Amplitude
period
Rise Time (square wave)
Fall Time (Square wave)
Duty-Cycle (Square Wave)
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scientists use seismic waves to map earths interior by seismographs that measure the times at witch seismic waves arrive at different distances from an earth quake.
Longitudinal waves have all the same properties as transverse waves: speed, frequency, wavelength, and amplitude
Mechanical waves were not discovered by a single individual, but have been studied and understood by scientists over many centuries. The ancient Greeks, such as Pythagoras and Aristotle, made observations and theories about waves, while later scientists like Isaac Newton and Thomas Young made significant contributions to our understanding of mechanical waves.
Wavelength, Amplitude, and Frequency.
The size and shape of the Earth's core can be used to measure its properties by studying seismic waves that pass through the Earth. By analyzing how these waves travel and are affected by the core's size and shape, scientists can determine important properties such as density, composition, and temperature of the core.
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Seismograph
Scientists use seismographs to measure the magnitude of earthquakes. Seismographs detect the seismic waves generated by an earthquake, and the amplitude of these waves is used to calculate the earthquake's size. The most common scale used to measure earthquake size is the Richter scale or the moment magnitude scale.
Scientists use sound waves to measure the depth of the ocean through a method called sonar. By sending sound pulses from a ship to the ocean floor and measuring the time it takes for the sound waves to bounce back, scientists can calculate the depth of the ocean at that location.
Scientists use seismic waves from earthquakes to study the interior layers of the Earth. By analyzing how these waves travel through the Earth's layers, scientists can determine the properties of each layer, such as density and composition. This information helps us understand the structure and composition of the Earth's interior.
the Doppler effect! d('_')b
Seismographs were invented to measure and record seismic waves produced by earthquakes. They help scientists study the properties of earthquakes, such as their location, magnitude, and depth, which aids in understanding the Earth's structure and monitoring seismic activity.
Scientists use characteristics such as wave velocity, propagation mode, and direction of particle motion to classify seismic waves. These properties help differentiate between the different types of waves produced by earthquakes and other seismic events.
Various scientists and physicists have studied mechanical waves, including names like Daniel Bernoulli, Leonhard Euler, and Thomas Young. These scientists made significant contributions to our understanding of mechanical wave behavior and properties.
scientists use seismic waves to map earths interior by seismographs that measure the times at witch seismic waves arrive at different distances from an earth quake.
All waves exhibit the properties of frequency, wavelength, amplitude, and speed. They also involve oscillations or disturbances that propagate through a medium or space.