Geothermal Development in Kenya-Country Updates
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Alcolapia Grahami ERSS
Lake Magadi Tilapia (Alcolapia grahami) Ecological Risk Screening Summary U.S. Fish & Wildlife Service, March 2015 Revised, August 2017, October 2017 Web Version, 8/21/2018 1 Native Range and Status in the United States Native Range From Bayona and Akinyi (2006): “The natural range of this species is restricted to a single location: Lake Magadi [Kenya].” Status in the United States No records of Alcolapia grahami in the wild or in trade in the United States were found. The Florida Fish and Wildlife Conservation Commission has listed the tilapia Alcolapia grahami as a prohibited species. Prohibited nonnative species (FFWCC 2018), “are considered to be dangerous to the ecology and/or the health and welfare of the people of Florida. These species are not allowed to be personally possessed or used for commercial activities.” Means of Introductions in the United States No records of Alcolapia grahami in the United States were found. 1 Remarks From Bayona and Akinyi (2006): “Vulnerable D2 ver 3.1” Various sources use Alcolapia grahami (Eschmeyer et al. 2017) or Oreochromis grahami (ITIS 2017) as the accepted name for this species. Information searches were conducted under both names to ensure completeness of the data gathered. 2 Biology and Ecology Taxonomic Hierarchy and Taxonomic Standing According to Eschmeyer et al. (2017), Alcolapia grahami (Boulenger 1912) is the current valid name for this species. It was originally described as Tilapia grahami; it has also been known as Oreoghromis grahami, and as a synonym, but valid subspecies, of -
Case Study Report For
Case Study One Indigenous Peoples’ Rights in the Kenya Lake System in the Great Rift Valley 1 By DR. KANYINKE SENA Indigenous Peoples’ Rights in the Kenya Lake System in the Great Rift Valley 1 CASE STUDY ONE Indigenous Peoples’ Rights in the Kenya World Heritage (IIPFWH), as a standing global Lake System in the Great Rift Valley body aimed at representing indigenous peo- ples voices in the World Heritage Committee processes.5 The Committee referred to the establishment of the IIPFWH, “As an impor- tant reflection platform on the involvement of Indigenous Peoples in the identification, conservation and management of World Heritage properties, with a particular focus on the nomination process.” 6 Pursuant to the mandate of the Forum, this report aims at analyzing Indigenous Peoples’ involvement in the Kenya Lakes System in the Great Rift Valley World Heritage Site. The report is as result of extensive literature re- view and interviews with communities in and around the lakes that comprise the Kenya K. Sena: Lake Bogoria Lakes System. The Kenya Lake System in the Great Rift Val- ley is a World Heritage site in Kenya which comprises three inter-linked, relatively shal- low, alkaline lakes and their surrounding territories. The lakes system includes Lakes Elementeita, Nakuru and Bogoria in the Rift Valley. The lakes cover a total area of 32,034 and was inscribed as a world heritage site in 2011. The inscription was based on the lakes system outstanding universal values and criterion (vii), (ix) and (x) as provided for, under paragraph 77 of the Operational Guidelines for the Implementation of the World Heritage Convention. -
Wetlands of Kenya
The IUCN Wetlands Programme Wetlands of Kenya Proceedings of a Seminar on Wetlands of Kenya "11 S.A. Crafter , S.G. Njuguna and G.W. Howard Wetlands of Kenya This one TAQ7-31T - 5APQ IUCN- The World Conservation Union Founded in 1948 , IUCN— The World Conservation Union brings together States , government agencies and a diverse range of non - governmental organizations in a unique world partnership : some 650 members in all , spread across 120 countries . As a union , IUCN exists to serve its members — to represent their views on the world stage and to provide them with the concepts , strategies and technical support they need to achieve their goals . Through its six Commissions , IUCN draws together over 5000 expert volunteers in project teams and action groups . A central secretariat coordinates the IUCN Programme and