GEOLOGY

Detailed explanation-1: -The most common measure of earthquake strength is the Richter scale, which measures the “moment magnitude” and describes horizontal movement. It is a logarithmic scale. A magnitude 6 earthquake has ten times more energy intensity or movement than a magnitude 5 on the Richter scale.

Detailed explanation-2: -The Richter scale measures the largest wiggle (amplitude) on the recording, but other magnitude scales measure different parts of the earthquake. The USGS currently reports earthquake magnitudes using the Moment Magnitude scale, though many other magnitudes are calculated for research and comparison purposes.

Detailed explanation-3: -The Richter Scale It was replaced with the Moment Magnitude Scale, which records all the different seismic waves from an earthquake to seismographs across the world. Richter’s equations are still used for forecasting future earthquakes and calculating earthquake hazards.

Detailed explanation-4: -The first widely-used method, the Richter scale, was developed by Charles F. Richter in 1934. It used a formula based on the amplitude of the largest wave recorded on a specific type of seismometer and the distance between the earthquake and the seismometer.

Detailed explanation-5: -The idea of a logarithmic earthquake magnitude scale was first developed by Charles Richter in the 1930’s for measuring the size of earthquakes occurring in southern California using relatively high-frequency data from nearby seismograph stations.