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Earthquakes differ from each other because the tension of the rocks under the earth are not the same strength. If you are talking about one earthquake having different intensities in different places, this is because some lands are farther away from the focus than others. The focus is the place deep in the ground where the rocks rub against each other.
cuz they are on the other side of each other
The epicenter
Earthquake intensity is recorded on the Modified Mercalli or the Macroseismic scale. These values are derived based on witness reports as to the perceived level of ground shaking as well as damage to buildings and other structures and ground accelerations as measured by seismometers.
No, the two standard scales used worldwide are the Richter and the Mercalli:Richter measures total energy release by the quake and is a single valueMercalli measures how the quake felt and the damage it caused at various sites, this gives high values near the epicenter and lower values further awayTo help distinguish them Richter magnitudes are given as a decimal number while Mercalli magnitudes are given in Roman Numerals.
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well i think its based on a sacle from 1083 to 22222
The epicenter
The epicenter
Earthquake intensity is measured using the modified Mercalli scale or the macroseismic scale. Their values are derived based on eye witness accounts of the violence of the shaking of the ground, the damage done to buildings and other structures and based on ground surface accelerations measured by seismometers.
Monochromatic - is whereone colour is used but in different valuse and intensity.
Strong-motion seismometers (which are also known as Accelerographs) are used to measure the intensity of earthquakes. It should be noted that intensity is different from magnitude and is measured using a differing scale (Moddified Mercalli or Macroseismic scale for intensity vs Moment Magnitude scale for earthquake magnitudes.)Seismometers / accelerometers measure the intensity of earthquakes.Seismometers - instruments that measure motions of the ground.The visual output, either on a monitor or on paper is called a seismographSeismometers are in part used to measure the intensity of earthquakes. The scale used to measure earthquake intensity is known as the Modified Mercalli scale. A variation of this is used in Europe and is known as the Macroseismic scale.Earthquakes are measured with a seismometer.Seismometers and accelerometers are used to measure the acceleration of the ground surface and the total amplitude of seismic waves during an earthquake.These values are used by seismologists to find the intensity of the earthquake (along with observations of the damage done to structures).Earthquakes are measured using machines called SEISMOMETERS which record the shaking as waves on a graph .The magnitude of most earthquakes is measured on the Richter scale, invented by Charles F. Richter in 1934. The Richter magnitude is calculated from the amplitude of the largest seismic wave recorded for the earthquake, no matter what type of wave was the strongest.
Strong-motion seismometers (which are also known as Accelerographs) are used to measure the intensity of earthquakes. It should be noted that intensity is different from magnitude and is measured using a differing scale (Moddified Mercalli or Macroseismic scale for intensity vs Moment Magnitude scale for earthquake magnitudes.)Seismometers / accelerometers measure the intensity of earthquakes.Seismometers - instruments that measure motions of the ground.The visual output, either on a monitor or on paper is called a seismographSeismometers are in part used to measure the intensity of earthquakes. The scale used to measure earthquake intensity is known as the Modified Mercalli scale. A variation of this is used in Europe and is known as the Macroseismic scale.Earthquakes are measured with a seismometer.Seismometers and accelerometers are used to measure the acceleration of the ground surface and the total amplitude of seismic waves during an earthquake.These values are used by seismologists to find the intensity of the earthquake (along with observations of the damage done to structures).Earthquakes are measured using machines called SEISMOMETERS which record the shaking as waves on a graph .The magnitude of most earthquakes is measured on the Richter scale, invented by Charles F. Richter in 1934. The Richter magnitude is calculated from the amplitude of the largest seismic wave recorded for the earthquake, no matter what type of wave was the strongest.
Earthquake intensity is recorded on the Modified Mercalli or the Macroseismic scale. These values are derived based on witness reports as to the perceived level of ground shaking as well as damage to buildings and other structures and ground accelerations as measured by seismometers.
My top 5 personal values are integrity, honesty, diligence, respect and loyalty. People have different personal values that are normally influenced by several factors.
Someone is able to find the values for different baseball cards online on several different websites including the following sites: Beckett, ESPN, and Dean's Cards.
Yes. The Mercalli intensity scale measures the effect of the earthquake on people and structures, and the intensity value will differ depending on how far you are from the epicenter. For instance, a 5.5 magnitude earthquake may be damaging (intensity VII) around the epicenter, but 300 miles away it may be barely felt (intensity II). The mercalli scale measures the intensity of an earthquake, where the Richter scale measures the magnitude. Also you have to consider where the earthquake occurred. you can have a 9.0 quake in the middle of the Australian outback but there is hardly anybody there so you would have a low mercalli scale reading. If you had that same quake in San Francisco then you are going to have a seriously high number on the mercalli scale
Many things can affect the intensity or the earth quake ⚡️💦