Israel National Bathymetric Survey (NBS). a Cooperative Project Between the GSI, IOLR, and MAPI
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Community Structure and Biogeography of Shore Fishes in the Gulf of Aqaba, Red Sea
Helgol Mar Res (2002) 55:252–284 DOI 10.1007/s10152-001-0090-y ORIGINAL ARTICLE Maroof A. Khalaf · Marc Kochzius Community structure and biogeography of shore fishes in the Gulf of Aqaba, Red Sea Received: 2 April 2001 / Received in revised form: 2 November 2001 / Accepted: 2 November 2001 / Published online: 24 January 2002 © Springer-Verlag and AWI 2002 Abstract Shore fish community structure off the Jorda- Introduction nian Red Sea coast was determined on fringing coral reefs and in a seagrass-dominated bay at 6 m and 12 m Coral reefs are one of the most complex marine ecosys- depths. A total of 198 fish species belonging to 121 gen- tems in which fish communities reach their highest de- era and 43 families was recorded. Labridae and Poma- gree of diversity (Harmelin-Vivien 1989). Morphological centridae dominated the ichthyofauna in terms of species properties and the geographical region of the coral reef richness and Pomacentridae were most abundant. Nei- determine the structure of the fish assemblages (Sale ther diversity nor species richness was correlated to 1980; Thresher 1991; Williams 1991). The ichthyofauna depth. The abundance of fishes was higher at the deep of coral reefs can be linked to varying degrees with adja- reef slope, due to schooling planktivorous fishes. At cent habitats (Parrish 1989) such as seagrass meadows 12 m depth abundance of fishes at the seagrass-dominat- (Ogden 1980; Quinn and Ogden 1984; Roblee and ed site was higher than on the coral reefs. Multivariate Ziemann 1984; Kochzius 1999), algal beds (Rossier and analysis demonstrated a strong influence on the fish as- Kulbicki 2000) and mangroves (Birkeland 1985; Thollot semblages by depth and benthic habitat. -
Boundary & Territory Briefing
International Boundaries Research Unit BOUNDARY & TERRITORY BRIEFING Volume 1 Number 8 The Evolution of the Egypt-Israel Boundary: From Colonial Foundations to Peaceful Borders Nurit Kliot Boundary and Territory Briefing Volume 1 Number 8 ISBN 1-897643-17-9 1995 The Evolution of the Egypt-Israel Boundary: From Colonial Foundations to Peaceful Borders by Nurit Kliot Edited by Clive Schofield International Boundaries Research Unit Department of Geography University of Durham South Road Durham DH1 3LE UK Tel: UK + 44 (0) 191 334 1961 Fax: UK +44 (0) 191 334 1962 E-mail: [email protected] www: http://www-ibru.dur.ac.uk The Author N. Kliot is a Professor and Chairperson of the Department of Geography, University of Haifa, and Head of the Centre for Natural Resources Studies at the University of Haifa. Her specialistion is political geography, and she is a member of the International Geographical Union (IGU) Commission on Political Geography. She writes extensively on the Middle East and among her recent publications are: Water Resources and Conflict in the Middle East (Routledge, 1994) and The Political Geography of Conflict and Peace (Belhaven, 1991) which she edited with S. Waterman. The opinions contained herein are those of the author and are not to be construed as those of IBRU Contents Page 1. Introduction 1 2. The Development of the Egypt-Palestine Border, 1906-1918 1 2.1 Background to delimitation 1 2.2 The Turco-Egyptian boundary agreement of 1906 4 2.3 The delimitation of the Egypt-Palestine boundary 7 2.4 The demarcation of the Egypt-Palestine boundary 7 2.5 Concluding remarks on the development of the Egypt- Palestine border of 1906 8 3. -
Field Identification Guide to the Sharks and Rays of the Red Sea and Gulf of Aden
