Presentation on theme: "Lab 2: The Interior of the Earth Key Q: What is the interior of the Earth like?"— Presentation transcript:
Lab 2: The Interior of the Earth Key Q: What is the interior of the Earth like?
Part A: Observing Waves & Measuring Wave Speed In our lab activity you learned that waves travel at a constant speed. Scientists cannot observe earthquake waves moving through the Earth in the same way you can observe waves moving through water. They can, however, record and study the energy from the earthquake waves as the waves arrive at a recording station (seismograph station). They can use information they record about the waves to make models of the interior of the Earth.
Part A: Observing Waves & Measuring Wave Speed Think about how what you studied relates to how scientists make models of the inside of the Earth. What part of your experiment represented: Th earthquake releasing energy in the Earth? The movement of energy waves from the earthquakes (seismic waves) in the Earth? The material in the Earth through which seismic waves travel? The arrival of a seismic wave at a seismograph station where earthquakes are detected?
Part A: Observing Waves & Measuring Wave Speed Vibrations of the earths crust are earthquakes. When an earthquake occurs energy waves radiate out in all directions. These waves are called seismic waves. Scientist cannot see seismic waves traveling through the Earth but they can detect them with a seismograph. Seismologists, scientists that study earthquakes, can use the information they gather from studying these waves to make a conceptual model of the interior of the earth
Part B: Kinds of Seismic Waves There are 3 kinds of seismic waves. Each one travels at a constant speed and creates a different movement. Studying these waves can allow scientists to: –Determine the amount of energy released by an earthquake (magnitude) –Determine the exact location of an earthquake –Create a model of the interior of the Earth.
Part B: Kinds of Seismic Waves P-waves –are the fastest moving waves. –Cause particles to move back and forth in place. –Move through solids, liquids, and gases.
Part B: Kinds of Seismic Waves S-waves –Move slower than P-waves. –Cause particles in materials to move side to side. –Travel only through solids.
Part B: Kinds of Seismic Waves L-waves –are the slowest moving waves. –Cause the surface to rise and fall like ocean waves. –Cause the most damage. –Travel through solids liquids, and gases.
Which wave… Travel through gases? Travel through liquids? Travel through solids? Fastest waves? Surface waves? Slowest waves? Cause particles to move back & forth in place? Cause particles to move side to side? Cause the most damage? Cause surface to rise and fall like ocean waves?
Seismologists: scientists that study earthquakes Seismic waves: earthquake waves Seismograph: Instrument that detects seismic waves. Fault: Fracture zone where rock has been moved Focus: area along the fault where movement first occurs Epicenter: Point on the earths surface directly above the focus.
Calculate the epicenter & magnitude of an earthquake http://www.sciencecourseware.org/virtualearthquake /vquakeexecute.html
Part C: Refraction of Waves We learned that waves travel at a constant speed when they travel through one kind of material. A waves speed depends on what material it is traveling through, so when the wave (P-wave) crosses a boundary line between 2 different materials in the Earth it REFRACTS.
Part C: Refraction of Waves ) 20° ( Greater angle 60° Boundary Line (between 2 layers of the Earth) P-wave wave speed = 30cm/s wave speed = 1m/s Angle of wave in relation to the boundary line changed due to change in wave speed REFRACTION: The change in direction of a wave due to its change in speed as it passes from one material to the next.
http://earthquake.usgs.gov/learn /animations/animation.php?flash _title=Shadow+Zone&flash_file= shadowzone&flash_width=220& flash_height=320 Annimation from usgs kids of shadow zones ADD IT!
Part D: Refraction of Earthquake Waves in the Earth P-waves –CAN travel through the whole planet. –Refract (change direction) at a boundary between the different layers of the Earth –We know they refract because the refraction creates shadow zones. (an area on the Earths surface where no seismic waves are received.) S-waves –Can NOT travel through the whole planet. –They can travel through the Crust & the Mantle but STOP at the Outer Core because it is liquid & S- waves only travel through solids
Part D: Refraction of Earthquake Waves in the Earth Shadow Zones: –An area on the Earths surface where no seismic waves are received. –Caused by the refraction of waves. –Shows that the earth has layers.
Layers of the Earth Crust: cool layer of rigid rock Lithosphere: rigid layer. Includes the Crust & the upper Mantle Mantle: semi-rigid layer Asthenosphere: Has plasticity (the ability to flow). lower portion of Mantle Outer Core: liquid layer. S waves stop here. Inner Core: solid