Meanwhile, the U.S. military
funded development of new, advanced seismometers to help monitor Soviet
nuclear tests. By the late 1950s, the World Wide Standardized Seismographic
Network had been deployed in over 40 countries.
The network operated 24
hours/day (because the Soviets didn't announce tests in advance).
The network recorded occasional
nuclear tests, but also seismic waves from every moderate to strong
earthquake anywhere in the world.
Data were made available
to seismologists, permitting more accurate location of earthquakes.
By the early 1960s, scientists
recognized that earthquakes occur mainly in narrow belts along oceanic
trenches, ridges, and fracture zones, and also throughout Alpine-Himalayan
belt.
By 1967, most of the theory
of plate tectonics was in place: The outer shell of Earth, called
its lithosphere, is broken up into numerous rigid plates. New
plate material forms where plates spread apart, and is consumed where
plates converge. Earthquakes (and active volcanoes) are concentrated
at the boundaries of these plates.