FAO SPECIES IDENTIFICATION GUIDE FOR FISHERY PURPOSES ISSN 1020-6868 FIELD IDENTIFICATION GUIDE TO THE SHARKS AND RAYS OF THE RED SEA AND GULF OF ADEN PERSGA FAO SPECIES IDENTIFICATION GUIDE FOR FISHERY PURPOSES FIELD IDENTIFICATION GUIDE TO THE SHARKS AND RAYS OF THE RED SEA AND GULF OF ADEN by Ramón Bonfil Marine Program Wildlife Conservation Society Bronx, New York, USA and Mohamed Abdallah Strategic Action Program Regional Organization for the Conservation of the Environment of the Red Sea and Gulf of Aden Jeddah, Saudi Arabia FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2004 iii PREPARATION OF THIS DOCUMENT This document was prepared under the coordination of the Species Identification and Data Programme of the Marine Resources Service, Fishery Resources and Environment Division, Fisheries Department, Food and Agriculture Organization of the United Nations (FAO). This field guide is largely based on material prepared for training courses on elasmobranch identification delivered in the region by the first author, and promoted by the Regional Organization for the Conservation of the Environment of the Red Sea and Gulf of Aden (PERSGA), as an activity of PERSGA’s Strategic Action Programme (SAP) towards capacity building and technical assistance in the Red Sea and Gulf of Aden region. Printing was supported by Japanese Government funds. The increasing recognition of the significance of sharks and batoid fishes as ecosystem health indicators, as well as their particular importance in exploited ecosystems in the Red Sea and the Gulf of Aden, have been key considerations to promote the preparation of this Field Guide. Furthermore, in recent years the reported catches of elasmobranchs in the Red Sea and the Gulf of Aden showed a marked increase. -
Active Faults' Geometry in the Gulf of Aqaba, Southern Dead Sea Fault, Illuminated by Multi Beam Bathymetric Data
Active faults' geometry in the Gulf of Aqaba, southern Dead Sea fault, illuminated by multi beam bathymetric data Item Type Preprint Authors Ribot, Matthieu; Klinger, Yann; Jonsson, Sigurjon; Avsar, Ulas; Pons-Branchu, Edwige; Matrau, Rémi; Mallon, Francis L Citation Ribot, M., Klinger, Y., Jónsson, S., Avsar, U., Pons-Branchu, E., Matrau, R., & Mallon, F. L. (2020). Active faults’ geometry in the Gulf of Aqaba, southern Dead Sea fault, illuminated by multi beam bathymetric data. doi:10.1002/essoar.10504675.1 Eprint version Pre-print DOI 10.1002/essoar.10504675.1 Publisher Wiley Rights Archived with thanks to Wiley Download date 25/09/2021 04:39:22 Link to Item http://hdl.handle.net/10754/665920.1 ESSOAr | https://doi.org/10.1002/essoar.10504675.1 | CC_BY_NC_ND_4.0 | First posted online: Sat, 7 Nov 2020 07:45:32 | This content has not been peer reviewed. manuscript submitted to Tectonics 1 Active faults' geometry in the Gulf of Aqaba, southern Dead Sea fault, 2 illuminated by multi beam bathymetric data 3 4 AUTHORS: Matthieu Ribot1,4, Yann Klinger1, Sigurjón Jónsson2, Ulas Avsar3, Edwige 5 Pons-Branchu4, Rémi Matrau2, and Francis L. Mallon2 6 7 (1) Université de Paris, Institut de physique du globe de Paris, CNRS, Paris, France. 8 (2) King Abdullah University of Science and Technology, Thuwal, Saudi Arabia. 9 (3) Middle East Technical University, Ankara, Turkey. 10 (4) Laboratoire des Sciences du Climat et de l’Environnement, Gif-sur-Yvette, France. 11 12 Corresponding author: Matthieu Ribot ([email protected]) 13 14 Key points 15 • High-resolution bathymetry of the Gulf of Aqaba 16 • Detailed map of a complex fault system including strike-slip and normal faulting 17 • Surface rupture of the Mw 7.3, 1995, Nuweiba earthquake and possible location of 18 future earthquakes 19 20 Abstract 21 Detailed knowledge of fault geometry is important for accurate seismic hazard assessments. -
Three Conquests of Canaan
ÅA Wars in the Middle East are almost an every day part of Eero Junkkaala:of Three Canaan Conquests our lives, and undeniably the history of war in this area is very long indeed. This study examines three such wars, all of which were directed against the Land of Canaan. Two campaigns were conducted by Egyptian Pharaohs and one by the Israelites. The question considered being Eero Junkkaala whether or not these wars really took place. This study gives one methodological viewpoint to answer this ques- tion. The author studies the archaeology of all the geo- Three Conquests of Canaan graphical sites mentioned in the lists of Thutmosis III and A Comparative Study of Two Egyptian Military Campaigns and Shishak and compares them with the cities mentioned in Joshua 