Blup Blup
The island is volcanic (a stratovolcano) and a weak thermal area exists on the north west coast. The island is only 3.5 km (2.2 mi) wide with an irregular coastline and ancient lava flows. It is thought that Blup Blup last erupted in the Holocene. Fresh water is available on the island from wells. Other islands in the vicinity include Kadovar and Wei Island. There is a small islet about 200 m (650 ft) off the south-west shore of the island called Mut Mut, where there is a geodetic monitoring facility.
Description
Blup Blup has been described as deeply eroded. The island features a well developed reef, a lagoon, cinder cones, and hot springs all of which suggest early volcanic activity.
History
The first recorded sighting by Europeans of Kadovar Island was by the Spanish navigator Iñigo Órtiz de Retes on 21 July 1545, when on board of the carrack San Juan tried to return from Tidore to New Spain.
See also
References
- ^ "Blup Blup". www.volcanodiscovery.com. Retrieved 2020-04-04.
- ^ Llanes, P.; Silver, E.; Day, S.; Hoffman, G. (2009). "Interactions between a transform fault and arc volcanism in the Bismarck Sea, Papua New Guinea". Geochemistry, Geophysics, Geosystems. 10 (6): n/a. Bibcode:2009GGG....10.6013L. doi:10.1029/2009GC002430. S2CID 129615507.
- ^ Coello, Francisco. "Conflicto hispano-alemán". Boletín de Sociedad Geográfica de Madrid, t.XIX. 2º semestre 1885, Madrid, p.317.
- "Blup Blup". Global Volcanism Program. Smithsonian Institution.
- Mut Mut in Papua New Guinea Geodetic Monitoring Site