallel ridges of debris deposited along the sides of a glacier. The unconsolidated debris can be deposited on top of the glacier by frost shattering of the valley walls or from tributary streams flowing into the valley, or may be subglacial debris carried to the surface of the glacier, melted out, and transported to the glacier margin. Lateral moraines can rise up to 140 meters (460 ft) over
7161-453: The selection of which activities to allow had non-native bias, as it precluded traditional sources of subsistence such as hunting and trapping. Parks in less frequently visited, northern parts of Canada were created with more consideration of Aboriginal usage. Kluane National Park and Reserve in the Yukon initially had restrictions on hunting in order to preserve the presence of wildlife in
7254-538: The several species of plants that reside there. Over one thousand hundred of these species are maintained which is extremely difficult due to the icy conditions of the location. As previously mentioned, bog peat is a popular aspect of the park as about 27% of the grounds are covered in it. The warm weather during the summer allows for certain foods to grow that are also digestible for humans as well as other wildlife. This includes cranberries, crowberries, bearberries, blueberries, cloudberries, and raspberries. As winter arrives,
7347-555: The spring. The majority of park users are scientists, students, and park staff. The visitors usually stay in the Churchill area and do not visit the park, as access is limited to private tours via helicopter, charted aircraft, and over-snow/tundra vehicles and/or all-terrain vehicles. New tourist activities have been considered after the signing of the Wapusk National Park Management Plan, but there
7440-774: The summer, Wapusk is known for their ponds, peat bogs, and small 6.5 foot trees that have remained standing for hundreds of years. The hot weather also attracts tourists with the bay that lies near the shoreline as visitors are able to explore the beaches. It is in the winter when an estimated thousand polar bears make their way through Cape Churchill to familiarize themselves with the cooler weather conditions. At Wapusk National Park, there can also be found over 250 rare bird species. Hundreds of thousands of both shorebirds and waterfowl birds nest here regularly. Other species of birds that can be spotted are great grey owls, stilt sandpipers, snow geese, arctic loons, Caspian terns, peregrine falcons, and much more. This park also draws people in due to
7533-419: The surface in the ablation zone , melting of surface ice or from debris that falls onto the glacier from valley sidewalls. Washboard moraines , also known as minor or corrugated moraines , are low-amplitude geomorphic features caused by glaciers. They consist of low-relief ridges, 1 to 2 meters (3 ft 3 in to 6 ft 7 in) in height and around 100 meters (330 ft) apart, accumulated at
7626-425: The town of Banff. The Banff hot springs were made more accessible after a tunnel was blasted in 1886. Horse-drawn carriages were replaced by buses and taxis, and by the 1960s small cabins had been largely replaced by hotels and motels as the community became geared towards building the national park as a tourist destination. In 1964, the first visitor service centre was established at Lake Louise Station, which included
7719-402: The valley floor, can be up to 3 kilometers (1.9 mi) long, and are steeper close to the glacier margin (up to 80 degrees) than further away (where slopes are typically 29 to 36 degrees. Ground moraines are till-covered areas with irregular topography and no ridges, often forming gently rolling hills or plains, with relief of less than 10 meters (33 ft). Ground moraine is accumulated at
7812-536: The warming temperatures in the case of earlier snow melt, warmer temperatures during the winter and wildfires. These rising temperatures increase insect harassment on caribous. The caribous then exert more energy fleeing this harassment rather than feeding. Caribou feed primarily upon lichens . Climate change has resulted in decreased lichen biomass in arctic regions, a trend that is projected to continue. The increase in wildfires impact lichen biomass and cover, which take up to 75 years to recover from fires. Climate change
7905-477: The winter habitats. Parks Canada teamed up with several forestry companies in 2004 to better protect and recover caribou population as they were listed under Threatened Species by the Species at Risk Act (SARA) . Wapusk National Park is already being heavily affected by climate change and warming temperatures. The changing dates of sea-ice breakup, up to three weeks earlier than usual, caused by warming temperatures
7998-579: Was an example of and the beginning of co-management, which ensured that Indigenous voices would be heard and given equal representatives on parks boards. Non-Indigenous groups were also dispossessed from their land during the creation of national parks, such as the Acadians of Kouchibouguac National Park in New Brunswick . This park was created in 1969 and included recognition of the Aboriginal groups who had once resided there but no recognition of
8091-734: Was clear from policy making that tourism became secondary to resource exploitation. The resources that were exploited from the national parks were essential to the CPR's income as it freighted these resources across the country. In 1887, the Rocky Mountains Park Act was established under the Macdonald government and it reflected the importance of resource exploitation for Canada's economy. Under this regulation, national parks were not fully preserved in their natural states as mining, logging and grazing continued to be permitted. When
8184-429: Was demonstrated by the creation of Bankhead, a coal town on the road to Lake Minnewanka. This coal town was not viewed as a detriment to the overall scenery of Banff National Park, but was instead an added attraction for visitors. In this case, resource exploitation and tourism worked in conjunction with each other to create a more profitable national park. Although tourism and resource development could work together, it
8277-523: Was derived from Provençal morre ('snout'), itself from Vulgar Latin * murrum ('rounded object'). The term was introduced into geology by Horace Bénédict de Saussure in 1779. Moraines are landforms composed of glacial till deposited primarily by glacial ice. Glacial till, in turn, is unstratified and unsorted debris ranging in size from silt -sized glacial flour to large boulders. The individual rock fragments are typically sub-angular to rounded in shape. Moraines may be found on
8370-522: Was set up to protect the environment and the Cree traditions. It is a young landscape formed by erosion from the last glacial period, which forms many subarctic habitats. Evidence of this is seen from the glacial features like moraines , eskers and strand lines left by moving glaciers. This glaciation resulted in environments like far extending beaches and plains dipping towards Hudson Bay . The geography consists of coastal tundra habitats with coastal marshes, beach ridges and freshwater sedges which make up
8463-456: Was the biggest campground in the national park system. Banff became a year-round recreational centre as the growth of winter sport activities provided added incentive for tourism. The implementation of T-bars and chairlifts on Banff's ski hills helped develop Banff into a ski and winter sports destination. Since the inception of Canada's national parks, business and profit has been a major element to their creation and development. Although tourism
8556-499: Was the first in Canada to be created through a comprehensive land claim settlement, and set a precedent for collaboration and co-management in future parks. In June 1984, the Inuvialuit Final Agreement was signed, which deviated from past parks by committing to a more extensive inclusion of Aboriginal interests and gave the Inuvialuit exclusive rights to hunting and harvesting game within the park. This agreement
8649-520: Was the first source of profit in the national parks, the exploitation of natural resources such as coal, lumber, and other minerals became another major area of revenue. These resources were found in abundance in the Rocky Mountains and were interpreted as being inexhaustible. Coal was the most plentiful and profitable of all the minerals and therefore its mining in parks was accepted by politicians and Canadian Pacific Railway officials. This
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