The lab acrobat pdf 91kb feb9 06 is also available in. Earthquakes and the earths interior earthquakes earthquakes occur when energy stored in elastically strained rocks is suddenly released. Combining the data obtained from seismological studies and. Complete the graphic organizer below by answering the question that is asked about each heading. Jan 16, 2008 seismic waves generated in earths interior provide images that help us to better understand the pattern of mantle convection that drives plate motions.
Earths interior structure seismic travel times in a. Oct 17, 2017 waves transfer energy from source to detector. Today s seismometers use the principle of electromotive force faraday and henry. Using simple calculations of the travel times of seismic waves in a constant velocity, spherical earth and comparison of the travel times with observations for the real earth, we find that the earths interior is not homogeneous. In view of the potential for major disaster, it should come as no surprise to you that many scientists study earthquakes. Earthquakes and the earth s interior earthquakes earthquakes occur when energy stored in elastically strained rocks is suddenly released. How do seismologists use seismic waves to understand the. Geologists have used s waves to help form the idea that the earth s core is molten because s waves have been found to not pass through the earth s center. The phases, frequencies, and amplitudes, phase and group velocities, travel times, etc of the waves that travel through the earth are all data that can be used to infer the earths structure. May 22, 2008 body waves can travel through the earths inner layers, but surface waves can only move along the surface of the planet like ripples on water. Seismic waves and the earths interior as we discussed in class, earthquakes occur when two portions of earth crust move with respect to each other. Microsoft word video notes earths interior seismic evidence. Seismic waves are sent through the earth during earthquakes, and those energy waves are what cause the ground to shake as they travel through it. From seismic tomography, first introduced in the late 1970s refs 1, 2, we now have a good understanding of the firstorder characteristics of the longwavelength 1,0002,000 km threedimensional elastic structure of earths.
Sep 29, 2017 boeing 737 max crashes immediately after takeoff here s what really happened to flight 610 duration. The speed of these waves are variable to the substance they pass through. How the study of seismic waves help us to understand the. Partly molten, floridasized blob forms atop earths core 7 february 20 this map shows earths surface superimposed on a depiction of what a new university of utah study.
Velocity tends to increase with depth through earth s crust and mantle, but drops sharply going from the mantle to the outer core. Primary waves p waves an earthquake wave in which rock particles vibrate parallel to the direction of the wave travel. Compressional or p for primary transverse or s for secondary love rayleigh an earthquake radiates p and s waves in all directions and the interaction of the p and s waves with earths surface and shallow structure produces surface waves. The scientific study of the earth s interior structure is enabled by the utilization of two types of energy waves. This shadow zone is explained by the refraction bending of p waves when they encounter the core boundary. How scientist get the information seismograph they get information by measuring seismic wave fields which are measured by a seismograph, geophone, hydrophone in water, or a accelerometer geophone whats a seismic wave. In addition to seismic waves from earthquakes, the interior of the earth is pervaded by seismic noise, a collective hum resulting from the bombardment of earths surface by a variety of sources. Earthquakes create seismic waves that travel through the earth. Geologists have used s waves to help form the idea that the earths core is molten because s waves have been found to not pass through the earths center. Seismometer physics is based on inertia resistance to change in position.
Scientists deduced the structure of earths interior and how waves move through it by analyzing thousands of earthquakes recorded at earths surface. Seismic wave propagation and earth models gfzpublic. The major boundaries of the earths interior were discovered by seismologists. The mere fact that body waves are waves therefore tells us quite a lot about them. Seismic waves travel more quickly through denser materials and therefore generally travel more quickly with depth. Nov 02, 2010 the cool thing about these waves is that they only travel through solids and wont pass through liquids or gases. The liquid layer of the earth s core that lies beneath the mantle and surrounds the inner core. The are many different seismic waves, but all of basically of four types. Seismic waves is a browserbased tool to visualize the propagation of seismic waves from historic earthquakes through earths interior and around its surface.
