{"id":26,"date":"2018-04-01T22:40:02","date_gmt":"2018-04-01T22:40:02","guid":{"rendered":"http:\/\/curtisarchie.com\/wpmocha\/?page_id=26"},"modified":"2022-09-19T18:36:55","modified_gmt":"2022-09-19T18:36:55","slug":"mud-volcanoes","status":"publish","type":"page","link":"http:\/\/curtisarchie.com\/wpmocha\/?page_id=26","title":{"rendered":"Mud Volcanoes"},"content":{"rendered":"<h1><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-2984 size-full\" src=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/Fig-4-producing-oilfields-and-mud-volcanoes.jpg\" alt=\"\" width=\"838\" height=\"438\" srcset=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/Fig-4-producing-oilfields-and-mud-volcanoes.jpg 838w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/Fig-4-producing-oilfields-and-mud-volcanoes-300x157.jpg 300w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/Fig-4-producing-oilfields-and-mud-volcanoes-768x401.jpg 768w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/Fig-4-producing-oilfields-and-mud-volcanoes-624x326.jpg 624w\" sizes=\"(max-width: 838px) 100vw, 838px\" \/><\/h1>\n<h4 style=\"text-align: center;\">Map showing the location of onshore mud volcanoes in relation to the oilfields.<\/h4>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-2981 size-full\" src=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/TRINIDAD-mud-volcanoes.jpg\" alt=\"\" width=\"10312\" height=\"5174\" srcset=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/TRINIDAD-mud-volcanoes.jpg 10312w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/TRINIDAD-mud-volcanoes-300x151.jpg 300w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/TRINIDAD-mud-volcanoes-768x385.jpg 768w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/TRINIDAD-mud-volcanoes-1024x514.jpg 1024w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/TRINIDAD-mud-volcanoes-624x313.jpg 624w\" sizes=\"(max-width: 10312px) 100vw, 10312px\" \/><\/h2>\n<h2 style=\"text-align: center;\">Location of active and fossil mud volcanoes (after Higgins and Saunders 1974) and the location of oil fields in Trinidad<\/h2>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-3112\" src=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/09\/mud-volcano-origins-4.jpg\" alt=\"\" width=\"1275\" height=\"580\" srcset=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/09\/mud-volcano-origins-4.jpg 1275w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/09\/mud-volcano-origins-4-300x136.jpg 300w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/09\/mud-volcano-origins-4-768x349.jpg 768w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/09\/mud-volcano-origins-4-1024x466.jpg 1024w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/09\/mud-volcano-origins-4-624x284.jpg 624w\" sizes=\"(max-width: 1275px) 100vw, 1275px\" \/><\/p>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=59\">Origin of mud volcanoes<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=3126\">TYPES OF MUD VOLCANOES<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=3135\" target=\"_blank\" rel=\"noopener noreferrer\">OFFSHORE MUD VOLCANOES<\/a><\/h2>\n<h1><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=4514\"><strong>Impact of Eruptions<\/strong><\/a><\/h1>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=2967\">Tabaquite Mud Volcano<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=34\">Devil&#8217;s Woodyard<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=115\">Cascadoux Mud Volcano<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=141\">Karamat Mud Volcano<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=157\">Lagon Bouffe<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=166\">Point Radix<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=181\">Quinam