Think about how the landmasses got from where they were to where they are today. Does seem realistic that the landmasses could have moved like this? Explain.

The shifting of landmasses is rooted in the theory of plate tectonics, which gained traction in the mid-20th century. It reveals that the Earth’s outer shell is divided into large, slow-moving plates that float atop the semi-fluid asthenosphere. Over millions of years, these tectonic plates can collide, pull apart, or slide past each other, leading to the formation of mountains, earthquakes, and volcanic activity, shaping our continents into their current configuration. This movement isn't just theoretical; it has been observed in real-time! For instance, the Atlantic Ocean is gradually widening as the North American and Eurasian plates drift apart. Furthermore, GPS technology tracks these movements with astonishing precision, providing tangible evidence that our planet's surface is on a slow but steady journey, proving that while it may seem far-fetched, the idea of moving continents is very much a reality.