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GEOTHERMAL ACTIVITY STATUS IN THE VOLCANIC CARIBBEAN ISLANDS Gerald W. Huttrer Geothermal Management Company, Inc., Frisco, Colorado Key Words: Caribbean, exploration, development, indicated work requirements ABSTRACT The Atlantic Crustal Plate is subducting westward beneath the Caribbean Plate resulting in formation of volcanic island chains that comprise: 1) an eastern, eastward-convex arc of older, extinct volcanoes and 2) a western arc of younger, dormant to active volcanoes. The two arcs join at Martinique and from there trend southwestward into the Paria Peninsula of Venezuela. Geothermal indicia including warm to hot springs, fumaroles, solfataras and mud pots exist, to varying extents, on Saba, St. Eustatius (Statia), St. Christopher (St. Kitts), Nevis, Montserrat, Guadeloupe, Dominica, Martinique, St. Lucia, St. Vincent and Grenada. Volcanic eruptions and associated geothermal phenomena have been documented on Montserrat, Guadeloupe, Dominica, Martinique, St. Vincent, Grenada and Kick-em-Jenny (a highly active seamount north of Grenada). Geothermal resource surface temperatures in the Lesser Antilles islands range from tepid to above boiling (superheated). Subsurface temperatures high enough to support utilization of a double flash energy conversion system have been recorded in the wells drilled for the 4.2 MW La Bouillante power plant on Guadeloupe while temperatures up to 214oC were measured in wells drilled near Soufrière, St. Lucia. Prior to 1995, geothermally oriented geologic, geochemical and geophysical studies were conducted on Guadeloupe, Dominica, Montserrat, St. Lucia and Grenada. Ten 500 meter deep wells were drilled at Watten Waven in Dominica; large diameter wells were drilled on Guadeloupe in 1982-1984 and two deep exploration wells were drilled in St. Lucia in 1984- 1987. Between 1995 and 1999, Caribbean geothermal activity was confined to prefeasibility and feasibility studies conducted on St. Vincent, Saba, Statia, St. Kitts and Nevis. The work included geologic, geochemical and some geophysical studies plus the acquisition of much non-resource related information. Though the signing of Power Purchase Agreements between utility companies, local governments and private developers has been reported on St. Vincent, Dominica and Grenada, to date no wells have been drilled. Low temperature geothermal waters are informally used for bathing on several islands and bath houses have been built on St. Lucia and Nevis. Otherwise, geothermal fluids are not being used. 1. INTRODUCTION The northern islands of the Lesser Antilles are all potential sites of geothermal resources because virtually all of the islands are underlain by active or dormant (but not extinct) volcanoes. The 11 islands falling into this category are, from north to south, Saba, St. Eustatius (Statia), St. Christopher (St. Kitts), Nevis, Montserrat, Guadeloupe, Dominica, Martinique, St. Lucia, St. Vincent and Grenada (Figure 1). The islands comprise two eastward convex arcs. South of Montserrat, these arcs merge to form a single curvilinear island chain that intersects the South American continent at the Peninsula de Paria of Venezuela. The western island arc and its southern extension are of relatively recent volcanic origin. The northern and eastern islands, though once loci of volcanism, are now mantled by thick sedimentary deposits. The reason for the active volcanism is that the Caribbean islands occupy a crustal plate that forms a “tongue” or buttress along the sides of which the North and South American Plates move westward and beneath which the Atlantic Plate is subducting westward (Figure 2). The Atlantic Plate subduction has created volcanic arcs typical of plate boundaries and, in the Caribbean, each volcano or group of volcanoes has formed the foundation of a discrete island. 2. GEOTHERMAL POWER GENERATION OPPORTUNITIES The potential for construction of small to medium sized (5-25 MW) geothermal power generation facilities and/or significant direct-use projects is excellent in many Caribbean islands. The countries are still developing, their transmission and distribution grids are extensive and their power and thermal energy requirements are growing. Excluding the French islands, the largest electrical loads are on St. Vincent, St. Lucia and Dominica where 10-20 MW is or will soon be needed. Next in size is Grenada where 8-12 MW could be used and finally come all the rest of the islands whose current needs range from 2 to 5 MW. In virtually all of the islands, generation (predominantly diesel-fueled, with some hydro), transmission and distribution costs (including all soft costs) range between $0.12 and $0.15 per kWh. It is important to note that while few of the utility companies have an accurate accounting of their real costs, it seems very likely that geothermally generated power could be provided for a lower cost than the utilities now pay in-house. In many countries, O&M-caused brownouts or power outages are all too common and are reportedly on the increase. Careful, realistic calculations of planned geothermal project economics and of current true power costs must be made. Assuming that they confirm the economic viability of a planned project, they will be critically important in convincing governments and utility officials that geothermal power will be less expensive and more reliable than their traditional generating systems. 217PDF Image | GEOTHERMAL ACTIVITY STATUS IN CARIBBEAN ISLANDS
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