Skip to content
Surf Wiki
Save to docs
history

From Surf Wiki (app.surf) — the open knowledge base

1949 Karlıova earthquake

Earthquake in Turkey

1949 Karlıova earthquake

Earthquake in Turkey

FieldValue
title1949 Karlıova earthquake
timestamp1949-08-17 18:44:17
isc-event896772
anss-urliscgem896772
local-date
local-time20:44:17
map2{{Location mapTurkeyrelief=1
lat39.0
long40.5
markBullseye1.png
marksize40
positiontop
width250
floatright
caption}}
magnitude7.1
6.7
location
countries affectedTurkey, Karlıova
intensity
typeStrike-slip
faultNorth Anatolian Fault
casualties320–450

| isc-event = 896772 | anss-url = iscgem896772 | local-date = | local-time = 20:44:17 6.7

Map of Anatolian plate showing main tectonic boundaries

The 1949 Karlıova earthquake occurred at 18:44 UTC on 17 August with an epicenter near Karlıova in Bingöl Province, Eastern Anatolia region of Turkey. It had an estimated magnitude of 6.7, a maximum felt intensity of X (Extreme) on the Mercalli intensity scale, and caused 320–450 casualties and destroyed 3,500 buildings.

Tectonic setting

The Karlıova region is the location of the triple junction between the boundaries of the Eurasian plate, Anatolian plate and the Arabian plate, the North Anatolian Fault, East Anatolian Fault and the Mus fold and thrust belt, which passes to the east into the Zagros fold and thrust belt. The earthquake occurred at the eastern end of the North Anatolian Fault.

Characteristics

The seismic moment estimated for this earthquake is 3.5E+26, equivalent to a magnitude of 7.1 on the moment magnitude scale. The estimated fault length involved is 63 km.

The earthquake ruptured the easternmost part of the Yedisu segment (FS3, also known as the Elamalı segment) and most of the Ilıpınar segment (FS2 & FS1), although it remains unclear whether the rupture continued as far as Karlıova itself.

References

References

  1. Boğaziçi Üniversitesi. "Bogazici University Kandilli Observatory and Earthquake Research Institute National Earthquake Monitoring Center (NEMC) List of major earthquakes 1900–2004".
  2. NGDC. "Comments for the Significant Earthquake".
  3. (2016). "Asian Law in Disasters: Toward a Human-Centered Recovery". [[Routledge]].
  4. (2009). "Collision and collapse at the Africa-Arabia-Eurasia subduction zone". Geological Society.
  5. Ellsworth, W.L.. "Earthquake Probabilities in the San Francisco Bay Region: 2002–2031". United States Geological Survey.
  6. (2014). "Kuzey Anadolu Fay Zonu, Ilıpınar Segmenti'nin (Karlıova, Bingöl) Paleosismolojisi (Paleoseismology of the Ilıpınar Segment (Karlıova, Bingöl), The North Anatolian Fault Zone)". Türkiye Jeoloji Bülteni (Geological Bulletin of Turkey).
  7. (2015). "Spatial slip behavior of large strike-slip fault belts: Implications for the Holocene slip rates of the eastern termination of the North Anatolian Fault, Turkey". Journal of Geophysical Research: Solid Earth.
  8. (1988). "Strike-slip fault geometry in Turkey and its influence on earthquake activity". Tectonics.
Info: Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

Want to explore this topic further?

Ask Mako anything about 1949 Karlıova earthquake — get instant answers, deeper analysis, and related topics.

Research with Mako

Free with your Surf account

Content sourced from Wikipedia, available under CC BY-SA 4.0.

This content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.

Report