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UNHCR LBN HLT MAP 2014-05-12 01 A1 Bekaa Governorate Reaching the Most Vulnerable Localities and Phcs SHC MMU.Mxd
SYRIA REFUGEE RESPONSE LEBANON, Bekaa Governorate Reaching the Most Vulnerable Localities in Lebanon, Health centers PHC,SHC and MMU 34°30'0"N 34°30'0"N 20 G" Location Health Facility Information Charbine El-Hermel Number P_Code Longitud_E Latitude_N ACS_CODE Governorate District Cadastral Name Village Name of Health Facility Name From MOPH List Arabic Name From MOPH List English El Ain El Ain PHCC 8 53217_31_001 36.37803046 34.22604727 53217Bekaa Baalbek Aain Baalbek Aarsal Ersal PHCC (Leshmania trained) 9 53231_31_001 36.41959158 34.17923604 53231Bekaa Baalbek Aarsal Baalbek Aarsal Ersal PHC - RHF Hariri Foundation / Irsaal Center ا ر ز ا - رل Bekaa Aarsal 53231 34.17923604 36.41959158 002_31_53231 10 Hermel Baalbek Aarsal MSF clinic at Al Irshad 11 53231_31_003 36.41959158 34.17923604 53231 Bekaa Aarsal El Hermel Baalbek Baalbek PHCC (RHF clinic ) 12 53111_31_001 36.21682 33.99931 Hariri foundation /Baalbeck .Hermil Gov در ا - ك - ؤ رق ا رري 53111Bekaa Baalbek Baalbek Baalbek Baalbek MSF clinic 13 53111_31_002 36.207957 34.005186 53111 Bekaa Baalbek Michaa Mrajhine 1918 v® Baalbek Baalbeck MOSA 14 53111_31_003 36.20795714 34.0051863 53111Bekaa Baalbek Baalbek G" G" Iaat Iaat MOPH primary health center Qaa Ouadi El-Khanzir Qaa Jouar Maqiye Iaat Governmental Health Center ات ا ا و 53123Bekaa Baalbek Iaat 34.03066923 36.16996004 001_31_53123 15 Laboue Larboue PHCC MOPH, Pending Funding Approval Zighrine 17 (Laboueh Municipality Center v® Batoul Hosp (hirmel ر ز د ا وة - ك 53234Bekaa Baalbek Laboue 34.1954277 36.35557781 001_31_53234 -
3Ws Mapping: January - December 2018
Livelihoods Sector 3Ws Mapping: January - December 2018 MSME/Cooperatives Support Job creation through investment in and Value Chains infrastructures and assets Number of Partners: 1 - 2 3 - 4 5 - 6 Aabboudiye Tall Bire Cheikhlar Aamayer Tall Meaayan Tall Kiri Kouachra 7 - 9 Baghdadi Tall Aabbas Ech-Charqi Ghazayle Tleil Biret Aakkar Qleiaat Aakkar Hayssa Khirbet Daoud Aakkar Tall Aabbas El-Gharbi Rihaniyet Aakkar Khirbet Char Rmoul Berbara Aakkar Qaabrine Khreibet Ej-Jindi Knisse 10 - 11 Mqaiteaa HalbaKroum El-AarabSouaisset Aakkar Machha Jdidet Ej-Joumeh Qoubber Chamra Cheikh Taba Aamaret Aakkar Zouarib Deir Dalloum Qantarat Aakkar Aain Yaaqoub Zouq El Hosniye Tikrit Ouadi El-Jamous Bezbina Bqerzla Mhammaret Bebnine Majdala Hmaire Aakkar Zouq Bhannine berqayel Minie Merkebta Fnaydeq Nabi Youcheaa Jdeidet El-Qaitaa Hrar Mina N 3 Beddaoui Mina N 2 Mina Jardin Trablous Et-Tell Michmich Aakkar TrablousTrablous El-Haddadine, jardins El-Hadid, El-Mharta Btermaz Hermel Miriata Trablous Ez-Zeitoun Bakhaaoun tarane Zgharta Qalamoun Bkeftine Sir Ed-Danniye Dedde Enfe Bqaa Sefrine Ras Baalbek El Gharbi Dar Chmizzine Batroun Bcharre Fekehe Aain Baalbek Aaynata Baalbek Laboue Aarsal -
Inter-Agency Q&A on Humanitarian Assistance and Services in Lebanon (Inqal)
INQAL- INTER AGENCY Q&A ON HUMANITARIAN ASSISTANCE AND SERVICES IN LEBANON INTER-AGENCY Q&A ON HUMANITARIAN ASSISTANCE AND SERVICES IN LEBANON (INQAL) Disclaimers: The INQAL is to be utilized mainly as a mass information guide to address questions from persons of concern to humanitarian agencies in Lebanon The INQAL is to be used by all humanitarian workers in Lebanon The INQAL is also to be used for all available humanitarian hotlines in Lebanon The INQAL is a public document currently available in the Inter-Agency Information Sharing web portal page for Lebanon: http://data.unhcr.org/syrianrefugees/documents.php?page=1&view=grid&Country%5B%5D=122&Searc h=%23INQAL%23 The INQAL should not be handed out to refugees If you and your organisation wish to publish the INQAL on any website, please notify the UNHCR Information Management and Mass Communication Units in Lebanon: [email protected] and [email protected] Updated in April 2015 INQAL- INTER AGENCY Q&A ON HUMANITARIAN ASSISTANCE AND SERVICES IN LEBANON INTER-AGENCY Q&A ON HUMANITARIAN ASSISTANCE AND SERVICES IN LEBANON (INQAL) EDUCATION ................................................................................................................................................................ 