The oceanic crust forms the outermost shell of the Earth beneath the ocean basins. Despite being relatively thin, typically around 5-10 kilometers thick, it plays a crucial role in supporting oceanic ecosystems and processes. Like the various layers of a cake, the oceanic crust is only one slice of the Earth's structure, but without it, the planet wouldn’t be quite the same.
- It is primarily composed of basalt, a dark volcanic rock rich in magnesium and iron.
- Due to its composition, it is denser compared to the continental crust.
- New oceanic crust forms at mid-ocean ridges, where tectonic plates pull apart, allowing magma to rise and cool.
Understanding the dynamics of the oceanic crust is essential for appreciating geological processes like earthquakes, and the formation of ocean features such as ridges and trenches.