General: Anonymous. Periplus Maris Erythraei (Or 'Voyage Around The
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000000548.Sbu.Pdf
SSStttooonnnyyy BBBrrrooooookkk UUUnnniiivvveeerrrsssiiitttyyy The official electronic file of this thesis or dissertation is maintained by the University Libraries on behalf of The Graduate School at Stony Brook University. ©©© AAAllllll RRRiiiggghhhtttsss RRReeessseeerrrvvveeeddd bbbyyy AAAuuuttthhhooorrr... Archaeological Investigation of the Buri Peninsula and Gulf of Zula, Red Sea Coast of Eritrea A Dissertation Presented by Amanuel Yosief Beyin to The Graduate School in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Anthropology (Archaeology) Stony Brook University May 2009 Stony Brook University The Graduate School Amanuel Yosief Beyin We, the dissertation committee for the above candidate for the Doctor of Philosophy degree, hereby recommend acceptance of this dissertation. John J. Shea Associate Professor, Anthropology David J. Bernstein Associate Professor, Anthropology John G. Fleagle Distinguished Professor, Anatomical Sciences Steven A. Brandt Associate Professor, Anthropology University of Florida, Gainesville This dissertation is accepted by the Graduate School Lawrence Martin Dean of the Graduate School ii Abstract of the Dissertation Archaeological Investigation of the Buri Peninsula and Gulf of Zula, Red Sea Coast of Eritrea by Amanuel Yosief Beyin Doctor of Philosophy in Anthropology (Archaeology) Stony Brook University 2009 This dissertation reports the results of archaeological survey and excavations on the Buri Peninsula and Gulf of Zula, Red Sea coast of Eritrea. Its primary goals were to seek evidence for prehistoric human settlement, and to define the geological, chronological and cultural contexts of the sites. The Red Sea Coast of Africa is thought to be an important refugium for humans dispersing from the interior of East Africa into Arabia and the Levant. -
Fish and Fishing
CHAPTER TWELVE Fish and Fishing D.T. Potts 1 Introduction The benefi ts of fi sh in the human diet have long been recognized. With an average protein content of 18 – 22 percent and other important elements (essential amino acids, calcium, fl ourine, iodine, iron, phosphorus; Vitamins A, B, and D), fi sh have been an important component of the low - protein, high - carbohydrate diets that have been common in the Near East throughout the pre - Modern era (Englund 1990 : 7 n33; see in general Van Neer 1994 ). Nowadays, the benefi ts of Omega 3 fatty acids in fi sh oil are promoted for their ability to help the body combat everything from Alzheimer ’ s disease to cancer, ulcers, and many more affl ictions. Nevertheless, considering the fact that the region dealt with in this volume contains long stretches of shoreline on at least seven seas (Aegean, Medi- terranean, Black, Red, Caspian and Arabian Seas, and the Persian Gulf), as well as a number of major rivers (Tigris, Euphrates, Karun, Orontes, Khabur, Balikh, Jordan, Greater Zab) and lakes (e.g., Lake Kinneret, Lake Van, Lake Parishan, Hamun - e Helmand), not to mention thousands of manmade irrigation canals, neither freshwater nor saltwater fi sh in Near Eastern antiquity have received the attention that they deserve. The purpose of this chapter is to provide a broad overview of a number of issues associated with fi sh. Topics discussed below include fi sh remains in archaeological contexts; evidence of fi shing sites; fi shing techniques and equipment; written sources on the organization of fi shing; fi sh preparation for consumption and the dietary contribution of fi sh in antiquity; A Companion to the Archaeology of the Ancient Near East, First Edition. -
Saudi Arabia.Pdf
A saudi man with his horse Performance of Al Ardha, the Saudi national dance in Riyadh Flickr / Charles Roffey Flickr / Abraham Puthoor SAUDI ARABIA Dec. 2019 Table of Contents Chapter 1 | Geography . 6 Introduction . 6 Geographical Divisions . 7 Asir, the Southern Region � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �7 Rub al-Khali and the Southern Region � � � � � � � � � � � � � � � � � � � � � � � � � �8 Hejaz, the Western Region � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �8 Nejd, the Central Region � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �9 The Eastern Region � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �9 Topographical Divisions . .. 9 Deserts and Mountains � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �9 Climate . .. 10 Bodies of Water . 11 Red Sea � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � 11 Persian Gulf � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � 11 Wadis � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � 11 Major Cities . 12 Riyadh � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �12 Jeddah � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �13 Mecca � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � -
