W Rift Workshop Kigali Varet

Total Page:16

File Type:pdf, Size:1020Kb

W Rift Workshop Kigali Varet Technical Workshop on the Geological Development and Geophysics of the Western Branch of the Greater East African Rift System with Emphasis on Factors that Control the Development of their Geothermal Systems. Kigali, Rwanda 9-11 March 2016 Critical datasets required for the successful development of integrated geothermal conceptual models: Summary of supportive information required before committing a prospect to exploratory drilling Jacques Varet SARL Géo2D (France) Ressources géologiques pour le Développement Durable Associate Professor, DeKUT, GETRI (Kenya) www.geo2d.com Western Rift Wokshop, Kigali, march 2016. J.Varet Gisenyi Diversity of geothermal systems - solutions > A very large range of geothermal resources available, which vary considerably according to the geological context on one side, and on the nature of the demand on the other side. > There is no generalized approach in committing a prospect that would fit as diversified applications as district heating in graben areas, heat pumps for household thermal regulation, engineered deep EGS, as well as high enthalpy geothermal exploration in geodynamically active areas. Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Do not just search for power for the grid! Geothermal can do more, diverse… > We will focus on the approach to geothermal systems in active rift zones, including volcanically active as well as tectonically active rifts, as expressed along the eastern and western branches of the EARV respectively. > Even though, there are still different types of possible geothermal developments – from community based small-zine systems to search for large electrical production serving the electric grid - implying quite different approaches. > Deciding upon exploratory drilling rely upon the quality of the expected resource (possibly high flow rate of high temperature fluids of compatible chemistry) but obviously also on the demand of the communities on and around the site, implying socio-economic as well as geoscientific studies. Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Any geothermal project necessitates transdisciplinary approach Géosciences: - Geology - Geophysics - Geochemistry - Drilling - Reservoirs Social Engineering - Thermics Sciences: - Mecanics - Sociology - Thermodynamics - Ethnology - Electricity - Economy - …. - Politics - …. Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets General methodology Development scheme Energy needs 2020 et 2050 Technical choice for geothermal production system Scenario 3 Area of production / distribution Licences Scenario 2 Scenario 1 Restricted areas (protection….) Various scenarios of Geothermal Resources development schemes for geothermal energy at local/regional level. Defining objectives Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Terrestrial heat flow higher along plate boundaries, notably expansion zones due to mantle melting (decompression) * 60 à 100 mW/m2 in stables zones (60-100 kW/Km2) * up to ten times more in active zones (of the order of the MW/Km2 i.e. renewable) Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Part of the Earth energy is dissipated along diverging plate margins, unfortunately most are immerged under oceans But most of the geothermal energy stock is available and economically valuable in normal gradient areas provided high permeabilities zones are present Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets EAR: the two asthenospheric domes of Ethiopa and Kenya : supposedly due to mantle plume, i.e. inducing anomalous hot upper-mantle Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets But rate varies from 2 cm/year in Afar to 5mm in Ethiopian rift and 2 mm in Western rift EARV From oceanic To continental rift Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Magmatic variations of continental rift systems: source magma as well as basic/salic proportions Barberi, F., Santacroce, R., & Varet, J. (1982) Chemical Aspects of Rift Magmatism. In. G.Palmason (Editor). Continental and Oceanic Rifts. Geodynamics Ser.8: 223-258. Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Continental rifts in Europe also associate graben tectonics and local volcanic units, some of them evolved (French Massif central) Perialpine Europe geodynamic context of continental rifts and volcanism Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets European rift zones : volcanic units and tectonic graben co-exist Graben, frequently assymetric, may display interesting thermal anomalies (ex. Limagne, France) Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Positive thermal anomalies coexist with negative ones due to thermal convection along faults (ex. Rhine graben, Soultz) Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Looking for heat sources along EARV There are 2 lava lakes in the world: Erta Alé and Nyiragongo i.e. emerged magma chambers Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets But surface hydrothermal manifestations have not the same importance Ma’alalta N. Afar Ethiopia Garrabayis Djibouti Rep. Gustave Courbet Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets L’Origine du Monde Magma genesis Repeated diking along single axis from shallow source (nearly tholeiitic) Fissural random emissions from deep source (K alkali basalt) Karisimbi Erta Ale, Afar southern flank, Ethiopia Rwanda Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets No possible heat source in such fissural basaltic lava fields (very suitable for potatoes plantations) Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Heat source northern Afar, parallel to Red Sea Erta Ale range provides from S to N a textbook petrological and volcanological evolution of oceanic type basalts from typical fissural stage up to elongated shield and central cumulovolcanoes with very shallow (1-3 Km deep) magma chambers. Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Afar volcanic axial ranges : emerged oceanic ridge segments Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Elliptic calderas along rift axis : Erta Ale vocano > 20 Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Erta Ale shield volcano > From picritic basalts to plagioclase rich intermediates > Up to ferrobasalts and dark trachytes Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Basaltic elliptic caldera collapseroof of very shallow magma chamber Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Central volcanoes : peralkaline rhyolites > Eruptive cycle up to trachytes and commendites (slightly peralkaline rhyolites) > Volcanological and petrological expression of a very shallow magma chamber Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Central volcanoes peralkaline rhyolites > Displaying shallow magma chambers > Low pressure & fO2 crystal fractionation > Confirmed by recent interferometry studies (following 2008 eruption ) 1 Km depth (Pagli et al. 2012) > Numerous fumaroles including HT Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Dalla filla rhyolite cone cumulo-volcano (Erta Ale range) Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Shallow heat sources (1 to 3 Km) Successive steps in volcanoe’s construction in Erta’Ale range from fissural to shield and stratovolcano, with development of a shallow magma chamber. From south to North due to decreasing spreading rate Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Erta Ale axial range volcano-magmatic evolution Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Erta Ale range: a complete magmatic sequence from basalts to rhyolites > Strong iron enrichment > Very low oxygen fugacities > Low depths magmatic differenciation > i.e. 1-3 Km heat sources Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Other extremity of Afar (Djibouti) Asal range first merged segment of Aden ridge Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets the Asal rift axis seen from lake Asal (260m bsl) > 30 Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets OCEANIC RIFT CONTEXT: STEAMING OPEN FISSURES IN FIALE CALDERA, ASAL Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Geological map of the Asal rift hyaloclastites in orange, recent basalts in deep blue and violet; early rift basalts (300.000 – 100.000 y.) in pale blue ; stratoid series (3 to 1 My) in very pale blue. Lacustrine deposits (diatomite) in yellow Ardoukoba 1978 (after Koreli Stieltjes, hotsprings ed. BRGM, Zone Nord 1978) Ghoubbet Project site Baie des requins Site Asal 1- 4 Fiale caldera Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Asal axial range nearer to tholeiites, compared with Erta Ale (low fO2 shallow fractionation) Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Plagioclase segregation in porphyritic basalts (near surface lava lake conditions) explains the iron enrichment in later liquids Western Rift Wokshop, Kigali, march 2016. J.Varet. Critical data sets Geophysical data (sismicity, MT restivity) allow to map the location & depth of the heat source (magma chamber) and of the reservoir zone (brittle magma-water interaction) Western