Road<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=197\">Digity Mud Volcano<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=238\">L&#8217;Envieusse Mud Volcano<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=251\">Anglais Point<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=272\">Palo Seco Mud Volcano<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=316\">Marac Mud Volcano<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=320\">Erin Bouffe<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=324\">L&#8217;Eau Michele<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=329\">Chatham<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=425\">Piparo Mud Volcano<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=1012\">Cedros<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=1022\">Rock Dome<\/a><\/h2>\n<h2><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=1018\">Moruga Bouffe<\/a><\/h2>\n<p><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=4124\"><strong>Mudflow deposits at Taparo Point<\/strong><\/a><\/p>\n<p><a href=\"http:\/\/curtisarchie.com\/wpmocha\/?page_id=4152\"><strong>Mudflow deposits at Erin Point<\/strong><\/a><\/p>\n<p>The term \u201cmud-volcano\u201d generally is applied to a more or less violent eruption or surfaces extrusion of watery mud or clay which almost invariably is accompanied by methane gas, and which commonly tends to build up a solid mud or clay deposit around its orifice which may have a conical or volcano-like shape. The source of a mud volcano commonly may be traced to a substantial subsurface layer or diapir of high\u00acly plastic, and probably undercompacted, mud or shale. Mud volcanoes also commonly appear to be related to lines of fracture, faulting, or sharp folding. There appears to be a close in\u00acterrelation between undercompacted (overpres\u00acsured) muds or shale bodies, mud or shale diapirs, mud lumps, and mud volcanoes; and all degrees of gradation from one to another. Mud volcanoes are one of the most useful surface sources of information on the nature of ma\u00acterials in mud diapirs and undercompacted shale bodies.<br \/>\nThe motivating force responsible for a mud volcano is, in part, simply the weight of rock overburden borne by the fluid content of un\u00acdecompacted shales. However, mud volcanoes all over the world are associated so invariably with quietly or explosively escaping methane gas that it is reasonable to conclude that the presence of methane gas in the subsurface is also an essential feature of the phenomenon. The mud of the volcanoes is a mixture of clay and salt water which is kept in the state of a slurry by the boiling or churning activity of escaping methane gas. Probably the methane gas was derived either directly from organic matter in muds or shales or from secondary accumulations in sand stringers within the source-rock shale or from larger reservoirs just above or just below such shales. Some liquid oil often, but not always, is associated with the hydrocarbon gases of mud volcanoes.<br \/>\nCommonly the activity of a mud volcano is simply a mild surface upwelling of muddy and usually saline water accompanied by gas bubbles. However, many ,instances are known of highly explosive eruptions where large masses of rock have been violently blown out hundreds of feet into the air and scattered widely over the countryside. These intermittent violent eruptions strongly suggest that motive force is not merely weight of gradually in\u00accreasing overburden but is due to periodic buildup and release of internal pressure from the generation of methane gas within the shale body or diapir. (Hedberg, H.D. , 1974 , Role of methane generation to undercompacted shales, Shale diapirs and mud volcanoes. Bull. AAPG, V. 58, No. 4, P. 661 \u2013 