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A recliner Recliner aboard a business jet. A recliner is an armchair or sofa that reclines when the occupant lowers the chair's back and raises its front. [1] [2] It has a backrest that can be tilted back, and often a footrest that may be extended by means of a lever on the side of the chair, or may extend automatically when the back is reclined.
Effective 2024, a 2023 law passed by parliament requires solar power on new government buildings. [33] The same law sets a target of 8 terawatt hours (TWh) of solar electricity generation by 2030, which equates to 5% of total 2022-2023 generation levels. For comparison, solar power produced 0.1% of Norway's electricity generation in 2023. [34]
The Oslofjord (Norwegian: Oslofjorden, Urban East Norwegian: [ˈʊ̂ʂlʊˌfjuːɳ]; English: Oslo Fjord [1] [2] [3]) is an inlet in southeastern Norway.The 120-kilometre (75 mi) fjord begins at the small village of Bonn in Frogn Municipality and stretching northwards to the city of Oslo, and then curving to the east and then south again.
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The Trollfjord or Trollfjorden is a fjord in Hadsel Municipality in Nordland county, Norway. The 2-kilometre (1.2 mi) long fjord cuts into the island of Austvågøya and flows out into the Raftsundet strait. The fjord has a narrow entrance and steep-sided mountains surrounding it. The name is derived from troll, a figure from Norse mythology.
The inland fjord areas of Hardanger are sheltered, with rich fruit districts specializing in apples and cherries. Stavanger is a leading industrial area in Western Norway. Ålesund contains many engineering firms, and the bulk of Norway's furniture industry. Along the coast fishing plays the same role that forestry does elsewhere.
The reaction ferry uses the power of the river to tack across the current; the powered cable ferry uses engines or electric motors (e.g., the Canby Ferry in the U.S. State of Oregon) to wind itself across; or is hand-operated, such as the Stratford-upon-Avon chain ferry in the UK and the Saugatuck Chain Ferry in Saugatuck, Michigan, United States.
The fjord was carved by the action of glaciers in the ice ages and was flooded by the sea when the later glaciers retreated. The geology of Lysefjorden was thoroughly investigated and described by Professor Bjørn G. Andersen in his Master's thesis (1954) "Om isens tilbaketrekking i området mellom Lysefjorden og Jøsenfjorden i Ryfylke" (On the glacial retreat in the area between the ...