3 FOOD ........................................................................................................................................................................ 35 FOOD AND ELIGIBILITY ............................................................................................................................................ -
Syria Refugee Response
SYRIA REFUGEE RESPONSE LEBANON, Bekaa & Baalbek-El Hermel Governorate Distribution of the Registered Syrian Refugees at the Cadastral Level As o f 3 0 Se p t e m b e r 2 0 2 0 Charbine El-Hermel BEKAA & Baalbek - El Hermel 49 Total No. of Household Registered 73,427 Total No. of Individuals Registered 340,600 Hermel 6,580 El Hermel Michaa Qaa Jouar Mrajhine Maqiye Qaa Ouadi Zighrine El-Khanzir 36 5 Hermel Deir Mar Jbab Maroun Baalbek 29 10 Qaa Baalbek 10,358 Qaa Baayoun 553 Ras Baalbek El Gharbi Ras Baalbek 44 Ouadi Faara Ras Baalbek Es-Sahel Ouadi 977 Faara Maaysra 4 El-Hermel 32 Halbata Ras Baalbek Ech-Charqi 1 Zabboud 116 Ouadi 63 Fekehe El-Aaoss 2,239 Kharayeb El-Hermel Harabta 16 Bajjaje Aain 63 7 Baalbek Sbouba 1,701 Nabha Nabi Ed-Damdoum Osmane 44 288 Aaynata Baalbek Laboue 34 1,525 Barqa Ram 29 Baalbek 5 Qarha Baalbek Moqraq Chaat Bechouat Aarsal 2,031 48 Riha 33,521 3 Yammoune 550 Deir Kneisset El-Ahmar Baalbek 3,381 28 Dar Btedaai Baalbak El-Ouassaa 166 30 Youmine 2,151 Maqne Chlifa Mazraat 260 beit 523 Bouday Mchaik Nahle 1,501 3 Iaat baalbek haouch 2,421 290 El-Dehab 42 Aadous Saaide 1,244 Hadath 1,406 Haouch Baalbek Jebaa Kfar Dane Haouche Tall Safiye Baalbek 656 375 Barada 12,722 478 466 Aamchki Taraiya Majdaloun 13 905 1,195 Douris Slouqi 3,210 Aain Hizzine Taibet Bourday Chmistar 361 Baalbek 160 2,284 515 Aain Es-Siyaa Chadoura Kfar Talia Bednayel 1,235 Dabach Haouch Baalbak Brital Nabi 159 En-Nabi 2,328 Temnine Beit Haouch 4,552 Chbay 318 El-Faouqa Chama Snaid Haour Chaaibe 1,223 605 Mousraye 83 Taala 16 9 Khodr 192 Qaa -
Contribution to the Knowledge of the Clown Beetle Fauna of Lebanon, with a Key to All Species (Coleoptera, Histeridae)
ZooKeys 960: 79–123 (2020) A peer-reviewed open-access journal doi: 10.3897/zookeys.960.50186 RESEARCH ARTICLE https://zookeys.pensoft.net Launched to accelerate biodiversity research Contribution to the knowledge of the clown beetle fauna of Lebanon, with a key to all species (Coleoptera, Histeridae) Salman Shayya1, Tomáš Lackner2 1 Faculty of Health Sciences, American University of Science and Technology, Beirut, Lebanon 2 Bavarian State Collection of Zoology, Münchhausenstraße 21, 81247 Munich, Germany Corresponding author: Tomáš Lackner ([email protected]) Academic editor: M. Caterino | Received 16 January 2020 | Accepted 22 June 2020 | Published 17 August 2020 http://zoobank.org/D4217686-3489-4E84-A391-1AC470D9875E Citation: Shayya S, Lackner T (2020) Contribution to the knowledge of the clown beetle fauna of Lebanon, with a key to all species (Coleoptera, Histeridae). ZooKeys 960: 79–123. https://doi.org/10.3897/zookeys.960.50186 Abstract The occurrence of histerids in Lebanon has received little specific attention. Hence, an aim to enrich the knowledge of this coleopteran family through a survey across different Lebanese regions in this work. Sev- enteen species belonging to the genera Atholus Thomson, 1859,Hemisaprinus Kryzhanovskij, 1976, Hister Linnaeus, 1758, Hypocacculus Bickhardt, 1914, Margarinotus Marseul, 1853, Saprinus Erichson, 1834, Tribalus Erichson, 1834, and Xenonychus Wollaston, 1864 were recorded. Specimens were sampled mainly with pitfall traps baited with ephemeral materials like pig dung, decayed fish, and pig carcasses. Several species were collected by sifting soil detritus, sand cascading, and other specialized techniques. Six newly recorded species for the Lebanese fauna are the necrophilous Hister sepulchralis Erichson, 1834, Hemisap- rinus subvirescens (Ménétriés, 1832), Saprinus (Saprinus) externus (Fischer von Waldheim, 1823), Saprinus (Saprinus) figuratus Marseul, 1855, and Saprinus (Saprinus) niger (Motschulsky, 1849) all associated with rotting fish and dung, and the psammophilousXenonychus tridens (Jacquelin du Val, 1853). -