673)<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-4512\" src=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2022\/09\/Slide10.jpg\" alt=\"\" width=\"1280\" height=\"720\" srcset=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2022\/09\/Slide10.jpg 1280w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2022\/09\/Slide10-300x169.jpg 300w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2022\/09\/Slide10-1024x576.jpg 1024w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2022\/09\/Slide10-768x432.jpg 768w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2022\/09\/Slide10-624x351.jpg 624w\" sizes=\"(max-width: 1280px) 100vw, 1280px\" \/><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-2985 size-full\" src=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-1.jpg\" alt=\"\" width=\"2155\" height=\"1985\" srcset=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-1.jpg 2155w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-1-300x276.jpg 300w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-1-768x707.jpg 768w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-1-1024x943.jpg 1024w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-1-624x575.jpg 624w\" sizes=\"(max-width: 2155px) 100vw, 2155px\" \/><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-2986 size-full\" src=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-2.jpg\" alt=\"\" width=\"2304\" height=\"1715\" srcset=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-2.jpg 2304w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-2-300x223.jpg 300w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-2-768x572.jpg 768w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-2-1024x762.jpg 1024w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-2-624x464.jpg 624w\" sizes=\"(max-width: 2304px) 100vw, 2304px\" \/><\/p>\n<h1><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2988\" src=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-3.jpg\" alt=\"\" width=\"2166\" height=\"2187\" srcset=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-3.jpg 2166w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-3-150x150.jpg 150w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-3-297x300.jpg 297w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-3-768x775.jpg 768w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-3-1014x1024.jpg 1014w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-3-624x630.jpg 624w\" sizes=\"(max-width: 2166px) 100vw, 2166px\" \/><\/h1>\n<h1><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2989\" src=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-4.jpg\" alt=\"\" width=\"2062\" height=\"2109\" srcset=\"http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-4.jpg 2062w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-4-293x300.jpg 293w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-4-768x786.jpg 768w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-4-1001x1024.jpg 1001w, http:\/\/curtisarchie.com\/wpmocha\/wp-content\/uploads\/2019\/08\/mud-volcano-eruption-june-2018-4-624x638.jpg 624w\" sizes=\"(max-width: 2062px) 100vw, 2062px\" \/><\/h1>\n<h1 style=\"text-align: left;\">Trinidad Mud Volcano References<\/h1>\n<p>Archie, C. 2002 Field Trip Guide to : (a) The Upper Cruse Formation at Anglais Point PaloSeco (b) The PaloSeco and Anglais point Mud Volcanoes<span style=\"display: inline !important; float: none; background-color: transparent; color: #333333; font-family: Georgia,'Times New Roman','Bitstream Charter',Times,serif; font-size: 16px; font-style: normal; font-variant: normal; font-weight: 400; letter-spacing: normal; line-height: 24px; orphans: 2; text-align: left; text-decoration: none; text-indent: 0px; text-transform: none; -webkit-text-stroke-width: 0px; white-space: normal; word-spacing: 0px; word-wrap: break-word;\"> GSTT field trip Guide<\/span><b><\/b><i><\/i><u><\/u><\/p>\n<p>Archie,C. 2003 A Visit to the Digity mud volcano, and examination of the sedimentology of the Forest Formation in Debe and Upper Morne L&#8217;Enfer Formation in Penal.