lower six ms shalto. figure showing the tectonic setting of earthquakes

Download Lower six Ms Shalto. Figure showing the tectonic setting of earthquakes

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  • Slide 1
  • Lower six Ms Shalto
  • Slide 2
  • Figure showing the tectonic setting of earthquakes
  • Slide 3
  • Movement and slipping along plate boundaries can form an earthquake. Depending on the type of movement, the earthquakes occur in either a shallow or deep level in the crust. The majority of tectonic earthquakes originate at depths not exceeding tens of kilometers.
  • Slide 4
  • Where old and cold oceanic crust descends beneath another tectonic plate, Deep Focus Earthquakes may occur at much greater depths (up to seven hundred kilometers!). These earthquakes occur at a depth at which the subducted crust should no longer be brittle, due to the high temperature and pressure. A possible mechanism for the generation of deep focus earthquakes is faulting. Earthquakes may also occur in volcanic regions and are caused there both by tectonic faults and by the movement of magma (hot molten rock) within the volcano. Such earthquakes can be an early warning of volcanic eruptions.
  • Slide 5
  • The fastest wave, and therefore the first to arrive at a given location. Also known as compressional waves, the P wave alternately compresses and expands material in the same direction it is traveling. Can travel through all layers of the Earth.
  • Slide 6
  • The S wave is slower than the P wave and arrives next, shaking the ground up and down and back and forth perpendicular to the direction it is traveling. Also know as shear waves.
  • Slide 7
  • They follow the P and S waves. These waves travel along the surface of the earth Also known as: Rayleigh waves, also called ground roll, travel like ocean waves over the surface of the Earth, moving the ground surface up and down. They cause most of the shaking at the ground surface during an earthquake. Love waves are fast and move the ground from side to side.
  • Slide 8
  • Intensity scales measure the amount of shaking at a particular location. The intensity of an earthquake will vary depending on where you are. Magnitude scales, like the Richter magnitude and moment magnitude, measure the size of the earthquake at its source. Magnitude does not depend on where the measurement of the earthquake is made. On the Richter scale, an increase of one unit of magnitude (for example, from 4.6 to 5.6) represents a 10-fold increase in wave amplitude on a seismogram or approximately a 30-fold increase in the energy released.
  • Slide 9
  • I. Not felt except by a very few under especially favorable conditions. II. Felt only by a few persons at rest, especially on upper floors of buildings. III. Felt quite noticeably by persons indoors, especially on upper floors of buildings. Many people do not recognize it as an earthquake. Standing motor cars may rock slightly. Vibrations similar to the passing of a truck. Duration estimated. IV. Felt indoors by many, outdoors by few during the day. At night, some awakened. Dishes, windows, doors disturbed; walls make cracking sound. Sensation like heavy truck striking building. Standing motor cars rocked noticeably. V. Felt by nearly everyone; many awakened. Some dishes, windows broken. Unstable objects overturned. Pendulum clocks may stop. VI. Felt by all, many frightened. Some heavy furniture moved; a few instances of fallen plaster. Damage slight. VII. Damage negligible in buildings of good design and construction; slight to moderate in well-built ordinary structures; considerable damage in poorly built or badly designed structures; some chimneys broken. VIII. Damage slight in specially designed structures; considerable damage in ordinary substantial buildings with partial collapse. Damage great in poorly built structures. Fall of chimneys, factory stacks, columns, monuments, walls. Heavy furniture overturned. IX. Damage considerable in specially designed structures; well-designed frame structures thrown out of plumb. Damage great in substantial buildings, with partial collapse. Buildings shifted off foundations. X. Some well-built wooden structures destroyed; most masonry and frame structures destroyed with foundations. Rails bent. XI. Few, if any (masonry) structures remain standing. Bridges destroyed. Rails bent greatly. XII. Damage total. Lines of sight and level are distorted. Objects thrown into the air.
  • Slide 10
  • The vibrations produced by earthquakes are detected, recorded, and measured by instruments call seismographs. The zig-zag line made by a seismograph, called a "seismogram," reflects the changing intensity of the vibrations by responding to the motion of the ground surface beneath the instrument. From the data expressed in seismograms, scientists can determine the time, the epicenter, the focal depth, and the type of faulting of an earthquake and can estimate how much energy was released.
