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Oslofjord
The Oslofjord ((ノルウェー語:Oslofjorden), (英語:Oslo Fjord)〔de Jong, Folkert. 2007. ''Marine Eutrophication in Perspective: On the Relevance of Ecology for Environmental Policy''. Berlin: Springer, p. 53.〕〔Braarud, Trygve. 1945. ''A Phytoplankton Survey of the Polluted Waters of Inner Oslo Fjord''. Oslo, I kommisjon hos Jacob Dybwad, p. 11ff.〕) is an inlet in the south-east of Norway, stretching from an imaginary line between the Torbjørnskjær and Færder lighthouses and down to Langesund in the south to Oslo in the north. It is part of the Skagerrak strait, connecting the North Sea and the Kattegat sea area, which leads to the Baltic Sea. The Oslofjord is not a fjord in the geological sense - in Norwegian the term ''"fjord"'' can refer to a wide range of waterways. The bay is divided into the inner (''indre'') and outer (''ytre'') Oslofjord at the point of the Drøbak Sound.
==Geography==
Each of the islands in the innermost part of the fjord has its own identity and distinguishing history. Among them are Hovedøya, Lindøya, Nakholmen, Bleikøya, Gressholmen, and Langøyene. These islands can be reached with the Oslo-boats from Vippetangen. Hovedøya contains monastery ruins, Gressholmen for its rabbits, Nakholmen, Bleikøya, Lindøya for their cosy cabins at the water’s edge, and finally Langøyene for its camping possibilities and beach.
The inner part of the Oslofjord has steep and forest covered hill slopes down towards the fjord.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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