Archaeoseismology

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Archaeoseismology is the study of past

natural effects".[2]

The main idea

Earthquakes in the distant past may provide important information for a regional seismic risk assessment. We have quantitative data concerning past earthquakes only from the beginning of the 20th century (as the

seismograph was invented only at the end of the 19th century), but humanity has had to deal with earthquakes throughout its existence. Thus we have extremely limited historical information about seismic risks. A methodology for reconstruction of historical earthquakes was held[clarification needed] during the 20th century, but with very limited results, especially for archaic[clarification needed] earthquakes. Thus research in archaeological sites is needed to try to identify damage and destruction from ancient earthquakes.[3]

Archaeological record

The archaeological record can carry three different types of evidence of seismic activity:

  • The
    archaeological remains are displaced due to the movement of an active fault.[4]
  • The remains and artefacts contained in destruction deposits, associated with the decline of soil or seismic vibration, can be used in the dating of earthquake damage. Other archaeological evidence, such as repairs, abandonment of an archaeological site or architectural changes, can help in identifying ancient earthquakes.[5]
  • Αncient buildings and other man-made structures can be studied for signs of ancient seismic disaster, often associated with soil vibration.[6]

Notable events

See also

References

  1. ^ Giner-Robles, J.L.; et al. (2012). "Archaeoseismology as an emerging science". Sequridad Y Medio Ambiente. Archived from the original on 18 March 2016. Retrieved 15 March 2016.
  2. .
  3. ^ Ambraseys, N. N., 1973. Earth Sciences in Archaeology and History. Antiquity, 47 pp. 229-230
  4. ^ Altunel, E.; et al. (2003). "Earthquake faulting at ancient Cnidus, SW Turkey". Turkish Journal of Earth Sciences. 12 (1): 137–151.
  5. .
  6. .

External links