Appendix 1
TABLE 1
Terms used on Estimation Charts, Diagrams And in
the Text
b Apparent explosions or sharp bursts of tremor. not
affecting tremor amplitudes before or after event.
R Volcanic tremor, narrow frequency range 1 to 3
c/s.
Rb Apparent explosions or sharp burst of tremor
simultaneous with start of tremor.
Rc Chuffing tremor, appears apparently during dying
phase of activity.
Rd Volcanic tremor of wide frequency range, sometimes
with rapidly varying power spectrum.
Rf Volcanic tremor of mixed high (9 to 12 c/s) and
low (1 to 3 c/s) frequencies, occurring for short
periods.
Rh Harmonic tremor, as (Wh) on all records made
before 9.9.67 and known as whistle phenomena. A high
frequency harmonic of R, directly related to gas emissions
of the volcano concerned.
L Local earthquake distance between 30 and I000 km,
indicated by time interval between P and S arrivals.
VL Very local earthquake distance less than 30 km,
indicated by time interval between P and S arrivals.
P Deep earthquake. P sharp compared to S arrival.
W Wind and rain.
X Instrumental, not seismic.
M Microseisms, as for oceans and lakes.
A Artificial man made noises.
Seismic Events Interpreted as of Volcanic Origin
with Relation to Frequency Spectrum
1 c/s to 3 c/s Volcanic tremor (R), dominant
frequency 1 c/s to 2 c/s.
1 c/s to 5 c/s Apparent explosions (b and Rb),
dominant frequency 1 c/s tu 2 c/s
1 c/s to 7 c/s Volcanic tremor (Rd), dominant
frequencies between 1 c/s and 3 c/s.
9 c/s to 12 c/s Volcanic tremor of high frequency
(Rf) normally superimposed on tremor (R).
Average Amplitude of Volcanic Tremor
(R)
Amplitude ranges of (R) mentioned in text and in Figures 2,
3 and 5, are readily taken from the initial evaluation
charts. The approximate equivalent amplitude of the ground
motion at 2 c/s from February 20, 1966.
High: 0.6 microns and above.
Medium: 0.4 to 0.6 microns.
Low: up to 0.4 microns.
These levels were determined by test signals between 40 and
400 microvolts fed Into the tape seismograph input, and the
corresponding ground amplitudes have been taken from the
calibration charts as shown in the manual for the Willmore
seismometer.
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