REGIONAL GEOGRAPHY of AFRICA. Uganda Certificate of Education
REGIONAL GEOGRAPHY OF AFRICA. Uganda Certificate of Education. GEOGRAPHY Code: 273/2, Paper 2 2 hours 30 minutes PART I : THE REST OF AFRICA. INSTRUCTIONS TO CANDIDATES: This paper consists of two sections: Part I Rest of Africa. Answer two questions from part I @ question carry 25marks. Any additional question (s) answered will not be marked. Four questions are set and a candidate is required to answer only two questions. This region covers 50% of paper 273/2. 1) Download and print out a hard copy then copy this notes in a fresh book for Rest of Africa paper2. 2) If You need a copy of this work organized by the teacher for Rest of Africa. Call 0775 534057 for a book of Africa and it will be delivered. Emihen – Utec 1 SIZE, SHAPE AND POSITION. POSITION OF AFRICA. Africa is one of the largest continents of the world. It’s the second to the largest landmass combined of Eurasia i.e. Europe and Asia continents. LOCATION: Africa lies between latitudes 37.51’N just West of Cape Blanc in Tunisia to Cape Aghulhas at Latitude 34.51’S a distance of 8,000kms. Africa also lies between Cape Ras Hagun 51.50’E and Cape Verde 17.32’W. SIZE: Africa covers land area of about 30,300,300km2. THE SHAPE: Africa’s shape is unbalanced; with her northern part being bulky and wide, while the southern part being thinner and narrower in appearance. Emihen-Utec 2 The Latitude EQUATOR divides the continent into TWO HALVES, there being approximately; 3800kms between the Cape Agulhas in the south and Equator while between Tunisia and Equator in the North is 4,100kms. -
Ocean Drilling Program Initial Reports Volume
Backman, J., Duncan, R. A., et al., 1988 Proceedings of the Ocean Drilling Program, Initial Reports, Vol. 115 1. INTRODUCTION1 Shipboard Scientific Party2 Leg 115 is the first of a nine-leg program of exploration of these volcanic islands and submarine (presumed volcanic) ridges the Indian Ocean. Previous drilling by the Deep Sea Drilling is consistent with northward motion of the Indian plate, fol- Program (DSDP), Legs 22 through 29 (1972-73), resulted in the lowed by northeastward motion of the African plate, over a first detailed information about the geologic and Oceanographic fixed melting anomaly at the location of Reunion during Ter- history of this major region of the oceans. Compared with the tiary time (Morgan, 1981; Duncan, 1981). In addition, this vol- Atlantic and Pacific Ocean Basins, however, the Indian Ocean is canic trail is parallel with the Ninetyeast Ridge, another subma- still relatively unexplored. During this multifaceted investiga- rine lineament linked to hotspot activity (now centered near the tion, we hoped to examine many fundamental questions. The Kerguelen Islands, Antarctic plate), and the two may record the scientific objectives of this leg fell into two main subject areas: northward motion of India during the opening of the Indian hotspot volcanism and paleoceanography. Ocean. Until Leg 115, however, the only accessible sampling loca- HOTSPOTS AND PLATE TECTONICS tions along the proposed Reunion hotspot track were the young An extraordinary feature of the Indian Ocean is the large volcanic islands at the southern end and the Deccan flood ba- number of elevated plateaus and ridges scattered throughout the salts at the northern end. -
Funded Projects