10-12 in the Light of Recent Archaeological Evidence the Conquest stories in the Book of Joshua. Altogether 116 sites were studied, and the com- parison between the texts and the archaeological results offered a possibility of establishing whether the cities mentioned, in the sources in question, were inhabited, and, furthermore, might have been destroyed during the time of the Pharaohs and the biblical settlement pe- riod. Despite the nature of the two written sources being so very different it was possible to make a comparative study. This study gives a fresh view on the fierce discus- sion concerning the emergence of the Israelites. It also challenges both Egyptological and biblical studies to use the written texts and the archaeological material togeth- er so that they are not so separated from each other, as is often the case. -
Geological Evolution of the Red Sea: Historical Background, Review and Synthesis
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/277310102 Geological Evolution of the Red Sea: Historical Background, Review and Synthesis Chapter · January 2015 DOI: 10.1007/978-3-662-45201-1_3 CITATIONS READS 6 911 1 author: William Bosworth Apache Egypt Companies 70 PUBLICATIONS 2,954 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Near and Middle East and Eastern Africa: Tectonics, geodynamics, satellite gravimetry, magnetic (airborne and satellite), paleomagnetic reconstructions, thermics, seismics, seismology, 3D gravity- magnetic field modeling, GPS, different transformations and filtering, advanced integrated examination. View project Neotectonics of the Red Sea rift system View project All content following this page was uploaded by William Bosworth on 28 May 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Geological Evolution of the Red Sea: Historical Background, Review, and Synthesis William Bosworth Abstract The Red Sea is part of an extensive rift system that includes from south to north the oceanic Sheba Ridge, the Gulf of Aden, the Afar region, the Red Sea, the Gulf of Aqaba, the Gulf of Suez, and the Cairo basalt province. Historical interest in this area has stemmed from many causes with diverse objectives, but it is best known as a potential model for how continental lithosphere first ruptures and then evolves to oceanic spreading, a key segment of the Wilson cycle and plate tectonics. -
The Legal Status of Tiran and Sanafir Islands Rajab, 1438 - April 2017
22 Dirasat The Legal Status of Tiran and Sanafir Islands Rajab, 1438 - April 2017 Askar H. Enazy The Legal Status of Tiran and Sanafir Islands Askar H. Enazy 4 Dirasat No. 22 Rajab, 1438 - April 2017 © King Faisal Center for Research and Islamic Studies, 2017 King Fahd National Library Cataloging-In-Publication Data Enazy, Askar H. The Legal Status of Tiran and Sanafir Island. / Askar H. Enazy, - Riyadh, 2017 76 p ; 16.5 x 23 cm ISBN: 978-603-8206-26-3 1 - Islands - Saudi Arabia - History 2- Tiran, Strait of - Inter- national status I - Title 341.44 dc 1438/8202 L.D. no. 1438/8202 ISBN: 978-603-8206-26-3 Table of Content Introduction 7 Legal History of the Tiran-Sanafir Islands Dispute 11 1928 Tiran-Sanafir Incident 14 The 1950 Saudi-Egyptian Accord on Egyptian Occupation of Tiran and Sanafir 17 The 1954 Egyptian Claim to Tiran and Sanafir Islands 24 Aftermath of the 1956 Suez Crisis: Egyptian Abandonment of the Claim to the Islands and Saudi Assertion of Its Sovereignty over Them 26 March–April 1957: Saudi Press Statement and Diplomatic Note Reasserting Saudi Sovereignty over Tiran and Sanafir 29 The April 1957 Memorandum on Saudi Arabia’s “Legal and Historical Rights in the Straits of Tiran and the Gulf of Aqaba” 30 The June 1967 War and Israeli Reoccupation of Tiran and Sanafir Islands 33 The Status of Tiran and Sanafir Islands in the Egyptian-Israeli Peace Treaty of 1979 39 The 1988–1990 Egyptian-Saudi Exchange of Letters, the 1990 Egyptian Decree 27 Establishing the Egyptian Territorial Sea, and 2016 Statements by the Egyptian President -
Seismic Hazards Implications of Uplifted Pleistocene Coral Terraces in the Gulf of Aqaba Received: 9 August 2016 W
