# earth science 8.2 measuring earthquakes measuring earthquakes

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- Slide 1
- Earth Science 8.2 Measuring Earthquakes Measuring Earthquakes
- Slide 2
- Earth Science 8.2 Measuring Earthquakes In 2003, a powerful earthquake shook Alaska wilderness south of Fairbanks along the Denali front. This earthquake was so strong it shook ponds in Louisiana and Texas. Seismic waves carry the energy released from an earthquake hundreds of kilometers away. Seismic waves transmit the energy of these vibrations from particle to particle. Like a bell hit with a hammer, the vibrations ring through the rocks the bedrock that makes up the lithosphere.
- Slide 3
- Earth Science 8.2 Measuring Earthquakes Earthquakes produce two main types of seismic waves Body waves Surface waves These seismic waves differ in their type of wave motion, their behavior as they travel through the Earth, and their speed. The waves that travel through the Earths interior are called body waves. There are two types of body waves P waves S waves
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- Earth Science 8.2 Measuring Earthquakes P waves and S waves: P waves are push-pull waves that push and pull particles as they move in a direction. They could also be said to compress- expand. P waves are also called compressional waves. P waves travel faster than S waves. P waves can travel through both liquids and solids. S waves shake particles at right angles to the waves direction. Like taking one end of a rope and shaking it, the waves move in a curve. S waves are also called transverse waves.
- Slide 5
- Earth Science 8.2 Measuring Earthquakes Surface waves: When body waves reach the surface, they produce surface waves. Surface waves travel more slowly than body waves do. Surface waves move up and down as well as side-to-side. Surface waves are usually much larger than body waves, so surface waves are usually the most destructive seismic waves.
- Slide 6
- Earth Science 8.2 Measuring Earthquakes Recording Seismic Waves: Scientists have developed an instrument to record seismic waves: the seismograph. A seismograph produces a time record of the ground motion during an earthquake. How it works: A seismograph has a weight suspended from a support that is attached to the bedrock. When seismic waves reach the bedrock, the inertia of the suspended weight keeps the weight arm almost stationary while the bedrock moves. In older seismographs, a pen suspended drew on a rotating cylinder and the traces showed the movement of the waves.
- Slide 7
- Earth Science 8.2 Measuring Earthquakes Seismogram: The time record that a seismograph produces is called a seismogram. A seismogram shows all three types of seismic waves. The stronger the earthquake, the larger the waves on the seismogram. The first wave to arrive is the P wave, followed soon after by the S wave. After the S waves, the Surface waves arrive showing much stronger movement. seismogram seismograph
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- Measuring Earthquakes: Richter Scale Intensity is a measure of the amount of earth shaking that happens at a given location in an earthquake. Magnitude (M) is a measure of the size of the seismic waves or the amount of energy released at the source of the earthquake. The Richter Scale and the Moment Magnitude Scale both measure earthquakes magnitude. The Modifed Mercalli Scale is based on earthquake intensity. seismogram seismograph
- Slide 9
- Measuring Earthquakes: Richter Scale seismogram Richter Scale: A familiar but outdated scale for measuring the magnitude of earthquakes is the Richter Scale. The Richter Scale is based on the height of the largest seismic wave (P,S, or surface wave) recorded on a seismograph. A 10X increase in wave height equals an increase of 1 on the Richter Scale. An increase for a M5.0 earthquake is 10 times greater than the shaking produced by a magnitude 4.0 on the Richter Scale.
- Slide 10
- Measuring Earthquakes: Momentary Magnitude Scale Moment Magnitude Scale: Today scientists use the moment magnitude scale to measure earthquakes. The moment magnitude scale is derived from the amount of displacement that occurs along a fault. The moment magnitude scale is also the only scale that estimates the energy released by earthquakes.
- Slide 11
- Measuring Earthquakes: Momentary Magnitude Scale Moment Magnitude Scale: The moment magnitude is generated using several factors in addition to seismographic data. These factors include Average amount movement Area of surface break Strength of the broken rock Together, these factors give a measure of how much energy is released when the rock slips and breaks and releases its energy as an earthquake.
- Slide 12
- Measuring Earthquakes: Modified Mercalli Scale Modified Mercalli Scale: Another scale used to rate earthquakes is the modified Mercalli scale. This scale rates an earthquakes intensity in terms of an earthquakes effects at different locations (how much shaking it creates or damage it does). The scale has 12 steps expressed as Roman numerals An earthquake that is barely felt rates a I. An earthquake which creates almost total destruction rates a XII The same earthquake can rate different Mercalli scale ratings at different locations.
- Slide 13
- Measuring Earthquakes: Locating an Epicenter Locating an Earthquake Epicenter: The difference in speeds between the P and the S waves provides a way to locate the epicenter. The P wave always travels faster, arriving before the S wave. The longer the distance away the epicenter, the greater the amount of time between the waves arriving. P wavesS Waves
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- Measuring Earthquakes: Triangulation Locating an Earthquake Epicenter: With this information, a receiver can judge the distance to the epicenter of the earthquake. If multiple receiving stations ( 3 or more) at different spots on the globe can all identify and coordinate their information, they can triangulate a location. Each station knows its distance to the epicenter. Triangulate means to use three or positions to determine an exact location.
- Slide 15
- Measuring Earthquakes: Time Travel Graphs Locating an earthquake epicenter: A time travel graph, data from seismographs from at least three different locations, and a globe can be used to determine an earthquakes epicenter. First, using the data from the each of the seismograph readings, you estimate the distance from each receiver to the epicenter. Second, you determine a circle from each receiver that shows the distance away the epicenter could be in any direction. Third, the point where all three circles intersect marks the epicenter
- Slide 16
- Vocabulary: Earthquakes Focus: the point beneath Earth's surface where rock that is under stress breaks Epicenter: point directly above the focus Seismic waves: vibrations that travel through Earth's surface carrying the energy created by an earthquake Primary waves: the earthquake waves that compress and expand the ground like an accordion Secondary waves: the waves that vibrate from side to side as well as up and down Surface waves: when Primary waves and Secondary waves reach the surface some of them are transformed into Surface waves Seismograph: the instrument that geologist use to record and measure the vibration of seismic wave Magnitude: the measurement of earthquake strength based on seismic waves and movement a long faults Mercalli Scale: rate earthquakes by their intensity Richter Scale: rate earthquakes by mechanical seismograph Moment Magnitude Scale: rates earthquakes by estimating the total energy released
- Slide 17
- Computer Lab: Todays assignment is to use the internet in the computer lab to research and answer the following questions with a short mini-report. Do NOT COPY, CUT, OR PASTE. Put in your OWN WORDS. What is the Richter Scale and by who and when was it invented? (one paragraph) Who invented the Mercalli Scale and when and where did he invent it? How is it different than the Richter Scale? (one paragraph) Who developed the Momentary Magnitude Scale and how is it different than the first two; the Richter and the Mercalli? (one paragraph) Locating a position by triangulation is used in many different applications. Find two other instances where triangulation is used to locate a position. (One paragraph)
- Slide 18

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