leads initiatives on the conservation and sustainable use of the world's biological diversity and the management of habitats and natural resources , as well as providing a range of services . The Union has helped many countries to prepare National Conservation Strategies , and demonstrates the application of its knowledge through the field projects it supervises . Operations are increasingly decentralized and are carried forward by an expanding network of regional and country offices , located principally in developing countries . IUCN — The World Conservation Union - seeks above all to work with its members to achieve development that is sustainable and that provides a lasting improvement in the quality of life for people all over the world . IUCN Wetlands Programme The IUCN Wetlands Programme coordinates and reinforces activities of the Union concerned with the management of wetland ecosystems . -
Direct Utilization of Geothermal Resources in Kenya
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Direct Utilization of Geothermal Resources in Kenya John Lagat Kenya Electricity Generating Company Ltd, P. O. Box 785 Naivasha 20117 E-mail: [email protected] Keywords: Geothermal, direct use, balneology, space 38oE heating, greenhouses, agriculture, aquaculture, industrial North Island processes 4oN L. Turkana ETHIOPIA ABSTRACT Central Island Geothermal resources in Kenya are mainly located along the Kenyan Rift, which is part of the eastern arm of the South Island African Rift. The primary forms of utilization of Cenozoic Barrier Volcano geothermal energy in Kenya currently are mainly electric volcanics power generation (168 MWe) and direct uses (~18 MWt) to UGANDA Namarunu a small extent. Though about 99% of geothermal utilization in the country is generation of electricity, direct uses are Emuruangogolak gaining momentum in various parts of the country. Farmers Mt. Elgon Silali have for decades, used geothermal heat to dry pyrethrum Paka KENYA Korosi flowers and condense steam for drinking at Eburru while L. Baringo Nyambeni the Oserian Development Company in Naivasha is using Arus-Bogoria geothermal energy to heat 50 hectares of greenhouses of cut Kisumu Oo roses for export. A tourist hotel at Lake Bogoria is utilizing Menengai Mt. Kenya spring water at 38°C to heat a spa pool. Despite the Eburru availability and enormous potential in direct use L. Naivasha applications, little use has been made of low enthalpy fluids Olkaria Longonot in Kenya. This paper therefore discusses direct use Suswa applications and available opportunities in swimming, Ol'Esakut Nairobi bathing, balneology, agricultural, aquiculture and in Olorgesaille o residential and industrial sectors L. -
Working Paper Or Information Paper
APIRG/19 WP/14 Appendix 3.2J INTERNATIONAL CIVIL AVIATION ORGANIZATION VOLCANIC ASH CONTINGENCY PLAN AFI REGION First Edition - October 2012 THIS DOCUMENT IS ISSUED BY THE DAKAR AND NAIROBI ICAO REGIONAL OFFICES UNDER THE AUTHORITY OF THE APIRG 1 Page 2 of 32 Volcanic Ash Contingency Plan – AFI Region FOREWARD Within and adjacent to the Africa and Indian Ocean (AFI) Region there are areas of volcanic activities which are likely to affect flight in the AFI Region. The major volcanoes in the region are located in the following States: Algeria, Cameroon, Cape Verde Islands, Chad, Comoros Island, Democratic Republic of Congo, Djibouti, Eritrea, Ethiopia, France (Reunion Island), Kenya, Madagascar, Mali, Niger, Nigeria, Rwanda, Sao Tome and Principe, Spain (Canary Islands, Madeira), Sudan, Tanzania and Uganda. The names of the concerned volcano are listed in APPENDIX K (source: Smithsonian Institution). This document is the AFI Air Traffic Management (ATM) Volcanic Ash Contingency Plan which sets out standardised guidelines and procedures for the provision of information to airlines and en-route aircraft before and during a volcanic eruption. Volcanic contamination, of which volcanic ash is the most serious, is a hazard for safe flight operations. Mitigating the hazards posed by volcanic ash in the atmosphere and/or at the aerodrome cannot be resolved in isolation but through collaborative decision-making (CDM) involving all stakeholders concerned. During an eruption volcanic contamination can reach and exceed the cruising altitudes of turbine-powered -
