-
motions ****ociated to
microseisms does not
generally exceed 10 micrometers. As
noted early in the
history of seismology,
microseisms are very well detected...
-
record many things, and
record many
little waves,
called microseisms.
These tiny
microseisms can be
caused by
heavy traffic near the seismograph, waves...
- (less than
several hundred meters depth)
regions of the
global ocean.
Microseisms were
first reported in
about 1900, and
seismic records provide long-term...
- low-frequency
loudspeaker mounted on top. They
noted their similarity to
microseisms observed on seismographs, and
correctly hypothesized that
these signals...
-
seismic sources such as volcanic, tectonic, glacial, fluvial,
oceanic microseism, atmospheric, and
artificial processes such as
explosions and
human activities...
- Gr**** σείειν (seíein), σεισμός (seismós), σεῖστρον (seîstron) aseismic,
microseism, microseismic, paleoseismology, seism, seismic, seismogram, seismograph...
-
surface waves. Low
frequency waves (below 1 Hz) are
commonly called microseisms and high
frequency waves (above 1 Hz) are
called microtremors. Primary...
-
surface waves,
fluidity of the Earth's core,
generation and
propagation of
microseisms,
submarine explosion seismology,
marine gravity surveys,
bathymetry and...
-
further classification of
ambient noise include secondary microseisms,
primary microseisms, and
seismic hum,
based on
different range of frequencies....
- Longuet-Higgins, M. S. (27
September 1950). "A
Theory of the
Origin of
Microseisms".
Philosophical Transactions of the
Royal Society A: Mathematical, Physical...
