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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Source Sulu Archipelago (Wikipedia)
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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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Source Wikidata: Sulu Archipelago
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Sulu Archipelago (Wikipedia)
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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 SourceWikidata: Sulu Archipelago
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