EARTHQUAKES AND EARTHS INTERIOR Flashcards
What is a shadow zone?
an area in the subsurface of the Earth where seismic waves are not seen
What rock makes up the oceanic crust?
basalt
How can geologists know what the interior of the Earth looks like when we can’t see it?
Geologists use a variety of methods to “see” the interior of the Earth including the study of seismic waves and the magnetic field.
Which peripheral hazard of earthquakes caused the damage shown in the photo?
Landslide
Aftershocks are usually
much weaker than the mainshock.
Which type of wave is a compressional body wave?
P-wave
What rock makes up the oceanic crust?
basalt
Which of the following is a good technique for building safer structures in an earthquake zone?
Use wood-frame construction.
Interpret the travel-time curve shown. Approximately how many minutes elapsed between the arrival of the first P-wave and the arrival of the first S-wave at Station 3?
7
The Earth’s magnetic field is thought to be a direct result of ________.
convection in the outer core.
The locations of major earthquakes
are usually along plate boundaries.
What rock makes up the continental crust?
granite
The inner core is ________.
solid.
What rock makes up the oceanic crust?
basalt
The 2010 Haiti earthquake was so destructive because
of poor construction standards that caused many buildings to collapse.
To find the location of an earthquake’s epicenter, you need to calculate the distance from the epicenter to ____ different seismometer stations.
3
A tsunami
may be just a broad, gentle swelling out at sea but grows as it approaches shore.
The earthquake foci pattern east of Australia and just north of New Zealand indicates which tectonic setting?
Convergent plate boundary
One difference between P- and S-waves is that
only P-waves can travel through a liquid.