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Rocky Mountain House

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Summit Fleet is an authentic made-in-Alberta Fleet Management Company. The leadership team has spent the majority of their fleet management careers in Alberta.

Point bar deposits account for a significant proportion of the subsurface reservoir, and are characterized by bedded, sandstone-dominated strata. In-situ development of heavy oil is sensitive to lateral and vertical lithological heterogeneity in the form of interbedded siltstone beds, which are locally common in the formation and must be taken into account in order to understand permeability distribution within the reservoir.

The objectives of this research are to integrate qualitative sedimentological observations with quantitative analyses of wireline log data in order to constrain the distribution of siltstone interbeds within the point bar deposit, to use this information to understand the deposition history of the fluvial system, and to provide insight into reservoir modeling. Quantitative statistical analyses of wireline log data, including autocorrelation analysis, Fourier transform analysis, and continuous wavelet transform analysis, reveal lithological cyclicity within the heterogeneous point bar sediments examined.

Cyclicity also increases in amplitude in the youngest layers of the laterally accreted point bar deposit; the overall finer-grained sediments correspond to decreasing energy levels and waning flow over the evolution of the fluvial system. Overall, the highest amplitude cycles were calculated at a wavelength of 3.

The control on cyclic sedimentation is difficult to discern from Cretaceous-aged point bar deposits. Through consideration of sedimentation rates from analogous modern fluvial systems, the smallest cycles observed might be attributed to seasonal variations in climate and associated flow fluctuation. The mappable variations in siltstone bed frequency and thickness across the ancient point bar deposit have implications for heavy oil development.

Low permeability siltstone beds associated with the shortest wavelength cycles i. Previous article in issue.

Rocky Mountain House

Trade with the local aboriginal peoples continued until when the companies merged, they continued to trade until and closed the Rocky Mountain House post. The name of the settlement however remained. Many travellers used this location as a stop on their way further west or northwest, just as they do into the 21st century. Rocky Mountain House became a firmly established town by

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Surrounded by nine acres of forest, Buffalo Mountain Lodge on Tunnel Mountain feels completely secluded yet is within walking distance of downtown Banff. The upper level of the Wapiti Longhouse boasts a high-beamed ceiling and a large stone fireplace, while the main-floor wine cellar is ideal for cocktail hour. You can even book the whole lodge and all 71 guest rooms for a private mountain getaway for you and your guests. Emerald Lake Lodge features three rooms that can hold weddings for up to 88 people or when you rent the place just for yourselves.

Thrill-seekers can hit the slopes, ride high in a gondola, or take a fast-paced tour led by a team of huskies. Those who like to set their own pace can explore the region on cross-country skis or snowshoes. Even those averse to the cold can stay in and cuddle by the fireplace, relax in a hot tub, or bundle up together on a romantic sleigh ride.

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Edmonton man keeps unopened Christmas gift from girl who dumped him 47 years ago

Life and career[ edit ] Early years — [ edit ] Neil Young [13] was born on November 12, , in Toronto , Ontario. Shortly after Young’s birth in , his family moved to rural Omemee, Ontario , which Young later described fondly as a “sleepy little place”. In , upon returning to Canada, Young moved from Omemee to Winnipeg for a year, before relocating to Toronto and Pickering.

Rocky Mountain House is a town in west-central Alberta, Canada located approximately 77 km (48 mi) west of the City of Red Deer at the confluence of the Clearwater and North Saskatchewan Rivers, and at the crossroads of Highway 22 (Cowboy Trail) and Highway 11 (David Thompson Highway). The surrounding Clearwater County’s administration office is located in Rocky Mountain House.

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Edmonton man keeps unopened Christmas gift from girl who dumped him 47 years ago

Edmonton man keeps unopened Christmas gift from girl who dumped him 47 years ago Search for teenage sweetheart led to Kelowna, B. Dec 24, Dec 24, 4: Facebook Related Stories How an Ontario woman reunited with a letter she wrote to Santa 50 years ago As Canadians tear open their presents this Christmas morning, there’s one dog-eared gift that an Edmonton man won’t be opening that came from an old girlfriend who dumped him 47 years ago.

Standing naked in a room bustling with women, Sindy Rodriguez began to cry. She covered her face with her hands, aware it was definitely not the time for tears.

Lithology[ edit ] The McMurray Formation consists of fine- to coarse-grained quartzitic sand and sandstone , interbedded with lesser amounts of silt , mud , clay and, less commonly, thin coal beds. The sands are very loose and friable , unless they are partially or fully cemented with bitumen or, less commonly, with calcite , iron oxides , or quartz. They can be differentiated in outcrops and, to a lesser degree, in the subsurface: It thins eastward into Saskatchewan where, in most areas, it is devoid of bitumen.

It has been removed by erosion north of the Athabasca Oil Sands area. It is underlain by Devonian formations that were tilted and eroded prior to the deposition of the McMurray, resulting in a shallow angular unconformity between the McMurray and the underlying units. The McMurray therefore rests on different Devonian units in different parts of the basin. Arrow indicates a fragment of fossil wood. Depositional History[ edit ] The McMurray Formation was deposited by an extensive drainage system that flowed northward following a regional north-south depression.

