ಸಣ್ಣ ಭೂಕಂಪ,

microseisms's Usage Examples:

Low frequency waves (below 1 Hz) are commonly called microseisms and high frequency waves (above 1 Hz) are called microtremors.

record many things, and record many little waves, called microseisms.

infrasonic microbaroms into the atmosphere, and seismic signals called microseisms coupled through the ocean floor to the solid Earth.

They noted their similarity to microseisms observed on seismographs, and correctly hypothesized that these signals.

energy is also present as pressure oscillations at great depth, producing microseisms.

reflection of a swell at the shore, and are the source of microbaroms and microseisms.

He was able to show that "microseisms were traveling, rather than standing waves and that their origins could.

microseismology The study of microseisms.

"A theory of the origin of microseisms".

to the event, as early as July 6, the area was experiencing unusual microseisms recorded at seismic station of the Commission on Volcanology (COMVOL).

but also used as a tool for investigating nature and source regions of microseisms as well as locating and tracking volcanic tremor and analyzing complex.

amplitude of ground motions associated to microseisms does not generally exceed 10 micrometers.

“Comparative spectra of microseisms and swell”, Bull.