Recommended publications
  • 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
    [Show full text]
  • How the Variety of Satellite Remote Sensing Data Over Volcanoes Can Assist Hazard Monitoring Efforts: the 2011 Eruption of Nabro Volcano T
    Remote Sensing of Environment 236 (2020) 111426 Contents lists available at ScienceDirect Remote Sensing of Environment journal homepage: www.elsevier.com/locate/rse How the variety of satellite remote sensing data over volcanoes can assist hazard monitoring efforts: The 2011 eruption of Nabro volcano T ∗ Gaetana Ganci , Annalisa Cappello, Giuseppe Bilotta, Ciro Del Negro Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Osservatorio Etneo, Catania, Italy ARTICLE INFO ABSTRACT Keywords: Satellite remote sensing is becoming an increasingly essential component of volcano monitoring, especially at Lav@Hazard little-known and remote volcanoes where in-situ measurements are unavailable and/or impractical. Moreover HOTSAT the synoptic view captured by satellite imagery over volcanoes can benefit hazard monitoring efforts. By MAGFLOW monitoring, we mean both following the changing styles and intensities of the eruption once it has started, as Satellite remote sensing well as nowcasting and eventually forecasting the areas potentially threatened by hazardous phenomena in an Numerical modelling eruptive scenario. Here we demonstrate how the diversity of remote sensing data over volcanoes and the mutual interconnection between satellite observations and numerical simulations can improve lava flow hazard mon- itoring in response to effusive eruption. Time-averaged discharge rates (TADRs) obtained from low spatial/high temporal resolution satellite data (e.g. MODIS, SEVIRI) are complemented, compared and fine-tuned with de- tailed maps of volcanic deposits with the aim of constraining the conversion from satellite-derived radiant heat flux to TADR. Maps of volcanic deposits include the time-varying evolution of lava flow emplacement derived from multispectral satellite data (e.g. EO-ALI, Landsat, Sentinel-2, ASTER), as well as the flow thickness var- iations, retrieved from the topographic monitoring by using stereo or tri-stereo optical data (e.g.
    [Show full text]
  • Dissertation
    DISSERTATION Titel der Dissertation ˝Geochemical and Petrographic Studies of the Volcano- Tectonic Evolution of Northern Afar: Implications for the Structural Setup of the Actively Expanding Erta’Ale Depression˝ Verfasser Mag. Miruts Hagos angestrebter akademischer Grad Doktor der Naturwissenschaften (Dr. rer. nat.) Wien, im November 2010 Studienkennzahl lt. Studienblatt: A 091 426 Dissertationsgebiet lt. Studienblatt: Erdwissenschaften Betreuer: Prof. Dr. Christian Koeberl PREFACE: This thesis presents the results of three full years of work conducted at the Department of Lithospheric Research, University of Vienna, on the rock samples and structural data collected from the Ethio-Afar volcanic province, Ethiopia. The main objective of this study was to establish the Oligocene–Present volcano-tectonic evolution of the northern Afar Depression and set the appropriate nature of the Afar Depression lithosphere. This work was done at the megascopic scale for the regional geological map and structural setup of the northern Ethiopian plateau and the northern Afar Depression volcanic provinces. The petrogenetic link between the Ethiopian flood and the Danakil Depression basalts was evaluated, using petrographic analyses of the samples together with their major and trace element composition, as well as the Sr and Nd isotopic composition of selected samples. Geochemical and isotopic data were obtained using instrumental neutron activation analysis (INAA), X-ray fluorescence (XRF) spectrometry, electron microprobe (EMP), and thermal ionization mass spectrometry (TIMS) at the Department of Lithospheric Research, University of Vienna. This thesis consists a total of eight chapters with a much summarized general introduction of the East African Rift System (Chapter 1) and review of the regional tectonics and magmatism throughout East Africa (Chapter 2) followed by short description of the methodologies used (Chapter 3).
