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Earthquakes - PH - teacher
Earthquakes - PH - teacher

Lab 3 - Geologic Structures, Maps, and Block Diagrams
Lab 3 - Geologic Structures, Maps, and Block Diagrams

Density
Density

The Senses
The Senses

vibrations and waves
vibrations and waves

Seismic waves - Albert
Seismic waves - Albert

Study guide - Earthquakes, volcanoes, fault types
Study guide - Earthquakes, volcanoes, fault types

... b. Most earthquakes have magnitudes too SMALL to be felt by humans—3.0 to 4.9 on the Richter scale. 3. The modified MERCALLI intensity scale describes earthquake intensity based on structural and geologic damage. 4. LIQUIFACTION shaking from an earthquake can make wet soil act like a liquid. 5. Ocea ...
Earthquakes and Plate Boundaries
Earthquakes and Plate Boundaries

2-Unit4Part2EarthsInteriors
2-Unit4Part2EarthsInteriors

EARTHQUAKES 22.5
EARTHQUAKES 22.5

... Surface Waves • Develop when seismic waves reach the earth’s surface. • Move more slowly than P waves or S waves. • Produce larger ground movements and greater damage. • Some are transverse, others are similar to ocean waves. ...
Document
Document

chpt 8Earthquake and volcanoes
chpt 8Earthquake and volcanoes

...  Elastic ...
Ch. 11 Earthquakes
Ch. 11 Earthquakes

... This theory states --- sudden return of elastically deformed rock to its undeformed shape. If the fault is locked, stress increases. When stress reaches passed a certain point, the rocks fracture, separate at weakest point, and spring back or rebound, to original shape. As they fracture and slip the ...
1: How far can seismic waves carry energy released from an
1: How far can seismic waves carry energy released from an

MECHANICAL VIBRATIONS EXPERIMENT
MECHANICAL VIBRATIONS EXPERIMENT

Earthquake Text Worksheet
Earthquake Text Worksheet

Earth`s interior volc eq2
Earth`s interior volc eq2

Earthquake destruction and seismic waves Page 1 of 3 I. Factors
Earthquake destruction and seismic waves Page 1 of 3 I. Factors

EarthquakesHnrs2
EarthquakesHnrs2

Animals - TeachingCave.com
Animals - TeachingCave.com

... evening. Their spots help camouflage them to get within 10-30 metres of their prey. Cheetahs are very fast but they cannot run for a long period of time. ...
What is an Earthquake
What is an Earthquake

Section 20.1 - CPO Science
Section 20.1 - CPO Science

...  A moving line of grocery carts is a good analogy of a moving lithospheric plate.  Although a plate may be moving as a single unit, its boundaries act like they were made of many small sections like the line of carts. ...
EARTHQUAKES OR EXPLOSIONS?
EARTHQUAKES OR EXPLOSIONS?

Earthquakes( Distribution)
Earthquakes( Distribution)

... Everyday there are several 100 earthquakes across the globe. All of the Earths major earthquake zones are found along the faults at plate boundaries. What are earthquakes? Seismic waves are the vibrations of energy created from the plate movement which cause earthquakes. These different waves can be ...
answer key
answer key

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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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