<span style=\"display: inline !important; float: none; background-color: transparent; color: #333333; font-family: Georgia,'Times New Roman','Bitstream Charter',Times,serif; font-size: 16px; font-style: normal; font-variant: normal; font-weight: 400; letter-spacing: normal; line-height: 24px; orphans: 2; text-align: left; text-decoration: none; text-indent: 0px; text-transform: none; -webkit-text-stroke-width: 0px; white-space: normal; word-spacing: 0px; word-wrap: break-word;\">GSTT Field Guide<\/span><\/p>\n<p>Archie,C. 2004 A visit to the Karamat Mud Volcano and examination of a Forest outcrop in Morne Diablo and Lower Morne L&#8217;Enfer Formation, Renal Rock Road.<span style=\"display: inline !important; float: none; background-color: transparent; color: #333333; font-family: Georgia,'Times New Roman','Bitstream Charter',Times,serif; font-size: 16px; font-style: normal; font-variant: normal; font-weight: 400; letter-spacing: normal; line-height: 24px; orphans: 2; text-align: left; text-decoration: none; text-indent: 0px; text-transform: none; -webkit-text-stroke-width: 0px; white-space: normal; word-spacing: 0px; word-wrap: break-word;\">GSTT Field Guide<\/span><\/p>\n<p>Archie, C. 2006 A guide to selected mud volcanoes of southern Trinidad on mobile shale, Trinidad\u00a0<span style=\"display: inline !important; float: none; background-color: transparent; color: #333333; font-family: Georgia,'Times New Roman','Bitstream Charter',Times,serif; font-size: 16px; font-style: normal; font-variant: normal; font-weight: 400; letter-spacing: normal; line-height: 24px; orphans: 2; text-align: left; text-decoration: none; text-indent: 0px; text-transform: none; -webkit-text-stroke-width: 0px; white-space: normal; word-spacing: 0px; word-wrap: break-word;\"> AAPG Hedberg conference\u00a0<\/span><\/p>\n<p>Archie, Curtis, 2007, Field Trip Guide To Selected Mud Volcanoes in southern Trinidad, Transactions of the 4th Geological Conference of the GSTT<\/p>\n<p>Archie, C. 2009 A Review Of Activity At Devil\u2019s Woodyard 2003 &#8211; 2008 The Hammer, August 2009, p. 26 &#8211; 36<\/p>\n<p>Archie, C. &amp; Moonan, X., 2011, GSTT Field trip to the Marac Quarry and Mud Volcano<\/p>\n<p>Archie, C. , 2012 , A pictoral survey of mud volcanoes in Trinidad, 5th GSTT Conference<br \/>\nArchie, C. , 2012, Activity at the Piparo and Devil&#8217;s Woodyard mud volcanoes : 2003 &#8211; Present, 5th GSTT Conference<\/p>\n<p>Archie, C. , 2012, THE PALO SECO AND ERIN MUD VOLCANOES ALONG THE SOUTHERN ANTICLINE OF TRINIDAD, 5th GSTT Conference<\/p>\n<p>Anderson, Robert 1911 A new gas volcano in Trinidad Science, V. 34, P 834 &#8211; 835<\/p>\n<p>Arnold R. 1912 Note on mud island appearing off Chatam coast, 31\/10\/1911. Petroleum World. March.<br \/>\nArnold R. &amp; Macready G.A. 1956 Island forming mud volcano in Trinidad, British West Indies. Bull. AAPG Vol 40 No 11 p 2748 &#8211; 2758<\/p>\n<p>Banerjee, K.S. &amp; Ifill, A., 2022, Assessment of natural radioactivity level before and after a mud-volcano eruption: A study from Piparo mud-volcano, Trinidad and Tobago, Journal of Environmental Radioactivity 251\u2013252 (2022) 106953<\/p>\n<p>Barr K.W. 1953 The mud volcanoes of Trinidad. Caribbean Quarterly Vol.3 No.2 p 80 &#8211; 85.<br \/>\nBirchwood K.M. 1965 Mud volcanoes in Trinidad. Inst. Petrol. Review Vol.19 No.221 p 164 &#8211; 167.<\/p>\n<p>Blake, O., Ramsook, R., Iyare, U.C., Moonan, X. &amp; Gopaul, R.C., 2021, Integrating pseudo-3D ERT and DEM to map the near-surface structures and morphology of the Piparo mud volcano, Trinidad. Journal of Applied Geophysics 194 (2021) 104442<\/p>\n<p>Bower T.H. 1951 Mudflow occurrence in Trinidad (BWI). Bull AAPG Vol.35, No.4 p 908 &#8211; 912.