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Pangaea was an ancient global supercontinent that united almost all of Earth’s landmasses into a single entity surrounded by a massive world ocean called Panthalassa. The story of this united Earth is a narrative of continental collision, extreme environments, and the eventual fracturing that shaped our modern world. 🌍 The Assembly (335 Million Years Ago)

The Fusion: Pangaea formed during the Carboniferous period when two massive smaller supercontinents—Laurasia (the north) and Gondwana (the south)—collided.

The Shape: It was a colossal, C-shaped landmass centered on the equator, stretching nearly from the North Pole to the South Pole.

Mountain Building: The violent crunching of tectonic plates during its formation pushed up massive mountain ranges, including early versions of the Appalachian Mountains and the Urals. 🏜️ Life and Climate on the United Earth

Extreme Deserts: Because the landmass was so vast, rain-bearing ocean winds could not reach the deep interior. This created scorching, arid deserts at the center of the supercontinent with intense seasonal temperature swings.

No Boundaries: Animals and plants could roam freely from modern-day New York to Morocco or Brazil to Angola without crossing an ocean.

The Inhabitants: Pangaea was the cradle for early dinosaurs, massive insects, conifers, and early reptiles, allowing identical species to colonize widely before the land split. ⚡ The Breakup (200 Million Years Ago)

The Rift: During the early Jurassic period, volcanic activity and churning mantle currents began tearing Pangaea apart.

The Atlantic Birth: A massive fissure tore open between Africa and North America. Magma welled up to fill the gap, creating a rift valley that slowly filled with water to become the Atlantic Ocean.

Isolation: As the pieces drifted away to form our current seven continents, isolated animal populations began to evolve independently, accelerating global biodiversity. 🔍 How We Discovered It Historical perspective [This Dynamic Earth, USGS]

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