Raoul Island
| Raoul Island | |
|---|---|
|
Rangitahua (Māori) Sunday Island | |
 Raoul Island as seen by STS-8 in 1983. Herald Islets at top right. North at top. | |
| Elevation | 516 m (1,693 ft) |
| Parent peak | Moumoukai Peak |
| Location | |
 | |
| Location | Kermadec Islands |
| Coordinates | 29°16′S 177°55′W / 29.27°S 177.92°W |
| Geology | |
| Type | Stratovolcano |
| Volcanic arc/belt | Kermadec Islands |
| Last eruption | 2006 |
The area of the island, including fringing islets and rocks mainly in the northeast, but also a few smaller ones in the southeast, is 29.38 km2 (11 sq mi). The highest elevation is Moumoukai Peak, at an elevation of 516 m (1,693 ft).
Considering offshore islets and rocks, the northernmost island of New Zealand is Nugent Island, about 100 metres (328 ft) in diameter, located 3.6 km (2.2 mi) northeast of Raoul Island. The coordinates of the northernmost point are 29°13′52″S 177°52′09″W / 29.23111°S 177.86917°W. Napier Island stretches almost as far north as Nugent Island, which reaches just a few metres further north.
History
Stone implements of the Polynesian type have been found on Raoul Island, and there is indication of a prehistoric settlement (see below). But the island was uninhabited when discovered by Western sailors.
From May 27 to June 16, 1917, the German raider Wolf, under the command of Korvettenkapitän Karl August Nerger, anchored in the protected bay to undertake engine overhaul and maintenance. During this period the Wolf captured the New Zealand steamship Wairuna (3,950 tons) and the American sailing bark Winslow (570 tons), commandeering all cargo and coal from both ships while at anchor.
The permanently manned Raoul Island Station has been maintained since 1937. It includes a government meteorological and radio station and hostel for Department of Conservation (DOC) officers and volunteers. The station stands on the northern terraces of the island, about 50 m (164 ft) in elevation above the cliffs of Fleetwood Bluff. Raoul Island Station represents the northernmost outpost of New Zealand.
Geography
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Two Holocene calderas are found at Raoul. The older caldera cuts the center of Raoul Island is about 2.5 km × 3.5 km (1.6 mi × 2.2 mi) long and wide respectively. Denham caldera, formed during a major dacitic explosive eruption about 2200 years ago, truncated the western side of the island and is 6.5 km × 4 km (4.0 mi × 2.5 mi) long and wide respectively. Its long axis is parallel to the tectonic fabric of the Havre Trough that lies west of the volcanic arc. Historical eruptions at Raoul during the 19th and 20th centuries have sometimes occurred simultaneously from both calderas, and have consisted of small-to-moderate phreatic eruptions, some of which formed ephemeral islands in Denham caldera. A 240 m (787 ft) high unnamed submarine cone, one of several located along a fissure on the lower NNE flank of Raoul volcano, has also erupted during historical time, and satellitic vents at Raoul are concentrated along two parallel NNE-trending lineaments. The Denham caldera was named for the nearby Denham Bay, itself named by Capt M H Denham in HMS Herald who came to complete a (chart) survey of the island on July 2, 1854. His son Fleetwood James Denham (16yrs) died from a tropical fever, and was buried near the beach at the head of Denham Bay, where a number of the grass-grown graves of former settlers were. The brass plaque heading this grave has been preserved.
Three small lakes, Blue Lake (1.17 km2 or 0.45 sq mi,[citation needed] about 40% overgrown), Green Lake (160,000 m2 or 1,700,000 sq ft) and Tui Lake (5,000 m2 or 54,000 sq ft, drinking water quality) are located in the northern caldera of Raoul Island. The plains surrounding the lakes are called Pumice Flats.
