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EARTHQUAKES & VOLCANOES
EARTHQUAKES & VOLCANOES

... Seismology is the study of earthquakes and seismic waves that move through and around the earth. A seismologist is a scientist who studies earthquakes and seismic waves. What Are Seismic Waves? • Seismic waves are the waves of energy caused by the sudden breaking of rock within the earth or an explo ...
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Chapter 6 Review – Earthquakes

... A geologist has data about an earthquake from two seismographic stations. Is this enough information to determine the location of the epicenter? Why or why not? ...
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Earthquake_Revised

... When plates move, stress is put on rocks. A rubber band (just like rocks) can only be stretched so far until it breaks; this is known as the elastic limit. Earthquakes are the Earth vibrating. ...
Unit C UA pt B - LD Industries
Unit C UA pt B - LD Industries

... ________ - relating to waves that travel through Earth as a result of explosions or earthquakes ________ - a large concentration of petroleum confined between layers of impermeable shale ________ - an instrument that records seismic waves ________ - a submerged ridge of rock, sand, or coral that ris ...
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... View, California, has a highly qualified staff of about 20 geophysicists and computer experts. 3DGeo’s mission is to become the leading Internet service provider for seismic data processing in the oil and gas exploration industry. 3DGeo has developed a portfolio of technically superior proprietary s ...
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... The Richter magnitude scale was developed in 1935 by Charles F. Richter of the California Institute of Technology as a mathematical device to compare the size of earthquakes. The Richter scale assigns a magnitude number to quantify the energy released by an earthquake. This scale is a base-10 logari ...
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... ____________________ from earthquakes travels through Earth. The energy travels as seismic waves which are ______________________caused by earthquakes. Seismic waves from even small earthquakes can be recorded by sensitive instruments around the world.  Focus and Epicenter All earthquakes start ben ...
< 1 ... 16 17 18 19 20 21 22 23 24 ... 27 >

Seismic communication



Seismic communication, sometimes called vibrational communication, describes the conveying of information through seismic vibrations of the substrate. The substrate may be the earth, a plant stem or leaf, the surface of a body of water, a spider’s web, a honeycomb, or any of the myriad types of soil substrates. Seismic cues are generally conveyed by Rayleigh waves generated through vibrations on the substrate, or acoustical waves that couple with the substrate. Vibrational communication is an ancient sensory modality and it is widespread in the animal kingdom where it has evolved several times independently. It has been reported in mammals, birds, reptiles, amphibians, insects, arachnids, crustaceans and nematode worms. Vibrations and other communication channels are not necessarily mutually exclusive, but can be used in multi-modal communication.
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