The Richter Scale, also referred to as the Magnitude Scale, measures the size and scope of earthquakes and seismic activity in general. This system of measurement was created by Charles Richter in 1935, at the California Institute of Technology. Since much of the western US state lies on a faultline, the development of an accurate system to measure earthquakes was especially important. The Richter scale was later used to measure seismic activity in other parts of the world.
An earthquake categorized as 2.0 or less on the Richter Scale is usually a very minor tremor and one that may not even be felt by laypeople in the area. Earthquakes listed as 3.0 are usually felt, although they seldom produce any damage. A 4.0 tremor is very noticeable and make cause minor damage, generally in private homes, where items may fall from shelves. Earthquakes listed as 5.0 may cause some buildings to collapse, while anything above 6.0 will result in severe structural damage. An earthquake categorized as 9.0 or above will produce fatal and catastrophic results.
An earthquake categorized as 2.0 or less on the Richter Scale is usually a very minor tremor and one that may not even be felt by laypeople in the area. Earthquakes listed as 3.0 are usually felt, although they seldom produce any damage. A 4.0 tremor is very noticeable and make cause minor damage, generally in private homes, where items may fall from shelves. Earthquakes listed as 5.0 may cause some buildings to collapse, while anything above 6.0 will result in severe structural damage. An earthquake categorized as 9.0 or above will produce fatal and catastrophic results.