PaleoEarth 1.1

Earth is a dynamic planet. Throughout its history, one constant has been its ever-changing state - from the continuous movement of tectonic plates to the evolving climate that sparked the genesis of life and the persistent barrage of asteroids, some triggering large-scale extinction events. PaleoEarth consolidates diverse datasets offering a distinctive insight into Earth's dynamic past. The key features encompass:

• Illustrating the movement of continental plates, subduction zones (where oceanic crust descends into the Earth's mantle), and mid-ocean ridges (where new oceanic crust is formed) over the past 400 million years.
• Mapping locations of significant asteroid impacts, tracing their journey from the impact site to their present position due to tectonic plate movements.
• Comparing Earth's past temperature and atmospheric CO2 levels to present-day metrics over the last 400 million years.
• Backtracking borders of specific countries over the last 400 million years, demonstrating how some major nations such as the Russian Federation and the People's Republic of China evolved from the amalgamation of smaller continental plates.