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Raoul Island

Raoul Island is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Raoul Island rather than just read about it. In short: Raoul Island (Sunday Island; Māori: Rangitāhua) is the largest and northernmost of the main Kermadec Islands, 900 km (560 mi; 490 nmi) south south-west of 'Ata Island of Tonga and 1,100 km (680 mi; 590 nmi) north north-east of New Zealand's North Island. It has been the source of vigorous volcanic activity during the past several thousand years that was dominated by dacitic explosive eruptions, with the largest bein…

Raoul Island — main illustration
Raoul Island — illustration

Key takeaways

  • Raoul Island belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Raoul Island to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Raoul Island from memory before moving on to harder problems.

Reference excerpt

Raoul Island (Sunday Island; Māori: Rangitāhua) is the largest and northernmost of the main Kermadec Islands, 900 km (560 mi; 490 nmi) south south-west of 'Ata Island of Tonga and 1,100 km (680 mi; 590 nmi) north north-east of New Zealand's North Island. It has been the source of vigorous volcanic activity during the past several thousand years that was dominated by dacitic explosive eruptions, with the largest being VEI-6. The anvil-shaped island has a total area of 29.38 km2 (11 sq mi). It has fringing islets and rocks mainly in the northeast, with a few smaller ones in the southeast. The highest elevation is Moumoukai Peak, at an elevation of 516 m (1,693 ft). Although Raoul is the only island in the Kermadec group large enough to support settlement, it lacks a safe harbour, and landings from small boats can be made only in calm weather. The island consists of two mountainous areas, one with summits of 516 metres (1,693 ft) and 498 metres (1,634 ft), and the other with a summit of 465 metres (1,526 ft), the two separated by a depression which is the caldera of the Raoul volcano.

History Evidence from archaeological sites on the northern coast of Raoul Island indicate that Polynesians settled there in the 14th century. A 1980 publication also suggested a lower layer of deposits dated to the 10th century, but this was rejected by the paper's author in 1991 in favour of the later date. Finds at the sites included stone implements of the Polynesian type, obsidian flakes, shells and charcoal. Obsidian of the same type has been found at early Māori sites at Shag River / Waihemo and Tai Rua, Otago on the South Island of New Zealand. There are also similarities to the Raoul settlement at archaic sites at Houhora and Papatowai. Higham and Johnson (1997) concluded that Raoul was settled from New Zealand but that the Kermadecs were a stepping stone in an early and rapid Polynesian migration from Polynesia to New Zealand and back although the occupation of the islands was relatively brief.

The island was uninhabited when first sighted by Western sailors and was named after Joseph Raoul, quartermaster of the Recherche, when it was sighted on 16 March 1793. Captain William Raven of the whaleship Britannia sighted the island on 6 March 1796 and called it Sunday Island, a name which was subsequently in common usage. Captain Henry Mangles Denham of HMS Herald charted the island in 1854. The last regular occupants, Tom Bell and his wife Frederica, spent thirty-six years on the island before the New Zealand government evacuated them in 1914. A landing party sent to investigate the island found out how hasty the evacuation of the Bells was – a 1914 calendar was still pinned to the kitchen wall and the family's furniture, cutlery, and child's toys had remained in place. The family arrived with six children and five more were born there. From 27 May to 16 June 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 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.

Weather station The New Zealand government has permanently staffed Raoul Island since 1937 until the evacuation of staff at the beginning of 2020 due to uncertainties around the COVID-19 pandemic. It included 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. The meteorological station (WMO ID 93997) was initially operated by New Zealand Post Office staff operating the radio station, but shortly after the end of World War 2, the New Zealand Meteorological Service took over the running of the station, with nine full-time staff. Each team undertook 12-month expeditions to the island to provide three hourly weather reports and once daily radiosonde flights using hydrogen filled balloons at 10:30 am. Weather reports were radioed back to New Zealand using HF radio to ZLW Wellington Radio. In addition to its primary purpose as a meteorological station, staff at the station also maintained a seismic monitoring station, made once a week measurements of sea temperature at Fishing Rock and the lake levels and temperatures of Blue and Green Lakes. In 1990 the surface weather observation programme was automated and the Department of Conservation took over responsibility for operational activities on the island. Raoul Island Station remains the northernmost outpost of New Zealand.

… excerpt ends here. Continue reading the full article.

Illustrations

Raoul Island illustration
Raoul Island illustration
Raoul Island: Map of the Kermadec Islands with Raoul Island
Map of the Kermadec Islands with Raoul Island
Raoul Island: Admiralty chart of Raoul Island, surveyed by Denham in 1854
Admiralty chart of Raoul Island, surveyed by Denham in 1854
Raoul Island: Raoul Island, looking towards the minor islands northeast
Raoul Island, looking towards the minor islands northeast

Worked examples

Example 1 — a first encounter with Raoul Island

Start with the simplest possible case. Write down what Raoul Island claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Raoul Island before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Raoul Island ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Raoul Island

In research
Raoul Island appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Raoul Island in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Raoul Island is common in secondary-school and first-year university syllabi. It links to neighbouring topics Active volcanoes, Calderas of New Zealand, Holocene calderas, so understanding it makes those chapters shorter.
In everyday life
Look for Raoul Island outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

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How to study Raoul Island in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Raoul Island means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Raoul Island out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Raoul Island in simple terms?

Raoul Island (Sunday Island; Māori: Rangitāhua) is the largest and northernmost of the main Kermadec Islands, 900 km (560 mi; 490 nmi) south south-west of 'Ata Island of Tonga and 1,100 km (680 mi; 590 nmi) north north-east of New Zealand's North Island. It has been the source of vigorous volcanic…

Why does Raoul Island matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Raoul Island?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Raoul Island.

Tags

  • Active volcanoes
  • Calderas of New Zealand
  • Holocene calderas
  • Important Bird Areas of the Kermadec Islands
  • Island restoration
  • Islands of the Kermadec Islands
  • Raoul Island
  • Stratovolcanoes of New Zealand
  • Submarine calderas
  • Uninhabited islands of New Zealand
  • VEI-6 volcanoes
  • Volcanic islands of New Zealand

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