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Chapter 10 Section 1 Notes
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EARTHQUAKES –vibrations in the ground that result from movement along breaks in the Earth’s lithosphere
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Forces that move TECTONIC PLATES also push and pull rocks along breaks in the lithosphere
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Most earthquakes occur along active PLATE BOUNDARIES
These are generally in the middle of oceans or along the edges of CONTINENTS
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Deep earthquakes occur along CONVERGENT plate boundaries , where denser oceanic plates subduct.
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Shallow earthquakes are common along DIVERGENT BOUNDARIES, where plates separate
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Earthquakes of varying depths occur where continents COLLIDE
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Pressure applies to rock can change the shape in a process called DEFORMATION. This can eventually BREAK the rock
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A FAULT is a break in the Earth’s lithosphere where one block of rock moves toward, away from, or past another block
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The 3 types of faults are strike-slip, REVERSE, and normal
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When rocks move in any direction along a fault, they release energy in Earth’s crust in SEISMIC WAVES
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Seismic waves originate along the FAULT where rocks first begin to move.
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The location inside the Earth is called the FOCUS of the earthquake
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The EPICENTER of an earthquake is the location on Earth’s surface directly above the focus.
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The energy released during an earthquake is strongest near the EPICENTER
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An earthquake’s energy travels in 3 kinds of SEISMIC WAVES
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PRIMARY WAVES cause particles in the ground to move in a push-pull motion similar to a coiled spring
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SECONDARY WAVES move rock particles side to side and up and down at right angles
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SURFACE WAVES move the ground up and down and side to side, like an ocean wave
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Scientists who study earthquakes are called SEISMOLOGISTS
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Seismic waves travel at different SPEEDS and in different DIRECTIONS depending on the materials they travel through.
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S waves cannot travel through liquids, including Earth’s OUTER CORE
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Seismic waves SLOW DOWN as they travel through hot material
Seismic waves SLOW DOWN as they travel through hot material. This helps support convection currents in the Earths MANTLE
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A SEISMOMETER measures and records how much the ground moves and can be used to dermine the distance seismic waves travel.
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A SEISMOGRAM is a graphical illustration of seismic waves
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RICHTER MAGNITUDE SCALE
Uses the amount of motion ata a given distance from an earthquake to determine the magnitude of the earthquake … The 1811 earthquake in this area was thought to be about an 8.0 …
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MOMENT MAGNITUDE SCALE
Measures the amount of energy released by an earthquake
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MODIFIED MERCALLI SCALE
Measures earthquake intensity based on the descriptions of the earthquakes effects on people and structures.
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CONVERGENT PLATE BOUNDARIES
In the US most earthquakes occur near transform faults and….
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EARTHQUAKE RISK Is based on past earthquake activity, the geology around a fault, population density, and building design.
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