Earthquakes
About 8,000 mini-quakes a day, and on average, one exceptionally big one per year

by Borgna Brunner

Source: NOAA
Earthquakes in residential areas, such as this 1964 one in Seward, Alaska, can cause unparalleled damage to life and property.
There are thousands upon thousands of earthquakes annually, ranging on average from 18 major quakes to more than 2 million very minor ones per year (approximately 8,000 per day). On average, we can expect one exceptionally big one (with a magnitude of 8 or higher) each year.


Earthquakes are caused by forces deep within Earth's interior that continuously affect its surface. When the energy from these forces is released suddenly—usually by shearing movements along faults in the Earth's crust—an earthquake results. See also plate tectonics.


Not "On the Richter Scale"

Although "on the Richter Scale" is still a commonly used expression, the scale, developed by Charles F. Richter of California Institute of Technology in 1935, is no longer the most commonly used magnitude measurement. One of its flaws is its imprecision in measuring the biggest earthquakes, those in the range of 8 or 9.


Different methods of measuring magnitude have superseded the Richter Scale, including surface-wave magnitude, which measures the seismic waves crackling around Earth's surface, and moment magnitude, the newest method, which is based on the size of the fault on which an earthquake occurs and the amount the Earth slips. Moment magnitude is the most uniformly applicable scale.

Intensity versus Magnitude

RELATED LINKS
Major Earthquakes Around the World, 2011

Estimated Earthquake Deaths in 2011

Ten Largest Earthquakes of the Century

25 Largest Earthquakes in the United States

The Great San Francisco Earthquake of 1906

Encyclopedia: Earthquakes

Encyclopedia: Tsunami

Frequency of Earthquakes

Seismology

Floods, Avalanches, and Tidal Waves

Quiz: Disasters
These two terms are often confused: intensity is based on the observed effects of an earthquake on its surroundings, whereas magnitude measures the amount of seismic energy released.

The Modified Mercalli (MM) Intensity Scale measures 12 increasing levels of intensity (each designated by a Roman numeral) from imperceptible shaking to catastrophic destruction. More subjective and less scientific than magnitude, intensity is nevertheless a meaningful way of capturing the terror and destruction of an earthquake. It is the intensity of the 1906 San Francisco earthquake that is remembered, not its magnitude.


The Twentieth Century's Largest Earthquake

Three of the ten largest earthquakes of the twentieth century occurred in Alaska, striking in 1957, 1964, and 1965. The strongest of these (magnitude: 9.2) took place on Good Friday in 1964, hitting 80 miles east of Anchorage. The biggest earthquake of the century struck Chile on May 22, 1960. Its magnitude, the highest ever recorded, was 9.5.

The deadliest earthquake of all time is believed to have occurred on Jan. 24, 1556, in Shaanxi (Shensi) Province, China — 830,000 were killed.

Tsunami

The Alaskan Good Friday earthquake was followed by tsunami, or tidal waves, that reached 50 feet high and traveled a phenomenal 8,445 miles at 450 miles per hour. Tsunami is a Japanese term (tsu, port; nami, waves) presumably referring to the rising height of tsunami as they approach shore.

Breaking on land, these tremendous waves can cause enormous destruction. The deadliest tsunami ever occurred on Dec, 26, 2004, killing more than 225,000 people and leaving millions homeless.

In addition to earthquakes, volcanoes can cause tsunami—after the eruption of Krakatoa on August 27, 1883, more than 36,000 people were killed by the tsunami alone.

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