An aftershock is a smaller earthquake that occurs after a previous large earthquake, known as the main shock. Aftershocks typically occur near the fault zone where the main shock rupture occurred.
In seismology, the hypocenter is the point within the Earth where an earthquake rupture starts.
A comprehensive analysis of seismic hazard, its significance, and methods to assess earthquake risks.
An in-depth exploration of seismic waves, their types, mechanisms, significance, and impact on Earth sciences and engineering.
Detailed article on seismographs, their historical context, types, key events, importance, applications, related terms, and more.
Seismology is the scientific study of earthquakes and the propagation of seismic waves through the Earth or other planet-like bodies.
An in-depth exploration of the Seismometer, its types, historical context, key events, and applications.
