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Geological Formation

Sulu Archipelago

Structural and Tectonic Formations

The Sulu Archipelago is a chain of islands in the Pacific Ocean in the southwestern Philippines, forming the northern limit of the Celebes Sea and the southern limit of the Sulu Sea. Rather than being a remnant land bridge, it represents the exposed edge of small submarine ridges produced by tectonic tilting of the sea floor. Its major islands, including Basilan, Jolo and Tawi-Tawi, are extinct volcanic cones, with Tawi-Tawi carrying a serpentine basement core overlain by limestone. The archipelago covers about 4,068 square kilometers and is organized into the three provinces of Basilan, Sulu and Tawi-Tawi. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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Caused By

Volcanism, Processes
Source Sulu Archipelago (Wikipedia)

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Sulu Archipelago
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Sulu Archipelago
Sources
Sulu Archipelago (Wikipedia)
  • Lead section
    The Sulu Archipelago (Tausug: Kapū'-pūan sin Sūg; Sulat Sūg: كَفُوْءْفُوْأَنْ سِنْ سُوْݢْ; Filipino: Kapuluan ng Sulu) is a chain of islands in the Pacific Ocean in the southwestern Philippines.
  • Caused By: Volcanism, Lead
    Basilan, Jolo, Tawi-Tawi and other islands in the group are extinct volcanic cones rising from the southernmost ridge.
View the Source
Wikidata: Sulu Archipelago
Wikidata Q1061195, class allow-list match (w-wdresolver-0926)View the Source
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