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2. Massage - Wikipedia

   en.wikipedia.org/wiki/Massage

   Some states allow license reciprocity, where licensed massage therapists who relocate can relatively easily obtain a license in their new state. [170] In 1997 there were an estimated 114 million visits to massage therapists in the US. [157] Massage therapy is the most used type of alternative medicine in hospitals in the United States. [159]

3. Rosen Method Bodywork - Wikipedia

   en.wikipedia.org/wiki/Rosen_Method_Bodywork

   Rosen Method Bodywork (or Rosen Method) is a type of Complementary and alternative medicine. This bodywork, described as 'psychosomatic', claims to help integrate one's bodily and emotional/mental experience. In the tradition of sensory awareness methods, Rosen Method Bodywork focuses clients' attention onto internal sensations and emotions ...

4. Massage table - Wikipedia

   en.wikipedia.org/wiki/Massage_table

   Massage table. A massage table is used by massage therapists to position the client to receive a massage. Most are manufactured with client comfort and therapist ergonomics in mind. A typical table has an easily cleaned, heavily padded surface, and a face cradle that allows the client to breathe easily while lying face down.

5. Expert debunks myths about what to do during an earthquake - AOL

   www.aol.com/news/2015-10-14-expert-debunks-myths...

   An enduring earthquake image of California is a collapsed adobe home with the door frame as the only standing part. From this came our belief that a doorway is the safest place to be during an ...

6. Aftershock - Wikipedia

   en.wikipedia.org/wiki/Aftershock

   e. In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency ...

7. Foreshock - Wikipedia

   en.wikipedia.org/wiki/Foreshock

   Foreshock activity has been detected for about 40% of all moderate to large earthquakes, [2] and about 70% for events of M>7.0. [3] They occur from a matter of minutes to days or even longer before the main shock; for example, the 2002 Sumatra earthquake is regarded as a foreshock of the 2004 Indian Ocean earthquake with a delay of more than two years between the two events.