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8th Grade Earth Science Name Date The Earth is Made of 5 Physical Parts • • • • • Lithosphere Asthenosphere Mesosphere Outer Core Inner Core Lithosphere • The cool, outermost layer of the earth. • The Lithosphere consists of: – Crust – Rigid, uppermost part of the mantle. • The Lithosphere is divided into 2 huge pieces called Tectonic Plates. Asthenosphere • The solid, soft layer of the mantle below the lithosphere. • The Asthenosphere is made up of mantle rock that flows very slowly, allowing the tectonic plates to move on top of it. Mesosphere • Middle Sphere • The Mesosphere is the solid lower part of the mantle below the asthenoshpere. Outer & Inner Core • Outer Core – The outer shell of the Earth’s core – It is made of liquid iron and nickel. • Inner Core – A sphere of solid iron and nickel. Plate Tectonics • Plate Tectonics is the theory that the lithosphere is divided into tectonic plates that move around on top of the Asthenosphere. • There are 3 types of Tectonic Plate Boundaries: – Convergent – Divergent – Transform Convergent Boundary • The boundary that is created when two tectonic plates collide. • There are 3 types of Convergent Boundaries: – Continental/Continental – Continental/Oceanic – Oceanic/Oceanic Continental/Continental • When two tectonic plates with continental crust collide, they buckle and thicken, pushing the continental crust upward. Continental/Oceanic • When a tectonic plate with continental crust crashes into a tectonic plate with oceanic crust, the oceanic plate slides under the continental plate. • The region where oceanic lithosphere sinks into Asthenosphere is called a subduction zone. Oceanic/Oceanic • When two oceanic plates collide, one of the oceanic plates is subducted, or sinks, under the other. Divergent Boundary • The boundary that is created when two tectonic plates separate. – Also called rift zones. • As the two tectonic plates move apart, magma rises to fill the gap. – At a mid-ocean ridge, the rising magma cools to form new oceanic lithosphere. Transform Boundary • The boundary that is created when two tectonic plates slide past each other horizontally. – As the two tectonic plates slide past one another, they are not smooth, they grind and jerk as they slide, producing earthquakes.