Raoul Island has a humid subtropical climate with warm, wet weather throughout the year.
| Climate data for Raoul Island | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Average high °C (°F) | 25.0 (77) |
25.7 (78.3) |
24.9 (76.8) |
23.6 (74.5) |
21.7 (71.1) |
20.1 (68.2) |
19.1 (66.4) |
19.0 (66.2) |
19.6 (67.3) |
20.5 (68.9) |
22.0 (71.6) |
23.6 (74.5) |
22.1 (71.8) |
| Average low °C (°F) | 19.7 (67.5) |
20.5 (68.9) |
19.9 (67.8) |
18.3 (64.9) |
16.4 (61.5) |
14.8 (58.6) |
13.7 (56.7) |
13.3 (55.9) |
14.0 (57.2) |
14.9 (58.8) |
16.4 (61.5) |
18.2 (64.8) |
16.7 (62.1) |
| Precipitation mm (inches) | 128 (5.04) |
153 (6.02) |
162 (6.38) |
102 (4.02) |
129 (5.08) |
171 (6.73) |
150 (5.91) |
132 (5.2) |
110 (4.33) |
86 (3.39) |
94 (3.7) |
141 (5.55) |
1,558 (61.34) |
| Source: NIWA National Climate Database[1] | |||||||||||||
Flora and fauna
The scientific categorisation of the flora and fauna of the island began in 1854 when HMS Herald, captained by Henry Mangles Denham, arrived to complete the charting of the island. He arrived on the 2nd and was occupied till 24 July, during which time he frequently had to move the ship on account of the rough weather experienced. William Grant Milne and John MacGillivray, naturalists on board the Herald, made a small collection of plants on Raoul. This was forwarded by Captain Denham to Sir W. Hooker, and was described by Sir Joseph Hooker in the Journal of the Linnean Society for 1857.
Raoul is part of the Kermadec Islands subtropical moist forests ecoregion and is largely covered with closed-canopy forest, predominantly of the evergreen Kermadec pōhutukawa (Metrosideros kermadecensis) and the Kermadec nikau palm (Rhopalostylis baueri, formerly described as Rhopalostylis cheesemanii). It is just far enough south that the occasional fertile coconut from Polynesia that washes up on shore and takes root will not survive in the longterm due to a lack of warmth.[2] The island has no native land mammals and was formerly home to vast colonies of seabirds who nested in the forests. The islands may once have had a species of megapode (based on early settler records) and a subspecies of Kereru.[3] Currently native landbirds on the island include the Kermadec Red-crowned Parakeet (Cyanoramphus novaezelandiae cyanurus), the Australasian Harrier, Pukeko, Tui and several introduced species.[4] The island forms part of the Kermadec Islands Important Bird Area, identified as such by BirdLife International because it is an important site for nesting seabirds.[5]
Polynesian visitors introduced the Polynesian rat in the 14th century and Norway rats, cats and goats were introduced by European and American visitors in the 19th and 20th centuries. The rats and cats greatly reduced the seabird colonies, which mostly withdrew to offshore islets, and exterminated the Red-crowned Parakeet, the last confirmed record of resident parakeets for over a century being made in 1836. Although the goats did not eliminate the tree canopy as they did on other islands, they greatly reduced the understory vegetation and were removed in 1986. The Department of Conservation eradicated rats and cats between 2002 and 2006, following which Red-crowned Parakeets soon returned naturally, presumably from the Herald Islets, 2–4 km (1.2–2.5 mi) away. The parakeets had been absent from the island for 150 years and their natural return was a notable event in parrot conservation.[6][7]
There are numerous invasive plant species on the island and a large scale weeding programme involving teams of DOC workers and volunteers has been under way for a number of years in an attempt to eradicate them.
The island is part of the Kermadec Islands Marine Reserve, New Zealand's largest marine reserve, which was created in 1990.
Satellite islands and rocks
The two largest satellite islands are North Island and South Island of Meyer Islands.
- Islands and rocks in the northeast of Raoul Island
- Fishing Rock
- Egeria Rock
- Meyer Islands
- North Island
- South Island
- Napier
- Nugent Island (northernmost island of New Zealand)
- Herald Islets
- Dayrell Island
- Chanter Islands
- Chanter (North) Island
- South Island
- West Island
- Islands and rocks in the southwest of Raoul Island
- Milne Islands
- Dougall Rocks
2006 eruption
On March 17, 2006 at 8:21 a.m. NZDT, a 40-second long volcanic eruption occurred at the Green Lake. At the time, Mark Kearney, a 33-year-old DOC worker, was at the crater taking water temperature measurements. A 5-hectare (12-acre) area around Green Lake was affected with ash, mud and boulders. Two DOC workers were forced to turn back after going to the crater to search for Kearney.