<br \/>\nBurke, K., Casey, J.; Robertson, P. 1984 Deformation of Orinoco Delta mud diapirs in the South Caribbean strikeslip plate boundary zone<br \/>\nEos, Transactions, American Geophysical Union, April 17, 1984, Vol. 65, Issue 16, pp. 190<br \/>\nCastrec-Rouelle,M., Bourles,D.L., Boulegue,J. Dia, A.N. 2002 Beryllium geochemistry constraints on the hydraulic behavior of mud<br \/>\nvolcanoes: The Trinidad island case. Earth and planetary science letters, V. 203, N 3-4, p.957-966<br \/>\nDeville,E. , Battani, A. Griboulard, R., Gueralis, S., Herbin, J.P., Houzay, J.P. &amp; Prinzhoffer,A. 2002 The origins and processes of mud<br \/>\nvolcanism: insight from Trinidad 16th Caribbean Geological Conference Abstracts, p75<br \/>\nDeville,E. , Battani, A. Griboulard, R., Gueralis, S., Herbin, J.P., Houzay, J.P. &amp; Prinzhoffer,A. 2003 Processes of mud volcanism in the<br \/>\nBarbados-Trinidad compressional system (SE Caribbean): New structural and geochemical data Geophysical research abstracts, V.5,<br \/>\n14128<br \/>\nDeville,E. , Battani, A. Griboulard, R., Gueralis, S., Herbin, J.P., Houzay, J.P. &amp; Prinzhoffer,A. 2003 Processes of mud volcanism in the<br \/>\nBarbados-Trinidad compressional system: New structural , thermal and geochemical data AAPG annual conference, Salt Lake City, Utah<br \/>\nDia, A. N.Castrec-Rouelle, M.; Boulegue, J.; Bourles, D. L. 1998 Deep-sourced fluids and recharge mechanism with surface aquifers; the<br \/>\nTrinidad mud volcanoes case Mineralogical Magazine, September 1998, Vol. 62A, Part 1, pp. 381-382<\/p>\n<p style=\"text-align: left;\">Dia, A.N. , Casterec-Rouelle, M. , Boulegue, J &amp; Comeau, P. 1999 Trinidad mud volcanoes : Where do the expelled fluids come from?<br \/>\nGeochima et Cosmochima Acta, Vol. 63, No. 7\/8, p 1023 &#8211; 1038<br \/>\nDrew I.M., Kerr P.F. &amp; Richardson D.S. 1970 Mud volcano clay, Trinidad, West Indies Bull AAPG V. 54 N.11 p 2101-2110.<\/p>\n<p>Faugeres, J. C., Gonthier, E.; Griboulard, R.; Grousset, F.; Boutolleau, V.; Aouni, M. 1992 Mud volcanoes from Trinidad; tectonic and sedimentary settings; comparison to the South Barbados Wedge Programme dynamique et bilans de la Terre; resultats des travaux 1988-1992<br \/>\nFeyzullayev,A. 2003 Geological conditions and peculiarities of the mud volcanoes formation Abstracts AAPG annual convention, Salt Lake City, Utah,<\/p>\n<p>Gopaul, R., Blake, O., Rambaran, V. Ali, I., Ousman, A., Iyare, U.C., Ramsook, R. &amp; Moonan, X. , 2019, 4D Resistivity and UAV Acquisition and Monitoring of the Piparo Mud Volcano, Trinidad, West Indies. AAPG 2019 International Conference and Exhibition, Buenos Aires, Argentina, August 27-30, 2019<\/p>\n<p>Herring A.T. &amp; Nettleton L.L. 1979 Quantitative analysis of a mud volcano gravity anomaly. Geophysics V.44 N.9 p 1518-1524.<br \/>\nHiggins G.E. &amp; Saunders J. 1974 Mud volcanoes &#8211; their nature and origin. Verhandl Naturf. Ges Base Vol.84 No.1 p 101 &#8211; 152<br \/>\nHiggins G.E. &amp; Saunders J.B. 1967 Report on the 1964 Chatam mud island Erin Bay, Trinidad, West Indies. Bull. AAPG Vol. 51 No.1 p 55- 64.<br \/>\nHiggins G.E. &amp; Saunders J.B. 1974 Mud volcanoes &#8211; their nature and origin. Contributions to the geology and paleobiology of the Caribbean and adjacent areas. Verhandl naturf. Ges. Basel, Band 84, Nr.1, 520pp.