Funded projects Since the year 2000, Child of Lebanon has been funding over 155 specific priority projects presented by the institutions. Of the $3,111,000 donation allocated since 1996, $2,827,000 was allocated for this purpose, or 91% of the total (and 100% the last 5 years. The cash balance was allocated to the institutions for their general purposes. Allocation of donations Total in $ 10 - 11 09 - 10 08 - 09 07 - 08 06 - 07 05 - 06 04 - 05 03 - 04 02 - 03 01 - 02 00 - 01 99 - 00 96 - 99 3,232,348 Donat ions raised 341, 737 341, 950 503, 176 718,928 282,538 210,676 200,792 171,922 150,787 127, 256 81,056 51, 300 50, 230 3,110,680 Donations allocated 341, 001 415, 930 471, 628 568,200 277,476 206,270 204,843 170,292 147,645 124, 950 80,915 51, 300 50, 230 2,826,605 Funded projects ($) 341, 001 415, 930 471, 628 568,200 277,476 198,470 187,800 137,800 118,000 72,900 37,400 - - 91% in % of alloc ation 100% 100% 100% 100% 100% 96% 92% 81% 80% 58% 46% - - 258,845 Allocation in cash000007,80017,04332,49229,64552,05043,51551,30025,000 Maison Notre Dame (Zahle) $6,000 repair of leaking roofs – 2000 / 01 $8,000 sewing & PC workshop - 01 / 02 Noting that many young girls of the region had their schooling interrupted at an early age by their parents wanting them to work in the fields, the “Maison” decided to offer free vocational training for those who could manage to attend the courses by setting up a sewing & PC workshop. -
The African Plate: a History of Oceanic Crust Accretion and Subduction Since the Jurassic
Tectonophysics 604 (2013) 4–25 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto The African Plate: A history of oceanic crust accretion and subduction since the Jurassic Carmen Gaina a,⁎, Trond H. Torsvik a,b,c, Douwe J.J. van Hinsbergen d, Sergei Medvedev a, Stephanie C. Werner a, Cinthia Labails e a CEED—Centre for Earth Evolution and Dynamics, University of Oslo, Norway b Geodynamics, Geological Survey of Norway, Norway c School of Geosciences, University of Witwatersrand, WITS, 2050, South Africa d Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands e BEICIP, France article info abstract Article history: We present a model for the Jurassic to Present evolution of plate boundaries and oceanic crust of the African Received 13 August 2012 plate based on updated interpretation of magnetic, gravity and other geological and geophysical data sets. Received in revised form 24 May 2013 Location of continent ocean boundaries and age and geometry of old oceanic crust (Jurassic and Cretaceous) Accepted 29 May 2013 are updated in the light of new data and models of passive margin formation. A new set of oceanic palaeo-age Available online 7 June 2013 grid models constitutes the basis for estimating the dynamics of oceanic crust through time and can be used as input for quantifying the plate boundary forces that contributed to the African plate palaeo-stresses and Keywords: fl Africa may have in uenced the evolution of intracontinental sedimentary basins. As a case study, we compute a Oceanic crust simple model of palaeo-stress for the Late Cretaceous time in order to assess how ridge push, slab pull and Relative and absolute motion horizontal mantle drag might have influenced the continental African plate. -
Rift-Valley-1.Pdf
R E S O U R C E L I B R A R Y E N C Y C L O P E D I C E N T RY Rift Valley A rift valley is a lowland region that forms where Earth’s tectonic plates move apart, or rift. G R A D E S 6 - 12+ S U B J E C T S Earth Science, Geology, Geography, Physical Geography C O N T E N T S 9 Images For the complete encyclopedic entry with media resources, visit: http://www.nationalgeographic.org/encyclopedia/rift-valley/ A rift valley is a lowland region that forms where Earth’s tectonic plates move apart, or rift. Rift valleys are found both on land and at the bottom of the ocean, where they are created by the process of seafloor spreading. Rift valleys differ from river valleys and glacial valleys in that they are created by tectonic activity and not the process of erosion. Tectonic plates are huge, rocky slabs of Earth's lithosphere—its crust and upper mantle. Tectonic plates are constantly in motion—shifting against each other in fault zones, falling beneath one another in a process called subduction, crashing against one another at convergent plate boundaries, and tearing apart from each other at divergent plate boundaries. Many rift valleys are part of “triple junctions,” a type of divergent boundary where three tectonic plates meet at about 120° angles. Two arms of the triple junction can split to form an entire ocean. The third, “failed rift” or aulacogen, may become a rift valley. -