  • Slide 11
  • An oceanic spreading ridge is the fracture zone along the ocean bottom where molten mantle material comes to the surface, thus creating new crust. This fracture can be seen beneath the ocean as a line of ridges that form as molten rock reaches the ocean bottom and solidifies.
  • Slide 12
  • Major earthquakes may occur along subduction zones. The most recent sub- duction zone type earth- quake occurred in 1700. Scientists believe, on average, one subduction zone earthquake occurs every 300-600 years.
  • Slide 13
  • A transform fault is a special variety of strike- slip fault that accom- modates relative horizontal slip between other tectonic elements, such as oceanic crustal plates.
  • Slide 14
  • Intraplate seismic activity occurs in the interior of a tectonic plate. Intraplate earthquakes are rare compared to those located at plate boundaries. Very large intraplate earthquakes can inflict very heavy damage. Distribution of seismicity associated with the New Madrid Seismic Zone since 1974.
  • Slide 15
  • Buckled roads and rail tracks Structural Damage
  • Slide 16
  • LandslidesAvalanches
  • Slide 17
  • Alterations to Water Courses Fire resulting from an earthquake
  • Slide 18
  • Earthquake activity beneath a volcano almost always increases before an eruption because magma and volcanic gas must first force their way up through shallow underground fractures and passageways. When magma and volcanic gases or fluids move, they will either cause rocks to break or cracks to vibrate. When rocks break, high-frequency earthquakes are triggered. However, when cracks vibrate either low-frequency earthquakes or a continuous shaking called volcanic tremor is triggered.
  • Slide 19
  • Satellites can record infrared radiation where more heat or less heat shows up as different colors on a screen. When a volcano becomes hotter, an eruption may be coming soon.
  • Slide 20
  • Slide 21
  • New Madrid, TennesseeSan Andreas Faultline
  • Slide 22
  • Scientists consider seismic activity as it is registered on a seismometer. A volcano will usually register some small earthquakes as the magma pushes its way up through cracks and vents in rocks as it makes its way to the surface of the volcano. As a volcano gets closer to erupting, the pressure builds up in the earth under the volcano and the earthquake activity becomes more and more frequent.
  • Slide 23
  • This is an image of an analog recording of an earthquake. The relatively flat lines are periods of quiescence and the large and squiggly line is an earthquake. Below is a digital seismogram. The data is stored electronically, easy to access and manipulate, and much more accurate and detailed than the analog recordings.
  • Slide 24
  • Tiltmeters attached to the sides of a volcano detect small changes in the slope of a volcano. When a volcano is about to erupt, the earth may bulge or swell up a bit. Installing a tiltmeter
  • Slide 25
  • Hydrogeologic responses to large distant earthquakes have important scientific implications with regard to our earths intricate plumbing system. The exact mechanism linking hydrogeologic changes and earthquakes is not fully understood, but monitoring these changes improves our insights into the responsible mechanisms, and may improve our frustratingly imprecise ability to forecast the timing, magnitude, and impact of earthquakes.
  • Slide 26
  • The cause of unusual animal behavior seconds before humans feel an earthquake can be easily explain-ed. Very few humans notice the smaller P wave that travels the fastest from the earthquake source and arrives before the larger S wave. But many animals with more keen senses are able to feel the P wave seconds before the S wave arrives. If in fact there are precursors to a significant earthquake that we have yet to learn about (such as ground tilting, groundwater changes, electrical or magnetic field variations), indeed its possible that some animals could sense these signals and connect the perception with an impending earthquake.
  • Slide 27
  • Slide 28
  • Tsunamis can be generated by: Large Earthquakes (megathrust events such as Sumatra, Dec. 26, 2004) Underwater or near-surface volcanic eruptions (Krakatoa, 1883) Comet or asteroid impacts (evidence for tsunami deposits from the Chicxulub impact 65 mya) Large landslides that extend into water (Lituya Bay, AK, 1958) Large undersea landslides (evidence for prehistoric u

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