Following the eruption, DOC decided to evacuate the remaining five staff members. A Mil Mi-8 helicopter and Piper PA-31 Navajo aircraft took off from Taupo at 11 a.m. that morning.[8] They arrived at the island in the late afternoon and undertook a 45 minute search for Kearney but no sign was seen. The evacuated staff members were brought back to Auckland that evening.
A Royal New Zealand Air Force P-3 Orion made an overflight on 21 March to provide further information on how safe it is to approach Green Lake. The Volcanologists aboard decided the area was still unsafe, and that the crater lake had risen by about 8 metres (26.2 ft) compared to measurements taken on 17 March. There was no cloud or ash plume.[9]
A group of police, the five evacuated workers, three other DOC staff and scientific staff left Tauranga on 18 March for the three-day boat trip to Raoul aboard the RV Braveheart to recover Kearney's body.[10] They were able to undertake a limited search, but decided that it was extremely unlikely that Kearney survived given the amount of devastation in the area around Green Lake. The Braveheart began the journey back to the mainland on 25 March, with three of the DOC workers staying on the island to continue research.[11] The three were joined by the other four evacuated workers at the start of May 2006. Two of the three will return to the mainland after the handover.[12]
Five hours after the eruption, the Aura satellite passed over and found an estimated 200 tonnes (197 long tons; 220 short tons) of sulfur dioxide had been released.[13] This confirmed that there were magmatic gases in the eruption, and the presence of degassing magma within the volcano. By the end of April, the activity in the area had decreased significantly and the "Alert Level" was lowered to 1.[14]
HMNZS Te Mana left for Raoul on 24 August 2006 on a resupply mission. Also on board were Kearney's sister, Merryn McDermott; three representatives of the Ngāti Kurī iwi; and Chris Carter, the Minister of Conservation. During a service held on 28 August, the Ngāti Kurī representatives performed a tapu lifting ceremony.[15] A plaque was erected to honour Kearney. Te Mana also allowed some volcanic monitoring to be undertaken using its SH-2G Super Seasprite helicopter. During a dawn flight, sample bottles were filled with crater lake water.[16]
A report by the New Zealand Department of Labour into the death was released on 14 October 2006. It cleared the Conservation Department and Geological and Nuclear Sciences of any negligence related to the death of Kearney. The report stated that the eruption was unpredictable and there was no indication of imminent seismic activity.[17]
As a geographically active 'hotspot', the Kermadec Islands also experience frequent earthquakes, the most recently significant of which occurred at 22:39 NZST on May 16, 2006.[18] The epicentre was approximately 290 km (180 mi) SSW from Raoul and measured 7.4 on the moment magnitude scale, and as such is classified as a 'major' earthquake by the United States Geological Survey. It was felt as far away as Christchurch, New Zealand some 1,500 km (930 mi) from the epicentre. Also of note on January 31, 2007 at 4:15:55 NZST a Magnitude 6.5 (Strong) earthquake shook the island. The epicenter was approximately 40 km (25 mi) S of Raoul and 10 km (6.2 mi) below the seabed. On December 9, 2007 at 8.28pm NZST a magnitude 7.6 earthquake shook the area, centered approximately 350 km (220 mi) north of Raoul Island at a depth of 188 km (117 mi).[19] On September 30, 2008 at 3:19:31 NZST a magnitude 7.0 earthquake centered 70 km (43 mi) S of Raoul occurred, with an approximate depth of 35 km (22 mi).[20] More recently onOctober 22, 2011 at 05:57:17 NZST a Magnitude 7.4 earthquake originating at 28.941S 176.045W at a depth of 39 km occurred according to the United States Geological Survey.
July 2011 7.6 Earthquake
July 7, 2011 - 7:03AM. A 7.6 Magnitude earthquake occurred at a depth of 24 km, 211 km east of Raoul Island. July 7, 2011 - 8.51 AM Pacific Tsunami Warning Center scientist Barry Hirshorn told Newstalk ZB the quake generated a 1.9 metre tsunami at Raoul Island.
October 2011 7.4 Earthquake
October 22, 2011 - 5.57PM. A 7.4 Magnitude earthquake occurred at a depth of 45 km, 230 km east of Raoul Island.
