ArticleslgStudy

earth science

Kermadec Islands

Kermadec Islands 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 Kermadec Islands rather than just read about it. In short: The Kermadec Islands ( KUR-mə-dek; Māori: Rangitāhua) are a subtropical island arc in the South Pacific Ocean 800–1,000 km (500–620 mi; 430–540 nmi) northeast of New Zealand's North Island, and a similar distance southwest of Tonga. The islands are part of New Zealand.

Kermadec Islands — main illustration
Kermadec Islands — illustration

Key takeaways

  • Kermadec Islands 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 Kermadec Islands to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Kermadec Islands from memory before moving on to harder problems.

Reference excerpt

The Kermadec Islands ( KUR-mə-dek; Māori: Rangitāhua) are a subtropical island arc in the South Pacific Ocean 800–1,000 km (500–620 mi; 430–540 nmi) northeast of New Zealand's North Island, and a similar distance southwest of Tonga. The islands are part of New Zealand. They are 33.6 km2 (13.0 sq mi) in total area and uninhabited, except for the permanently staffed Raoul Island Station, the northernmost outpost of New Zealand. The islands are listed with the New Zealand outlying islands. The islands are an immediate part of New Zealand, but not part of any region or district, but instead an Area Outside Territorial Authority.

Toponymy The islands were named after the Breton captain Jean-Michel Huon de Kermadec, who visited the islands as part of the d'Entrecasteaux expedition in the 1790s. The topographic particle "Kermadec" is of Breton origin and is a lieu-dit in Pencran in Finistère where ker means village, residence and madec a proper name derived from mad (which means 'good') with the suffix -ec, used to form adjectives indicating a property. The Māori name is Rangitāhua which is also used for Raoul Island.

History As indicated by their name for the islands, Rangitāhua (lit. 'the stopping-off place'), Polynesian people "stopped off" on the Kermadec Islands in around the 14th century (and perhaps previously in the 10th century). Their arrival is also evident in the presence of introduced taro and candlenut growing wild in certain areas of Raoul Island supported by its relatively warm climate. However, the first Europeans to reach the area – arriving on board the Lady Penrhyn in May 1788 – found no inhabitants on these volcanic islands. British, American and Australian whaling vessels cruised offshore in the 19th century and often visited the islands in search of water, wood and food. The first such vessel on record was the whaler Fanny that visited Raoul Island in 1823. On 1 August 1886, HMS Diamond annexed the islands for the United Kingdom. Letters patent issued on 18 January 1887, assigned the islands to the colony of New Zealand following a request from the colony's parliament. European settlers have lived on the island for varying lengths of time, from the early nineteenth century until 1937, growing food for the whalers. The Thomas Bell family settled on the island from 1878 to 1914. One of the Bell daughters, Bessie Dyke, recounted the family's experience to writer Elsie K. Morton who published their story in 1957 as Crusoes of Sunday Island.

Raoul Island Station

The Raoul Island Station consists of a government meteorological and radio station, and a hostel for Department of Conservation officers and volunteers, that has been maintained since 1937. It lies on the northern terraces of Raoul Island, at an elevation of about 50 m (160 ft), above the cliffs of Fleetwood Bluff. It is the northernmost inhabited outpost of New Zealand.

Nuclear testing proposals In 1955, the British Government required a large site remote from population centres to test the new thermonuclear devices it was developing. Various islands in the South Pacific and Southern Oceans were considered, along with Antarctica. In May 1955, the Minister for Defence, Selwyn Lloyd, on advice from the Admiralty report, concluded that the Kermadec Islands would be suitable. As the island group was part of New Zealand, Anthony Eden, who had recently become the Prime Minister of the United Kingdom, wrote to the Prime Minister of New Zealand, Sidney Holland, to ask for permission to use the islands. Holland refused, fearing an adverse public reaction in the upcoming 1957 general election. Despite reassurances and pressure from the British government, Holland remained firm.

Geography The islands lie within 29° to 31.5° south latitude and 178° to 179° west longitude, 800–1,000 km (500–620 mi; 430–540 nmi) northeast of New Zealand's North Island, and a similar distance southwest of Tonga. The total area of the islands is 33.6 km2 (12.97 sq mi).

