Earth Quakes Flashcards

1
Q

What is the difference between the hypocenter and the epicenter of an earthquake?

A

The hypocenter (focus) is the point within the Earth where the rupture begins, while the epicenter is the point on the surface directly above it.

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2
Q

How do intensity and magnitude differ in describing an earthquake?

A

Intensity measures ground shaking and damage at specific locations, whereas magnitude quantifies the energy released at the source, using data from seismic records.

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3
Q

What happens when earthquake magnitude increases by 2 units?

A

The seismic wave amplitude increases about 10-fold (roughly 100-fold overall for 2 units) and the energy released increases roughly 30–32 times per unit, resulting in around 1,000 times more energy for a 2-unit jump.

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4
Q

How does earthquake frequency relate to magnitude?

A

Larger magnitude earthquakes occur less frequently, while smaller ones are much more common.

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5
Q

What are the main types of seismic waves?

A

Seismic waves include body waves (P and S waves) that travel through the interior and surface waves (Rayleigh and Love waves) that travel along the Earth’s surface.

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6
Q

What are the characteristics of P waves?

A

P waves are compressional waves that are the fastest, arriving first at a seismic station, and can travel through solids, liquids, and gases.

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7
Q

How do S waves differ from P waves?

A

S waves are shear waves that arrive after P waves, travel only through solids, and typically have a larger amplitude.

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8
Q

Why are surface waves particularly destructive?

A

Surface waves have the slowest velocity but the highest amplitude, causing extensive ground shaking and damage near the surface.

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9
Q

What does the elastic rebound theory explain?

A

It explains that strain energy builds in rocks until they reach their elastic limit, after which they rupture suddenly, releasing stored energy as an earthquake.

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10
Q

How are earthquakes recorded?

A

Seismographs record the motion of seismic waves, and the resulting records—seismograms—help determine the earthquake’s location, magnitude, and fault type.

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11
Q

How is the epicenter of an earthquake determined?

A

By using the time difference between P and S wave arrivals at multiple stations and applying triangulation with travel-time curves.

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12
Q

What are foreshocks and aftershocks?

A

Foreshocks are smaller quakes that sometimes occur before a mainshock, while aftershocks follow the main event, gradually decreasing in magnitude and frequency.

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13
Q

How do megathrust earthquakes generate tsunamis?

A

They occur at subduction zones where enormous thrust faults rupture, causing significant vertical displacement of the seafloor that displaces large volumes of water, triggering tsunamis.

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14
Q

What are some challenges in predicting earthquakes?

A

Predicting the exact time of earthquakes is difficult; however, long-range forecasts use seismic gaps, strain estimates from plate movements, and paleoseismology to assess risk.

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15
Q

Where do most earthquakes occur globally?

A

Earthquakes are concentrated along plate boundaries, particularly in earthquake belts like the Pacific “Ring of Fire” where subduction, transform, and convergent boundaries exist.

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