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  2. Business letter - Wikipedia

    en.wikipedia.org/wiki/Business_letter

    Business letters can have many types of content, for example to request direct information or action from another party, to order supplies from a supplier, to point out a mistake by the letter's recipient, to reply directly to a request, to apologize for a wrong, or to convey goodwill. A business letter is sometimes useful because it produces a ...

  3. Earthquake - Wikipedia

    en.wikipedia.org/wiki/Earthquake

    Most earthquake clusters consist of small tremors that cause little to no damage, but there is a theory that earthquakes can recur in a regular pattern. [32] Earthquake clustering has been observed, for example, in Parkfield, California where a long-term research study is being conducted around the Parkfield earthquake cluster. [33]

  4. Moment magnitude scale - Wikipedia

    en.wikipedia.org/wiki/Moment_magnitude_scale

    Nonetheless, seismic moment is regarded as the fundamental measure of earthquake size, [44] representing more directly than other parameters the physical size of an earthquake. [45] As early as 1975 it was considered "one of the most reliably determined instrumental earthquake source parameters".

  5. Seismic magnitude scales - Wikipedia

    en.wikipedia.org/wiki/Seismic_magnitude_scales

    An earthquake's seismic moment can be estimated in various ways, which are the bases of the M wb, M wr, M wc, M ww, M wp, M i, and M wpd scales, all subtypes of the generic M w scale. See Moment magnitude scale § Subtypes for details. Seismic moment is considered the most objective measure of an earthquake's "size" in regard of total energy. [50]

  6. Seismic moment - Wikipedia

    en.wikipedia.org/wiki/Seismic_moment

    Seismic moment is a quantity used by seismologists to measure the size of an earthquake.The scalar seismic moment is defined by the equation =, where . is the shear modulus of the rocks involved in the earthquake (in pascals (Pa), i.e. newtons per square meter)

  7. Elastic-rebound theory - Wikipedia

    en.wikipedia.org/wiki/Elastic-rebound_theory

    In geology, the elastic-rebound theory is an explanation for how energy is released during an earthquake. As the Earth's crust deforms, the rocks which span the opposing sides of a fault are subjected to shear stress. Slowly they deform, until their internal rigidity is exceeded.

  8. List of historical earthquakes - Wikipedia

    en.wikipedia.org/wiki/List_of_historical_earthquakes

    Historical earthquakes is a list of significant earthquakes known to have occurred prior to the early 20th century. As the events listed here occurred before routine instrumental recordings – later followed by seismotomography imaging technique, [1] observations using space satellites from outer space, [2] artificial intelligence (AI)-based early earthquake warnings [3] – they rely mainly ...

  9. Seismology - Wikipedia

    en.wikipedia.org/wiki/Seismology

    Seismology (/ s aɪ z ˈ m ɒ l ə dʒ i, s aɪ s-/; from Ancient Greek σεισμός (seismós) meaning "earthquake" and -λογία (-logía) meaning "study of") is the scientific study of earthquakes (or generally, quakes) and the generation and propagation of elastic waves through planetary bodies.