Continental Drift Simulation: Earth's Moving Continents
As South America and Africa inch apart, the Atlantic Ocean widens, showcasing a geological process that began 140 milli…
Pangaea Supercontinent: 200 Million Years Ago
Around 200 million years ago, Earth's landmass was a single, colossal continent — Pangaea. Pangaea was the last time al…
Pangaea Supercontinent: Formation and Breakup
The jagged coastlines of Africa and South America fit together like puzzle pieces, a hint at a time when all land was o…
Nankai Trough Earthquake: Japan's Deadly Risk
Japan's Nankai Trough fault line, off the country's coast, threatens up to 298,000 people in its path. This geological…
Mount Everest's Slow Rise Visualized
Mount Everest is still growing, as the Himalayas rise each year at a pace unlike most other mountains. This process beg…
Continental Drift: Pangaea to Today's Seven Continents
Pangaea, the supercontinent that once dominated Earth, began to split about 200 million years ago, forming the continen…
Andes Mountains Formation: Nazca Plate Subduction
The Nazca Plate dives beneath the South American Plate at a rate of 7–8 centimetres per year. The Andes Mountains, an 8…
The Science Behind Mountain Formation: Plate Tectonics Explained
Mountains are monumental results of Earth's dynamic geological processes. They form over millions of years as continent…
The Structure of Earth's Layers and Their Roles
Earth is composed of several layers, each crucial for the planet's dynamics and life. From the atmosphere protecting ag…