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River Delta
A river delta is a landform created by deposition of sediment that is carried by a river as the flow leaves its mouth and enters slower-moving or stagnant water.[1][2] This occurs where a river enters an ocean, sea, estuary, lake, reservoir, or (more rarely) another river that cannot carry away the supplied sediment. The size and shape of a delta is controlled by the balance between watershed processes that supply sediment, and receiving basin processes that redistribute, sequester, and export that sediment.[3][4] The size, geometry, and location of the receiving basin also plays an important role in delta evolution. River deltas are important in human civilization, as they are major agricultural production centers and population centers
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Alluvial Fan

An alluvial fan is an accumulation of sediments shaped like a section of a shallow cone,[1] with its apex at a point source of sediments, such as a narrow canyon emerging from an escarpment.[2] They are characteristic of mountainous terrain in arid to semiarid climates,[3][4] but are also found in more humid environments subject to intense rainfall[1] and in areas of modern glaciation.[4] They range in area from less than 1 square kilometre (0.39 sq mi)[4][5] to almost 20,000 square kilometres (7,700 sq mi).[6] Alluvial fans typically form where flow emerges from a confined channel and is free to spread out and infiltrate the surface
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Distributary
A distributary, or a distributary channel, is a stream that branches off and flows away from a main stream channel. Distributaries are a common feature of river deltas. The phenomenon is known as river bifurcation. The opposite of a distributary is a tributary. Distributaries are found where a stream nears a lake or an ocean. They can also occur inland, on alluvial fans, or where a tributary stream bifurcates as it nears its confluence with a larger stream. In some cases, a minor distributary can divert so much water from the main channel that it can become the main route. Many of Papua New Guinea's major rivers flow into the Gulf of Papua through marshy, low-lying country, allowing for wide, many-branched deltas. These include the Fly River, which splits into three major and several minor rivers close to its mouth. The Bamu River splits into several channels close to its mouth, among them the Bebea, Bina, Dibiri, and Aramia
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Peachland
Peachland is a district municipality of over 5000 residents[4] in the Okanagan Valley. It is located on the west side of Okanagan Lake in British Columbia, Canada.[5] It was founded in 1899[6] by John Moore Robinson,[7] although the region had long been home to the Okanagan people. Peachland is approximately half-an-hour's drive south of the city of Kelowna and about a 20-minute drive north of Summerland. The Okanagan Valley is very narrow in the area and there are few terraces that mark former lake levels and the former lake bottom. As a result, the city is largely located on a steep sidehill. Like many other areas in the Okanagan, Peachland is rapidly growing, with new residents coming from all across Canada. Across the lake from Peachland is Rattlesnake Island, home of the legendary Ogopogo
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Summerland, British Columbia

Summerland (2016 population 11,615[2]) is a town on the west side of Okanagan Lake in the interior of British Columbia, Canada. The district is between Peachland to the north and Penticton to the south. The largest centre in the region is Kelowna, approximately 50 km (31 mi) to the north (via Highway 97), and Vancouver is approximately 425 km (264 mi) away to the west. The district is famous for "Bottleneck drive", a system of roads connecting various wineries.

The current Mayor is Toni Boot. The district's (2016 federal) Member of Parliament is Dan Albas of the Conservative Party of Canada
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Naramata, British Columbia
Naramata is a community within the Regional District of Okanagan–Similkameen in British Columbia, Canada. Naramata is situated in the Okanagan Valley on the southeast shore of Lake Okanagan, to the north of Penticton. In 2010, Naramata was the second Community in Canada to be designated Cittaslow. Founded in 1907 by John Moore Robinson as a prime agricultural area. He advertised and sold parcels of land to people from other parts of Canada as well as the British Isles. At the time Naramata became known as a cultural centre. People from across the Okanagan would arrive by boat for concerts, plays, operas, regattas- and as Robinson and his wife were spiritualists-seances. In fact, it is said the name of the village came about during one. Paddlewheelers regularly stopped at the local wharf carrying freight and passengers up and down Lake Okanagan
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