What Is Mantle Convection and Earth's Structure?
Think of the Earth like a giant layered cake - but one that's constantly moving on the inside! Mantle convection is the slow, churning motion happening in the Earth's mantle, which is the thick layer of hot rock sitting between our thin crust and the super-hot core below.
The Earth has four main layers: the crust (where we live), the mantle (extending about 2,900 kilometers down), the outer core (liquid metal), and the inner core (solid metal). The mantle makes up about 84% of Earth's volume, so understanding what happens there is pretty important.
What keeps this massive rock layer moving? It's all about heat from three main sources: radioactive elements like uranium breaking down, leftover heat from when Earth first formed billions of years ago, and heat released when the outer core solidifies.
Quick Fact: The mantle is so thick that if Earth were the size of an apple, the mantle would be most of the fruit part!