The depression was created by the dissolution of thick salt deposits in the Devonian Elk Point Group deep within the subsurface. The drainage system was encroached upon from the north by a rising sea, and as this marine transgression progressed, depositional environments changed from fluvial at the base Lower Member , to estuarine Middle Member , to shore-face at the top Upper Member , and finally to open marine in the overlying Clearwater Formation.

The channel sand deposits host the majority of the bitumen which lies in the pore spaces between the sand grains. They are flanked by off-channel deposits that consist primarily of mud and silt that accumulated in the floodplain, tidal flat, swamp, and brackish-bay environments that existed contemporaneously with the channels.

Fight for Freedom: Favour for friend landed innocent woman in Alberta prison

The leadership team has spent the majority of their fleet management careers in Alberta. With offices in Calgary, Edmonton and Fort McMurray, we understand the unique operating conditions and challenges that face western Canadian-based fleets. United States Capabilities Summit Fleet now has the ability to assist our Canadian clients with all their vehicle and fleet management requirements in the United States through our wholly-owned subsidiary Summit Acceptance Corp.

All requirements can be managed from right here in Canada with no complicated hand-off to a US counterpart or an affiliate company. We are a people first company, which when coupled with the latest Fleet Management technology, delivers best-in-class service. The ability to leverage this western based infrastructure and the light duty fleet expertise provided in the group is extremely valuable for Summit Fleet and our clients.

The McMurray Formation is a stratigraphic unit of Early Cretaceous age (late Barremian to Aptian stage) of the Western Canada Sedimentary Basin in northeastern Alberta. It takes the name from Fort McMurray, and was first described in the outcrops exposed along the banks of the Athabasca River, 5 kilometres ( mi) north of Fort McMurray, by F.H. McLearn in

Alberta, the westernmost of Canada’s three Prairie provinces, shares many physical features with its neighbours to the east, Saskatchewan and Manitoba. Land and Resources Physiography, climate, soil and vegetation combine to create four biophysical regions within Alberta. The Prairie region includes most of southern Alberta, more precisely the land south and east of an arc stretching from Waterton in the southwest corner to a point along the Saskatchewan border east of Red Deer.

This gently rolling grassland is relatively dry and mostly treeless. The terrain varies locally, in places broken by deep river valleys and rising from less than m in the northeast to over 1, m in the Cypress Hills in the southeast. The parkland region predominates in central Alberta, forming a crescent to the west and north of the Prairie region and including most of the North Saskatchewan River drainage basin. This area varies from the flatland of old lake bottoms to rolling landscape with numerous lakes and depressions.

It contains both treed and grassy terrain, with soil and climatic factors favourable to agriculture. The boreal forest region covers the northern half of the province. Here great rivers and lakes dominate the landscape, draining northward to the Arctic Ocean. Soil and climatic factors make agriculture difficult, except in the Peace River region of the northwest, where parkland conditions create the world’s most northerly grain-growing area.

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First settlement[ edit ] The Calgary area was inhabited by pre- Clovis people whose presence has been traced back at least 11, years. He was a Hudson’s Bay Company trader and the first recorded European to visit the area. John Glenn was the first documented European settler in the Calgary area, in

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Hoodoos in Dinosaur Provincial Park In central and northern Alberta the arrival of spring is marked by the early flowering of the prairie crocus anemone ; this member of the buttercup family has been recorded flowering as early as March, though April is the usual month for the general population. Both yellow and white sweet clover can be found throughout the southern and central areas of the province. The trees in the parkland region of the province grow in clumps and belts on the hillsides.

These are largely deciduous , typically aspen , poplar , and willow. Many species of willow and other shrubs grow in virtually any terrain. On the north side of the North Saskatchewan River evergreen forests prevail for thousands of square kilometres. Aspen poplar , balsam poplar or in some parts cottonwood , and paper birch are the primary large deciduous species. Conifers include jack pine , Rocky Mountain pine, lodgepole pine , both white and black spruce , and the deciduous conifer tamarack.

Fauna[ edit ] The bighorn sheep is Alberta’s provincial animal The four climatic regions alpine , boreal forest , parkland , and prairie of Alberta are home to many different species of animals.

McMurray Formation

Last Edited November 22, Alberta, the westernmost of Canada’s three Prairie provinces, shares many physical features with its neighbours to the east, Saskatchewan and Manitoba. Alberta, the westernmost of Canada’s three Prairie provinces, shares many physical features with its neighbours to the east, Saskatchewan and Manitoba. Land and Resources Physiography, climate, soil and vegetation combine to create four biophysical regions within Alberta.

Standing naked in a room bustling with women, Sindy Rodriguez began to cry. She covered her face with her hands, aware it was definitely not the time for tears.

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I recently moved out from Nova Scotia after Xmas looking to meet someone and see what it leads to. I enjoy being outside. Hanging out with my kids and going on adventures. I’m new to Alberta!

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