Historical Ties: India’S Relations with Africa Date Back Several Centuries
EDITORIAL 30TH JULY 2019 GREAT GAME IN AFRICA Context Defence Minister’s recent visit to Mozambique, which is a good moment to reflect on the growing significance of the East African coastal countries and the islands off it for the geopolitics of the Indo-Pacific. Introduction: During the visit to Mozambique, he is expected to sign a number of agreements, including on hydrographic survey, sharing of white shipping information and the monitoring of its exclusive zone. He is also expected to deliver two fast patrol naval craft to the country as part of India’s expanding security cooperation with Mozambique. India and Africa - Historical Ties: India’s relations with Africa date back several centuries. The presence of Indians in East Africa is documented in the 'Periplus of the Erythraean Sea' or Guidebook of the Red Sea by an ancient Greek author written in 60 AD. The geographical proximity and easy navigability in Indian Ocean resulted in well- established trade network between India and the Swahili Coast predating European exploration. More concrete relation between India and Africa begins to emerge during the Islamic age which is evident through the accounts of Venetian traveller Marco Polo. Political connection during the colonial era was linked through M.K Gandhi who began his political career in South Africa, became the leader of colonized and established Indian Natal Congress in 1894. After India got independent, it raised voice for African liberation taking their case to all the available international forums. End of racial struggle and decolonization became the rallying point of India–Africa relations. India was a forerunner as a champion of the interests of the developing countries from Africa, particularly through the Bandung Declaration of 1955, the Group of 77, and the Non-Aligned Movement (NAM). -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
Alexandria, Egypt, Before Alexander the Great: a Multidisciplinary Approach Yields Rich Discoveries
Alexandria, Egypt, before Alexander the Great: A multidisciplinary approach yields rich discoveries Jean-Daniel Stanley*, Geoarchaeology Program, Rm. E-206, drilling, photography, and television, along with refinement of Paleobiology, Smithsonian Institution National Museum of applicable high-resolution seismic methodologies and surveys Natural History (NMNH), Washington, D.C. 20013-7012, by research submarine and remote operated vehicle. Coastal USA; Richard W. Carlson*, Carnegie Institution of Washing- geoarchaeology reached a subdiscipline threshold ~25 years ton, Department of Terrestrial Magnetism, Washington, D.C. ago, at the time of publication of the multi-authored volume on 20015, USA; Gus Van Beek*, Anthropology, Smithsonian Insti- Quaternary coastlines and marine archaeology edited by Mas- tution NMNH, Washington, D.C., 20013-7012, USA; Thomas F. ters and Flemming (1983). Since then, the number of studies Jorstad*, Geoarchaeology Program, Rm. E-206, Paleobiology, that emphasize integration of varied geological and archaeo- Smithsonian Institution NMNH, Washington, D.C. 20013-7012, logical approaches in the marine realm has progressively risen. USA; Elizabeth A. Landau*, Geological Sciences, San Diego Of special note is the increased use of a classic geological State University, San Diego, California 92182-1020, USA methodology, sediment coring, to help resolve archaeological problems at sites that presently lie beneath the waves. This sub- ABSTRACT bottom technology has been applied with successful results in Historic records refer to Rhakotis as a settlement on Egypt’s most world oceans, especially in the Mediterranean (Morhange Mediterranean coast before Alexander the Great founded the et al., 2005; Marriner and Morhange, 2007; Stanley, 2007). famous Mediterranean port city of Alexandria in B.C. -
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. -
Y-Chromosome & Mitochondrial DNA Variation
