Fjords of Norway (Landscape Video Series) 4K/Ultra HD Vineyards of Porquerolles – Ile de Porquerolles, France (Landscape Video Series) 4K/Ultra HD features stunning and spectacular aerial, walking, and drone video footage great for travel, visit, and tourism planning set to original music. The video is the perfect companion for indoor exercise routines involving treadmills, steppers, cycling, and rowing. Norway is a country located in Northern Europe on the northern and western parts of the Scandinavian Peninsula. The majority of the country borders water, including the Skagerrak inlet to the south, the North Sea to the southwest, the North Atlantic Ocean (Norwegian Sea) to the west, and the Barents Sea to the north. It has a land border with Sweden to the east and a shorter border with Finland and an even shorter border with Russia to the northeast. In total, there are about 1,190 fjords in Norway and the Svalbard islands.
In geology, a fjord or fiord is a long, narrow inlet with steep sides or cliffs, created by a glacier. There are many fjords on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, New Zealand, Norway, Novaya Zemlya, Labrador, Nunavut, Newfoundland, Quebec, Scotland, South Georgia Island, Isla de los Estados, and Washington state. Norway’s coastline is estimated at 29,000 kilometres (18,000 mi) with nearly 1,200 fjords, but only 2,500 kilometres (1,600 mi) when fjords are excluded.
During the last glacial period, as well as in many earlier ice ages, virtually the entire country was covered with a thick ice sheet. The movement of the ice carved out deep valleys. As a result of the ice carving, Sognefjorden is the world’s second deepest fjord and Hornindalsvatnet is the deepest lake in Europe. When the ice melted, the sea filled many of these valleys, creating Norway’s famous fjords. The glaciers in the higher mountain areas today are not remnants of the large ice sheet of the ice age—their origins are more recent. The regional climate was up to 1–3 °C (1.8–5.4 °F) warmer in 7000 BC to 3000 BC in the Holocene climatic optimum, (relative to the 1961-90 period), melting the remaining glaciers in the mountains almost completely during that period.
This scenery video features original music by Drum Knight:
https://www.youtube.com/channel/UC9g64WbKxOH-yyA6O-6eBDA
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