Oceans - Learn with Mrs. Schulz
... -The difference between high and low tide is called tidal range. -The Sun is further from the Earth than the moon thus it has less influence on the tides, but when they are all aligned they work together to create a bigger tidal range. When they are at right angles the Sun works against the Moon’s g ...
... -The difference between high and low tide is called tidal range. -The Sun is further from the Earth than the moon thus it has less influence on the tides, but when they are all aligned they work together to create a bigger tidal range. When they are at right angles the Sun works against the Moon’s g ...
Current Systems in Planetary Magnetospheres and Ionospheres
... just outside the ionospause. In the plane perpendicular to the solar wind convection electric field, the magnetic field lines are bent and diverge as shown in Fig. 2, squeezing out the solar wind plasma from the dayside equatorial region and creating a void of charged particles in the magnetic barri ...
... just outside the ionospause. In the plane perpendicular to the solar wind convection electric field, the magnetic field lines are bent and diverge as shown in Fig. 2, squeezing out the solar wind plasma from the dayside equatorial region and creating a void of charged particles in the magnetic barri ...
EARTHQUAKES.2
... vibrate back and forth perpendicular to the direction the wave is moving Slower than P waves (4-5 kms./s) TRAVEL THROUGH SOLIDS ONLY ...
... vibrate back and forth perpendicular to the direction the wave is moving Slower than P waves (4-5 kms./s) TRAVEL THROUGH SOLIDS ONLY ...
Earthquakes
... vibrate back and forth perpendicular to the direction the wave is moving Slower than P waves (4-5 kms./s) TRAVEL THROUGH SOLIDS ONLY ...
... vibrate back and forth perpendicular to the direction the wave is moving Slower than P waves (4-5 kms./s) TRAVEL THROUGH SOLIDS ONLY ...
File
... • Seismic waves that travel along Earth’s Surface • When P and S waves reach the surface, they make Surface waves • There are two types, Love waves and Rayleigh waves • Cause lots of damage ...
... • Seismic waves that travel along Earth’s Surface • When P and S waves reach the surface, they make Surface waves • There are two types, Love waves and Rayleigh waves • Cause lots of damage ...
Earthquake Lesson
... • Seismic waves that travel along Earth’s Surface • When P and S waves reach the surface, they make Surface waves • There are two types, Love waves and Rayleigh waves • Cause lots of damage ...
... • Seismic waves that travel along Earth’s Surface • When P and S waves reach the surface, they make Surface waves • There are two types, Love waves and Rayleigh waves • Cause lots of damage ...
Activity 2 Modelling Convection Currents
... the same general pattern as the Earth’s crust, only on a much smaller scale. This is crucial because the giant internal convection current in the mantle has enough energy to move whole continents, making mountains and valleys, and divide oceans. 4. Make sure that students store their videos for inc ...
... the same general pattern as the Earth’s crust, only on a much smaller scale. This is crucial because the giant internal convection current in the mantle has enough energy to move whole continents, making mountains and valleys, and divide oceans. 4. Make sure that students store their videos for inc ...
Earthquakes
... • Scientists calculate the difference between arrival times of the P waves and S waves • The further away an earthquake is, the greater the time between the arrival of the P waves and the S waves ...
... • Scientists calculate the difference between arrival times of the P waves and S waves • The further away an earthquake is, the greater the time between the arrival of the P waves and the S waves ...
P and S waves moving through the Earth`s Interior
... measurements, the seismologists can get a better understanding of the composition of what the waves are traveling through. The waves travel at a higher velocity when going through denser materials. By noting where the waves have considerable velocity changes, the seismologists can infer where the co ...
... measurements, the seismologists can get a better understanding of the composition of what the waves are traveling through. The waves travel at a higher velocity when going through denser materials. By noting where the waves have considerable velocity changes, the seismologists can infer where the co ...
19.1 Earthquakes
... similar to pushing a slinky in the direction in which it is stretched 2) Secondary Waves: (S-waves) similar to holding a jump rope in one hand and raising and lowering it 3) Surface Waves (Love and Rayleigh): the most destructive, cause the ground to move sideways and up and down like an ocean wave ...
... similar to pushing a slinky in the direction in which it is stretched 2) Secondary Waves: (S-waves) similar to holding a jump rope in one hand and raising and lowering it 3) Surface Waves (Love and Rayleigh): the most destructive, cause the ground to move sideways and up and down like an ocean wave ...
19.1 Earthquakes
... similar to pushing a slinky in the direction in which it is stretched 2) Secondary Waves: (S-waves) similar to holding a jump rope in one hand and raising and lowering it 3) Surface Waves (Love and Rayleigh): the most destructive, cause the ground to move sideways and up and down like an ocean wave ...
