Porak: Difference between revisions
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'''Porak''' or '''Axarbaxar''' ("gutted belly" in Azerbaijani<ref name="BubnovLebedev2014">{{cite journal|last1=Bubnov|first1=S. N.|last2=Lebedev|first2=V. A.|last3=Chernyshev|first3=I. V.|last4=Sagatelyan|first4=A. K.|last5=Dokuchaev|first5=A. Ya.|last6=Gol’tsman|first6=Yu. V.|last7=Oleinikova|first7=T. I.|last8=Griboedova|first8=I. G.|title=The potentially active Porak neovolcanic center (Lesser Caucasus, Armenia): The composition of lavas and melt sources|journal=Doklady Earth Sciences|volume=459|issue=1|year=2014|pages=1365–1370|issn=1028-334X|doi=10.1134/S1028334X14110014}}</ref>) is a [[stratovolcano]] located in the [[Vardenis]] volcanic ridge. It lies about {{convert|20|km|0|abbr=on}} southeast of [[Lake Sevan]] and the [[volcanic field]] spans the border between [[Armenia]] and [[Azerbajian]] with [[lava flow]]s running into both countries. Ten [[satellite cone]]s and fissure vents lie on the flanks of the volcano.<ref>{{cite gvp|vn=214090|name=Porak|accessdate=20 July 2015}}</ref> |
'''Porak''' or '''Axarbaxar''' ("gutted belly" in Azerbaijani<ref name="BubnovLebedev2014">{{cite journal|last1=Bubnov|first1=S. N.|last2=Lebedev|first2=V. A.|last3=Chernyshev|first3=I. V.|last4=Sagatelyan|first4=A. K.|last5=Dokuchaev|first5=A. Ya.|last6=Gol’tsman|first6=Yu. V.|last7=Oleinikova|first7=T. I.|last8=Griboedova|first8=I. G.|title=The potentially active Porak neovolcanic center (Lesser Caucasus, Armenia): The composition of lavas and melt sources|journal=Doklady Earth Sciences|volume=459|issue=1|year=2014|pages=1365–1370|issn=1028-334X|doi=10.1134/S1028334X14110014}}</ref>) is a [[stratovolcano]] located in the [[Vardenis]] volcanic ridge. It lies about {{convert|20|km|0|abbr=on}} southeast of [[Lake Sevan]] and the [[volcanic field]] spans the border between [[Armenia]] and [[Azerbajian]] with [[lava flow]]s running into both countries. Ten [[satellite cone]]s and fissure vents lie on the flanks of the volcano.<ref>{{cite gvp|vn=214090|name=Porak|accessdate=20 July 2015}}</ref> |
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The Porak volcano itself and the third stage has been dated 15 ± 15 ka by K-Ar dating.<ref name="BubnovLebedev2014" /> Two long lava flows, one of which 21km long, stretch from the field north and northeastwards. There are thermal springs in the area, and the Middle Pleistocene |
The Porak volcano itself and the third stage has been dated 15 ± 15 ka by K-Ar dating.<ref name="BubnovLebedev2014" /> Two long lava flows, one of which 21km long, stretch from the field north and northeastwards. There are thermal springs in the area, and the Middle Pleistocene '''Khonarassar''' fault area lies to the north of the Porak centre.<ref name="KarakhanianDjrbashian2002" /><ref>[http://www.bgs.ac.uk/vogripa/searchVOGRIPA.cfc?method=detail&id=95]</ref> The complex is built on partly [[sedimentary rock]] and partly [[volcanogenic]] [[Late Cretaceous]] and [[Eocene]] series with [[Paleogene]] intrusions.<ref name="BubnovLebedev2014" /> |
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==Description== |
==Description== |
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Revision as of 17:18, 21 July 2015
| Porak, Axarbaxar | |
|---|---|
 A pyroclastic cone of the Porak volcanic field. | |
| Highest point | |
| Elevation | 2,800 m (9,200 ft) |
| Geography | |
  Porak, Axarbaxar Location on Armenia–Azerbaijan border | |
| Location | Armenia – Azerbaijan border |
| Parent range | Vardenis |
| Geology | |
| Mountain type | Stratovolcano |
| Last eruption | 778 BCE ± 5 years |
