Monitoring Earthquakes

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Mind Map on Monitoring Earthquakes, created by Sandra Gong101 on 10/21/2015.
Sandra Gong101
Mind Map by Sandra Gong101, updated more than 1 year ago
Sandra Gong101
Created by Sandra Gong101 over 10 years ago
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Resource summary

Monitoring Earthquakes
  1. The Seismograph

    Annotations:

    • Seismic waves cause the seismograph's drum to vibrate. But the suspended weight with the pen attached moves very litle. There fore, the pen stays in place and records the drum's vibration.
    1. Measuring Seismic Waves
      1. Reading a Seismogram
      2. Instruments That Monitor Faults

        Annotations:

        • To monitor faults, geologists have developed instruments to measure changes in elevation, tilting of the land surface, and ground moments along faults. 
        1. Tiltmeters

          Annotations:

          • Measures tilting or raising of the ground. Used by geologists consist of two bulbs that are filled with a liquid and connected by a hollow stem. Each bulb contains a measuring scale to measure the depth of the liquid in that bulb.
          1. Creep Meters

            Annotations:

            • Creep meter uses a wire stretched across a fault to measure horizontal movement of the ground. Geologists determine how much the fault has moved by measuring how much the weight has moved against a scale.
            1. Laser-Ranging Devices

              Annotations:

              • A laser-ranging device uses a laser beam to detect horizontal fault movements. 
              1. GPS Satelltes

                Annotations:

                • Scientists can monitor changes in elevation as well as horizontal movement along faults using a network of Earth-orbiting satellites called GPS.
              2. Using Seismographic Data

                Annotations:

                • Seismographs and fault-monitoring devices provide data used to map faults and detect changes along faults. Geologists are also trying to use these data to develop a method of predicting earthquakes.
                1. Mapping Faults

                  Annotations:

                  • When seismic waves hit a fault, the waves are reflected off the fault. Seismographs can detect these reflected seismic waves.
                  1. Monitoring Changes Along Faults

                    Annotations:

                    • How rocks move along a fault depends on how much friction there is between the sides of the fault.
                    1. Friction

                      Annotations:

                      • The force that opposes the motion of one surface as it moves across another surface
                    2. Trying to Predict Earthquakes

                      Annotations:

                      • Even with data from many sources, geologists can't predict when and where a quake will strike. Stress along a fault increases until an earthquake occurs. Sometimes stored energy builds up along a fault, but an earthquake fails to occur. 
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