Seismological Society of America was created in 1906.
The distance between a seismological recording station and the earthquake source is determined from the arrival times of seismic waves at the station. By comparing the arrival times of P-waves and S-waves, seismologists can calculate the distance to the earthquake source using the difference in their arrival times.
The distance between a seismological recording station and the earthquake source is determined from the arrival time of P and the S waves. P waves are faster than S waves and surface waves.
Free Anti Revolutionary Party was created in 1898.
John Tuzo Wilson used a combination of geological evidence, seismological data, and geomagnetic observations to develop the theory of plate tectonics. By integrating these different lines of evidence, he proposed a model where the Earth's lithosphere is divided into several rigid plates that move and interact along their boundaries.
Sound waves are not characteristic of earthquakes. Earthquakes are typically associated with seismological waves, such as primary (P) waves, secondary (S) waves, and surface waves, that travel through the Earth's crust. Sound waves, on the other hand, are mechanical waves that require a medium, like air, to travel through, and are not directly related to seismic activity.
Seismological Society of Japan was created in 1880.
National Seismological Service was created in 1910.
The Violin Society of America was created in 1973.
Mineralogical Society of America was created in 1919.
The Renaissance Society of America was created in 1954.
Genetics Society of America was created in 1931.
Autism Society of America was created in 1965.
Botanical Society of America was created in 1893.
Geological Society of America was created in 1888.
Microscopy Society of America was created in 1942.
Bibliographical Society of America was created in 1904.
The Huguenot Society of America was created in 1883.