Free Online Flashcard Deck

5 Earthquakes and Seismic Hazards Free Online FlashCards

Study 5 Earthquakes and Seismic Hazards with 12 free online flashcards. Review key terms, definitions, and concepts with this interactive flashcard deck.

12 cards
01
Front

What is a fault in the context of earthquakes?

Back

A fault is a fracture in rock where sudden slip can release energy and cause an earthquake.

02
Front

How do P waves move, and when do they arrive?

Back

P waves compress and expand material in the direction they travel. They are the fastest seismic waves and arrive first.

03
Front

How do a seismometer and a seismogram differ?

Back

A seismometer detects ground motion; a seismogram is the recording it produces.

04
Front

What is liquefaction during an earthquake?

Back

Liquefaction occurs when strong shaking makes some water-saturated, loose sediments temporarily lose strength, causing settlement or ground movement.

05
Front

How do earthquake hazard and risk differ?

Back

Hazard is the potential for damaging shaking or related effects; risk concerns the expected harm to people and property, which increases when exposure or vulnerability is greater.

06
Front

What should you do during shaking using Drop, Cover, and Hold On?

Back

Drop to your hands and knees, cover your head and neck under sturdy shelter if available, and hold on until the shaking stops.

07
Front

What is an earthquake’s focus?

Back

The focus, or hypocenter, is the underground point where an earthquake rupture begins.

08
Front

What is an earthquake’s epicenter?

Back

The epicenter is the point on Earth’s surface directly above the earthquake’s focus.

09
Front

How do S waves move, and what materials can they travel through?

Back

S waves move material perpendicular to their direction of travel. They travel through solids, not liquids, and arrive after P waves.

10
Front

Why can surface waves be especially damaging?

Back

Surface waves move along or near Earth’s surface and often produce strong, damaging ground motion.

11
Front

How do seismic-wave arrival times help locate an earthquake?

Back

The time difference between P-wave and S-wave arrivals helps estimate a station’s distance from the earthquake source; readings from multiple stations narrow down its location.

12
Front

How do earthquake magnitude and intensity differ?

Back

Magnitude describes an earthquake’s size; intensity describes the shaking and effects at a particular place.