Bismarck Archipelago
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The Bismarck Archipelago is a group of islands off the northeastern coast of New Guinea in the western Pacific Ocean and part of Papua New Guinea.
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[edit] Geography
The Bismarck archipelago includes mostly volcanic islands spread into 4 provinces with an area of 49,700 km² (19,189 sq mi) where the most important islands include:
- East New Britain Province (4)
- New Britain or Niu Briten, main island
- Duke of York Islands
- Manus Province (9)
- Admiralty Islands
- Manus Island, main island
- Lou Island
- Los Negros Island
- Ndrova Island
- Tong Island
- Baluan Island
- Pak Island
- Purdy Islands
- Rambutyo Island
- St Andrews Islands
- Western Islands with
- Aua Island
- Hermit Islands
- Kaniet Islands
- Ninigo Islands
- Wuvulu Island
- New Ireland Province (12)
- New Ireland or Niu Ailan, main island
- New Hanover or Lavongai
- Feni Islands
- Lihir Island
- Tabar Group
- Tanga Group
- Saint Matthias Group
- West New Britain Province (18)
- New Britain or Niu Briten, main island
- Vitu Islands
- Bougainville Province (14) Autonomous and lying southeast of the the Feni Islands **
- Bougainville Island
- Buka Island
- Carteret Islands
- Green Islands (which sometimes are included despite not really being part of the area.)
[edit] History
| This section does not cite any references or sources. Please improve this section by adding citations to reliable sources. Unverifiable material may be challenged and removed. (July 2007) |
The area is named in honour of the German chancellor Otto von Bismarck.
The first inhabitants of the Archipelago arrived around 33,000 years ago after sailing from what is now Papua New Guinea. Later arrivals included the Lapita people.
The first European to visit these islands was Dutch explorer Willem Schouten in 1616. [1] [2]
The islands remained unsettled by western Europeans until they became part of the German protectorate of German New Guinea in 1884.
On 13 March 1888, a volcano erupted on Ritter Island causing a megatsunami. Almost 100% of the volcano fell in to the ocean leaving a small crater lake.[3]
Following the outbreak of World War I, the Australian Naval and Military Expeditionary Force seized the islands in 1914 and Australia later received a League of Nations mandate for the islands. They remained under Australian control — interrupted only by Japanese occupation during World War II — until Papua New Guinea became independent in 1975.
[edit] Notes
- ^ Sigmond,J.P and Zuiderbann, L.H.(1976) Dutch Discoveries of Australia, Rigby, Australia. ISBN 07270 08005
- ^ Spate, O.H.K. (1979) The Spanish Lake, Australian National University, Second Edition, 2004. ISBN 1920942 173
- ^ Ward, Steven N.; Day, Simon (September 2003). "Ritter Island Volcano —lateral collapse and the tsunami of 1888". Geophysical Journal International 154 (3): pp.891-902. Blackwell Publishing. doi:10.1046/j.1365-246X.2003.02016.x. Retrieved on 2007-12-17. “In the early morning of 1888 March 13, roughly 5 km3 of Ritter Island Volcano fell violently into the sea northeast of New Guinea. This event, the largest lateral collapse of an island volcano to be recorded in historical time, flung devastating tsunami tens of metres high on to adjacent shores. Several hundred kilometres away, observers on New Guinea chronicled 3 min period waves up to 8 m high, that lasted for as long as 3 h. These accounts represent the best available first-hand information on tsunami generated by a major volcano lateral collapse. In this article, we simulate the Ritter Island landslide as constrained by a 1985 sonar survey of its debris field and compare predicted tsunami with historical observations. The best agreement occurs for landslides travelling at 40 m s-1, but velocities up to 80 m s-1 cannot be excluded. The Ritter Island debris dropped little more than 800 m vertically and moved slowly compared with landslides that descend into deeper water. Basal friction block models predict that slides with shorter falls should attain lower peak velocities and that 40+ m s-1 is perfectly compatible with the geometry and runout extent of the Ritter Island landslide. The consensus between theory and observation for the Ritter Island waves increases our confidence in the existence of mega-tsunami produced by oceanic volcano collapses two to three orders of magnitude larger in scale.”
[edit] External links
- about the provincesid:Kepulauan Bismarck
bg:Архипелаг Бисмарк ca:Arxipèlag Bismarck de:Bismarck-Archipel et:Bismarcki saarestik el:Αρχιπέλαγος του Βίσμαρκ es:Archipiélago Bismarck fr:Archipel Bismarck gl:Arquipélago Bismarck it:Arcipelago di Bismarck lt:Bismarko salynas nl:Bismarck-archipel ja:ビスマルク諸島 no:Bismarckarkipelet pl:Archipelag Bismarcka ru:Архипелаг Бисмарка sr:Бизмарков архипелаг fi:Bismarckinsaaret sv:Bismarckarkipelagen uk:Бісмарка архіпелаг zh:俾斯麦群岛
