Jump to content

1970 Colombia earthquake

Coordinates: 1°36′S 72°32′W / 1.6°S 72.53°W / -1.6; -72.53
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Dawnseeker2000 (talk | contribs) at 00:34, 13 December 2015 (simplify). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

1970 Colombia earthquake
1970 Colombia earthquake is located in Colombia
1970 Colombia earthquake
UTC time??
Magnitude8.0 Mw [1]
Depth645 km (401 mi) [1]
Epicenter1°36′S 72°32′W / 1.6°S 72.53°W / -1.6; -72.53 [1]
Areas affectedColombia
Casualties1 dead, several injured [2]

The 1970 Colombia earthquake occurred in Colombia on July 31.

Details and aftermath

The shock killed one person and injured several others. Because it was a deep-focus earthquake, shaking occurred over an extensive area, including San Juan, Bogotá, Caracas, Buenos Aires, and São Paulo; it was felt as far north as Mexico City.[3] Its depth forestalled more serious casualties,[3] and there were no aftershocks.[4]

The depth of the earthquake prompted scientists in South America to install seismometer networks focused on long-period earthquakes.[3] Until the 1994 Bolivia earthquake, the 1970 Colombia earthquake was famous among seismologists as the largest deep earthquake.[5]

Analysis

A study completed by Dziewonski and Gilbert (1974) determined that the earthquake had featured isotropic compression, or an increase in density near the rupture point similar to an implosion;[6] this was released to great controversy.[5] They also claimed that the compression had been initiated 80 seconds before the actual earthquake's short-period shaking. Many studies have reached differing conclusions including a dearth of isotropic movement, and many scientists feel that resolution created errors in Dziewonski and Gilbert's findings.[7] In 1997, Russakoff, Ekstrom, and Trump reassessed their findings utilizing more advanced equipment that factored in shear wave splitting and coupling (the measure of how tightly locked two sides of a fault or plate are) and confirmed that there was very little isotropic compression.[5]

References

  1. ^ a b c d ISC (2015), ISC-GEM Global Instrumental Earthquake Catalogue (1900-2009), Version 2.0, International Seismological Centre
  2. ^ IISEE. "IISEE Catalogue Search parameters page". Catalog of Damaging Earthquakes in the World. Retrieved August 18, 2013.
  3. ^ a b c "Historic Earthquakes: Colombia 1970". United States Geological Survey. November 1, 2012. Retrieved July 30, 2013.
  4. ^ Karato, Shun'ichiro (2003). The Dynamic Structure of the Deep Earth: An Interdisciplinary Approach. Princeton University Press. p. 162. ISBN 978-0691095110.
  5. ^ a b c Russakoff, Ekstrom, and Trump, pg. 20423.
  6. ^ Kennett, L.N. and Simons, R.S. (1976). "An Implosive Precursor to the Colombia Earthquake 1970 July 31". Geophysical Journal International. 44. Oxford University Press: 471. Bibcode:1976GeoJI..44..471K. doi:10.1111/j.1365-246X.1976.tb03668.x.{{cite journal}}: CS1 maint: multiple names: authors list (link) CS1 maint: unflagged free DOI (link)
  7. ^ Russakoff, Ekstrom, and Trump, pg. 20424.

Sources