... similar to pushing a slinky in the direction in which it is stretched 2) Secondary Waves: (S-waves) similar to holding a jump rope in one hand and raising and lowering it 3) Surface Waves (Love and Rayleigh): the most destructive, cause the ground to move sideways and up and down like an ocean wave ...
Key to pre/post test - TSDCurriculum
... ways humans find out about the structure and temperatures is inside of the earth. 1. Seismic waves. 2. Experiments on the properties of materials (such as density of iron at different temperatures and pressures) Learning Goals: We know what is inside of the earth by information from seismic waves an ...
... ways humans find out about the structure and temperatures is inside of the earth. 1. Seismic waves. 2. Experiments on the properties of materials (such as density of iron at different temperatures and pressures) Learning Goals: We know what is inside of the earth by information from seismic waves an ...
The Layer`s Of The Earth!
... or the liquid layers of the earth. It pushes and pulls the rock it moves through just like sound waves push and pull the air. ...
... or the liquid layers of the earth. It pushes and pulls the rock it moves through just like sound waves push and pull the air. ...
Kein Folientitel
... component with a hot dilute loss-cone superposed. The region of instability in parameter space is illustrated below (left). Apparently, the instability depends also on the electron density and temperature. Ring current ions and electrons can, due to cyclotron wave turbulence, scatter into the loss c ...
... component with a hot dilute loss-cone superposed. The region of instability in parameter space is illustrated below (left). Apparently, the instability depends also on the electron density and temperature. Ring current ions and electrons can, due to cyclotron wave turbulence, scatter into the loss c ...
View a pdf
... 10 million years ago. 16. Coriolis Effect 17. Cross-Bedding 18. Cyclones and Anticyclones ...
... 10 million years ago. 16. Coriolis Effect 17. Cross-Bedding 18. Cyclones and Anticyclones ...
Earthquakes – Chapter 6
... Second to be recorded Slower and more destructive than P waves Rocks are moved from side to side as the wave passes, moving at right angles to the direction of wave motion • Transverse waves, like water waves • Move through solid only ...
... Second to be recorded Slower and more destructive than P waves Rocks are moved from side to side as the wave passes, moving at right angles to the direction of wave motion • Transverse waves, like water waves • Move through solid only ...
12/9 Convection Currents
... The figure to the right shows a convection cells in Earth’s mantle. A convection cell is one complete loop of convection current. Use the figure to answer the questions that ...
... The figure to the right shows a convection cells in Earth’s mantle. A convection cell is one complete loop of convection current. Use the figure to answer the questions that ...
Lecture 9: Tides
... Lunar tidal bulge, solar tidal bulge, neap tide, spring tide, new moon, half moon, full moon, tangential velocity, orbital velocity, centripetal force, barycenter, center-seeking force, tidal cycle, amphidromic point Dates: none Numbers: How far is the moon from the Earth in terms of Earth diameters ...
... Lunar tidal bulge, solar tidal bulge, neap tide, spring tide, new moon, half moon, full moon, tangential velocity, orbital velocity, centripetal force, barycenter, center-seeking force, tidal cycle, amphidromic point Dates: none Numbers: How far is the moon from the Earth in terms of Earth diameters ...
Lecture 10: Tides
... Lunar tidal bulge, solar tidal bulge, neap tide, spring tide, new moon, half moon, full moon, tangential velocity, orbital velocity, centripetal force, barycenter, center-seeking force, tidal cycle, amphidromic point Dates: none Numbers: How far is the moon from the Earth in terms of Earth diameters ...
... Lunar tidal bulge, solar tidal bulge, neap tide, spring tide, new moon, half moon, full moon, tangential velocity, orbital velocity, centripetal force, barycenter, center-seeking force, tidal cycle, amphidromic point Dates: none Numbers: How far is the moon from the Earth in terms of Earth diameters ...
Types of seismic waveS
... 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 on different surface characteristics; for example, in the case of horizontally polarized S waves, the groun ...
... 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 on different surface characteristics; for example, in the case of horizontally polarized S waves, the groun ...
Earth`s Interior and Geophysical Properties
... -400 km - concentric layers at these depths -670 km - deepest quakes * These layers are probably “pressure collapse” layers @ 670 km olivine ---> perovskite We also have samples of mantle rocks in the form of Ophiolites. How do ophiolites form? ...
... -400 km - concentric layers at these depths -670 km - deepest quakes * These layers are probably “pressure collapse” layers @ 670 km olivine ---> perovskite We also have samples of mantle rocks in the form of Ophiolites. How do ophiolites form? ...
Chapter 14 - Earth`s Interior
... • Heat inside the Earth drives the core’s geodynamo and the mantle’s convection. • Earth’s interior is explored by using information from seismic waves and their passage through the body of the Earth. ...
... • Heat inside the Earth drives the core’s geodynamo and the mantle’s convection. • Earth’s interior is explored by using information from seismic waves and their passage through the body of the Earth. ...