    [Show full text]
  • USGS Open-File Report 2009-1133, V. 1.2, Table 3
    Table 3. (following pages). Spreadsheet of volcanoes of the world with eruption type assignments for each volcano. [Columns are as follows: A, Catalog of Active Volcanoes of the World (CAVW) volcano identification number; E, volcano name; F, country in which the volcano resides; H, volcano latitude; I, position north or south of the equator (N, north, S, south); K, volcano longitude; L, position east or west of the Greenwich Meridian (E, east, W, west); M, volcano elevation in meters above mean sea level; N, volcano type as defined in the Smithsonian database (Siebert and Simkin, 2002-9); P, eruption type for eruption source parameter assignment, as described in this document. An Excel spreadsheet of this table accompanies this document.] Volcanoes of the World with ESP, v 1.2.xls AE FHIKLMNP 1 NUMBER NAME LOCATION LATITUDE NS LONGITUDE EW ELEV TYPE ERUPTION TYPE 2 0100-01- West Eifel Volc Field Germany 50.17 N 6.85 E 600 Maars S0 3 0100-02- Chaîne des Puys France 45.775 N 2.97 E 1464 Cinder cones M0 4 0100-03- Olot Volc Field Spain 42.17 N 2.53 E 893 Pyroclastic cones M0 5 0100-04- Calatrava Volc Field Spain 38.87 N 4.02 W 1117 Pyroclastic cones M0 6 0101-001 Larderello Italy 43.25 N 10.87 E 500 Explosion craters S0 7 0101-003 Vulsini Italy 42.60 N 11.93 E 800 Caldera S0 8 0101-004 Alban Hills Italy 41.73 N 12.70 E 949 Caldera S0 9 0101-01= Campi Flegrei Italy 40.827 N 14.139 E 458 Caldera S0 10 0101-02= Vesuvius Italy 40.821 N 14.426 E 1281 Somma volcano S2 11 0101-03= Ischia Italy 40.73 N 13.897 E 789 Complex volcano S0 12 0101-041
    [Show full text]
  • The Eruptive History and Magmatic Evolution of Aluto Volcano: New Insights Into Silicic Peralkaline Volcanism in the Ethiopian Rift
    Journal of Volcanology and Geothermal Research 328 (2016) 9–33 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores The eruptive history and magmatic evolution of Aluto volcano: new insights into silicic peralkaline volcanism in the Ethiopian rift William Hutchison a,⁎, David M. Pyle a,TamsinA.Mathera,GezahegnYirgub, Juliet Biggs c,BenjaminE.Cohend, Dan N. Barfod d,EliasLewie a COMET, Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK b School of Earth Sciences, Addis Ababa University, P.O. Box 1176, Addis Ababa, Ethiopia c COMET, School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK d NERC Argon Isotope Facility, Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, G75 0QF, UK e IGSSA, Addis Ababa University, PO Box 1176, Addis Ababa, Ethiopia article info abstract Article history: The silicic peralkaline volcanoes of the East African Rift are some of the least studied volcanoes on Earth. Here we Received 6 July 2015 bring together new constraints from fieldwork, remote sensing, geochronology and geochemistry to present the Received in revised form 30 August 2016 first detailed account of the eruptive history of Aluto, a restless silicic volcano located in a densely populated sec- Accepted 19 September 2016 tion of the Main Ethiopian Rift. Prior to the growth of the Aluto volcanic complex (before 500 ka) the region was Available online 21 September 2016 characterized by a significant period of fault development and mafic fissure eruptions. The earliest volcanism at Keywords: Aluto built up a trachytic complex over 8 km in diameter.
