Earth is also home to many different types of climates and weather patterns. Some places are hot and dry, while others are cold and snowy. Some regions receive heavy rainfall, creating lush rainforests, while others experience mild temperatures and four distinct seasons. These variations make our planet even more fascinating and unique.
Crust: The crust is the outermost layer of the Earth. It\\\’s like the thin, hard shell that covers an egg. It\\\’s divided into two types: the continental crust and the oceanic crust. The continental crust is what makes up the continents, while the oceanic crust lies beneath the oceans. The crust is where we live, and it\\\’s made up of rocks, soil, mountains, and even the ground we walk on!
Mantle: Beneath the crust is the mantle. Think of it as a thick layer of hot, gooey material. The mantle is responsible for most of the Earth\\\’s heat and is made up of solid and semi-solid rocks. It\\\’s so hot that some rocks in the mantle melt and become molten rock called magma. Magma can sometimes escape to the surface through volcanic eruptions.
Outer Core: Going deeper, we reach the outer core. This layer is made up of liquid metal, mostly iron and nickel. It\\\’s like a super-hot, swirling soup! The outer core is responsible for generating the Earth\\\’s magnetic field, which protects us from harmful solar radiation and guides compasses to help us find directions.
Inner Core: At the very center of the Earth lies the inner core. It\\\’s a solid ball of extremely hot and dense metal, mostly iron and nickel. The intense pressure from the layers above keeps the inner core in a solid state, even though it\\\’s incredibly hot. It\\\’s like a super-hot, solid metal ball!
Weight
0.450 kg
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