File:Folded layers of bedded chert formation in Busuanga, Palawan 01.jpg

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English: Shown is a closer view of an outcrop of the late Permian to Jurassic-aged Liminangcong chert formation exposed along the Coron-Busuanga road near the Marina del Sol yacht club. Visible here are the folded beds of chert formed from the deposition of siliceous (radiolarian) fossils. The folding was produced by millions of years of tectonic activity which also uplifted the island from deep below the ocean. Geologist's hammer for scale.
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Author Paul Christian B. Yang-ed

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current13:42, 4 July 2023Thumbnail for version as of 13:42, 4 July 20232,604 × 4,624 (7.07 MB)Paul Christian B. Yang-ed (talk | contribs)Uploaded own work with UploadWizard

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