    [Show full text]
  • Measuring Volcanic Plume and Ash Properties from Space
    Measuring Volcanic Plume and Ash Properties from Space R.G. Grainger*1, D.M. Peters1, G.E. Thomas1, A.J.A. Smith1, R. Siddans2, E. Carboni1, and A. Dudhia1 1Sub-Department of Atmospheric, Oceanic and Planetary Physics, University of Oxford, Parks Road, Oxford, OX1 3PU, England 2Science and Technology Facilities Council Rutherford Appleton Laboratory, Harwell Science and Innovation Campus, Didcot, OX11 0QX, England *Corresponding author(email:[email protected]) Number of Words:10,416 Abbreviated Title: Volcanic Plume and Ash Properties 1 Abstract: The remote sensing of volcanic ash plumes from space can pro- vide a warning of an aviation hazard and knowledge on eruption processes and radiative effects. In this paper new algorithms are presented to provide volcanic plume properties from measurements by the Michelson Interferom- eter for Passive Atmospheric Sounding (MIPAS), the Advanced Along Track Scanning Radiometer (AATSR) and Spinning Enhanced Visible and Infrared Imager (SEVIRI). A challenge of remote sensing is to provide near real-time methods to identify, and so warn, of the presence of volcanic ash. To achieve this, a singular vector decomposition method has been developed for the MIPAS instrument on board the Environmental Satellite (ENVISAT). This method has been applied to observations of the ash clouds from the erup- tions of Nabro and the Puyehue-Cord´on Caulle in 2011 and lead to a more sensitive volcanic signal flag which was capable of tracking changes in the volcanic signal spectra as the plume evolved. A second challenge for remote sensing is to identify the ash plume height. This is a critical parameter for the initialisation of algorithms that numerically model the evolution and transport of a volcanic plume.
    [Show full text]
  • Region 2 Africa and Red
    Appendix B – Region 2 Country and regional profiles of volcanic hazard and risk: Africa and Red Sea S.K. Brown1, R.S.J. Sparks1, K. Mee2, C. Vye-Brown2, E.Ilyinskaya2, S.F. Jenkins1, S.C. Loughlin2* 1University of Bristol, UK; 2British Geological Survey, UK, * Full contributor list available in Appendix B Full Download This download comprises the profiles for Region 2: Africa and Red Sea only. For the full report and all regions see Appendix B Full Download. Page numbers reflect position in the full report. The following countries are profiled here: Region 2 Africa and Red Sea Pg.90 Algeria 98 Cameroon 103 Chad 109 Democratic Republic of Congo 114 Djibouti 121 Equatorial Guinea 127 Eritrea 133 Ethiopia 139 Kenya 147 Libya 154 Mali 159 Niger 164 Nigeria 169 Rwanda 174 Sao Tome and Principe 180 Sudan 185 Tanzania 191 Uganda 198 Brown, S.K., Sparks, R.S.J., Mee, K., Vye-Brown, C., Ilyinskaya, E., Jenkins, S.F., and Loughlin, S.C. (2015) Country and regional profiles of volcanic hazard and risk. In: S.C. Loughlin, R.S.J. Sparks, S.K. Brown, S.F. Jenkins & C. Vye-Brown (eds) Global Volcanic Hazards and Risk, Cambridge: Cambridge University Press. This profile and the data therein should not be used in place of focussed assessments and information provided by local monitoring and research institutions. Region 2: Africa and Red Sea Figure 2.1 The distribution of Holocene volcanoes through the Africa and Red Sea region. The capital cities of the constituent countries are shown. Description Of all the regions of world we have the least historic and geologic information about Africa’s 152 volcanoes.
