Exploring Cebu's Geological Marvel: The Tunlob Schist

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Before the islands rose, the Tunlob Schist already had a story to tell. Photo from Fatima Buenaflor Servano Deep beneath Cebu’s bustling cities and rolling hills lies a geological treasure. The Tunlob Schist is a rock formation dating back to the Jurassic period (approximately 201-145 million years

Deep beneath the vibrant cities and picturesque landscapes of Cebu lies a hidden gem - the Tunlob Schist. This rock formation, dating back to the Jurassic period (approximately 201-145 million years ago), offers a fascinating glimpse into the prehistoric origins of the Philippines. Found within the Pandan Formation, the Tunlob Schist provides valuable insights into the tectonic evolution of the region, shedding light on how the Philippine archipelago was formed through the collision of ancient oceanic plates.

The Tunlob Schist is a part of the Pandan Formation, a late Cretaceous geological unit in Cebu comprising metamorphic and sedimentary rocks. This medium-grade metamorphic rock was formed under intense heat and pressure underground, indicating that Cebu was once part of a dynamic tectonic boundary where plates collided and subducted millions of years ago. Studies reveal that the minerals and geochemical signatures found in the Tunlob Schist are associated with the Australian continental margin, suggesting that Cebu's rocks may have originated from ancient fragments of the Australian crust.

The fascinating composition of the Tunlob Schist, including minerals like chlorite, muscovite, and quartz, indicates that it likely originated from deep-sea sediments or volcanic rocks that underwent significant transformation over millions of years. Dating back to the Late Cretaceous period, with possible origins in the Jurassic era, this rock formation is exposed in areas where erosion has unveiled the Earth's ancient past, offering a unique window into the region's geological history.

The discovery of the Tunlob Schist is a significant find that serves as a geological time capsule, providing valuable insights into the tectonic origin of the Philippines and its connection to Australia and an ancient ocean basin. By studying this rock, scientists can better understand how the island of Cebu was shaped through subduction and mountain-building processes. For geologists and enthusiasts, the Tunlob Schist represents a tangible link to the Jurassic era, making it a remarkable discovery and a national treasure in Cebu.

As research continues, the Tunlob Schist remains a testament to Cebu's ancient past, offering a glimpse into a time when dinosaurs roamed the Philippine island as it was still taking shape. This Jurassic-age rock holds the potential to reveal valuable information about the forces that shaped Cebu into the majestic island it is today. For those intrigued by the mysteries beneath our feet, Cebu's geological wonders provide a captivating journey through deep time.



Source: Sugbo.ph
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