Earthquakes and Earth's Interior Quiz Part 1

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Created by:

leslieharris1  on November 15, 2011

Subjects:

earthquakes, geology, seismology

Description:

Chapter 14 Essentials of Geology by Pearson

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Earthquakes and Earth's Interior Quiz Part 1

Earthquake
The vibration of Earth produced by the rapid release of energy
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Earthquake The vibration of Earth produced by the rapid release of energy
Focus The source of the energy that radiates in all directions from here in the form of waves
Faults Large fractures in the Earth's crust that are associated with movements that produce earthquakes
Plate Tectonics Theory Most of the motion along faults can be explained by this
Seismology The study of earthquake waves; dates back to the Chinese almost 2000 years ago
Seismologists People who study earthquakes and their characteristics
H.F. Reid First explained mechanism for earthquakes
Mechanism for earthquakes Rocks on either side of fault are deformed by tectonic forces, bend and store elastic energy, frictional force is overcome
Elastic rebound Slippage at the weakest point (the focus) occurs; vibrations occur as the deformed rock "springs back" to its original shape
Focus Point at the depth where the rocks ruptured to produce earthquakes; place where quake waves originate
Aftershocks smaller quakes produced after a major quake caused by rocks shifting to new positions
Foreshocks small earthquakes that come before a major earthquakes
San Andreas Most studied fault system
Fault creep Slow gradual displacement of some portions of fault
50 to 200 years Great earthquakes should occur about
Seismograph Instruments that record seismic waves
Large hollow jar Chinese used this to measure seismic activity with suspended free motion mass
Seismograms Records obtained from seismographs
Types of seismic waves Surface, Body
Surface waves Travel along the Earth's surface; cause greatest destruction; slow & great
Two kinds of body waves Primary (P) and Secondary (S)
Body waves Travel through Earth's interior; two types
Primary (P) waves travel 1.7 times faster than S waves; travel through whole interior; motion is back & forth
Secondary (S) waves shaking motion at right angles; travels only through solids; slower velocity than P waves; slightly greater amplitude than P waves
Waves Wavelength, crest, trough and amplitude
Epicenter location on the surface directly above the focus; located using the difference in velocities of P & S waves
Three At least this many station recordings needed to locate an epicenter
Travel-time graph used to determine each station's distance to the epicenter
Locating the epicenter a circle with radius equal to distance to epicenter drawn around each station; point where all 3 circles intersect is epicenter
95% percent of energy released by earthquakes; originates in a few relatively narrow zones that wind around the globe
Major earthquake zones Circum-Pacific belt, Mediterranean Sea region to Himalayan complex & oceanic ridge system (underwater mountains)
5 to almost 700 km Range of depths of earthquakes
Types of earthquakes Shallow, Intermediate & Deep Focus
Shallow surface to 70 km; occur along oceanic ridge system; nearly all damaging quakes originate at this depth; not much room so more damage
Intermediate between 70to 300 km
Deep Focus over 300 km; almost all occur in circum-pacific belt
90% Percent of all earthquakes occur at depths of less than 100 km
Two measurements of earthquake size Intensity and Magnitude
Intensity a measure of the degree of quake shaking at a given locale based on amount of damage
Magnitude estimates the amount of energy released at the source of the quake
Modified Mercalli Intensity Scale developed using CA buildings; drawback not true measure of quakes actual severity; Guiseppe Mercalli; 1-12 in Roman numerals; I - least; XII - most; used after quake

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