    [Show full text]
  • First Recorded Eruption of Nabro Volcano, Eritrea, 2011
    Bull Volcanol (2015) 77: 85 DOI 10.1007/s00445-015-0966-3 RESEARCH ARTICLE First recorded eruption of Nabro volcano, Eritrea, 2011 Berhe Goitom1,2 & Clive Oppenheimer3 & James O. S. Hammond4 & Raphaël Grandin 5 & Talfan Barnie6 & Amy Donovan3 & Ghebrebrhan Ogubazghi2 & Ermias Yohannes 7 & Goitom Kibrom7 & J- Michael Kendall1 & Simon A. Carn 8 & David Fee9 & Christine Sealing8 & Derek Keir10 & Atalay Ayele11 & Jon Blundy1 & Joanna Hamlyn12 & Tim Wright12 & Seife Berhe 13 Received: 23 March 2015 /Accepted: 10 August 2015 /Published online: 7 September 2015 # The Author(s) 2015. This article is published with open access at Springerlink.com Abstract We present a synthesis of diverse observations of the erupted lavas and tephra range from trachybasaltic to the first recorded eruption of Nabro volcano, Eritrea, which trachybasaltic andesite, and crystal-hosted melt inclusions began on 12 June 2011. While no monitoring of the volcano contain up to 3,000 ppm of sulphur by weight. The eruption was in effect at the time, it has been possible to reconstruct the was preceded by significant seismicity, detected by regional nature and evolution of the eruption through analysis of re- networks of sensors and accompanied by sustained tremor. gional seismological and infrasound data and satellite remote Substantial infrasound was recorded at distances of hundreds sensing data, supplemented by petrological analysis of to thousands of kilometres from the vent, beginning at the erupted products and brief field surveys. The event is notable onset of the eruption and continuing for weeks. Analysis of for the comparative rarity of recorded historical eruptions in ground deformation suggests the eruption was fed by a shal- the region and of caldera systems in general, for the prodi- low, NW–SE-trending dike, which is consistent with field and gious quantity of SO2 emitted into the atmosphere and the satellite observations of vent distributions.
    [Show full text]
  • Volcans Monde SI Dec2010
    GEOLOGICAL MAP OF THE WORLD AT 1: 25,000,000 SCALE, THIRD EDITION - Compilator: Philippe Bouysse, 2006 ACTIVE AND RECENT VOLCANOES This list of 1508 volcanoes is taken from data of the Global Volcanism Program run by the Smithsonian Institution (Washington, D.C., USA) and downloaded in April 2006 from the site www.volcano.si.edu/world/summary.cfm?sumpage=num. From the Smithsonian's list, 41 locations have been discarded due to a great deal of uncertainties, particularly as concerns doubtful submarine occurrences (mainly ship reports of the 19th and early 20th centuries). Also have been omitted submarine occurrences from the axes of "normal" oceanic accretionary ridges, i.e. not affected by hotspot activity. NOTES Volcano number: the numbering system was developped by the Catalog of Active Volcanoes of the World in the 1930s and followed on by the Smithsonian Institution, namely in the publication of T. Simkin & L.Siebert: Volcanoes of the World (1994). Name and Geographic situation: some complementary information has been provided concerning a more accurate geographic location of the volcano, e.g. in the case of smaller islands or due to political changes (as for Eritrea). Geographic coordinates: are listed in decimal parts of a degree. The position of volcano no. 104-10 (Tskhouk-Karckar, Armenia) was corrected (Lat. 39°.73 N instead of 35°.73 N). An asterisk (*) in column V.F. indicates the position of the center point of a broad volcanic field. Elevation: in meters, positive or negative for submarine volcanoes. Time frame (column T-FR): this is a Smithsonian' classification for the time of the volcano last known eruption: D1= 1964 or later D2= 1900 – 1963 D3= 1800 – 1899 D4= 1700 – 1799 D5= 1500 – 1699 D6= A.D.1 – 1499 D7= B.C.
    [Show full text]
  • Dabbahu (Teru Woreda) in Northern Afar a Major Ethiopian Geothermal Site Leased by AGAP
    Proceedings, 7th African Rift Geothermal Conference Kigali, Rwanda 31st October – 2nd November 2018 Dabbahu (Teru Woreda) in Northern Afar A major Ethiopian Geothermal Site Leased by AGAP Ismael Ali Gardo & Jacques Varet AGAP (Afar community based geothermal development company), Semara, Afar Regional State, Ethiopia & SARL Géo2D, Orléans, France [email protected]; [email protected] Keywords: Teru, Dabbahu, Boina, Geothermal exploration, Afar Regional State, major site in Ethiopia ABSTRACT AGAP (Afar Geothermal Development Company) is a community-based organization founded in 2015 that aims at developing geothermal sites in the Regional State of Afar. After a comprehensive regional survey, in this region that is characterized by active volcanism and tectonics, the first-priority targets were identified in Northern Afar. The choice of this target results mainly from social considerations. Differing from Southern Afar where the Awash basin provides significant water inflow, Northern Afar is particularly dry, and droughts are significantly increased by the ongoing climate change. The only option is immigration. AGAP considers that geothermal is eventually the most viable solution for the pastoralist communities in the region to continue living on their land and could even ultimately provide climate resilience. From the reconnaissance study undertaken with the support of Geo2D, two priority targets were identified, out of which Dabbahu (Teru Woreda, also called Boina, meaning fumarole in Afar language) appears to be quite promising and eventually one of the major geothermal sites in Ethiopia. The Teru plain (which gave the name to the Woreda) lies at an altitude of 330 to 370 metres along the eastern foot of the Nubian escarpment.
