Volcanic eruptions are caused by the release of pressure inside the Earth, leading to the expulsion of magma through volcanic vents. This process results in the formation of cone-shaped mountains or hills known as volcanoes. The magma, which originates from the asthenosphere, rises through cracks in

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Explore the composition of Earth's layers through classifying them based on chemical and physical properties. Learn about the lithosphere and its role, including the movement of tectonic plates on the asthenosphere. Discover the distinctions between oceanic and continental plates, their thickness va

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The Earth's interior comprises the lithosphere, asthenosphere, outer core, and inner core, heated by radioactive decay and residual heat. The lithosphere is rigid, while the asthenosphere beneath can flow plastically. Magma is generated at mid-ocean ridges, hotspots, and subduction zones, where plat

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Explore the differences between oceanic and continental crust, the distinctions of lithosphere and asthenosphere, the dynamics of convergent and divergent boundaries, as well as the concepts of folding and faulting in geological formations. Delve into the characteristics of oceanic crust versus ocea

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Delve into the depths of Earth's layers from the crust to the core, learning about its compositional and structural zones. Discover the significance of seismic waves in unraveling the mysteries of Earth's interior, and grasp the fundamental concepts behind the planet's lithosphere and asthenosphere.

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Deep parts of Earth's interior are studied indirectly through geophysics, including seismic waves, magnetic fields, gravity, and heat. Seismic studies reveal Earth's layers - crust, mantle, and core - each with distinct properties and compositions. The lithosphere, comprising the upper mantle and cr

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