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Fig. 5. Photographs showing earthquake surface faults or cracks observed from the field survey.
We cannot identify any phase discontinuities showing appearance of earthquake surface faults along either the MFT or other faults.
Earthquake surface ruptures appeared along these faults and on the Aso volcanic edifice, which in turn generated landslides.
In a series of simulations, the team bombarded the rings with the equivalent of earthquake surface waves of standard frequencies ranging from 30 to 150 hertz, or vibrations per second.
The conflict between the historical catalogue and earthquake surface ruptures is an opportunity to refine the date of occurrence of these geological events.
In the western region of Aso caldera, earthquake surface ruptures, hereafter referred to as surface ruptures, appeared on the Kitamukiyama ridge.
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The blue circles indicate the epicenter locations of the 1942 and 1958 earthquakes (surface magnitudes of 7.9 and 7.8, respectively) based on Mendoza and Dewey (1984).
At the 2016 Kumamoto earthquake, intensive surface ruptures were found along the Futagawa fault, but surface ruptures along the northernmost part of the Hinagu fault were also observed [e.g., GSI (Geospatial Information Authority of Japan 2016)].
When an earthquake's surface waves hit the foundation of a building, it causes a similar motion.
It is known that during a pure strike-slip earthquake, the surface may not experience any significant vertical displacements.
It is well known that during the occurrence of an earthquake, the surface experiences horizontal as well as vertical displacements, depending upon the type of rupture fault.
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