    [Show full text]
  • The 2011 Eruption of Nabro Volcano, Eritrea: Perspectives on Magmatic Processes from Melt Inclusions
    Contributions to Mineralogy and Petrology (2018) 173:1 https://doi.org/10.1007/s00410-017-1425-2 ORIGINAL PAPER The 2011 eruption of Nabro volcano, Eritrea: perspectives on magmatic processes from melt inclusions Amy Donovan1,3 · Jon Blundy2 · Clive Oppenheimer3 · Iris Buisman4 Received: 22 February 2017 / Accepted: 14 November 2017 © The Author(s) 2017. This article is an open access publication Abstract The 2011 eruption of Nabro volcano, Eritrea, produced one of the largest volcanic sulphur inputs to the atmosphere since the 1991 eruption of Mt. Pinatubo, yet has received comparatively little scientific attention. Nabro forms part of an off-axis alignment, broadly perpendicular to the Afar Rift, and has a history of large-magnitude explosive silicic eruptions, as well as smaller more mafic ones. Here, we present and analyse extensive petrological data obtained from samples of trachybasal- tic tephra erupted during the 2011 eruption to assess the pre-eruptive magma storage system and explain the large sulphur emission. We show that the eruption involved two texturally distinct batches of magma, one of which was more primitive and richer in sulphur than the other, which was higher in water (up to 2.5 wt%). Modelling of the degassing and crystallisa- tion histories demonstrates that the more primitive magma rose rapidly from depth and experienced degassing crystallisa- tion, while the other experienced isobaric cooling in the crust at around 5 km depth. Interaction between the two batches occurred shortly before the eruption. The eruption itself was likely triggered by recharge-induced destabilisation of vertically extensive mush zone under the volcano. This could potentially account for the large volume of sulphur released.
    [Show full text]
  • Insights from a 2015–2020 Sentinel‐1 Insar Survey
    Albino, F. , & Biggs, J. J. (2021). Magmatic Processes in the East African Rift System: Insights from a 2015-2020 Sentinel-1 InSAR survey. Geochemistry, Geophysics, Geosystems, 22(3), [e2020GC009488]. https://doi.org/10.1029/2020GC009488 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1029/2020GC009488 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via AGU at https://doi.org/10.1029/2020GC009488 .Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ RESEARCH ARTICLE Magmatic Processes in the East African Rift System: 10.1029/2020GC009488 Insights From a 2015–2020 Sentinel-1 InSAR Survey Key Points: F. Albino1 and J. Biggs1 • InSAR survey (2015–2020) detects deformation at 14 Holocene 1COMET, School of Earth Sciences, University of Bristol, Bristol, UK volcanoes in the East African Rift System • Episodes of uplift are detected on several centers with no historical eruptions (Corbetti, Suswa) Abstract The East African Rift System (EARS) is composed of around 78 Holocene volcanoes, but • New subsidence signals are caused relatively little is known about their past and present activity. This lack of information makes it difficult by lava compaction at Kone and to understand their eruptive cycles, their roles in continental rifting and the threat they pose to the geothermal activity at Olkaria population.
    [Show full text]