Scientists Found 450-Million-Year-Old Fossils at Earth's Highest Point

Scientists Found 450-Million-Year-Old Fossils at Earth's Highest Point Mount Everest’s summit — 8,848.86 meters above sea level — is made of ancient limestone filled with 450‑million‑year‑old sea fossils. These fossils formed on the floor of the Tethys Ocean, a massive ocean that once existed between India and Asia. This video explains how the Indian Plate drifted north for 50 million years, collided with the Eurasian Plate, and crumpled the ocean floor upward to create the Himalayas. You’ll learn how plate tectonics, continental drift, subduction, and continent‑continent collision lifted marine rock nearly nine kilometers into the sky — and why Everest still rises about 2 mm per year while glaciers and rivers carve it down. Everest isn’t just a mountain. It’s a piece of ancient ocean… lifted to the roof of the world. 00:00 – Fossils at the Top of Everest 00:25 – A Seabed Above the Sky 00:45 – The Lost Tethys Ocean 01:10 – The Force That Lifted an Ocean Floor 01:35 – What Mountains Really Are 01:55 – Earth’s Moving Plates 02:20 – India’s 50‑Million‑Year Drift North 02:45 – How Distance Adds Up Over Time 03:10 – Ocean Crust vs Continental Crust 03:35 – The Three Types of Plate Boundaries 04:00 – Why Mountains Aren’t Volcanoes 04:25 – Subduction and Crustal Crumpling 04:50 – The Rise of the Tibetan Plateau 05:15 – How the Himalayas Formed 05:40 – Mountain Ranges Tell Their Age 06:10 – Everest Still Rises Today 06:30 – Fossils at the Roof of the World 06:55 – Measuring Everest’s Height 07:15 – Earthquakes Reset the Mountain Clock 07:35 – Rivers Carve, Mountains Rebound 08:00 – Why Some Ranges Shrink 08:20 – The Future of Mountains 08:45 – The Ground Never Stopped Moving #MountEverest #Himalayas #TethysOcean #PlateTectonics #HowMountainsForm #ContinentalDrift #SubductionZone #EverestFossils #EverestLimestone #IndianPlate #EurasianPlate #EarthScience #GeologyExplained #MindFiss #HiddenHistory