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77-516: Gros Morne National Park is a Canadian national park and World Heritage Site located on the west coast of Newfoundland . At 1,805 km (697 sq mi), it is the second largest national park in Atlantic Canada after Torngat Mountains National Park , which has an area of 9,700 km (3,700 sq mi). The park takes its name from Newfoundland's second-highest mountain peak (at 806 m or 2,644 ft) located within

154-684: 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

231-624: 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

308-404: 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

385-591: 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

462-542: A newly designated formation could not be named the Kaibab Formation, since the Kaibab Limestone is already established as a formation name. The first use of a name has precedence over all others, as does the first name applied to a particular formation. As with other stratigraphic units, the formal designation of a formation includes a stratotype which is usually a type section . A type section

539-617: A permanent natural or artificial feature of the geographic area in which they were first described. The name consists of the geographic name plus either "Formation" or a descriptive name. Examples include the Morrison Formation , named for the town of Morrison, Colorado , and the Kaibab Limestone , named after the Kaibab Plateau of Arizona. The names must not duplicate previous formation names, so, for example,

616-535: 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

693-456: A rare example of the process of continental drift, where deep ocean crust and the rocks of the earth's mantle lie exposed." The Gros Morne National Park Reserve was established in 1973, and was made a national park on October 1, 2005. The park was the subject of a short film in 2011's National Parks Project . The park's rock formations, made famous by Robert Stevens and Harold Williams , include oceanic crust and mantle rock exposed by

770-522: A region or predict likely locations for buried mineral resources. The boundaries of a formation are chosen to give it the greatest practical lithological consistency. Formations should not be defined by any criteria other than lithology. The lithology of a formation includes characteristics such as chemical and mineralogical composition, texture, color, primary depositional structures , fossils regarded as rock-forming particles, or other organic materials such as coal or kerogen . The taxonomy of fossils

847-458: A single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by Abraham Gottlob Werner in his theory of the origin of the Earth, which was developed over

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924-696: 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

1001-615: 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

1078-560: 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

1155-449: Is not a valid lithological basis for defining a formation. The contrast in lithology between formations required to justify their establishment varies with the complexity of the geology of a region. Formations must be able to be delineated at the scale of geologic mapping normally practiced in the region; the thickness of formations may range from less than a meter to several thousand meters. Geologic formations are typically named after

1232-560: Is central to the geologic discipline of stratigraphy , and the formation is the fundamental unit of stratigraphy. Formations may be combined into groups of strata or divided into members . Members differ from formations in that they need not be mappable at the same scale as formations, though they must be lithologically distinctive where present. The definition and recognition of formations allow geologists to correlate geologic strata across wide distances between outcrops and exposures of rock strata . Formations were at first described as

1309-582: 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

1386-482: 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

1463-455: Is ideally a good exposure of the formation that shows its entire thickness. If the formation is nowhere entirely exposed, or if it shows considerably lateral variation, additional reference sections may be defined. Long-established formations dating to before the modern codification of stratigraphy, or which lack tabular form (such as volcanic formations), may substitute a type locality for a type section as their stratotype. The geologist defining

1540-1014: Is referred to as the Humber Zone, a Miogeocline , the Highlands of which contain the largest external basement massif of the Grenville Orogeny in the Appalachian Orogen . This Precambrian basement is known as the Long Range Inlier , Long Range Complex or Basement Gneiss Complex, consisting of quartz – feldspar gneisses and granites that are up to 1550 Ma in age. Mt. Gros Morne and Mt. Big Level lie within this Inlier. The western boundary of this inlier (along Western Brook Pond , St. Pauls Inlet, and south of Portl Creek Pond) consists of Devonian and Ordovician thrust faults , where crystalline rocks thrust over Cambrian –Ordovician carbonate rocks and

1617-449: 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

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1694-602: 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

1771-521: The moose , part of a booming population that was introduced to Newfoundland around 1900. Other common wildlife in the park include red foxes and Arctic foxes , an ecotype of caribou ( R.t caribou ), black bears , snowshoe hares , red squirrels , lynxes , river otters and beavers . Harbour seals are common in St. Pauls inlet, and cetaceans ( minkes , humpbacks , fins , pilots , orcas , atlantic white-sided dolphins , harbour porpoises ) may be in

1848-685: The obduction process of plate tectonics , as well as sedimentary rock formed during the Ordovician , Precambrian granite and Palaeozoic igneous rocks. The Global Boundary Stratotype Section and Point (GSSP) of the Tremadocian stage and the all Ordovician system is defined in the Green Point section within this park. The park is located in the Great Northern Peninsula of Western Newfoundland. This peninsula

1925-561: 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

2002-521: 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

2079-636: 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

2156-490: The Bay of Islands Complex, Little Post Complex, and Old Man Cove Formation . Finally, a Pleistocene ice cap flowed radially across the island, developing fjords such as Bonne Bay . The Tablelands, found between the towns of Trout River and Woody Point in south west of Gros Morne National Park, look more like a barren desert than traditional Newfoundland. This is due to the ultramafic rock – peridotite – which makes up

2233-540: 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

2310-692: 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 Formation (geology) A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of

2387-570: The Lower Paleozoic Humber Arm Allochthon . The Rocky Harbour mélange is a Lower–Middle Ordovician collection of greywacke , quartzite , dolomite shale , chert , limestone blocks within a black, green, and red scaly shale matrix , which occurs along the shore from West Brook Pond to Humber Arm (Bay of Islands). The south portion of the park, Table Mtn. (Tablelands) and North Arm Mtn., consists of Upper Cambrian and Lower Ordovician ophiolites known as

