Shifts in geological layers on different sides of a fault...
The rocks on one side move with respect to the rocks on the other side.
No single change occurs before all earthquakes.
before shokes
seismic gap
Seismographs cannot measure volcanoes. When you research about seismographs, it may show thing about volcanoes. This is because right before a volcano erupts, it can cause little earthquakes and seismographs measure earthquakes!
Tectonic plates.
There have not been any eruptions though rare earthquakes have occurred before.
Marriage records are available to the general public. Between 1952 and 1996, marriage records were maintained by the Georgia Division of Health. Copies of marriage records that occurred before 1952 and after 1996 can be obtained from the Probate Court in the county where the marriage occurred.
The historical record of earthquakes is very slim. Earthquakes happened thousands of years before man began keeping records. There are some historical evidence of past earthquakes and the ruins they left so they did happen. No one can tell you when the first one happened.
They can calculate intensity based on how the earthquake was felt at different places and what damage occurred from old newspaper reports and other historic documents.
The largest landslide on record occurred on May 18, 1980 when the north face of Mount St. Helens slid away just a few seconds before the volcano's historic eruption. Other, larger landslides probably occurred before records were kept of such things.
That is impossible to determine. The United States averages over 1000 tornadoes every year, many of them occurred before we started keeping records of them.
No single change occurs before all earthquakes.
before shokes
Given that the eruption of Mt Lamington occurred long before written records or human habitation, it is unknown, but unlikely whether it came as a shock.
to compare between the answers the scientist is going to get after so the scientist is compare before and after
earthquakes that immediately follow a major earthquake are called "aftershocks" as to small earthquakes before large earthquakes are called "foreshocks".
The earthquakes are generated by magma forcing its way though and fracturing rock.