The Ministry of Civil Defence had issued the advisory while it assessed the severity of the threat to New Zealand. The Ministry was warning people in coastal areas to stay off beaches and out of the water. People were advised to avoid sightseeing and remain on alert in case the earthquake has generated a tsunami, however by mid-morning warnings had lifted.[21]
Mihai Muncus-Nagy
Department of Conservation volunteer Mihai Muncus-Nagy, a 33 year old biologist from Romania, went missing on Raoul Island on 2 January 2012.[22] He went to Raoul at the end of October 2011.[23] His vehicle and gear was found close to where he was carrying out water temperature readings on the morning of 2 January 2012.
The remaining staff and volunteers searched the shore, but had not found any further signs of him. A helicopter was sent to Raoul by the Rescue Coordination Centre New Zealand (RCCNZ) from Taupo, New Zealand to carry out an aerial search. A DOC boat was also used in the search.[23]
Muncus-Nagy has been presumed drowned.[23]
See also
- Earthquakes in New Zealand
- List of extinct birds
- List of islands of New Zealand
- List of volcanoes in New Zealand
- New Zealand outlying islands
References
- ↑ "NIWA National Climate Database".
- ↑ International Palm Society
- ↑ Tennyson, A. & Martinson, P. (2006) Extinct Birds of New Zealand Te Papa Press, Wellington ISBN 978-0-909010-21-8
- ↑ C. R. Veitch, C. M. Miskelly, G. A. Harper, G. A. Taylor, and A. J. D. Tennyson (2004) "Birds of the Kermadec Islands, South-west Pacific" Notornis 51(2): 61–90
- ↑ BirdLife International. (2012). Important Bird Areas factsheet: Kermadec Islands. Downloaded from http://www.birdlife.org on 2012-02-03.
- ↑ Ortiz-Catedral, Luis; et al. (2009). "Recolonization of Raoul Island by Kermadec red-crowned parakeets Cyanoramphus novaezelandiae cyanurus after eradication of invasive predators, Kermadec Islands archipelago, New Zealand". Conservation Evidence 6: 26–30. Retrieved 2009-06-22.
- ↑ "Conservation breakthrough as kakariki re-colonise remote island". Massey University. 2009-06-15. Retrieved 2009-06-15.
- ↑ "DoC evacuates as Raoul Island erupts, 'one missing'". New Zealand Press Association. 17 March 2006.
- ↑ "Raoul crater ruled unsafe". The Press. 22 March 2006.
- ↑ "Raoul five return to look for mate". The Dominion Post. 20 March 2006.
- ↑ "DOC searchers on Raoul Island to head home". Radio New Zealand. 25 March 2006.
- ↑ "Raoul survivors return to island". NZPA. 25 March 2006.
- ↑ Alert Bulletin, Raoul Island volcano, 24 March 2006
- ↑ Alert Bulletin, Raoul Island volcano, 26 April 2006
- ↑ "A place of death, and reconnection". Dominion Post. 2006-08-26. Retrieved 2006-08-26.
- ↑ "Frigate leaves for Raoul Island". Dominion Post. 2006-08-24. Retrieved 2006-08-26.
- ↑ "Family 'let down' by Raoul report". The Dominion Post. 2006-10-14. Retrieved 2006-10-21.
- ↑ Magnitude 7.4 - Kermadec Islands Region, United States Geological Survey
- ↑ Quakes
- ↑ Earthquake
- ↑ "Tsunami - Potential threat to New Zealand Cancellation Update 2". Ministry of Civil Defence. Retrieved 22 October 2011.
- ↑ Anderson, Charles (8 January 2012). "Lost biologist drawn to NZ". Stuff.co.nz. Retrieved 8 January 2012.
- ↑ 23.0 23.1 23.2 "Search for DOC man on Raoul Island called off". Stuff.co.nz. 4 January 2012. Retrieved 8 January 2012.
Further reading
- Oliver, R., 'The Vegetation of the Kermadec Islands'. Transactions and Proceedings of the Royal Society of New Zealand, Volume 42, 1909, p. 121. URL: RSNZ, accessed 3 January 2007.
- Polynesian stone implements
- "Raoul Island". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=0402-03%3D.
External links
- A visit to Raoul in 2002 by Dr. Floor Anthoni
- A history of the Bell family who lived on Raoul/Sunday Island from 1878 to 1914
- Kermadec Islands Marine Reserve (New Zealand Department of Conservation)
- Raoul Island volcano webcam and seismic information
- LINZ - highly detailed map
Coordinates: 29°15′S 177°55′W / 29.250°S 177.917°W
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