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Earth’s Interior & Earthquakes

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Presentation on theme: "Earth’s Interior & Earthquakes"— Presentation transcript:

1 Earth’s Interior & Earthquakes

2 Part of the Earth Layers defined by composition Crust
Thin, rocky outer layer of Earth Either oceanic crust or continental crust Oceanic crust is 7 km thick

3 Mantle Core 82% of the Earth’s volume
Solid rock at the top, liquid at the bottom Core Composed of iron-nickel alloy Extreme pressure found in the center of the core

4 Layers defined by Physical Properties
Lithosphere The crust and uppermost mantle Cool, rigid shell 100 km thick Asthenosphere Soft, comparatively weak layer Below the lithosphere Rock close to melting

5 Outer Core Inner Core Liquid layer 2260 km thick
Metallic iron generates Earth’s magnetic field Inner Core Solid layer having a radius of 1220 km High temperatures and high pressure Nickel mostly

6 Earthquakes

7 What is an earthquake? Vibration of Earth produced by a sudden release of energy Movements along the fault line.

8 Focus, Epicenter and Faults
Focus – point within the Earth where the Earthquake starts Epicenter – location on the surface of Earth directly above the focus Fault- associated with earthquake activity where movement has occurred

9 Elastic Rebound Hypothesis
Release of built-up energy Most earthquakes are produced by the rapid release of elastic energy stored in rock that has been subjected to great forces When the strength of the rock is exceeded, it suddenly breaks, causing vibration of an earthquake

10 Foreshock vs. Aftershock
Foreshock – small quake that comes before a major earthquake Aftershock – small quake that comes after a major earthquake

11 Seismology Seismology – study of earthquake waves
Seismograph – instruments that record earthquake waves Seismograms – the record made by a seismograph

12 Earthquake waves Surface
Seismic waves that travel along Earth’s outer layer Move up, down, and side to side Most destructive earthquake waves Last to arrive at the seismograph

13 Earthquake waves P waves S waves
They push (compress) and pull (expand) rocks in the direction the wave travels Also known as compression waves Can travel through solid, liquid, and gas Fastest waves S waves Shakes particles at right angles to their direction of travel Also known as transverse waves Can only travel through solids Slower than P waves but faster than surface waves

14 Exit Ticket C A B Identify the waves recorded at A, B and C on the diagram


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