Document
... perpendicular to the direction the wave is moving. • Water (more or less) • Slinky demo ...
... perpendicular to the direction the wave is moving. • Water (more or less) • Slinky demo ...
JOUR
... factors can be calculated to determine the stability degree or condition of the emulsion. 2. An excellent improvement in electric stability versus shear rate was observed. 3. Shear rate variation causes a similar response in the filtration loss for all tested emulsions. Increasing shear rate to the ...
... factors can be calculated to determine the stability degree or condition of the emulsion. 2. An excellent improvement in electric stability versus shear rate was observed. 3. Shear rate variation causes a similar response in the filtration loss for all tested emulsions. Increasing shear rate to the ...
Earthquakes
... • Move along the Earth’s surface • Produces motion in the upper crust – Motion can be up and down – Motion can be around – Motion can be back and forth ...
... • Move along the Earth’s surface • Produces motion in the upper crust – Motion can be up and down – Motion can be around – Motion can be back and forth ...
File
... and always arrive after P waves. Side to side. (body) • Surface Waves – Cause motion mostly in the upper few KM of earth’s crust. Travel more slowly and are more destructive than body waves. Can move up and down or side to side. ...
... and always arrive after P waves. Side to side. (body) • Surface Waves – Cause motion mostly in the upper few KM of earth’s crust. Travel more slowly and are more destructive than body waves. Can move up and down or side to side. ...
HERE
... • Move much slower than the body wave- roughly speed of sound. Only 1 mile in 5 seconds (or about 700 mi/hr) • Can only travel through the crust of the Earth (surface). • These waves have the biggest amplitude (height of the wave). As a result they do the MOST damage on the surface. • Click HERE for ...
... • Move much slower than the body wave- roughly speed of sound. Only 1 mile in 5 seconds (or about 700 mi/hr) • Can only travel through the crust of the Earth (surface). • These waves have the biggest amplitude (height of the wave). As a result they do the MOST damage on the surface. • Click HERE for ...
Introduction to Lateral Force Resisting Systems
... beams. They are supported on one end only and the loads are perpendicular to the beam. As in a beam, buildings are designed for ...
... beams. They are supported on one end only and the loads are perpendicular to the beam. As in a beam, buildings are designed for ...
a. Transverse or Shear wave
... Travel through the crust of the earth and attenuate (gradually disappear); Scientists have found that attenuation occurs more slowly in older rock (like the eastern US, but more quickly in younger rock (western US) a. ...
... Travel through the crust of the earth and attenuate (gradually disappear); Scientists have found that attenuation occurs more slowly in older rock (like the eastern US, but more quickly in younger rock (western US) a. ...
2.3 VELOCITY STRUCTURE OF THE EARTH In the following years
... ScSScS (or ScS2) bounces twice at the CMB and once at the surface. Such reflections are known as multiple ScS. ScS is a more distinct arrival than PcP because the liquid core does not transmit shear waves. The SH part of the motion in the incident ScS In fact, the ray path names (SCS, etc...) are wa ...
... ScSScS (or ScS2) bounces twice at the CMB and once at the surface. Such reflections are known as multiple ScS. ScS is a more distinct arrival than PcP because the liquid core does not transmit shear waves. The SH part of the motion in the incident ScS In fact, the ray path names (SCS, etc...) are wa ...
Mechanical Waves (Chapter 17) 1. What does a wave transfer
... 5. What does “transparent” mean? Object can be seen through because all or most of light is being transmitted. 6. What does “translucent” mean? Object is somewhat see-through because some light is being transmitted. An object on the other side of a translucent material will likely appear fuzzy, with ...
... 5. What does “transparent” mean? Object can be seen through because all or most of light is being transmitted. 6. What does “translucent” mean? Object is somewhat see-through because some light is being transmitted. An object on the other side of a translucent material will likely appear fuzzy, with ...
Unit 3: Earthquake Waves Introduction
... Arrive at seismic recording stations first Can travel through solids, liquids and gases (Solids and Fluids) ...
... Arrive at seismic recording stations first Can travel through solids, liquids and gases (Solids and Fluids) ...
Chapter 19 - Earthquakes
... Builds up overtime Overcomes strength of rocks and causes movement along fractures in rock ...
... Builds up overtime Overcomes strength of rocks and causes movement along fractures in rock ...
Tsunami - Meaning,Safety
... In the past the scientific community sometimes referred to them as ‘tidal waves’ or ‘seismic sea waves’. Tsunamis are the hydrosphere’s most destructive force. They are giant waves that are caused by sudden movement of the seabed during an earthquake ...
... In the past the scientific community sometimes referred to them as ‘tidal waves’ or ‘seismic sea waves’. Tsunamis are the hydrosphere’s most destructive force. They are giant waves that are caused by sudden movement of the seabed during an earthquake ...
Shear wave splitting
Shear wave splitting, also called seismic birefringence, is the phenomenon that occurs when a polarized shear wave enters an anisotropic medium (Fig. 1). The incident shear wave splits into two polarized shear waves (Fig. 2). Shear wave splitting is typically used as a tool for testing the anisotropy of an area of interest. These measurements reflect the degree of anisotropy and lead to a better understanding of the area’s crack density and orientation or crystal alignment.We can think of the anisotropy of a particular area as a black box and the shear wave splitting measurements as a way of looking at what is in the box.