Color and Lenses - Thomas C. Cario Middle School
... AN EARTHQUAKE BEGINS AT THE… 10.________: The point beneath Earths surface where rock that is under stress breaks. 11.________: The point on the surface of the Earth directly above the focus. ...
... AN EARTHQUAKE BEGINS AT THE… 10.________: The point beneath Earths surface where rock that is under stress breaks. 11.________: The point on the surface of the Earth directly above the focus. ...
Questions: What are Earthquakes
... 1. ___________ is a change in shape of rock due to stress. 2. ___________ is the sudden return of rock that has been deformed to its original undeformed state. 3. Where do earthquakes occur? 4. What is the difference between p and s waves? 5. Describe the three types of plate motion and the faults t ...
... 1. ___________ is a change in shape of rock due to stress. 2. ___________ is the sudden return of rock that has been deformed to its original undeformed state. 3. Where do earthquakes occur? 4. What is the difference between p and s waves? 5. Describe the three types of plate motion and the faults t ...
Earthquake Locations/Terminology Elastic Rebound Theory Seismic
... S-Waves: Second fastest, side to side, travel through solids Surface Waves: Slowest waves, very destructive, role on surface ...
... S-Waves: Second fastest, side to side, travel through solids Surface Waves: Slowest waves, very destructive, role on surface ...
HOTSPOTS
... P-WAVES can travel through any material, but they bend when moving through liquid. This bending creates “SHAWDOW ZONE” S-WAVES can only travel through solids, so they create a much larger “shadow zone” on the other side of the Earth. ...
... P-WAVES can travel through any material, but they bend when moving through liquid. This bending creates “SHAWDOW ZONE” S-WAVES can only travel through solids, so they create a much larger “shadow zone” on the other side of the Earth. ...
Earthquakes
... landslides are caused. 8: The ground is moves like a wave, buildings fall and massive damage. ...
... landslides are caused. 8: The ground is moves like a wave, buildings fall and massive damage. ...
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.