The Genetic Structure of the Kuwaiti and Failaka Island Populations: Y-chromosome & Mitochondrial DNA Variation By Jasem Bader Theyab M.A., University of Kansas, 2010 Copyright 2013 Submitted to the graduate degree program in Anthropology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Doctor of Philosophy. ________________________________ Chairperson, Dr. Michael H. Crawford ________________________________ Dr. Majid Hannoum ________________________________ Dr. Deborah Smith ________________________________ Dr. Bartholomew C. Dean ________________________________ Dr. John Kelly Date Defended: May 28, 2013 The Dissertation Committee for Jasem Bader Theyab certifies that this is the approved version of the following dissertation: The Genetic Structure of the Kuwaiti and Failaka Island Populations: Y-chromosome & Mitochondrial DNA Variation ________________________________ Chairperson, Dr. Michael H. Crawford Date approved: May 31, 2013 ii Abstract Recent studies applying multidisciplinary approaches suggest that the Anatomically Modern Homo sapiens (AMHS) passed through the Arabian Peninsula in their major diaspora out of Africa. The Arabian Peninsula is connected to three continents: Africa, Asia, and Europe. In addition to the major diaspora, the Arabian Peninsula has witnessed numerous migrations among the three continents. The populations of the Arabian Peninsula have been investigated to better understand their evolutionary history. This dissertation investigated the paternal genetic structure of the Kuwaiti and Failaka Island populations using 15 loci Y-STR data. In addition, the maternal genetic structure of Failaka Island has been investigated using mtDNA HVS-I sequence data. This is the first genetic study to characterize Failaka Island population. The result showed that the Kuwaiti population has a high frequency of Y- haplogroup J1 (37%) similar to other Arabian populations. -
IBF List of Designated Risk Areas October 2020
IBF LIST of designated risk areas, with applicable benefits (as of 1st November 2020): 1) IBF Warlike Operations Area – 12 nm. off the mainland Yemeni Coast, excluding Maritime Security Transit Corridor (MSTC) in the Red Sea - Charts 1 and 2a bonus equal to basic wage, payable for 5 days minimum + per day if longer; doubled compensations for death and disability; right to refuse sailing, with repatriation at company’s cost and compensation equal to 2 month’s basic wage 1a) IBF Warlike Operations Area – all ports in Yemen – Chart 2a bonus equal to basic wage, payable for 5 days minimum + per day if longer; doubled compensations for death and disability; right to refuse sailing, with repatriation at company’s cost and compensation equal to 2 month’s basic wage 2) “IBF High Risk Area” – Gulf of Aden + 12 nm. off Somali East Coast (Shown in red shade on Chart 2 below, excluding the Internationally Recognized Transit Corridor (IRTC) as detailed in Chart 2a) bonus equal to basic wage, payable for the actual duration of stay / transit; doubled compensations for death and disability; right to refuse sailing, with repatriation at company’s cost increased BMP level 3) “IBF Extended Risk Zone” – West Indian Ocean and the Red Sea, up to the Yemen/Saudi Arabia border at 16⁰ 22’N (shown on chart 2a and 2b) and including the MSTC (shown on charts 1 and 3) but excluding the Warlike Operations Areas and the High Risk Area designated in 1, and 2a above. bonus equal to basic wage, payable only on the day the vessel is attacked; doubled compensations -
Structure and Transport of the East African Coastal Current
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/248793481 Structure and transport of the East African Coastal Current Article in Journal of Geophysical Research Atmospheres · January 1991 DOI: 10.1029/91JC01942 CITATIONS READS 48 209 3 authors, including: Michele Fieux Pierre and Marie Curie University - Paris 6 56 PUBLICATIONS 1,894 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: It is in a book: " L'océan à découvert " , 321 p. , sept 2017, CNRS Editions View project All content following this page was uploaded by Michele Fieux on 09 June 2018. The user has requested enhancement of the downloaded file. