Karaca Dag

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  • Turkey
  • Turkey
  • Shield
  • Unknown
  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 37.67°N
  • 39.83°E

  • 1957 m
    6419 ft

  • 213011
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Karaca Dag.



 Available Weekly Reports

There are no Weekly Reports available for Karaca Dag.

There are no Holocene eruptions known for Karaca Dag. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Pearce J A, Bender J F, de Long S E, Kidd W S F, Low P J, Guner Y, Saroglu F, Yilmaz Y, Moorbath S, Mitchell J G, 1990. Genesis of collision volcanism in eastern Anatolia, Turkey. J Volc Geotherm Res, 44: 184-229.

Karaca Dag (also known as Karacalidag) is a broad, 1957-m-high basaltic shield volcano in SE Turkey about 100 km north of the Syrian border. The volcano lies on the Arabian foreland about 150 km SW of the boundary with the Anatolian Plate and has been active since the Pliocene along a N-S-trending set of fissures and craters associated with the nearby Akcakale graben. Potassium-Argon dates of mid-Pleistocene age have been obtained from Karaca Dag lava flows, but Landsat imagery suggests that some lava flows, particularly those on the east flank, may perhaps be only a few thousand years old (Pearce et al., 1990).