Crust, Mantle, Outer Core, Inner core
The Earth's crust is divided into several major tectonic plates that float on the semi-fluid asthenosphere below. These plates are in constant motion, leading to phenomena like earthquakes and volcanic activity along plate boundaries. The largest plates include the Pacific Plate, Eurasian Plate, and North American Plate.
The layer of the Earth that contains continents and other landforms is called the crust. The crust is the outermost layer of the Earth's structure and is composed of solid rocks. It is divided into two types: continental crust and oceanic crust.
The Earth can be divided into three main parts: the core, mantle, and crust. The core is the innermost layer composed of a solid inner core and a liquid outer core. The mantle is the middle layer made up of semi-solid rock, and the crust is the outermost layer where we find the continents and ocean basins.
Crust
The part of the Earth between the core and the crust is the mantle. It is a layer of hot, solid rock that surrounds the Earth's core. The mantle is responsible for movements of tectonic plates and is divided into the upper and lower mantle.
The crust is typically thicker beneath continents compared to oceans. Continental crust can be up to 40 km thick, while oceanic crust is generally around 5-10 km thick.
The crust has about 13 major plates.
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The Crust
The hard outer layer of the earth is called the crust. The crust can be divided into the continental crust and the oceanic crust.
The Earth's crust is divided into continental crust and oceanic crust. Underneath the crust and attached to it is the uppermost brittle mantle, which, together with the crust is referred to as the lithosphere.
The Earth's crust is divided into continental crust and oceanic crust. Underneath the crust and attached to it is the uppermost brittle mantle, which, together with the crust is referred to as the lithosphere.
The outer core is broken into platesinner and outer core
Yes
crust
The Earth's crust
lithosphere and crust