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 96, NO. C12, PAGES 22,245-22,257, DECEMBER 15, 1991 Structure and Transport of the East African Coastal Current JOHN C. SWALLOW Drakewalls, Gunnislake, Cornwall, England FRIEDRICH SCHOTT lnstitut fiir Meereskunde an der Universitiit Kiel, Kiel, Germany MICH•,LE FIEUX Laboratoire d'Oc•anographie Dynamique et de Climatologie, Universit• Paris VI, Paris The East African Coastal Current (EACC) runs northward throughout the year between latitudes 11øSand 3øS, with surfacespeeds exceeding 1 m s-1 in northernsummer. Mean transport from five sectionsnear 4ø-5øS is 19.9Sv (1 Sv -- 106 m3 s-1) northwardin theupper 500 dbar, out to 120km offshore. Below that, between 500 and 1000 dbar, there appears to be a weak variable transport of the order of 1 Sv. Comparing transports in the EACC with those in the boundary current north of Madagascar, it seems that most of the water in the upper 300 dbar of the northern branch of the South Equatorial Current goes into the EACC. -
Djibouti: Z Z Z Z Summary Points Z Z Z Z Renewal Ofdomesticpoliticallegitimacy
briefing paper page 1 Djibouti: Changing Influence in the Horn’s Strategic Hub David Styan Africa Programme | April 2013 | AFP BP 2013/01 Summary points zz Change in Djibouti’s economic and strategic options has been driven by four factors: the Ethiopian–Eritrean war of 1998–2000, the impact of Ethiopia’s economic transformation and growth upon trade; shifts in US strategy since 9/11, and the upsurge in piracy along the Gulf of Aden and Somali coasts. zz With the expansion of the US AFRICOM base, the reconfiguration of France’s military presence and the establishment of Japanese and other military facilities, Djibouti has become an international maritime and military laboratory where new forms of cooperation are being developed. zz Djibouti has accelerated plans for regional economic integration. Building on close ties with Ethiopia, existing port upgrades and electricity grid integration will be enhanced by the development of the northern port of Tadjourah. zz These strategic and economic shifts have yet to be matched by internal political reforms, and growth needs to be linked to strategies for job creation and a renewal of domestic political legitimacy. www.chathamhouse.org Djibouti: Changing Influence in the Horn’s Strategic Hub page 2 Djibouti 0 25 50 km 0 10 20 30 mi Red Sea National capital District capital Ras Doumeira Town, village B Airport, airstrip a b Wadis ERITREA a l- M International boundary a n d District boundary a b Main road Railway Moussa Ali ETHIOPIA OBOCK N11 N11 To Elidar Balho Obock N14 TADJOURA N11 N14 Gulf of Aden Tadjoura N9 Galafi Lac Assal Golfe de Tadjoura N1 N9 N9 Doraleh DJIBOUTI N1 Ghoubbet Arta N9 El Kharab DJIBOUTI N9 N1 DIKHIL N5 N1 N1 ALI SABIEH N5 N5 Abhe Bad N1 (Lac Abhe) Ali Sabieh DJIBOUTI Dikhil N5 To Dire Dawa SOMALIA/ ETHIOPIA SOMALILAND Source: United Nations Department of Field Support, Cartographic Section, Djibouti Map No. -
Arabian Peninsula from Wikipedia, the Free Encyclopedia Jump to Navigationjump to Search "Arabia" and "Arabian" Redirect Here
Arabian Peninsula From Wikipedia, the free encyclopedia Jump to navigationJump to search "Arabia" and "Arabian" redirect here. For other uses, see Arabia (disambiguation) and Arabian (disambiguation). Arabian Peninsula Area 3.2 million km2 (1.25 million mi²) Population 77,983,936 Demonym Arabian Countries Saudi Arabia Yemen Oman United Arab Emirates Kuwait Qatar Bahrain -shibhu l-jazīrati l ِش ْبهُ ا ْل َج ِزي َرةِ ا ْلعَ َربِيَّة :The Arabian Peninsula, or simply Arabia[1] (/əˈreɪbiə/; Arabic jazīratu l-ʿarab, 'Island of the Arabs'),[2] is َج ِزي َرةُ ا ْلعَ َرب ʿarabiyyah, 'Arabian peninsula' or a peninsula of Western Asia situated northeast of Africa on the Arabian plate. From a geographical perspective, it is considered a subcontinent of Asia.[3] It is the largest peninsula in the world, at 3,237,500 km2 (1,250,000 sq mi).[4][5][6][7][8] The peninsula consists of the countries Yemen, Oman, Qatar, Bahrain, Kuwait, Saudi Arabia and the United Arab Emirates.[9] The peninsula formed as a result of the rifting of the Red Sea between 56 and 23 million years ago, and is bordered by the Red Sea to the west and southwest, the Persian Gulf to the northeast, the Levant to the north and the Indian Ocean to the southeast. The peninsula plays a critical geopolitical role in the Arab world due to its vast reserves of oil and natural gas. The most populous cities on the Arabian Peninsula are Riyadh, Dubai, Jeddah, Abu Dhabi, Doha, Kuwait City, Sanaʽa, and Mecca. Before the modern era, it was divided into four distinct regions: Red Sea Coast (Tihamah), Central Plateau (Al-Yamama), Indian Ocean Coast (Hadhramaut) and Persian Gulf Coast (Al-Bahrain).