Guessanym

Are these nodes
actually related?

earthquake

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Guessanym
Earthquake

earthquake

Depth
2
Use as Polynym Mark Unseen (✓)
Keyword:   both
Context:   relation 1.7:1). The differences in travel time from the epicenter to the observatory are a measure of the distance and can be used to image both sources of earthquakes and structures within the Earth.
Nodes:
    • sources of earthquakes
    • structures within the Earth
Full context:   Every earthquake produces different types of seismic waves, which travel through rock with different velocities: Propagation velocity of the seismic waves through solid rock ranges from approx. 3 km/s (1.9 mi/s) up to 13 km/s (8.1 mi/s), depending on the density and elasticity of the medium. In the Earth's interior, the shock- or P waves travel much faster than the S waves (approx. relation 1.7:1). The differences in travel time from the epicenter to the observatory are a measure of the distance and can be used to image both sources of earthquakes and structures within the Earth. Also, the depth of the hypocenter can be computed roughly.
— Marked as seen, but always open to review —
Polynym
Bagua

natural disaster

Source
I Ching
Area
Philosophy
Mode
type
Depth
8
User
scotty
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