www.nature.com/scientificreports OPEN Seismic Hazards Implications of Uplifted Pleistocene Coral Terraces in the Gulf of Aqaba Received: 9 August 2016 W. Bosworth1, P. Montagna2,3,4, E. Pons-Branchu3, N. Rasul5 & M. Taviani2,6,7 Accepted: 27 January 2017 The Gulf of Aqaba transform plate boundary is a source of destructive teleseismic earthquakes. Published: xx xx xxxx Seismicity is concentrated in the central sub-basin and decreases to both the north and south. Although principally a strike-slip plate boundary, the faulted margins of the Gulf display largely dip-slip extensional movement and accompanying footwall uplift. We have constrained rates of this uplift by measurements of elevated Pleistocene coral terraces. In particular the terrace that formed during the last interglacial (~125 ka) is found discontinuously along the length of the Gulf at elevations of 3 to 26 m. Global sea level was ~7 m higher than today at 125 ka indicating net maximum tectonic uplift of ~19 m with an average rate of ~0.015 cm/yr. Uplift has been greatest adjacent to the central sub-basin and like the seismicity decreases to the north and south. We suggest that the present pattern of a seismically active central region linked to more aseismic areas in the north and south has therefore persisted for at least the past 125 kyr. Consequently the potential for future destructive earthquakes in the central Gulf is greater than in the sub-basins to the north and south. Geologic Setting. The Gulf of Aqaba and Dead Sea fault system originated in the Miocene as a transform plate boundary linking the northern Red Sea to the East Anatolian fault and Zagros-Bitlas convergence zone in eastern Turkey1–5 (Figs 1 and 2). -
Report- the Large Cities at a Glance- Compendium of Maps, ICBS
Table of Contents Israeli Association for Cartography and Geographic Information Systems • About……………………………………………………………………………………….………….. 1 • Activities in Israel…………………………………………………………………..………..…….2 • Participation in ICA events……………………………………………………………..………5 Governmental Agencies • The Survey of Israel……………………………………………………………………..………..8 • Central Bureau of Statistics………………………………………………………..………..18 Map Libraries and Private Collectors National Library • Eran Laor Cartographic Collection- National Library of Israel………………..23 Academic Collections • Bloomfield Library for the Humanities and Social Sciences -Hebrew University in Jerusalem- Map Library and Geography Department……...25 • Tel Aviv University Geography Library………………………………………………….28 • Tel Hai Historical Map Archive- Tel Hai Academic College…………………...30 • Yad Izhak Ben-Zvi Map Archive………………………………………………………..…..31 • Younes & Soraya Nazarian Library- Map Collection, University of Haifa.33 Private Collectors • Bar Stav Collection of Ancient Maps of the Holy Land………………………….34 Private Sector • Ad-Or- Mapping the Old City of Jerusalem………………………………………….35 • Amud Anan Online Geo-Encyclopedia………………………………………………….36 • Avigdor Orgad Maps…………………………………………………………………………….37 • Blushtein Mapot Veod L.T.D. ……………………………………………………………….38 • Bonus-Yavne Publishing …………………………………………………………………….39 • GeoCartography Knowledge Group………………………………………………………40 • Israel Hiking and Biking Map ……………………………………………………………….42 • Mapa ………………………………………………………………………………………………..43 • Mind the Map ……………………………………………………………………………………..46 • Soffer -
Saudi Arabia and the Law of the Sea
633 SAUDI ARABIA AND THE LAW OF THE SEA James P. Piscatori* The Middle East, broadly defined, is Red Sea is important as the gateway to penetrated by five bodies of water, the the Suez Canal, which itself was eco five "fingers" of the Mediterranean, nomically and strategically significant Black, Caspian, and Red Seas, and the prior to 1967, because it reduces by Persian Gulf. The Red Sea and Gulf one-half the Gulf to London journey. have received particular attention in The recently reopened canal probably recent history. The significance of the will be highly significant again as it is Red Sea stems, first of all, \ from its widened and deepened to accommodate connection to the Arab-Israeli conflict. ships of the 150,OOO-ton range and Israel has one non-Mediterranean port, eventually of the 270,OOO-ton range? Eilat, which can