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2464-691: 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

2541-522: 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

2618-473: The Tablelands. It is thought to originate in the Earth's mantle and was forced up from the depths during a plate collision several hundred million years ago. Peridotite lacks some of the usual nutrients required to sustain most plant life and has a toxic quality, hence its barren appearance. Peridotite is also high in iron, which accounts for its brownish colour (rusted colour). Underneath this weathered zone,

2695-494: The area especially during the capelin season in early summer. Many bird species can be found in the park, from shorebirds along the ocean to birds of the bogs and interior forests. In 1987, the park was designated a UNESCO World Heritage Site for both its geological history and its exceptional scenery. The geology of the park in particular illustrates the concept of plate tectonics, and has shed important light on geological evolution and its processes. In respect of its key role in

2772-610: 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

2849-484: 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

2926-585: 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

3003-605: 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

3080-456: 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,

3157-533: 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

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3234-462: 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

3311-601: The development of an understanding of plate tectonics, the Mohorovičić discontinuity at Gros Morne was included by the International Union of Geological Sciences (IUGS) in its assemblage of 100 'geological heritage sites' around the world in a listing published in October 2022. Hiking the trails is a popular activity at Gros Morne. There are about 20 marked day trip trails, exploring coastal and interior areas of

3388-550: The essential geologic time markers, based on their relative ages and the law of superposition . The divisions of the geological time scale were described and put in chronological order by the geologists and stratigraphers of the 18th and 19th centuries. Geologic formations can be usefully defined for sedimentary rock layers, low-grade metamorphic rocks , and volcanic rocks . Intrusive igneous rocks and highly metamorphosed rocks are generally not considered to be formations, but are described instead as lithodemes . "Formation"

3465-564: 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

3542-436: 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

3619-400: The fjord is extremely pure and is assigned the highest purity rating available for natural bodies of water. Pissing Mare Falls , the highest waterfall in eastern North America and 199th highest in the world, flows into Western Brook Pond. Sedimentary rocks, some of them calcareous, underlie the westernmost shores. Elsewhere, granitic gneiss is dominant. The most notable animal in the park is

3696-522: The formation is expected to describe the stratotype in sufficient detail that other geologists can unequivocally recognize the formation. Although formations should not be defined by any criteria other than primary lithology, it is often useful to define biostratigraphic units on paleontological criteria, chronostratigraphic units on the age of the rocks, and chemostratigraphic units on geochemical criteria, and these are included in stratigraphic codes. The concept of formally defined layers or strata

3773-515: 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

3850-781: 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

3927-527: 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

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4004-594: 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

4081-610: 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

4158-718: The multi-day Long Range Traverse between Western Brook Pond and Gros Morne Mountain. The park is home to many arts festivals, including Gros Morne Theatre Festival, Writers at Woody Point, Gros Morne Summer Music, and Trails, Tales and Tunes. 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

4235-410: 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

4312-626: 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

4389-589: 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,

4466-494: The park. One of the more strenuous dayhikes is the 16 km hike over Gros Morne Mountain. This trail is also called the James Callaghan Trail after the former British Prime Minister , who visited in 1976, in recognition of his conservation efforts. A small controversy arose after Callaghan did not visit the trail that had been named in his honour. The interior of the park can also be accessed, notably through

4543-578: The park. Its French meaning is "large mountain standing alone," or more literally "great sombre." Gros Morne is a member of the Long Range Mountains , an outlying range of the Appalachian Mountains , stretching the length of the island's west coast. It is the eroded remnants of a mountain range formed 1.2 billion years ago. In 1987, the park was awarded World Heritage Site status by UNESCO because "The park provides

4620-476: 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

4697-623: 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

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4774-488: The period from 1774 to his death in 1817. The concept became increasingly formalized over time and is now codified in such works as the North American Stratigraphic Code and its counterparts in other regions. Geologic maps showing where various formations are exposed at the surface are fundamental to such fields as structural geology , allowing geologists to infer the tectonic history of

4851-473: 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

4928-558: 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

5005-405: 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

5082-500: 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

5159-476: The rock is really a dark green colour. The many soil associations mapped in the park reflect the wide variety of bedrock. The Silver Mountain soil association , dominant in the northeastern area, is a very stony sandy loam developed on glacial till overlying granite, granitic gneiss and schist. Similar rocks underlie the St. Paul's Inlet association farther west. Sedimentary rocks (including some dolomitic limestone) in

5236-453: 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

5313-574: The southeastern sector support the North Lake association of stony sandy loam. An association of mostly-shallow loam, the Cox's Cove, occupies a discontinuous band over shale, slate, limestone and sandstone near the coast. The coastal strip north of Bonne Bay is mostly underlain by the peaty Gull's Marsh association and the coarse Sally's Cove association except for an area of clay (Wood's Island association) around Rocky Harbour. The stony infertile soils of

5390-425: 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

5467-555: The ultramafic tablelands south of Bonne Bay belong to the Serpentine Range association. Western Brook Pond is a fresh water fjord which was carved out by glaciers during the most recent ice age from 25,000 to about 10,000 years ago. Once the glaciers melted, the land, which had been pushed down by the weight of the ice sheet, rebounded and the outlet to the sea was cut off. The 16-kilometre (9.9 mi) long narrow "pond" then filled in with fresh water. The water in

5544-579: 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

5621-734: 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

5698-429: 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

5775-456: 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

5852-499: 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

5929-520: 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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