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Fluid Venting System - Hydrocarbon Leakage Indicators
Picture

Photo album of mud volcanoes in Azerbaijan
​                                                                                                                                                                                                                                                - 
by Martin Hovland

​"Mud volcanoes are some of the world's most dynami and statically unstable clastic features. We define a mud volcano as a positive topographical feature constructed mainly of mud, and other sedimentary constituents, which periodically or continuously vents liquid mud, including water, oil, and gas."  -  Hovland et al. (1997).
​
Picture
Lokbatan mud volcano and oil field in the background. A man is collecting salt from the Lokbatan lagune.
The Lokbatan mud volcano had a violent and hot eruption in October 2001.


​

​This photo album includes pictures of mud volcanoes at Garadagh, Lake Masasyr-Gel, Lokbatan, Dashgil, Kotyrdag and ​Perigishgy as shown below. 
A muddy "bathtub" - a gryphon, in Garadagh.
The side view of the muddy "bathtub" - gryphon, in Garadagh.
A close up of the side view of the muddy "bathtub" - gryphon, Garadagh.
A close up to the crest of the "bathtub" - gryphon, Garadagh.
The top of the "bathhub" - gryphon, Garadagh. Notice that there is a mud trail formed by continuous gas bubbling in the middle of the mud pool.
A close up to the mud trail formed by the continuous gas bubbling in the middle of the mud pool, Garadagh.
The focused bubble seep points on the liquid mud surface, Garadagh.
A raising mud cone in Garadagh.
A picture of Planke in Garadagh. The first author of "Mud and fluid migration in active mud volcanoes in Azerbaijan" - Planke et al. (2003).
The background landscape of the muddy "bathtub" in the first photo, Garadagh.
A mud volcano shown on the background landscape, Garadagh.
A mud volcano shown on the background landscape, Garadagh.
The salt lake "Massasyr-Gel". Plank and Hovland are taking salt samples. The authors of "Mud and fluid migration in active mud volcanoes in Azerbaijan" - Planke et al. (2003).
Planke is next to a pile of salt in the lake Massasyr-Gel.
A view on Lake Massasyr-Gel.
The salt lake Masasyr-Gel.
Around the salt lake Masasyr-Gel
Dry mud floor in Lokbatan which is partially covered by vegetation.
Dry mud floor in Lokbatan which is partially covered by vegetation.
A small hole had been dig in the dry mud for temperature measurement, Lokbatan.
A small hole had been dig in the dry mud for temperature measurement, Lokbatan.
A small hole had been dig in the dry mud for temperature measurement, Lokbatan.
A small hole had been dig in the dry mud for temperature measurement, Lokbatan.
The edge of the salt lake in Lokbatan, and the Lokbatan mud volcano in the background.
A close up to the salt on the floor, Lokbatan.
A man is collecting salt in the lake, Lokbtan.
A man is collecting salt from the Lokbatan lagune.
Collecting sample of the fluid in the mini pool, Lokbatan.
Oil feld in Dashgil.
A gryphon in Dashgil.
Gryphon of Dashgil.
Gryphons in Dashgil.
Gryphons in Dashgil.
Mud cones in Dashgil.
Mud cones in Dashgil.
A salse in Dashgil.
The crest of a gryphon in Dashgil.
A small gryphon in Dashgil.
A salse in Dashgil.
A salse in Dashgil.
A gryphon in Dashgil.
A dry-out mud cone in Dashgil.
Dry-out mud gryphon, Dashgil.
The crest of a gryphon, Dashgil.
Mud flow riches in hydrocarbon, Dashgil.
Mud flow riches in hydrocarbon, Dashgil.
Taking temperature of the mud flood, Deashgil.
Taking temperature of a small gryphon, Dashgil.
Taking temperature of a small gryphon, Dashgil.
A tiny gryphon, Dashgil.
Gryphones observed in Dashgil.
A gryphon in Dashgil.
A gryphon in Dashgil.
The crest of a gryphon, Dashgil.
The crest of a gryphon, Dashgil.
The crest of a gryphon, Dashgil.
Close up to the crater of the gryphon in Dashgil.
Mud cracks observed in Dashgil.
Oil field in Kotyrdag.
Stiff mud extrusion by overpressured fluid in Kotyrdag.
Stiff mud extrusion by overpressured fluid in Kotyrdag.
A close up to the mud extrusion in Kotyrdag.
A close up to the mud extrusion in Kotyrdag.
A close up to the mud extrusion in Kotyrdag.
A close up to the mud extrusion in Kotyrdag.
A close up to the mud extrusion driven by overpressured fluid in Kotyrdag.
Kotyrdag
Kotyrdag
A mud cone in Perigishgy.
Taking temperature at the top of the mud cone in Perigishgy.
Mud flow is putting out from the mud cone, Perigishgy.
Mud flow is putting out from the mud cone with brown colour liquid (hydrocarbon), Perigishgy.
Liquid hydrocarbon (brown) is coming out with the mud flow, Perigishgy.
Liquid hydrocarbon (brown) is coming out with the mud flow, Perigishgy.
A close up to the flank of the mud cone, Perigishgy.


​References

Hovland, M., Hill, A., & Stokes, D. (1997). The structure and geomorphology of the Dashgil mud volcano, Azerbaijan. Geomorphology, 21(1), 1-15.
Planke, S., Svensen, H., Hovland, M., Banks, D. A., & Jamtveit, B. (2003). Mud and fluid migration in active mud volcanoes in Azerbaijan. Geo-Marine Letters, 23(3-4), 258-268.
 
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