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  2. Geology of the Northern Mariana Islands - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Northern...

    The bulk of geological research in the Northern Mariana Islands has focused on the large, populous island of Saipan. The U.S. Geological Survey first mapped the island in 1956 and it was remapped again in 2007. The oldest rocks exposed at the surface are Eocene volcanic rocks, belonging to the Izu-Bonin-Mariana (IBM) arc system. Saipan is on ...

  3. Mariana Islands - Wikipedia

    en.wikipedia.org/wiki/Mariana_Islands

    The Mariana Islands are the southern part of a submerged mountain range that extends 1,565 miles (2,519 km) from Guam to near Japan. Geographically, the Marianas are part of a larger region called Micronesia, situated between 13° and 21°N latitude and 144° and 146°E longitude. The Mariana Islands have a total land area of 1,008 km 2 (389 sq ...

  4. Geography of Sri Lanka - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Sri_Lanka

    More than 90% of Sri Lanka's surface lies on Precambrian strata, some of it dating back 2 billion years. [6] The granulite facies rocks of the Highland Series (gneisses, sillimanite-graphite gneisses, quartzite, marbles, and some charnockites) make up most of the island and the amphibolite facies gneisses, granites, and granitic gneisses of the Vijayan Series occur in the eastern and ...

  5. Geological Society of Sri Lanka - Wikipedia

    en.wikipedia.org/.../Geological_Society_of_Sri_Lanka

    The society was established in 1983 at the Department of Geology, University of Peradeniya [2] by a group of senior academic and professional geologists of Sri Lanka. [3] Despite academic geological studies in Sri Lanka dating back to at least 1902 of Ananda Coomaraswamy's times, the country had never before had a forum for geologists such as ...

  6. Daikoku Seamount - Wikipedia

    en.wikipedia.org/wiki/Daikoku_Seamount

    Daikoku Seamount (Japanese: 大黒海山) is a submarine volcano located in the Northern Mariana Islands, in the western Pacific Ocean. It is situated on the Mariana volcanic arc . The seamount rises over 2,500 m (8,202 ft) meters from the seafloor, with its summit about 323 m (1,060 ft) below sea level.

  7. Ruby Seamount - Wikipedia

    en.wikipedia.org/wiki/Ruby_Seamount

    Ruby Seamount is an active volcanic seamount in the Northern Mariana Islands region of the Pacific Ocean about 50 km (31 mi) north-west of Saipan. [ 5 ] [ 1 ] It is in a region where the Pacific Plate is subducting under the Philippine Sea Plate producing arc volcanism .

  8. Category:Geology of Sri Lanka - Wikipedia

    en.wikipedia.org/wiki/Category:Geology_of_Sri_Lanka

    Geology of Sri Lanka This page was last edited on 2 January 2020, at 01:10 (UTC). Text is available under the Creative Commons Attribution-ShareAlike 4.0 ...

  9. Zealandia Bank - Wikipedia

    en.wikipedia.org/wiki/Zealandia_Bank

    Zealandia Bank, also known as Farallon de Torres or Piedras de Torres in Spanish, or Papaungan in Chamorro, consists of two rocky pinnacles about 1.5 kilometers apart, in the Northern Mariana Islands in the Pacific Ocean. One reaches a height of approximately 1 meter (3.3 ft) at low tide; the other does not normally broach the surface.