Lihir
Native name:
Niolam
NASA Space Shuttle image of Lihir Island
Lihir is located in Papua New Guinea
Lihir
Lihir
Geography
LocationMelanesia
Coordinates3°7′30″S 152°38′30″E / 3.12500°S 152.64167°E / -3.12500; 152.64167
ArchipelagoBismarck Archipelago
Total islands4
Major islands1
Length22 km (13.7 mi)
Width14.6 km (9.07 mi)
Highest elevation700 m (2300 ft)
Administration
Papua New Guinea
ProvinceNew Ireland Province
Demographics
Population25,608

Lihir Island (a.k.a. Niolam Island) is the largest island in the Lihir group of islands, 22 km long and 14.5 km wide, in Papua New Guinea's New Ireland Province. It consists of a complex of several overlapping basaltic stratovolcanoes rising 700 m above sea level. While the volcanoes are not currently active, geothermal activity is still present. The island is in what was the forearc basin associated with the subduction of the Pacific Plate beneath the North Bismarck Plate.[1] Subduction stopped about 10 million years ago with the collision of the Ontong Java plateau with the subduction zone.[2]

The name Lihir comes from the Patpatar language, cognate of the native name Lir. Niolam, also spelled Nualam or Nuolam, means "big island" (nua "island" + lam "big").[3]

The island is located 900 km (560 mi) north east of Port Moresby. Annual rainfall averages 4,800 mm (190 in); temperature ranges between 19 and 35 degrees Celsius. The population of the Lihir Group increased from 12,570 in 2000[4] to an estimated 25,608 in 2011.[5] Residents are of Melanesian descent and have predominantly a subsistence lifestyle.

Lihirians follow traditional belief systems, although official census records indicate that 99% of the PNG population are Christians, with Catholicism being the largest denomination. Most villages are located on the coastal fringe, although it is thought that originally some villages were located inland but were moved to the coast at the encouragement of missionaries.

The economic focal point of the island is the Lihir Gold Mine.[6] Lihir represents one of the largest epithermal gold deposits in the world and it is hosted by high-potassic igneous rocks.[7] The mine is operated by Newmont. The mine holds one of the world's largest gold resources (46 million ounces). Grab samples from the submarine Conical Seamount, located about 8 km south of Lihir Island, contain high gold concentrations of up to 230 g/t Au (avg. 26 g/t, n=40) that are hosted by high-potassic trachybasalts.[8]

The mine is located on a geothermically active area and to enable the mine to proceed, steam relief wells have been drilled to release subterranean pressure. The steam has, in part, been captured and is used to operate a 50 MW geothermal power station which generates approximately 25% of the mine's power requirements. Mine tailings are discharged into the sea.

The largest settlement on the Island is Londolovit, where most of the expatriate mine employees live. Basic shopping and health care facilities are located there. The local hospital has inpatient and outpatient facilities and provides health care services to both the expatriate and local communities.

An airstrip large enough to land a small jet is also located north of Londolovit, at Kunaye[9] village

As is the case in many tropical regions, mosquito-borne viruses are present on the island, as is malaria.

Land ownership follows traditional models with land being owned by clans. Insofar as it relates to land ownership, the society is matrilineal with land being passed through the female generations. The land cannot be sold; however, usage rights can be granted.

The Island has two large Primary Schools and a Secondary School Located on the Mining impacted area. The largest of the two Primary schools is Sekunkun Primary School[10] which is on the North Eastern part of the Island. The school has total of over 600 students and 19 teachers.

See also

References

  1. ↑ "Submarine Volcanoes". Department of Geosciences, Oregon State University. Retrieved 9 March 2011.
  2. ↑ McInnes, Brent I. A.; Jannene S. McBride; Noreen J. Evans; David D. Lambert; Anita S. Andrew (1999-10-15). "Osmium Isotope Constraints on Ore Metal Recycling in Subduction Zones". Science. AAAS. 286 (5439): 512–516. doi:10.1126/science.286.5439.512. PMID 10521343.
  3. ↑ Neuhaus, Karl (2015). Grammar of the Lihir Language of New Ireland, Papua New Guinea. Boroko, Port Moresby: Institute of Papua New Guinea Studies. p. 30.
  4. ↑ (PNG Census 2000)
  5. ↑ (PNG Census 2011)
  6. ↑ Muller D., Groves D.I. (2016) Potassic igneous rocks and associated gold-copper mineralization (4th ed.). Mineral Resource Reviews. Springer-Verlag Heidelberg, 311 pp
  7. ↑ Muller, Daniel; Leander Franz; Peter Herzig; Steve Hunt (2001). "Potassic igneous rocks from the vicinity of epithermal gold mineralization at Lihir Island, Papua New Guinea". Lithos. 57 (2–3): 163–186. Bibcode:2001Litho..57..163M. doi:10.1016/s0024-4937(01)00035-4.
  8. ↑ Muller, Daniel; Leander Franz; Sven Petersen; Peter Herzig; Mark Hannington (2003). "Comparison between magmatic activity and gold mineralization at Conical Seamount and Lihir Island, Papua New Guinea". Mineralogy and Petrology. 79 (3–4): 259–283. Bibcode:2003MinPe..79..259M. doi:10.1007/s00710-003-0007-3. S2CID 129643758.
  9. ↑ "List of Cities and Towns in Papua New Guinea". Global Banking & Finance Review. 9 May 2013. Retrieved 2020-10-17.
  10. ↑ "Sekunkun Primary School, Londolovit, Phone +675 7489 1137". pg.oceaniabiz.com. Retrieved 2020-10-17.
Lihir Group seen from space (Mahur Island not visible)
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.