Climate The climate of the islands is subtropical, with a mean monthly temperature of 22.4 °C (72.3 °F) in February and 16.0 °C (60.8 °F) in August. Rainfall is approximately 1,500 mm (60 in) annually, with lower rainfall from October to January.

Islands

The group includes four main islands as well as some isolated rocks. These are:

Raoul Island or Sunday Island is by far the largest of the islands. It lies 900 km (560 mi; 490 nmi) south-southwest of 'Ata, the southernmost island of Tonga, and 1,100 km (680 mi; 590 nmi) north-northeast of New Zealand. Raoul Island has an area of 29.38 km2 (11.34 sq mi) with numerous smaller satellite islands; its highest point, Moumoukai Peak, is 516 m (1,693 ft) high. Macauley Island, the second largest, is located 110 km (68 mi; 59 nmi) south-southwest of Raoul Island. Together with neighbouring Haszard Island, its area is 3.06 km2 (1.18 sq mi). Macdonald Rock is about 4 km (2.5 mi; 2.2 nmi) north of Macauley Island. Curtis Island, the third largest, lies 35 km (22 mi; 19 nmi) south-southwest of Macauley Island. It reaches a height of 137 m (449 ft) and has an area of 0.59 km2 (0.23 sq mi) with neighbouring Cheeseman Island. Nugent Island is the northernmost island. It is approximately 100 metres (109 yd) across. L'Esperance Rock, formerly French Rock, is 80 km (50 mi; 43 nmi) south-southwest of Curtis Island. It is 250 m (820 ft) in diameter, 0.05 km2 (0.019 sq mi) in area, and 70 m (230 ft) high. L'Havre Rock, about 8 km (5.0 mi; 4.3 nmi) north-northwest of L'Esperance Rock, is submerged except at low tide. Seamounts north and south of the Kermadec Islands are an extension of the ridge running from Tonga to New Zealand (see Geology). Star of Bengal Bank, 103 km (64 mi) south-southwest of L'Esperance Rock, has a least depth of 48 metres (157 ft).

Geology

… excerpt ends here. Continue reading the full article.

Illustrations

Kermadec Islands illustration
Kermadec Islands illustration
Kermadec Islands: Raoul Island from space
Raoul Island from space
Kermadec Islands: View from Raoul Island
View from Raoul Island
Kermadec Islands: Bathymetry of the Kermadec volcanic island arc and surrounding areas
Bathymetry of the Kermadec volcanic island arc and surrounding areas

Worked examples

Example 1 — a first encounter with Kermadec Islands

Start with the simplest possible case. Write down what Kermadec Islands 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 Kermadec Islands 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 Kermadec Islands 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 Kermadec Islands

In research
Kermadec Islands 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 Kermadec Islands 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
Kermadec Islands is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1887 establishments in New Zealand, Archipelagoes of New Zealand, Archipelagoes of the Pacific Ocean, so understanding it makes those chapters shorter.
In everyday life
Look for Kermadec Islands 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.
Ask Teacher Smith questions about this articleOpens your AI tutor with a question about “Kermadec Islands” →

Affiliate

Preply — study more efficiently by working with a personal tutor. 50% off.

How to study Kermadec Islands in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Kermadec Islands 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 Kermadec Islands out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Kermadec Islands in simple terms?

The Kermadec Islands ( KUR-mə-dek; Māori: Rangitāhua) are a subtropical island arc in the South Pacific Ocean 800–1,000 km (500–620 mi; 430–540 nmi) northeast of New Zealand's North Island, and a similar distance southwest of Tonga. The islands are part of New Zealand.

Why does Kermadec Islands 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 Kermadec Islands?

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 Kermadec Islands.

Tags

  • 1887 establishments in New Zealand
  • Archipelagoes of New Zealand
  • Archipelagoes of the Pacific Ocean
  • Ecoregions of New Zealand
  • Important Bird Areas of the Kermadec Islands
  • Island restoration
  • Kermadec Islands
  • Oceanian ecoregions
  • States and territories established in 1887
  • Tropical and subtropical moist broadleaf forests
  • Volcanism of New Zealand

Keep exploring