Plate Kinematics of the Afro-Arabian Rift System with an Emphasis on the Afar Depression
Scholars' Mine Doctoral Dissertations Student Theses and Dissertations Fall 2012 Plate kinematics of the Afro-Arabian Rift System with an emphasis on the Afar Depression Helen Carrie Bottenberg Follow this and additional works at: https://scholarsmine.mst.edu/doctoral_dissertations Part of the Geology Commons, and the Geophysics and Seismology Commons Department: Geosciences and Geological and Petroleum Engineering Recommended Citation Bottenberg, Helen Carrie, "Plate kinematics of the Afro-Arabian Rift System with an emphasis on the Afar Depression" (2012). Doctoral Dissertations. 2237. https://scholarsmine.mst.edu/doctoral_dissertations/2237 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. iii iv PLATE KINEMATICS OF THE AFRO-ARABIAN RIFT SYSTEM WITH EMPHASIS ON THE AFAR DEPRESSION, ETHIOPIA by HELEN CARRIE BOTTENBERG A DISSERTATION Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE & TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree DOCTOR OF PHILOSOPHY in GEOLOGY & GEOPHYSICS 2012 Approved by Mohamed Abdelsalam, Advisor Stephen Gao Leslie Gertsch John Hogan Allison Kennedy Thurmond v 2012 Helen Carrie Bottenberg All Rights Reserved iii PUBLICATION DISSERTATION OPTION This dissertation has been prepared in the style utilized by Geosphere and The Journal of African Earth Sciences. Pages 6-41 and Pages 97-134 will be submitted for separate publications in Geosphere and pages 44-96 will be submitted to Journal of African Earth Sciences iv ABSTRACT This work utilizes the Four-Dimensional Plates (4DPlates) software, and Differential Interferometric Synthetic Aperture Radar (DInSAR) to examine plate-scale, regional- scale and local-scale kinematics of the Afro-Arabian Rift System with emphasis on the Afar Depression in Ethiopia. -
Media and Muslim Women Empowerment
DIPARTIMENTO DI SCIENZE POLITICHE Cattedra di Cultura e Politica dell'Islam MEDIA AND MUSLIM WOMEN EMPOWERMENT RELATORE Prof.ssa Francesca Maria Corrao CANDIDATA Julia del Papa Matr. 613772 CORRELATORE Prof.ssa Emiliana De Blasio ANNO ACCADEMICO 2011-2012 Table of Contents Abstract .................................................................................................... 3 Introduction ............................................................................................. 4 Women and Islam ................................................................................... 7 Women in Islam ....................................................................................................... 7 Women in the Quran and the Sunna ........................................................................ 7 Motherhood in Islam .............................................................................................. 11 Islam in Different Countries ................................................................................... 14 Brief History of Islam in Relation to the Role of Muslim Women ........................ 20 Interpretations of the Quran ................................................................................... 22 Islamic Feminism ................................................................................................... 24 Final Considerations............................................................................................... 26 Women in the Arab World Today ......................................................