posted on Mar, 11 2010 @ 12:50 PM
Getting a general historical perspective about earthquakes
The largest recorded earthquake in the United States was a magnitude 9.2 which struck Prince William Sound, Alaska, on March 28, 1964 UTC.
The largest recorded earthquake in the world was a magnitude 9.5 (Mw) in Chile on May 22, 1960.
The earliest reported earthquake in California was felt in 1769 by the exploring expedition of Gaspar de Portola while the group was camping about 48
kilometers (30 miles) southeast of Los Angeles.
Before electronics allowed recordings of large earthquakes, scientists built large spring-pendulum seismometers in an attempt to record the
long-period motion produced by such quakes.
The largest one weighed about 15 tons. There is a medium-sized one three stories high in Mexico City that is still in operation.
The average rate of motion across the San Andreas Fault Zone of California during the past three million years is 56 millimeter/year (two
This is about the same rate at which your fingernails grow. Assuming this rate continues, scientists project that Los Angeles and San Francisco will
be adjacent to one another in approximately 15 million years.
The East African Rift System is a 50-60 kilometers (31-37 miles) wide zone of active volcanics and faulting that extends north-south in eastern Africa
for more than 3000 kilometers (1864 miles) from Ethiopia in the north to Zambezi in the south.
It is a rare example of an active continental rift zone, where a continental plate is attempting to split into two plates which are moving away from
The first "pendulum seismoscope" to measure the shaking of the ground during an earthquake was developed in 1751, and it wasn't until 1855 that
earth faults were recognized as the source of earthquakes.
Moonquakes ("earthquakes" on the moon) do occur, but they happen less frequently and have smaller magnitudes than earthquakes on the earth.
It appears they are related to the tidal stresses associated with the varying distance between the earth and the moon. They also occur at great depth,
about halfway between the surface and the center of the moon.
Although both are sea waves, a tsunami and a tidal wave are two different unrelated phenomena.
A tidal wave is a shallow water wave caused by the gravitational interactions between the sun, moon, and earth.
A tsunami is a sea wave caused by an underwater earthquake or landslide (usually triggered by an earthquake) displacing the ocean water.
The hypocenter of an earthquake is the location beneath the earth's surface where the rupture of the fault begins.
The epicenter of an earthquake is the location directly above the hypocenter on the surface of the earth.
The greatest mountain range is the Mid-Ocean Ridge, extending 64,374 kilometers (40,000 miles) from the Arctic Ocean to the Atlantic Ocean, around
Africa, Asia, and Australia, and under the Pacific Ocean to the west coast of North America.
It has the greatest height of 4207 meters (13,800 feet) above the base ocean depth.
The world's greatest land mountain range is the Himalaya-Karakoram.
It countains 96 of the world's 109 peaks of over 7317 meters (24,000 feet).
The longest range is the Andes of South America which is 7564 kilometers (4700 miles) in length.
Both were created by the movement of tectonic plates.
It is estimated that there are 500,000 detectable earthquakes in the world each year.
One hundred thousand of those can be felt, and 100 of them cause damage.
It is thought that more damage was done by the resulting fire after the 1906 San Francisco earthquake than by the earthquake itself.
A seiche (SAYSH) is what happens in the swimming pools of Californians during and after an earthquake.
It is "an internal wave oscillating in a body of water" or, in other words, it is the sloshing of the water in a swimming pool, or any body of
water, caused by the ground shaking in an earthquake.
It may continue for a few moments or hours, long after the generating force is gone.
A seiche can also be caused by wind or tides.
Each year the southern California area has about 10,000 earthquakes.
Most of them are so small that they are not felt. Only several hundred are greater than magnitude 3.0, and only about 15-20 are greater than magnitude
If there is a large earthquake, the aftershock sequence will produce many more earthquakes of all magnitudes for many months.
The magnitude of an earthquake is a measured value of the earthquake size.
The magnitude is the same no matter where anyone is, or how strong or weak the shaking was in various locations.
The intensity of an earthquake is a measure of the shaking created by the earthquake, and this value does vary with location.
The Wasatch Range, with its outstanding ski areas, runs North-South through Utah, and like all mountain ranges it was produced by a series of
The 386 kilometers-long (240-miles) Wasatch Fault is made up of several segments, each capable of producing up to a M7.5 earthquake.
During the past 6000 years, there has been a M6.5+ about once every 350 years, and it has been 150 years since the last powerful earthquake.
There is no such thing as "earthquake weather".
Statistically, there is an equal distribution of earthquakes in cold weather, hot weather, rainy weather, etc.
Furthermore, there is no physical way that the weather could affect the forces several miles beneath the surface of the earth.
