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  2. Manihiki Plateau - Wikipedia

    en.wikipedia.org/wiki/Manihiki_Plateau

    The North Plateau is small and almost separated from the rest of the Manihiki Plateau. [4] The High Plateau is the largest part of Manihiki covering 400,000 km 2 (150,000 sq mi) above 4000 m. The second largest part is the Western Plateaus covering 250,000 km 2 (97,000 sq mi) above 5000 m and reaching 3,500–4,000 m (11,500–13,100 ft) below ...

  3. Shatsky Rise - Wikipedia

    en.wikipedia.org/wiki/Shatsky_Rise

    The Shatsky Rise is Earth's third largest oceanic plateau, [1] (after Ontong Java and Kerguelen) located in the north-west Pacific Ocean 1,500 km (930 mi) east of Japan.It is one of a series of Pacific Cretaceous large igneous provinces (LIPs) together with Hess Rise, Magellan Rise, and Ontong Java-Manihiki-Hikurangi. [2]

  4. Manihiki - Wikipedia

    en.wikipedia.org/wiki/Manihiki

    Manihiki is an atoll in the northern group of the Cook Islands known informally as the "Island of Pearls". It is located in the Northern Cook Island chain , approximately 1,299 kilometres (807 mi) north of the capital island of Rarotonga , making it one of the most remote inhabitations in the Pacific Ocean .

  5. Geography of the Cook Islands - Wikipedia

    en.wikipedia.org/wiki/Geography_of_the_Cook_Islands

    Island Group Island Area (km 2) Population Density Northern: Penrhyn: 10 226 22.6 Northern: Rakahanga: 4 80 20.0 Northern: Manihiki: 5 213 42.6 Northern: Pukapuka

  6. Ontong Java Plateau - Wikipedia

    en.wikipedia.org/wiki/Ontong_Java_Plateau

    The Ontong Java Plateau (OJP) is a massive oceanic plateau located in the southwestern Pacific Ocean, north of the Solomon Islands. The OJP was formed around 116 million years ago (Ma), [ 1 ] with a much smaller volcanic event around 90 Ma.

  7. Category:Manihiki - Wikipedia

    en.wikipedia.org/wiki/Category:Manihiki

    This page was last edited on 29 September 2021, at 07:14 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.

  8. Paraná and Etendeka traps - Wikipedia

    en.wikipedia.org/wiki/Paraná_and_Etendeka_traps

    The basalt samples at Paraná and Etendeka have an age of about 132 Ma, during the Valanginian stage of the Early Cretaceous. [3] Indirectly, the rifting and extension are probably the origin of the Paraná and Etendeka traps and it could be the origin of the Gough and Tristan da Cunha Islands as well, as they are connected by the Walvis Ridge (Gough/Tristan hotspot).

  9. Talk:Manihiki Plateau - Wikipedia

    en.wikipedia.org/wiki/Talk:Manihiki_Plateau

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