Currency exchange in Swan River is limit to banks or credit unions, kiosks and dealers. Shopping around for currency exchange service if the exchange amount is over $500 Canadain for most customers. Make sure to compare rate at the same time, ask fee structure beside exchange and inquire about time frame to settle the fund.
Usually banks do not keep foreign currency banknotes in stock, customers have to order with banks and wait for 3 - 5 business days to pick up. In addition, when you sell your foreign banknotes to local banks, banks may not pay you immediately, banks need to send your banknotes to their back office to vertify.
Currency exchange kiosk in airport target customers who are looking for convenient service, small amount exchange. Usually the fee or the rate are not favourable for customers.
The general rule is the more convenient location, the less favourable rate and higer fees.
There are a few currency exchange dealers in Swan River. Different companies have different specilities, some focus on cash exchagne, some others conduct currency exchange by wire transfer. When you comapre the rates, please try to get quote witnin 30 minutes, becasue currency exchange rates are constantly changeing, also ask the fees they charge beside exchange.
Each currency exchange dealers, which include banks, credit unions and other dealers, offer similar but different rate. The difference is getting more significantly, when the exchange amount is getter larger, such as over $10,000 Canadian dollar. Shop around is still the best way to get the best currency exchange rate. Please make sure when you compare the rate, ask when the money will be available, what is other fees. The general idea is the more convenient locaiton, the worse rate applied.
Swan River is a town in Manitoba, Canada. It is surrounded by the Rural Municipality of Swan River and in the Swan River Valley. Swan River acts as the hub to the surrounding communities of Minitonas, Benito, Bowsman, Birch River, and the other communities in the valley. As of 2016, Swan River was Manitoba's 16th largest in population, which was 4,014 as of the 2016 Canadian Census according to Statistics Canada, with an additional 2,829 people living in the surrounding rural municipality of Swan River.
Located in a valley between the Duck Mountains and the Porcupine Hills, the town of Swan River is close to the Saskatchewan boundary in west-central Manitoba. The town is situated along the Swan River which flows into Swan Lake, 55 km (34 mi) to the north-east. Swan Lake is believed to be named for the swans that once frequented the lake, but are nowadays only seasonal visitors. Henry Kelsey became the first European explorer to visit the area in 1690. The name of the lake is first noted on a map created by Peter Fidler in 1795 and again on a French map in 1802 (as L du Cigne). The first permanent European settlement dates back to 1770, when fur traders from both the Hudson's Bay Company and the North West Company established outposts along the Swan River where they bought and sold goods to local Cree peoples by way of birch bark canoes. In 1876, the musical band of the North-West Mounted Police, the forerunner of the Royal Canadian Mounted Police, made its debut in what was later to become Swan River. The instruments used in the band were purchased by the 20 officers in the band and shipped from Winnipeg by dog sled. The first pioneers arrived in the Swan Valley through the Duck Mountains in 1897 and quickly developed the farming potential of the area. The proposed construction of a line of the Canadian Northern Railway was announced in 1898 and the town was founded in 1900, though it was little more than a post office at the time. Swan River was officially incorporated as a town in 1908.
The Swan River Valley is not truly a river valley, but is instead a western extension of the Manitoba lowlands into the Manitoba Escarpment. The Valley is surrounded by escarpment features on three sides: the Duck Mountains to the south; the Porcupine Hills to the north; and Thunder Hill to the west. To the east is Lake Winnipegosis, which is a modern remnant of glacial Lake Agassiz, a lake that filled the valley after the last ice age (the valley was then a bay on the western shore of the lake). Valley soils are formed from a mixture of glacial till and lacustrine clay. Sandy beach ridges (marking the western shore of Lake Agassiz at various times) lie throughout the area: a prominent beach ridge lies under the town's golf course, just west of town. Valley soils are typically very fertile and deep, and are the area's greatest natural resource. But they also have a high calcium carbonate content and an alkaline pH, which limits their productivity in some crops (for example, blueberries). The underlying bedrock is composed of Cretaceous shales, and, below that, sandstone, which overlie deeper deposits of Devonian limestone, which in turn overlie Precambrian granite.
The Valley is near the southern limit of the boreal forest in its transition zone to aspen parkland. Valley trees include white spruce, black spruce, tamarack larch, balsam fir, jack pine, quaking aspen, balsam poplar, and paper birch. Most of the forest has been cleared from the flat valley bottom for agricultural purposes, but the surrounding hills are still heavily forested, and are designated as forest reserves. Numerous peaty bogs and wetlands are present in the area, including hundreds of oxbow lakes of the meandering Swan and Woody rivers. The surrounding hills have many lakes, as does the lower lake bottom land near the eastern edge of the valley.
The climate of west-central Manitoba features extreme seasonal variation, with winter temperatures below −30 °C (−22 °F) and summer temperatures above 30 °C (86 °F) not uncommon. The town therefore has very distinct seasons. Snow usually covers the ground from early November to early April, and only two Christmases have been recorded that have not been "white" (snow-covered) since such records have been kept. The transition from winter to spring to summer is rapid, with the snow of late March turning to the full green of summer by mid-May. The onset of autumn, then winter, is equally rapid, as daytime high temperatures above 20 °C (68 °F) are common in late September, while temperatures above freezing are rare by early November, only seven weeks later. Summer, although short, is pleasant and very green, owing to the fertility of local soils and adequate rainfall. Most precipitation falls as rain in the summer - usually in brief thunderstorms - or in less violent but more protracted snow or rainshowers in spring and fall. Little precipitation falls in winter because the air is then too cold to hold significant amounts of moisture. However, because the temperature rarely goes above the melting point of water in winter, what precipitation that does fall falls as snow, and accumulates on the ground, building to a depth of about 45 cm (18 in) before finally starting to melt in March.