Some of the wave energy reflects off the boundary between the mantle and core. P waves are capable of passing through both solid and liquid, and travels faster. Scientists deduced the structure of earth s interior and how waves move through it by analyzing thousands of earthquakes recorded at earth s surface. As discussed, the routes taken by p and s waves through the interior of the earth are determined completely by the velocities at which these waves travel at each point in the interior. Examination of the travel time data and calculations provides suggestions about the actual nature of the earths interior structure. The most important information on the constitution of the earths interior has been obtained from studies of seismic body waves longitudinal and transverse seismic waves propagating through the earth. A the focus of the earthquake is directly below the epicenter. Scientists have seismographs set up all over the world to track movement of the earths crust. Measurements are made from seismometers distributed throughout the world and with varying sensitivities. When an earthquake occurs, it is the cause of seismic waves, including both waves that travel along the surface love waves and rayleigh waves and waves that travel through the body of the earth pwaves and swaves, known collectively as body waves.
Seismic waves generated in earths interior provide images that help us to better understand the pattern of mantle convection that drives plate motions. Sesmic waves, earthqukes and interior of the earth rashids. Over the past eight years, tromp has been at the forefront of research on how to improve seismic tomography to obtain highdefinition, accurate images of the earth s interior. Feb 03, 2017 seismic waves are sent through the earth during earthquakes, and those energy waves are what cause the ground to shake as they travel through it. Using seismic waves to image earths internal structure. Traveling through the interior of the earth, body waves arrive before the surface waves emitted by an earthquake. Historical geologyseismic waves wikibooks, open books. Discuss seismicwave shadow zones and what they indicate about earths interior. Body waves can travel through the earths inner layers, but surface waves can only move along the surface of the planet like ripples on water. How do scientists use seismic waves to map the earths. What can earthquakes tell us about the interior of the earth. Observed p waves arriving at nearby 200km seismic stations were moving at 6km s p waves arriving at stations 200km were moving at 8km s inferred that nearby stations were recording waves moving through the less dense crust whereas far away stations must be recording waves which were traveling through a denser material.
Interior of the earth lab microsoft word 121kb feb9 06 is a word file that is what the students use and fill out. Feb 03, 2006 the phases, frequencies, and amplitudes, phase and group velocities, travel times, etc of the waves that travel through the earth are all data that can be used to infer the earth s structure. Historical geologyseismic waves wikibooks, open books for. Students test several models of the interior of the earth beginning with a simple homogeneous earth and moving toward more complex multilayered earth models. Because radon is inert, it does not combine with other. For pwaves, there is a shadow zone in earth ranging in an arc from 103 o to 142 o from the epicenter of the quake. This release of energy causes intense ground shaking in the area near the source of the earthquake and sends waves of elastic energy, called seismic waves, throughout the earth. The division of the earth into the earth s crust, mantle and core, the later division into socalled bullen zones, or the latest laterally. Jul 19, 2018 seismic waves are used to determine the depth of layers of molten and semi molten material under the top surface. Seismic wave fields are recorded by a seismometer, hydrophone in water, or accelerometer. From earthquakes to music is a 2hour interactive program that we use to present seismology in an approachable way. Earths interior structure page 1 of 22 purdue university. How do scientists use seismic waves to determine the interior.
Seismic body waves can be refracted and reflected just as sound and light waves are. How seismic waves give scientist information about earths. Seismic waves are used to determine the depth of layers of molten and semi molten material under the top surface. Waves that travel outwards in 3d from the epicentre of an earthquake or more precisely the focus, as the epicentre is the point on the surface where waves first appear can be reflected when they hit the interface between crust and mantle as they travel downwards, so return. Seismic waves and the earth s interior as we discussed in class, earthquakes occur when two portions of earth crust move with respect to each other. Some seismologists, however, study earthquakes for another reason.
Seismic velocities depend on the material properties such as composition, mineral phase and packing structure, temperature, and pressure of the media through which seismic waves pass. This fact sheet uses data from the 1994 magnitude 6. Reflection used on the upper portion of the crust use earthquakes or manmade seismic events collect reflections of seismic waves from surfaces below you. This quiz and worksheet combination will help you test your understanding of how. In 1909, andrija mohorovicic, a croatian seismologist, discovered the boundary between the crust and the mantle by observing the sudden increase of seismic waves as they passed from the crust to the mantle. By analyzing these seismic waves, seismologists can explore the earth s deep interior. Seismic waves are recorded by a machine called a seismograph, which tells us about the strength and s. Robertson abstract evidence on the structure and composition of the earths interior comes from 1 observations of surface rocks, 2 geophysical data from earthquakes, flow of heat from the interior, the magnetic field, and gravity, 3 laboratory ex. Scientists are able to determine the interior surfaces of the earth by measuring the seismic waves that an earthquake emits. Seismic waves are waves of energy that travel through the earths layers and are a result of earthquakes, volcanic eruptions, massive landslides and large humanmade explosions. Modeling the interior of the earth using seismic waves.