only be reached Finally, the Soviet base at Berbera in through the Red Sea and then through Somalia highlights the vulnerability of the Gulf of 'Aqaba. Denial of entry to access to the sea itself. Israel through closure of the Straits of Of far greater importance is the Tiran was considered a casus belli in Persian Gulf. Indeed, the growing indus 1967, and in 1973 a blockade of the trial dependence on oil, even more than entire sea was carried out at the Bab the discovery and exploitation of the al-Mandab Strait to support the war aims of the Arab front. Some strategists *1 wish to acknowledge with gratitude the believe that in a long war similar action assistance of Professors K. -
OECD Economic Surveys
OECD Economic Surveys Israel March 2018 OVERVIEW www.oecd.org/eco/surveys/economic-survey-israel.htm This Overview is extracted from the Economic Survey of Israel. The Survey is published on the responsibility of the Economic and Development Review Committee (EDRC) of the OECD, which is charged with the examination of the economic situation of member countries. This document and any map included herein are without prejudice to the status of or sovereignty over any territory, to the delimitation of international frontiers and boundaries and to the name of any territory, city or area. OECD Economic Surveys: Israel© OECD 2018 You can copy, download or print OECD content for your own use, and you can include excerpts from OECD publications, databases and multimedia products in your own documents, presentations, blogs, websites and teaching materials, provided that suitable acknowledgment of OECD as source and copyright owner is given. All requests for public or commercial use and translation rights should be submitted to [email protected]. Requests for permission to photocopy portions of this material for public or commercial use shall be addressed directly to the Copyright Clearance Center (CCC) at [email protected] or the Centre français d’exploitation du droit de copie (CFC) at [email protected]. OECD Economic Surveys: Israel © OECD 2018 Executive summary ● The economy is strong ● Income inequality has fallen, but economic disparities and a lack of social cohesion persist ● Reforming education, infrastructure and product markets will enhance inclusiveness and productivity The statistical data for Israel are supplied by and under the responsibility of the relevant Israeli authorities. -
Innovative Solutions for Water Wars in Israel, Jordan, and The
INNOVATIVE SOLUTIONS FOR WATER WARS IN ISRAEL, JORDAN AND THE PALESTINIAN AUTHORITY J. David Rogers K.F. Hasselmann Chair, Department of Geological Engineering 129 McNutt Hall, 1870 Miner Circle University of Missouri-Rolla, Rolla, MO 65409-0230 [email protected] (573) 341-6198 [voice] (573) 341-6935 [fax] ABSTRACT In the late 1950s Jordan and Israel embarked on a race to collect, convey and disperse the free-flowing waters of the Jordan River below the Sea of Galilee. In 1955 the Johnston Unified Water Plan was adopted by both countries as a treaty of allocation rights. By 1961 the Jordanians completed their 110-km long East Ghor Canal, followed by Israel’s 85-km long National Water Carrier, initially completed in 1964 and extended in 1969. The Johnston allocation plan was successfully implemented for 12 years, until the June 1967 war between Israel and her neighbor Arab states. The Israelis have spearheaded the effort to exploit the region’s limited water resources, using wells, pipelines, canals, recharge basins, drip irrigation, fertigation, wastewater recharge, saline irrigation and, most recently, turning to desalination. In 1977 they began looking at various options to bring sea water to the depleted Dead Sea Basin, followed by similar studies undertaken by the Jordanians a few years later. A new water allocation plan was agreed upon as part of the 1994 Israel-Jordan peace treaty, but it failed to address Palestinian requests for additional allotments, which would necessarily have come from Jordan or Israel. The subject of water allocation has become a non-negotiable agenda for the Palestinian Authority in its ongoing political strife with Israel.