Geology Area South of Magadi
_£I Report No. 61 GOVERNMENT OF KENYA MINISTRY OF COMMERCE AND INDUSTRY GEOLOGICAL SURVEY OF KENYA GEOLOGY OF THE AREA SOUTH OF MAGADI DEGREE SHEET 58, N.W. QUARTER (with coloured geological map) by B. H. BAKER, B.Sc, F.G.S. Geologist Eight Shillings - 1963 "ISfiICrLIBSARY ïIE-- :i963l4 j». ^itfageningen _ .The'Netherlands Li / J Scanned from original by ISRIC - World Soil Information, as ICSU World Data Centre for Soils. The purpose is to make a safe depository for endangered documents and to make the accrued information available for consultation, following Fair Use Guidelines. Every effort is taken to respect Copyright of the materials within the archives where the identification of the Copyright holder is clear and, where feasible, to contact the originators. For questions please contact soil.isricPwur.nl indicating the item reference number concerned. GEOLOGY OF THE AREA SOUTH OF MAGADI DEGREE SHEET 58, N.W. QUARTER (with coloured geological map) by B. H. BAKER, B.Sc, F.G.S. Geologist 165^G FOREWORD The publication of the report on the geology of the area south of Magadi completes the account of the southern end of the Rift Valley as it occurs in Kenya. The Magadi area itself was described by Mr. Baker in Report No. 42 (1958). During the mapping of the continua tion of the Magadi area the discovery of some critical exposures enabled the correction of an error of succession in the lower Pleistocene rocks that had been made during the survey of the Magadi area. The area is wild and desolate, but of considerable interest scenically, with the western Rift wall a little beyond its west boundary, rugged hills of ancient rocks in the south-east and two prominent volcanoes, Lenderut and Shombole, rising from the Rift floor. -
Geothermal Potential of the Kenya Rift
Presented at Short Course III on Exploration for Geothermal Resources, organized by UNU-GTP and KenGen, at Lake Naivasha, Kenya, October 24 - November 17, 2008. GEOTHERMAL TRAINING PROGRAMME Kenya Electricity Generating Co., Ltd. STATUS OF GEOTHERMAL EXPLORATION IN KENYA AND FUTURE PLANS FOR ITS DEVELOPMENT Peter A. Omenda Kenya Electricity Generating Company Ltd. (KenGen) P.O. Box 785, Naivasha KENYA [email protected] ABSTRACT The high temperature geothermal prospects in Kenya are located within and are associated with the development of the Kenya Rift. Kenya Rift is a continental scale volcano-tectonic feature that stretches from northern to southern Africa. Development of the Rift started during the Oligocene (30million years ago) and activity has continued to recent times. The last 2 million years saw the development of large shield volcanoes within the axis of the rift. These centres are the most important geothermal prospects within the rift. Association between rifting and most of the occurrences of geothermal energy is mainly due to shallow magma chambers underneath the young volcanoes within the rift axis. KenGen in collaboration with the Ministry of Energy of the Government of Kenya has undertaken detailed surface studies of most of the prospects in the central sector of the rift which comprises Suswa, Longonot, Olkaria, Eburru, Menengai, Lakes Bogoria and Baringo, Korosi and Paka volcanic fields. Electric power is currently being generated at Olkaria with 130MWe installed while exploration drilling has been undertaken at Eburru and a 2.5MWe pilot plant is planned for development by KenGen and commissioning by 2009. Common methods that have been used by KenGen during exploration expeditions include geology (lithology, geochronology, structures); geophysics (seismic, gravity, magnetic, and resistivity); geochemistry (fluid and thermometry), heat flow and environmental baseline assessments. -
Geothermal Mapping Using Temperature Measurements
