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The Global Volcanism Program has no activity reports for Jabal ad Druze.
The Global Volcanism Program has no Weekly Reports available for Jabal ad Druze.
The Global Volcanism Program has no Bulletin Reports available for Jabal ad Druze.
The Global Volcanism Program is not aware of any Holocene eruptions from Jabal ad Druze. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Jabal ad Druze page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Al-Arab, Djebel | Druz, Jabal al | Duruz, Jabal ed | Duraz, Jebel | Drouz, Djebel ed|
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Snow-capped Tell Qeni is the highest point of the Jabal ad Druze volcanic field, the southernmost in Syria. It lies in the Haurun-Druze Plateau in SW Syria near the border with Jordan. The most prominent feature of this volcanic field is 1803-m-high Jabal ad Druze. The alkaline volcanic field consists of a group of 118 basaltic volcanoes active from the lower-Pleistocene to the Holocene.
Anonymous photo by Wikipedia user KFZI310, 2006.
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. 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.
Bender F, 1975. Geology of the Arabian Peninsula - Jordan. U S Geol Surv Prof Pap, 560-I: 1-36.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
Krienitz M-S, Haase K M, Mezger K, Shaikh-Mashail M A, 2007. Magma genesis and mantle dynamics at the Harrat Ash Shamah volcanic field (southern Syria). J Petr, 48: 1513-1542.
Mouty M, Delaloye M, Fontignie D, Piskin O, Wagner J-J, 1992. The volcanic activity in Syria and Lebanon between Jurassic and Actual. Schweiz Mineral Petrogr Mitt: 72: 91-105.
Shaw J E, Baker J A, Menzies M A, Thirlwall M F, Ibrahim K M, 2003. Petrogenesis of the largest intraplate volcanic field on the Arabian Plate (Jordan): a mixed lithosphere-asthenosphere source activated by lithospheric extension. J Petr, 44: 1657-1679.
|Large Eruptions of Jabal ad Druze||Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).|
|WOVOdat||WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.|
|EarthChem||EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).|
|Smithsonian Collections||Search the Smithsonian's NMNH Department of Mineral Sciences collections database. Go to the "Search Rocks and Ores" tab and use the Volcano Name drop-down to find samples.|