Earthquake

From Conservapedia

Jump to: navigation, search
Japan quake 2011.

An earthquake is when the Earth shakes a perceptible amount. As a counterexample to the liberal theory of an Old Earth, earthquakes have been increasing in frequency throughout recorded history:[1]

  • from A.D. 1 to 1800 there was a major earthquake only about every 60 years.
  • in the 19th century there were about 31 earthquakes of magnitude 7 or higher, which averages to about a major earthquake every 3 years.
  • in the 20th century there were 222 such major earthquakes, or on average about one major earthquake every 6 months.
  • in the first decade of the 21st century (2001-2010) there were about 151 such major earthquakes, or on average more than 1 per month.

Atheistic scientists often claim that earthquakes are caused by tectonic activity in an area after the release of stored energy from the rock. But, in fact, earthquakes often do not occur on tectonic plate boundaries or faults where previous movement has occurred. There are currently 500,000 detectable earthquakes in the world each year.

Earthquakes are a significant natural disaster to populations living in areas prone to them, and emergency responses to the hazard vary with economic development. The most powerful and destructive earthquakes occur at tectonic plate boundaries like the San Andreas Fault.

The severity of earthquakes is measured using the Moment Magnitude scale, which replaced the Richter scale in the 1970s. The largest quake ever recorded had a magnitude of 9.5; it struck Chile in 1960.[2] Technically the Moment Magnitude scale only measures the absolute magnitiude; the Mercalli scale is used to measure the felt magnitude - essentially how much the ground shakes over the epicenter of the quake.

Contents

Causes of Earthquakes

Plate Boundaries

Where tectonic plates are moving relative to each other, stress is created as friction prevents the edges of the plates from moving smoothly. When the stress has increased enough to overcome the friction, the plates will release the stored energy by moving abruptly, causing an earthquake.


Intra-Plate Earthquakes

Large movements of plates may cause stress zones that extend far from the boundaries. When this stress includes a weak area in the plate - known as a fault - the fault can release energy by slipping abruptly, again causing an earthquake.


Vulcanism

The movement of magma within volcanoes can induce earthquakes. These are often an indicator of an approaching eruption, as at Mount St Helens.


Earthquakes and a young Earth

Severe earthquakes have doubled every forty years. [3]. If the planet was not young, it would be completely unstable. See Counterexamples to an Old Earth.


Japan quake World latest USGS - PD.jpg



See Also

External links


References

  1. http://www.city-data.com/forum/alaska/1226039-increasing-frequency-major-earthquakes-2013-earthquake.html#ixzz2URWtQ6yV
  2. http://earthquake.usgs.gov/earthquakes/world/10_largest_world.php
  3. Geological Catalogs (Science Frontiers)
Personal tools