Presented at Short Course VII on Exploration for Geothermal Resources, organized by UNU-GTP, GDC and KenGen, at Lake Bogoria and Lake Naivasha, Kenya, Oct. 27 – Nov. 18, 2012. GEOTHERMAL TRAINING PROGRAMME Kenya Electricity Generating Co., Ltd. GEOTHERMAL MAPPING USING TEMPERATURE MEASUREMENTS Godwin M. Mwawongo Geothermal Development Company P. O. Box 100746, Nairobi 00101 KENYA [email protected] ABSTRACT Shallow temperature gradient holes are reliable in mapping geothermal prospects with heat loss features as surface manifestation. The sun least affects ground temperatures at 1 m depth and temperatures in the North rift are least affected by seasonal changes. Over 10,736 MWt is lost naturally from Menengai to Paka along the Kenyan rift. Most of the geothermal surface manifestations associated with the heat loss are oriented in the NW-SE with a few located in the NE-SW direction. Estimated down-hole temperature at I km depth is over 200oC. Fluid flow in the prospects from Lake Baringo to Paka is from East to West with an outflow to the north. 1. INTRODUCTION Kenya is located in East Africa where the Great African Rift virtually splits the landmass into two. 14 geothermal prospects have been identified within the Kenyan Rift Valley starting from Barrier in the north to Lake Magadi in the south with a potential of over 3,000 MWe (Figure 1). The rift is a graben and during the formation of the prospects, hot rocks were brought closer to the surface and with intensive faulting and presence of water, the geothermal systems were formed as shown in the model in Figure 2. -
Mineral Reactions in the Sedimentary Deposits of the Lake Magadi Region, Kenya
Mineral reactions in the sedimentary deposits of the Lake Magadi region, Kenya RONALD C. SURD AM Department of Geology, University of Wyoming, Laramie, Wyoming 82071 HANS P. EUGSTER Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, Maryland 21218 ABSTRACT hand, the initial alkalic zeolite that will form in a specific alkaline lake environment cannot yet be predicted with confidence. Among The authigenic minerals, principally zeolites, in the Pleistocene to the many parameters controlling zeolite distribution, the compo- Holocene consolidated and unconsolidated sediments of the sitions of the volcanic glasses and of the alkaline solutions are cer- Magadi basin in the Eastern Rift Valley of Kenya have been inves- tainly of primary importance. tigated. Samples were available from outcrops as well as drill cores. Most zeolite studies are concerned with fossil alkaline lakes. The following reactions can be documented: (1) trachytic glass + While it is generally easy to establish the composition of the vol- H20 —» erionite, (2) trachytic glass + Na-rich brine —* Na-Al-Si gel, canic glass, the brines responsible for the authigenic reactions have + + (3) erionite + Na analcime + K + Si02 + H20, (4) Na-Al-Si long since disappeared. To overcome this handicap, it is desirable gelanalcime + H20, (5) calcite + F-rich brine—> fluorite + C03 , to investigate an alkaline lake environment for which glass as well (6) calcite + Na-rich brine —» gaylussite, and (7) magadiite —• as brine compositions can be determined — in other words, a + quartz + Na + H20. Erionite is the most common zeolite present, modern alkaline lake environment. Such an environment is Lake but minor amounts of chabazite, clinoptilolite, mordenite, and Magadi of Kenya. -
Geology of the Area South of Magadi, Kenya
%% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% % % % % % % % % % % % % % % % % % % % % % % % % % % % % % % % % %% % % % % % % % % % % % % % % % % % % % % % % % % % % % % % % %% %% % % % % % % %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% % GEOLOGIC HISTORY % % % % % % % % % % % % % % % % % % % Legend % % % % % % % % % % % % % % % % % % % %% % %% %% % HOLOCENE % %% %% %% %% %% % % Pl-na %% %% %% % % Alasho ash %% %% %% % Evaporite Series (0-9 ka): trona with interbedded clays. The Magadi Soda Company currently mines the % % % Sediments Metamorphics %% %% %% %% %% %% %% %% %% %% %% %% % trona at Lake Magadi in the region to the north. Samples of this formation from Natron indicate significantly % %% %% %% %% %% %% %% % % Pl-nv %% % % Alasho centers %% %% %% % G% eology of the Area South of Magadi, Kenya more halite than trona compared to Lake Magadi (Bell and Simonetti 1996). %% % % Holocene Kurase Group %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% %% % % % % % Pl-pt % % % % Magadi Trachyte Xl % % % % PLEISTOCENE % % % % Trona Crystalline Limestone % % % % For area to North see: Geology of the Magadi Area, KGS Report 42; Digital version by A. Guth % % % 36.5 °E % % % % 36.0 °E % % % % % High Magadi Beds (9-23.7 ka): yellow-brown silts over laminated clays with fish remains. Deposited % during % % Pl-gv % -2.0 ° -2.0 ° % % Gelai Xp % %% % a period of higher lake levels in both lakes Natron and Magadi. Coarser pebble beds seen near Len% derut Alluvial fan Undiff. Pelitic -