The changes in barometric pressure in the atmosphere are very small compared to the forces in the crust, and the effect of the barometric pressure
does not reach beneath the soil.
From 1975-1995, there were only four U.S. states that did not have any earthquakes: Florida, Iowa, North Dakota, and Wisconsin.
The core of the earth was the first internal structural element to be identified.
In 1906, R.D. Oldham discovered internal structural source from his studies of earthquake records.
The inner core of the earth is solid, and the outer core is liquid; and so, does not transmit the shear wave energy released during an earthquake.
The swimming pool at the University of Arizona, in Tucson, lost water from sloshing (seiche) caused by the 1985 M8.1 Michoacan, Mexico, earthquake
2000 kilometer (1240 miles) away.
Earthquakes occur in the central portion of the United States too!
Some very powerful earthquakes occurred along the New Madrid fault in the Mississippi Valley in 1811-1812.
The effects of shaking from these magnitude 8+ earthquakes caused church bells to ring in Boston, Massachusetts, nearly 1600 kilometers (1000 miles)
Most earthquakes occur at depths of less than 80 kilometer (50 miles) from the earth's surface.
The San Andreas fault, in California, is NOT a single, continuous fault, but rather it is actually a fault zone made up of many segments.
Movement may occur along any of the many fault segments along the zone at any time.
The San Andreas fault system is more that 1300 kilometers (800 miles) long, and in some spots it is as much as 16 kilometers (10 miles) deep.
The world's deadliest recorded earthquake occurred in 1556, in central China.
It struck a region where most people lived in caves carved from soft rock. These dwellings collapsed during the earthquake, killing an estimated
In 1976, another deadly earthquake struck in Tangshan, China, where more than 250,000 people were killed.
Florida and North Dakota have the smallest number of earthquakes in the United States.
The deepest earthquakes typically occur at plate boundaries where the earth's crust is being subducted into the earth's mantle.
These occur as deep as 750 kilometers (400 miles) below the surface.
Alaska is the most earthquake-prone state in the U.S. and one of the most seismically active regions in the world.
Alaska experiences a magnitude 7 earthquake almost every year, and a magnitude 8 or greater earthquake on average every 14 years.
The majority of the earthquakes and volcanic eruptions occur along plate boundaries; such as, the boundary between the Pacific Plate and the North
One of the most active plate boundaries where earthquakes and eruptions are frequent, for example, is around the massive Pacific Plate commonly
referred to as the "Pacific Ring of Fire".
The earliest recorded evidence of an earthquake was traced back to 1831 B.C. in the Shandong province of China, but there is a fairly complete record
starting in 780 B.C. during the Zhou Dynasty in China.
It was recognized as early as 350 B.C. by the Greek scientist Aristotle that soft ground shakes more than hard rock in an earthquake.
The cause of earthquakes was stated correctly in 1760 by British engineer John Michell, one of the first fathers of seismology, in a memoir where he
wrote that earthquakes and the waves of energy that they make are caused by "shifting masses of rock miles below the surface".
In 1663, the European settlers experienced their first earthquake in America.
Human beings can detect sounds in the frequency range 20-10,000 Hertz.
If a P wave refracts out of the rock surface into the air, and it has a frequency in the audible range, it will be heard as a rumble.
Most earthquake waves have a frequency of less than 20 Hz, so the waves themselves are usually not heard. Most of the rumbling noises heard during an
earthquake are the buildings and their moving contents.
When the Chilean earthquake occurred in 1960, seismographs recorded seismic waves that traveled all around the earth.
These seismic waves shook the entire earth for many days! This phenomenon is called the free oscillation of the earth.
The San Andreas Fault of California was named in 1895 by geologist A.C. Lawson.
He named it after the San Andreas Lake, a sag pond through which the fault passes about 20 miles south of San Francisco.
He probably did not realize at the time that the fault ran almost the entire length of California!
The interior of Antarctica has icequakes which, although they are much smaller, are perhaps more frequent than earthquakes in Antarctica.
The icequakes are similar to earthquakes, but occur within the ice sheet itself instead of the land underneath the ice.
Some polar observers have reported that they can hear the icequakes and see them on the South Pole seismograph station, but they are much too small to
be seen on enough stations to obtain a location.
—The information for this page was provided
by the United States Geological Survey’s (USGS) Earthquake Hazards Program
as part of their effort to reduce earthquake hazard in the United States.
The USGS is a component of the congressionally established,
multi-agency National Earthquake Hazards Reduction Program (NEHRP).
More information with references to earthquakes may be seen at this seismo- unit.
If there are any numbers below, use them to see other pages in this unit.