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・ Danube Commission (1948)
・ Danube company
・ Danube Cossack Host
・ Danube Cossacks
・ Danube crested newt
・ Danube Delta
・ Danube delta dwarf goby
・ Danube Delta horse
・ Danube Express
・ Danube fan
・ Danube Flotilla
・ Danube glaciation
・ Danube International School
・ Danube Legion
・ Danube Palace
Danube Planum
・ Danube Private University
・ Danube Promenade
・ Danube Province
・ Danube River Commission
・ Danube River Conference of 1948
・ Danube school
・ Danube Seven
・ Danube Sinkhole
・ Danube Swabians
・ Danube Technologies
・ Danube University Krems
・ Danube Valley Railway
・ Danube Valley Railway (Baden-Württemberg)
・ Danube Valley Railway (Bavaria)


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Danube Planum : ウィキペディア英語版
Danube Planum

Danube Planum is a rifted mesa on the surface of Jupiter's moon Io. It is located on Io's trailing hemisphere at . Danube Planum is 244.22 kilometers across〔 and 5.5 km tall. The mountain is bisected by a 15-to-25-kilometer-wide, northeast-southwest-trending canyon, splitting the mountain into two main east and west mountains, with several additional blocks at the southern end of the fracture.〔 The outer margin of the plateau is marked by 2.6-to-3.4-km-tall scarps. Mass wasting in the form of landslide deposits are visible along the base of the western half of Danube Planum.〔 Two volcanic depressions, known as paterae, lie at northern and southern ends of mountain. The volcano at the northern end, Pele, is one of the most active volcanoes on Io. One of the faults that helped form Danube Planum may also act as a conduit for magma to rise to the surface at Pele.
In 1985, the International Astronomical Union officially named the mountain after the Danube River, one of a number of places the mythological Io passed during her wanderings.〔
== References ==


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Danube Planum」の詳細全文を読む



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