A number of scales are used to measure earthquakes. These are broadly split into two main types. Magnitude scales and intensity scales.
Magnitude scales give an indication of the amount of energy released during an earthquake and intensity scales give an indication of the sevirity of ground shaking and resultant damage in a given location.
For more information on these, please see the related questions.
The most commonly referred to scale by the press and the public is the Richter scale for measuring earthquake magnitude. However this was actually replaced in the 1970s by the Moment Magnitude scale which is the magnitude scale favoured and in use by seismologists.
Seismometers measure the amplitude of seismic waves as well as the velocity and acceleration of the grounds surface. This allows seismologists to estimate the magnitude of an earthquake (the amount of energy released). From the energy emission per unit time they can estimate the power of the earthquake.
Magnitude of the 2011 Japan earthquake on moment magnitude scale is 9.0.The use of the Richter magnitude scale has largely been replaced by the moment magnitude scale in most countries. The United States Geological Survey (USGS), for example, uses the moment magnitude scale designated as MMS or Mw to measure all large earthquakes.UPDATE: Official magnitude was updated to 9.1 on Nov 7, 2016.
They could use the information from the seismic wave scale
I would use the odometer on my car. If that does not help I would use a map and a ruler and measure it to scale.
Geologists use the moment magnitude scale (Mw) to rate the magnitude of an earthquake today. This scale takes into account the seismic moment, which provides a more precise measurement of an earthquake's size compared to the Richter scale.
Earthquake
Scientists most often use the Richter scale or the moment magnitude scale to express the magnitude of an earthquake. These scales measure the energy released by an earthquake and provide a numerical value to indicate its intensity.
Yes we still use the richtor scale today,, to find the force of the earthquake.
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.
The power of an earthquake is measured using a seismometer to record the seismic waves produced by the earthquake. The magnitude of an earthquake is typically measured using the Richter scale or moment magnitude scale.
You use a seismometer. Then, measure the magnitude according to the Richter scale.
They measure the amplitude of the L waves to rate the earthquake.
The most commonly referred to scale by the press and the public is the Richter scale for measuring earthquake magnitude. However this was actually replaced in the 1970s by the Moment Magnitude scale which is the magnitude scale favoured and in use by seismologists.
The strength of an earthquake is typically measured using the moment magnitude scale (Mw), which takes into account the seismic energy released by the earthquake. This scale provides a single number that represents the overall size of the earthquake. Another commonly used scale is the Richter scale, which measures the amplitude of seismic waves.
The Richter Scale to rate magnitude and seismograph to measure strength
Intensity is commonly measured using scales such as the Richter scale for earthquakes, the Beaufort scale for wind speed, the decibel scale for sound, and the Mercalli scale for earthquake intensity as felt by humans.