- Bismarck Archipelago
The Bismarck Archipelago is a group of islands off the northeastern coast of
New Guinea in the westernPacific Ocean and part ofPapua New Guinea .History
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. [ 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 ]The islands remained unsettled by western Europeans until they became part of the German
protectorate ofGerman New Guinea in 1884. The area was named in honour of the German chancellorOtto von Bismarck .On
13 March 1888 , avolcano erupted onRitter Island causing amegatsunami . Almost 100% of the volcano fell in to the ocean leaving a smallcrater lake . [cite journal
quotes =
last = Ward
first = Steven N.
authorlink =
coauthors = Day, Simon
date =
year = 2003
month = September
title = Ritter Island Volcano —lateral collapse and the tsunami of 1888
journal = Geophysical Journal International
volume = 154
issue = 3
pages = 891
publisher = Blackwell Publishing
location =
doi = 10.1046/j.1365-246X.2003.02016.x
bibcode =
oclc =
id =
url = http://www.blackwell-synergy.com/doi/abs/10.1046/j.1365-246X.2003.02016.x?journalCode=gji
language =
format =
accessdate = 2007-12-17
quote = 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.]Following the outbreak of
World War I , theAustralian Naval and Military Expeditionary Force seized the islands in 1914 andAustralia later received aLeague of Nations mandate for the islands. They remained under Australian control — interrupted only byJapan ese occupation duringWorld War II — until Papua New Guinea became independent in 1975.Geography
The Bismarck
archipelago includes mostlyvolcanic island s spread into 4 provinces with an area of convert|49700|km2|sqmi|0|abbr=on 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 Feni Islands **
**Bougainville Island
**Buka Island
**Carteret Islands
** Green Islands (which sometimes are included despite not really being part of the area.)Notes
Bibliography
*Firth, Stewart (1983). "New Guinea Under the Germans". Carlton, Australia: Melbourne University Press. ISBN 0522842208.
*Howe, K. R., Robert C. Kiste, Brij V. Lal, eds. (1994). "Tides of History: The Pacific Islands in the Twentieth Century". Honolulu: University of Hawaii Press. ISBN 0824815971.
*King, David "et al." (1982). "Papua New Guinea Atlas: A Nation in Transition". Bathurst, Australia: R. Brown and the University of Papua New Guinea. ISBN 0909197148.
*Moore, Clive (2003). "New Guinea: Crossing Boundaries and History". Honolulu: University of Hawaii Press. ISBN 0824824857.
*Ryan, Peter, ed. (1972). "Encyclopedia of Papua New Guinea". 3 volumes; Vol I: A - K, maps, black and white illustrations, xv + 588pp. Vol II: l - Z, maps, black and white illustrations, 589-1231pp. Vol III: Index, folding colour map in rear pocket, map, colour illustration, v + 83pp. Carlton, Australia: Melbourne University Press. ISBN 9780522840254.External links
* [http://www.pngtourism.org.pg/png/export/sites/TPA/provinces/index.html about the provinces]
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