earthquakes Flashcards
seismic gap theory
A seismic gap is a segment of an active fault known to produce significant earthquakes, that has not slipped in an unusually long time when compared with other segments along the same structure. Seismic gap hypothesis/theory states that, over long periods of time, the displacement on any segment must be equal to that experienced by all the other parts of the fault.[1] Any large and longstanding gap is therefore considered to be the fault segment most likely to suffer future earthquakes.
gas measurement
measuring radon gas, increase then sudden decrease immediately before earthquake occurs
deep earthquake
300-700km
intermediate earthquake
70-300km
shallow earthquake
0-70km
epicentre
point on earth surface above focus
focus
origin of earthquake
stress:
a force that can cause a change in an object or a physical body
strain:
strain is the change in the form or shape of the object or physical body on which stress is applied.
density of earth
5.5g/cm^3
density of surface rocks
2.7 – 2.9 g/cm^3
density of inner core
12-15 g/cm^3