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chapter 12 – earthquakes
chapter 12 – earthquakes

... a. convergent oceanic plates i. Two plates are moving towards each other with one plate subducting or sinking under the other plate ii. As the top plate scrapes across the bottom plate, earthquakes occur. b. divergent oceanic plates i. Two plates are moving away from each other. ii. The spreading mo ...
Presentation
Presentation

Lecture PowerPoint Slides
Lecture PowerPoint Slides

... in composition and Earth’s core is primarily composed of iron + nickel Similar in composition to Earth’s mantle ...
Earthquake Epicenters Plate Tectonics
Earthquake Epicenters Plate Tectonics

PHY1025F-2014-V01-Oscillations-Lecture Slides
PHY1025F-2014-V01-Oscillations-Lecture Slides

Earth Science Day 04: Earthquakes
Earth Science Day 04: Earthquakes

... Shaking and trembling of the earth’s crust. More than 1,000,000 occur a year or one every 30 seconds Faulting is the most common cause Earthquakes continue until all the energy is absorbed into the surrounding Earth’s material (dirt, rocks, buildings, etc.) TSUNAMIS- an earthquake occurs on the ocea ...
Arthropod Crossword Puzzle
Arthropod Crossword Puzzle

Arthropod Crossword Puzzle
Arthropod Crossword Puzzle

... arachnid's body that lies between the head and the abdomen. 7. A class of myriapod arthropods having the body segments containing two pairs of legs. 9. Bloodsucking arachnids that are larger than the related mites. 12. Excretory glands in some crustaceans near the base of the large antennae. 13. Art ...
18.12 FORCED-DAMPED VIBRATIONS
18.12 FORCED-DAMPED VIBRATIONS

... The plot of magnification factor against the ratio of frequencies (w /wn) for different values of z is shown in Fig. 18.22(a). The curves show that as the damping increases or z increases, the maximum value of the magnification factor decreases and vice-versa. When there is no damping (z = 0), it re ...
Section 19.1 Forces Within Earth
Section 19.1 Forces Within Earth

... the damage and loss of life. ...


File
File

Types of seismic waveS
Types of seismic waveS

... Secondary waves (S-waves) are shear waves that are transverse in nature. These waves arrive at seismograph stations after the faster moving P waves during an earthquake and displace the ground perpendicular to the direction of propagation. Depending on the propagational direction, the wave can take ...
Exercise 3 - Earthquake Hazards
Exercise 3 - Earthquake Hazards

MS Word Technical Paper Template - PBD-III
MS Word Technical Paper Template - PBD-III

Chapter: Chapter 5: Earthquakes and Earth`s Interior
Chapter: Chapter 5: Earthquakes and Earth`s Interior

ppt file - Angelfire
ppt file - Angelfire

earthquake
earthquake

... 8.2 Measuring Earthquakes Earthquake Waves  Body Waves • Identified as P waves or S waves • P waves - Are push-pull waves that push (compress) and pull (expand) in the direction that the waves travel - Travel through solids, liquids, and gases - Have the greatest velocity of all earthquake waves ...
Volcanoes and Igneous Activity Earth
Volcanoes and Igneous Activity Earth

Volcanoes and Igneous Activity Earth
Volcanoes and Igneous Activity Earth

TRAVEL TIME CURVE USED TO FIND VELOCITY AT DEPTH
TRAVEL TIME CURVE USED TO FIND VELOCITY AT DEPTH

... S WAVES CANNOT TRAVEL THROUGH LIQUID ( = 0) LIKE OUTER CORE IN CRUST, VP ABOUT 6.5 km/s - 14,650 miles/hr ...
Richter scale - Plain Local Schools
Richter scale - Plain Local Schools

earthquake - SPS186.org
earthquake - SPS186.org

File
File

... characteristics and properties of sound waves. Dolphins, sperm whales, and orca whales use echolocation to navigate and detect prey in dark, murky waters. Bats also use echolocation to detect prey. Elephants produce infrasound waves, which travel partially through the ground. They can detect these s ...
Earthquakes Terminology of Earthquakes Elastic Rebound Theory
Earthquakes Terminology of Earthquakes Elastic Rebound Theory

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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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