<br \/>\nKerr, P. , Drew, I.M. &amp; Richardson, D.S. 1970 Mud volcano clay, Trinidad, West Indies Bull AAPG V. 54, No 11, p 2101 &#8211; 2110<br \/>\nKnight, J.C. , Scott, J.P. &amp; Grierson, L.H. 1998 The Devil&#8217;s Woodyard mud volcano of Trinidad: Chemistry and mineralogy 15th Caribbean geological conference &#8211; Articles, Field guides &amp; abstracts, p84<br \/>\nKnight, J.C. , Scott, J.P. &amp; Grierson, L.H. 2002 The Devil&#8217;s Woodyard mud volcano of Trinidad: Chemistry and mineralogy<br \/>\nCaribbean geology- into the third millennium :Transactions of the15th Caribbean geological conference, p221- 228<br \/>\nKugler H.G. 1932 Contributions to the knowledge of sedimentary volcanism in Trinidad. Jour. Inst. petrol. technol. Vol.19 No.119 p 743 &#8211; 760.<br \/>\nKugler H.G. 1936 Nature and significance of sedimentary volcanism. Sci. Petroleum 1 p 297 &#8211; 299 (Oxford University Press)<br \/>\nKugler H.G. 1968 Sedimentary Volcanism. Trans. 4th Caribbean Geological Conference, Trinidad p 11 &#8211; 13.<br \/>\nMann, P., and Wood, L 2003 Shale diapirs, mud volcanoes, and fluid systems in offshore Trinidad and eastern Venezuela AAPG International meeting, Barcelona, Spain, September, 2003<br \/>\nNettleton, L. L. &amp; Herring, A. T. 1979 Quantitative analysis of a mud volcano gravity anomaly Geophysics, September 1979, Vol. 44, Issue 9, pp. 1518-1524<br \/>\nNettleton, L. L. &amp; Herring, A. T. 1979 Quantitative analysis of a mud volcano gravity anomaly Abstracts &#8211; Society of Exploration Geophysicists International Meeting, 1979, Issue 49, pp. 67<\/p>\n<p>Schulze-Makuch et al, 2020, A chemical and microbial characterization of selected mud volcanoes in Trinidad reveals pathogens introduced by surface water and rain water, Science of the Total Environment 707 (2020) 136087<\/p>\n<p>Stauffer, H., 1935, The mudflow movement on September 13th \u2013 14th in the L\u2019Envieuse Estate, Cedros<\/p>\n<p>Sullivan, S., Wood, L. &amp; Mann, P., 2004,Distribution, Nature and Origin of Mobile Mud Features Offshore Trinidad, Gulf Coast Section of the SEPM 24th Bob F. Perkins Research Conference<\/p>\n<p>Wach, G.D. &amp; Archie,C. 2006 Reservoir distribution and production in mobile shale basins &#8211; examples from the Cruse Formation of on mobile shale,\u00a0 Southern Trinidad, AAPG Hedberg conference<br \/>\nWeeks W.G. 1929 Notes on a new mud volcano in the sea off the south coast of Trinidad. Jour. Petrol. Tech. Vol.15 No.74 p 385 &#8211; 391.<\/p>\n<p>Wharton, S.R. &amp; Hudson, D. 1995 Report on a recent eruption of the mud volcano, Devil&#8217;s Woodyard, south Trinidad Abstracts 3rd GSTT Conference and 14th Caribbean Geological Conference and 14th Caribbean Geological conference, Trinidad, p. 85<br \/>\nWilson C.C &amp; Birchwood K.M. 1965 The Trinidad mud volcano island of 1964. Proc. Geol. Soc. London No. 1626 p 169 &#8211; 174.<br \/>\nWilson C.C. 1930 Mud Flow. Jour. Inst. Petrol. Vol.10 p 578 &#8211; 580.<br \/>\nYassir N.A. 1987 Mud Volcanoes : Evidence of neotectonic activity. Mem. Geol. Soc. China N.9 p 513-524.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Map showing the location of onshore mud volcanoes in relation to the oilfields. Location of active and fossil mud volcanoes (after Higgins and Saunders 1974) and the location of oil fields in Trinidad Origin of mud volcanoes TYPES OF MUD VOLCANOES OFFSHORE MUD VOLCANOES Impact of Eruptions Tabaquite Mud Volcano Devil&#8217;s Woodyard Cascadoux Mud Volcano [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":362,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=\/wp\/v2\/pages\/26"}],"collection":[{"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=26"}],"version-history":[{"count":45,"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=\/wp\/v2\/pages\/26\/revisions"}],"predecessor-version":[{"id":4541,"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=\/wp\/v2\/pages\/26\/revisions\/4541"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=\/wp\/v2\/media\/362"}],"wp:attachment":[{"href":"http:\/\/curtisarchie.com\/wpmocha\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=26"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}