Porak or Axarbaxar ("gutted belly" in Azerbaijani[1]) is a stratovolcano located in the Vardenis volcanic ridge. It lies about 20 km (12 mi) southeast of Lake Sevan and the volcanic field spans the border between Armenia and Azerbajian with lava flows running into both countries. Ten satellite cones and fissure vents lie on the flanks of the volcano.[2]
The Porak volcano itself and the third stage has been dated 15 ± 15 ka by K-Ar dating.[1] Two long lava flows, one of which 21km long, stretch from the field north and northeastwards. There are thermal springs in the area, and the Middle Pleistocene Khonarassar fault area lies to the north of the Porak centre.[3][4] The complex is built on partly sedimentary rock and partly volcanogenic Late Cretaceous and Eocene series with Paleogene intrusions.[1]
Description
There are four stages of trachyandesitic lava flows, the oldest composing the Porak volcano itself and the younger three derived from cones and fissures.[1] Two lava flows overly Sevan Lake deposits with thin soil cover form an early Holocene stage. The second stage forms lava flows entering Lake Alaghel and is devoid of soil cover.[3]
Several archaeological sites (one of these dated by radiocarbon analysis on charcoal to be no younger than 3080±40 BP-3200±40 BP) are constructed on the two oldest Holocene stages but not on the most recent stage. Third-stage lava flows run at the edge of one of these sites which was constructed on lavas from the previous two stages, suggesting that the site was affected by historical volcanic activity. There is also evidence of strong earthquake activity 6640±90 BP and between 782 and 773 BC.[3]
Khorkhor inscription
The Khorkhor inscription, in which Argishti I of Urartu records the conquest of the city of Behoura records that during the siege the town was destroyed by an earthquake and eruption of "Mount Bamni". Historians consider it likely that Porak volcano is Mount Bamni and that Behoura was one of the archeological sites in the area.[3] The location of Behoura is controversial, however. The identification of another inscription by Argishti's successor, Sarduri II, gives evidence of another eruption of Porak.[5][6]
Older evidence of volcanic activity, including lacustrine deposits, indicate temporary disappearance of forests in the area before 6,270BP, likely due to forest fires induced by volcanic activity. Petroglyphs dated about 5,000BP also portray volcanic activity.[3][5]
See also
References
- ^ a b c d Bubnov, S. N.; Lebedev, V. A.; Chernyshev, I. V.; Sagatelyan, A. K.; Dokuchaev, A. Ya.; Gol’tsman, Yu. V.; Oleinikova, T. I.; Griboedova, I. G. (2014). "The potentially active Porak neovolcanic center (Lesser Caucasus, Armenia): The composition of lavas and melt sources". Doklady Earth Sciences. 459 (1): 1365–1370. doi:10.1134/S1028334X14110014. ISSN 1028-334X.
- ^ "Porak". Global Volcanism Program. Smithsonian Institution. Retrieved 20 July 2015.
- ^ a b c d e Karakhanian, A.; Djrbashian, R.; Trifonov, V.; Philip, H.; Arakelian, S.; Avagian, A. (2002). "Holocene-historical volcanism and active faults as natural risk factors for Armenia and adjacent countries". Journal of Volcanology and Geothermal Research. 113 (1–2): 319–344. doi:10.1016/S0377-0273(01)00264-5. ISSN 0377-0273.
- ^ [1]
- ^ a b Karakhanian, A.; Jrbashyan, R.; Trifonov, V.; Philip, H.; Arakelian, S.; Avagyan, A.; Baghdassaryan, H.; Davtian, V. (2006). "Historical volcanoes of Armenia and adjacent areas: What is revisited?". Journal of Volcanology and Geothermal Research. 155 (3–4): 338–345. doi:10.1016/j.jvolgeores.2006.04.008. ISSN 0377-0273.
- ^ Haroutiunian, Rouben A. (2006). "The historical volcanoes of Armenia and adjacent areas revisited". Journal of Volcanology and Geothermal Research. 155 (3–4): 334–337. doi:10.1016/j.jvolgeores.2006.04.005. ISSN 0377-0273.