By analyzing these seismic waves, seismologists can explore the earths deep interior. Some types of seismic waves travel through the interior of the earth and are detected by seismic stations on the other side of the earth. The propagation velocity of seismic waves depends on density and elasticity of the medium as well as the type of wave. Seismic sea waves tsunami tidal waves that result from vertical displacement along a fault located on the ocean floor, or from a large underwater landslide triggered by an earthquake. Nov 26, 2012 in addition to seismic waves from earthquakes, the interior of the earth is pervaded by seismic noise, a collective hum resulting from the bombardment of earth s surface by a variety of sources.
Caltechs journey to the center of the earth caltech gps. Types of seismic waves there are 2 types of seismic waves. This is an inquirybased student exercise designed to explore how we use seismic waves to understand the structure of the earth s interior. Heading evidence from rock samples evidence from seismic waves earth s interior question what did scientists. Velocity tends to increase with depth through earths crust and mantle, but drops sharply going from the mantle to the outer core. In this and succeeding articles we shall be interested only in body waves, since by traveling through the earth. How do scientists use seismic waves to determine the. Boeing 737 max crashes immediately after takeoff heres what really happened to flight 610 duration. There is a lot of analysis that is conducted on seismic data to produce pictures of the interior. The most important information on the constitution of the earth s interior has been obtained from studies of seismic body waves longitudinal and transverse seismic waves propagating through the earth. Seismic waves generated in earths interior provide images that help us to better understand the pattern of mantle convection that drives plate. So there you have two examples of how seismic waves can be used. Insidetheearth earthquakes and earth s interior outline. The division of the earth into the earths crust, mantle and core, the later division into socalled bullen zones, or the latest laterally.
What is the role of seismic waves in the study of the. The cool thing about these waves is that they only travel through solids and wont pass through liquids or gases. Earths hum helps probe planets interior earths layers. These waves travel through the interior of the earth and can be measured with sensitive detectors called seismographs. Easytouse controls speedup, slowdown, or reverse the wave propagation. The seismic waves that shake the ground during a quake also penetrate earths. Using a technique that is similar to a medical ct cat scan, researchers at princeton are using seismic waves from earthquakes to create images of the earths subterranean structures such as tectonic plates, magma reservoirs and mineral. Since waves encounter different material like solid, molten they are used to guess the direction from which the waves occured from.
Sesmic waves, earthqukes and interior of the earth. Pdf this chapter outlines some of the understanding of the earths interior derived from. Earthquakes and the earths interior tulane university. On opposite sides of a fault line, forces in the earth attempt to move different portions of the crust in opposite directions. The waves spread through the planet in a series of expanding spheres. These waves are not created by the tidal effect of the moon or sun. Past approaches for making these images incorporate only three types of seismic waves.
Waves that travel outwards in 3d from the epicentre of an earthquake or more precisely the focus, as the epicentre is the point on the surface where waves first appear can be reflected when they hit the interface between crust and mantle as they travel downwards, so return towards the. They also tend to reflect at sudden changes in density. From the study of seismic wave refraction and reflection, scientists infer earths internal structure by locating boundaries, or discontinuities, in its composition and physical properties. Examine p and s waves moving through earths interior. Using seismic waves to image earths internal structure nature. Heading evidence from rock samples evidence from seismic waves earths interior question what did scientists. Modeling of seismic wave propagation at the scale of the. On seismograms, seismic waves recorded from more distant facilities are closer 10. Earthquakes radiate seismic energy as both body and surface waves. Seismic waves we ve all felt seismic waves from an earthquake, but to understand the phenomenon it must be measured.
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