Mention106833
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| so:text | Earthquakes generate elastic waves when one block of material slides against another; the break between the two blocks being called a fault. Explosions generate elastic waves by an impulsive change in volume in the material. Small explosive charges are used in controlled-source seismic experiments in which the waves penetrate only a few kilometres into the earth. (en) |
| so:isPartOf | https://en.wikiquote.org/wiki/David_Gubbins |
| so:description | Seismology and Plate Tectonics (1990) (en) |
| qkg:hasContext | qkg:Context52344 |
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