Vocab Flashcards
Ring of Fire
The Ring of Fire is a region around much of the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur.
Strike-slip fault
Strike-slip tectonics is concerned with the structures formed by, and the tectonic processes associated with, zones of lateral displacement within the Earth’s crust or lithosphere.
Normal fault
normal fault - a dip-slip fault in which the block above the fault has moved downward relative to the block below.
Reverse fault
A reverse fault is the opposite of a normal fault—the hanging wall moves up relative to the footwall.
P-waves
A P wave is one of the two main types of elastic body waves, called seismic waves in seismology.
S-waves
In seismology, S waves, secondary waves, or shear waves are a type of elastic wave and are one of the two main types of elastic body waves, so named because they move through the body of an object, unlike surface waves.
epicenter
the point on the earth’s surface vertically above the focus of an earthquake.
focus
The focus is the place inside Earth’s crust where an earthquake originates.
Richter magnitude scale
The Richter scale – also called the Richter magnitude scale or Richter’s magnitude scale – is a measure of the strength of earthquakes, developed by Charles F. Richter and presented in his landmark 1935 paper, where he called it the “magnitude scale”.
explosive volcano
In volcanology, an explosive eruption is a volcanic eruption of the most violent type.
nonexplosive volcano
Nonexplosive eruptions are the most common type of volcanic eruptions.
Krakatoa
Krakatoa, also transcribed Krakatau, is a caldera in the Sunda Strait between the islands of Java and Sumatra in the Indonesian province of Lampung.
Yellowstone supervolcano
The Yellowstone Caldera is a volcanic caldera and supervolcano in Yellowstone National Park in the Western United States, sometimes referred to as the Yellowstone Supervolcano.
San Andreas fault
The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers through California.
Mid-oceanic ridge
A mid-ocean ridge is a seafloor mountain system formed by plate tectonics. It typically has a depth of ~ 2,600 meters and rises about two kilometers above the deepest portion of an ocean basin.