The most complete information about the recurrence interval of earthquakes on the Hayward Fault comes from: a eyewitness accounts and newspaper articles b examining damage in very old buildings c radiometric dates from offset material found in trenches in the fault zone d comparing with the recurrence interval on other strike-slip faults
The most complete information about the recurrence interval of earthquakes on the Hayward Fault comes from:
| a |
eyewitness accounts and newspaper articles |
|
| b |
examining damage in very old buildings |
|
| c |
radiometric dates from offset material found in trenches in the fault zone |
|
| d |
comparing with the recurrence interval on other strike-slip faults |
An earthquake is defined as a sudden release of energy stored in rocks. The majority of the earthquakes are located on the tectonic plate boundaries of the world. It is the result of a slip movement in the tectonic plates.
The recurrence interval is the average time period or interval between earthquake occurrences in a fault. The probability of the occurrence of an earthquake can be predicted by analyzing the recurrence intervals.
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