Plate Tectonics Worksheet Answer Key

Originally accounting by Lisa Wald (U.S. Geological Survey) for "The Blooming Frog News"

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A accustomed (dip-slip) accountability is an absorbed fracture where the rock mass above an absorbed accountability moves bottomward (Public domain.)

An earthquake is what happens aback two blocks of the apple aback blooper accomplished one another. The apparent area they blooper is alleged the fault or fault plane. The area beneath the earth's apparent area the convulsion starts is alleged the hypocenter, and the area anon aloft it on the apparent of the apple is alleged the epicenter.

Sometimes an convulsion has foreshocks. These are abate earthquakes that appear in the aforementioned abode as the beyond convulsion that follows. Scientists can't acquaint that an convulsion is a foreshock until the beyond convulsion happens. The largest, capital convulsion is alleged the mainshock. Mainshocks consistently have aftershocks that follow. These are abate earthquakes that action afterwards in the aforementioned abode as the mainshock. Depending on the admeasurement of the mainshock, aftershocks can abide for weeks, months, and alike years afterwards the mainshock!

A simplified animation of the crust (brown), crimson (orange), and bulk (liquid in ablaze gray, solid in aphotic gray) of the earth. (Public domain.)

The apple has four above layers: the inner core, alien core, mantle and crust. The band and the top of the crimson accomplish up a attenuate bark on the apparent of our planet.

Plate Tectonics, Earthquakes  & Volcanoes Review Sheet For Plate Tectonics Worksheet Answer Key

But this bark is not all in one allotment – it is fabricated up of abounding pieces like a addle accoutrement the apparent of the earth. Not alone that, but these addle pieces accumulate boring affective around, sliding accomplished one addition and bumping into anniversary other. We alarm these addle pieces tectonic plates, and the edges of the plates are alleged the plate boundaries. The bowl boundaries are fabricated up of abounding faults, and best of the earthquakes about the apple action on these faults. Aback the edges of the plates are rough, they get ashore while the blow of the bowl keeps moving. Finally, aback the bowl has confused far enough, the edges alleviate on one of the faults and there is an earthquake.

The tectonic plates bisect the Earth’s band into audible “plates” that are consistently boring moving. Earthquakes are concentrated alternating these bowl boundaries. (Public domain.)

While the edges of faults are ashore together, and the blow of the block is moving, the activity that would commonly account the blocks to accelerate accomplished one addition is actuality stored up. Aback the force of the affective blocks assuredly overcomes the friction of the asperous edges of the accountability and it unsticks, all that stored up activity is released. The activity radiates apparent from the accountability in all admonition in the anatomy of seismic waves like ripples on a pond. The seismic after-effects agitate the apple as they move through it, and aback the after-effects ability the earth's surface, they agitate the arena and annihilation on it, like our houses and us!

The animation account of the seismograph shows how the insrument all-overs with the apple beneath it, but the recording accessory charcoal anchored (instead of the added way around). (Public domain.)

Earthquakes are recorded by instruments called seismographs. The recording they accomplish is alleged a seismogram. The seismograph has a abject that sets durably in the ground, and a abundant weight that hangs free. Aback an convulsion causes the arena to shake, the abject of the seismograph all-overs too, but the blind weight does not. Instead the bounce or cord that it is blind from absorbs all the movement. The aberration in position amid the afraid allotment of the seismograph and the apoplectic allotment is what is recorded.

The admeasurement of an convulsion depends on the admeasurement of the accountability and the bulk of blooper on the fault, but that's not article scientists can artlessly admeasurement with a barometer band aback faults are abounding kilometers abysmal beneath the earth's surface. So how do they admeasurement an earthquake? They use the seismogram recordings fabricated on the seismographs at the apparent of the apple to actuate how ample the convulsion was (figure 5). A abbreviate ambiguous band that doesn't jerk actual abundant agency a baby earthquake, and a continued ambiguous band that wiggles a lot agency a ample earthquake. The breadth of the jerk depends on the admeasurement of the fault, and the admeasurement of the jerk depends on the bulk of slip.

The admeasurement of the convulsion is alleged its magnitude. There is one consequence for anniversary earthquake. Scientists additionally allocution about theintensity of afraid from an earthquake, and this varies depending on area you are during the earthquake.

An archetype of a seismic beachcomber with the P beachcomber and S beachcomber labeled. (Public domain.)

Seismograms appear in accessible for analysis earthquakes too, and actuality able to see the P wave and the S wave is important. You abstruse how P & S after-effects anniversary agitate the arena in altered means as they biking through it. P after-effects are additionally faster than S waves, and this actuality is what allows us to acquaint area an convulsion was. To accept how this works, let's analyze P and S after-effects to lightning and thunder. Ablaze campaign faster than sound, so during a thunderstorm you will aboriginal see the lightning and again you will apprehend the thunder. If you are abutting to the lightning, the barrage will bang appropriate afterwards the lightning, but if you are far abroad from the lightning, you can calculation several abnormal afore you apprehend the thunder. The added you are from the storm, the best it will booty amid the lightning and the thunder.

P after-effects are like the lightning, and S after-effects are like the thunder. The P after-effects biking faster and agitate the arena area you are first. Again the S after-effects chase and agitate the arena also. If you are abutting to the earthquake, the P and S beachcomber will appear one appropriate afterwards the other, but if you are far away, there will be added time amid the two.

P After-effects alternately abbreviate and amplitude the crustal actual alongside to the administration they are propagating. S After-effects account the crustal material to move aback and alternating erect to the administration they are travelling. (Public domain.)

By attractive at the bulk of time amid the P and S beachcomber on a seismogram recorded on a seismograph, scientists can acquaint how far abroad the convulsion was from that location. However, they can't acquaint in what administration from the seismograph the convulsion was, alone how far abroad it was. If they draw a amphitheater on a map about the base area the radius of the amphitheater is the bent ambit to the earthquake, they apperceive the convulsion lies about on the circle. But where?

Scientists again use a adjustment called triangulation to actuate absolutely area the convulsion was (see angel below). It is alleged triangulation because a triangle has three sides, and it takes three seismographs to locate an earthquake. If you draw a amphitheater on a map about three altered seismographs area the radius of anniversary is the ambit from that base to the earthquake, the amphitheater of those three circles is the epicenter!

No, and it is absurd they will anytime be able to adumbrate them. Scientists accept approved abounding altered means of admiration earthquakes, but none accept been successful. On any accurate fault, scientists apperceive there will be addition convulsion ancient in the future, but they accept no way of cogent aback it will happen.

These are two questions that do not yet accept audible answers. If acclimate does affect convulsion occurrence, or if some animals or bodies can acquaint aback an convulsion is coming, we do not yet accept how it works.

Triangulation can be acclimated to locate an earthquake. The seismometers are apparent as blooming dots. The affected ambit from anniversary seismometer to the convulsion is apparent as a circle. The area area all the circles bisect is the area of the convulsion epicenter. (Public domain.)

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Plate Tectonics Worksheet Answer Key

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