-
motions ****ociated to
microseisms does not
generally exceed 10 micrometers. As
noted early in the
history of seismology,
microseisms are very well detected...
-
further classification of
ambient noise include secondary microseisms,
primary microseisms, and
seismic hum,
based on
different range of frequencies....
-
Seismograms can
record many things, and
record many
little waves,
called microseisms.
These tiny
events can be
caused by
heavy traffic near the seismograph...
-
sources such as volcanoes,
plate tectonics, glaciers, rivers,
oceanic microseisms, and the atmosphere; and
artificial processes such as explosions. Paleoseismology...
- (less than
several hundred meters depth)
regions of the
global ocean.
Microseisms were
first reported in
about 1900, and
seismic records provide long-term...
-
surface waves. Low
frequency waves (below 1 Hz) are
commonly called microseisms and high
frequency waves (above 1 Hz) are
called microtremors. Primary...
- Longuet-Higgins. Longuet-Higgins
introduced the
theory of the
origin of
microseisms and is the
inventor of "rhombo blocks", a
mathematical toy consisting...
-
surface waves,
fluidity of the Earth's core,
generation and
propagation of
microseisms,
submarine explosion seismology,
marine gravity surveys,
bathymetry and...
-
destructive lahar.
Signs of
reactivation began to
occur in 1961 in the form of
microseisms; previously,
several specialists warned that the Irazú
Volcano could...
- low-frequency
loudspeaker mounted on top. They
noted their similarity to
microseisms observed on seismographs, and
correctly hypothesized that
these signals...