Influence of Regional Tectonics and Pre-Existing Structures on the Formation of Elliptical Calderas in the Kenyan Rift
Downloaded from http://sp.lyellcollection.org/ by guest on September 23, 2021 Influence of regional tectonics and pre-existing structures on the formation of elliptical calderas in the Kenyan Rift E. A. M. ROBERTSON1*, J. BIGGS1, K. V. CASHMAN1, M. A. FLOYD2 & C. VYE-BROWN3 1School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 2JN, UK 2Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA 3British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK *Corresponding author (e-mail: [email protected]) Abstract: Calderas are formed by the collapse of large magma reservoirs and are commonly ellip- tical in map view. The orientation of elliptical calderas is often used as an indicator of the local stress regime; but, in some rift settings, pre-existing structural trends may also influence the orien- tation. We investigated whether either of these two mechanisms controls the orientation of calderas in the Kenyan Rift. Satellite-based mapping was used to identify the rift border faults, intra-rift faults and orientation of the calderas to measure the stress orientations and pre-existing structural trends and to determine the extensional regime at each volcano. We found that extension in north- ern Kenya is orthogonal, whereas that in southern Kenya is oblique. Elliptical calderas in northern Kenya are orientated NW–SE, aligned with pre-existing structures and perpendicular to recent rift faults. In southern Kenya, the calderas are aligned NE–SW and lie oblique to recent rift faults, but are aligned with pre-existing structures. -
Status of Geothermal Exploration in Kenya and Future Plans for Its Development
Presented at Short Course IV on Exploration for Geothermal Resources, organized by UNU-GTP, KenGen and GDC, at Lake Naivasha, Kenya, November 1-22, 2009. Kenya Electricity Generating Co., Ltd. GEOTHERMAL TRAINING PROGRAMME Geothermal Development Company STATUS OF GEOTHERMAL EXPLORATION IN KENYA AND FUTURE PLANS FOR ITS DEVELOPMENT Peter A. Omenda Geothermal Development Company P. O. Box 100746, Nairobi 00101 KENYA [email protected] ABSTRACT The high temperature geothermal prospects in Kenya are located within and are associated with the development of the Kenya Rift. Kenya Rift is a continental scale volcano-tectonic feature that stretches from northern to southern Africa. Development of the Rift started during the Oligocene (30million years ago) and activity has continued to recent times. The last 2 million years saw the development of large shield volcanoes within the axis of the rift. These centres are the most important geothermal prospects within the rift. Association between rifting and most of the occurrences of geothermal energy is mainly due to shallow magma chambers underneath the young volcanoes within the rift axis. KenGen in collaboration with the Ministry of Energy of the Government of Kenya has undertaken detailed surface studies of most of the prospects in the central sector of the rift which comprises Suswa, Longonot, Olkaria, Eburru, Menengai, Lakes Bogoria and Baringo, Korosi and Paka volcanic fields. Electric power is currently being generated at Olkaria with 130MWe installed while exploration drilling has been undertaken at Eburru and a 2.5MWe pilot plant is planned for development by KenGen and commissioning by 2009. Common methods that have been used by KenGen during exploration expeditions include geology (lithology, geochronology, structures); geophysics (seismic, gravity, magnetic, and resistivity); geochemistry (fluid and thermometry), heat flow and environmental baseline assessments.