Navigation Through Three Straits in the Middle East
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This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Quaternary Science Reviews 29 (2010) 3843e3860 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev North Atlantic influence on 19the20th century rainfall in the Dead Sea watershed, teleconnections with the Sahel, and implication for Holocene climate fluctuations Yochanan Kushnir a,*, Mordechai Stein a,b a Lamont-Doherty Earth Observatory, The Earth Institute, Columbia University, 61 Route 9W, Palisades, NY 10964, USA b Geological Survey of Israel, 30 Malkhe Israel Street, 95501 Jerusalem, Israel article info abstract Article history: The importance of understanding processes that govern the hydroclimate of the Mediterranean Basin is Received 14 February 2010 highlighted by the projected significant drying of the region in response to the increase in greenhouse Received in revised form gas concentrations. Here we study the long-term hydroclimatic variability of the central Levant region, 3 August 2010 situated in the eastern boundary of the Basin, as reveled by instrumental observations and the Holocene Accepted 9 September 2010 record of Dead Sea level variations. -
West Africa Part III: Central Africa Part IV: East Africa & Southern Africa Name: Date
Part I: North Africa Part II: West Africa Part III: Central Africa Part IV: East Africa & Southern Africa Name: Date: AFRI CA Overview RICA lies at the heart of the earth's land Then, during the nineteenth century, masses. It sits astride the equator, with European traders began setting up trading sta . almost half the continent to the north tions along the coast of West Africa. The of the equator, and half to the south. It con traders, and their governments, soon saw great tains some of the world's greatest deserts, as opportunity for profit in Africa. Eventually, well as some of the world's greatest rivers. It many European countries took control of the has snow-capped mountains, and parched, arid land and divided it into colonies. plains. The first humans came from Africa. By the middle of the twentieth century, peo And in the millennia since those fust humans ple all across Africa had demanded indepen walked the plains of Africa, many different cul dence from colonial rule. By the end of the tures have arisen there. century, government had passed firmly into Physically, Africa is one enormous plateau. It African hands. However, the newly independ has no continental-scale mountain chains, no ent nations must still deal with the legacy of peninsulas, no deep fjords. Most of the conti colonialism. The boundaries the European nent is more than 1000 feet (300m) above sea powers created often cut across ethnic and cul level; over half is above 2500 feet (800 m). tural groups. Many African nations today are Africa's early history reflects the wide stretch still struggling to reconcile the different cul of the continent. -
Transit Passage in the Russian Arctic Straits
International Boundaries Research Unit MARITIME BRIEFING Volume 1 Number 7 Transit Passage in the Russian Arctic Straits William V. Dunlap Maritime Briefing Volume 1 Number 7 ISBN 1-897643-21-7 1996 Transit Passage in the Russian Arctic Straits by William V. Dunlap Edited by Peter Hocknell 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 Preface The Russian Federation, continuing an initiative begun by the Soviet Union, is attempting to open the Northern Sea Route, the shipping route along the Arctic coast of Siberia from the Norwegian frontier through the Bering Strait, to international commerce. The goal of the effort is eventually to operate the route on a year-round basis, offering it to commercial shippers as an alternative, substantially shorter route from northern Europe to the Pacific Ocean in the hope of raising hard currency in exchange for pilotage, icebreaking, refuelling, and other services. Meanwhile, the international law of the sea has been developing at a rapid pace, creating, among other things, a right of transit passage that allows, subject to specified conditions, the relatively unrestricted passage of all foreign vessels - commercial and military - through straits used for international navigation. In addition, transit passage permits submerged transit by submarines and overflight by aircraft, practices with implications for the national security of states bordering straits. This study summarises the law of the sea as it relates to straits used for international navigation, and then describes 43 significant straits of the Northeast Arctic Passage, identifying the characteristics of each that are relevant to a determination of whether the strait will be subject to the transit-passage regime. -
Geog 120: World Geography American University of Phnom Penh
Geog 120: World Geography American University of Phnom Penh Map Quizzes: List of physical features 1. Africa Atlas Drakensberg Seas and Oceans Deserts Mediterranean Atlantic Kalahari Strait of Gibraltar Namib Suez Canal Sahara Mozambique Channel Ogaden Red Sea Libyan Gulf of Suez 2. Asia Lakes Lake Chad Seas and Oceans Lake Malawi (Nyasa) Lake Tanganyika Andaman Sea Lake Victoria Arabian Sea Lake Albert Aral Sea Lake Rudolph Arctic Ocean Atlantic Ocean Rivers Black Sea Caspian Sea Congo East China Sea Limpopo Indian Ocean Niger Inland Sea (also know as Setonaikai, Zambezi Japan) Nile Mediterranean Sea Orange Pacific Ocean Vaal Red Sea Sea of Japan Mountains Sea of Okhotsk 2 South China Sea Mountain Ranges Yellow Sea Caucuses Elburz Straits, Channels, Bays and Gulfs Himalayas Hindu Kush Bay of Bengal Ural Bosporus Zagros Dardanelles Gulf of Aden Gulf of Suez Deserts Gulf of Thailand Arabian Gulf of Tonkin Dasht-E-Kavir Persian Gulf Gobi Strait of Taiwan Negev Strait of Malacca Takla Makan Strait of Hormuz Strait of Sunda Suez Canal 3. The Americas Lakes Seas and Oceans Baykal Bering Tonle Sap Caribbean Sea Atlantic Ocean Pacific Ocean Rivers Straits, Channels, Bays and Gulfs Amur Brahmaputra Gulf of Mexico Chang Jiang Hudson Bay Euphrates Panama Canal Ganges Strait of Magellan Huang He (Yellow) Indus Lakes Irrawaddy Mekong Great Salt Tigris Great Lakes (Lakes Tonle Sap (River and Lake) Superior, Michigan, Huron, 3 Erie, and Ontario) 4. Australia and the Pacific Manitoba Titicaca Winnipeg Seas and Oceans Coral Sea Rivers Tasman Sea Pacific Ocean Amazon Indian Ocean Colorado Columbia Hudson Straits, Channels, Bays and Gulfs Mississippi Bass Strait Missouri Cook Strait Ohio Gulf of Carpentaria Orinoco Torres Strait Paraguay Plata Parana Rivers Rio Grande Darling St. -
Intefwaitional EXPLORATIWWTS O Meetlnq-NO~~R Sketch
INTEfWAiTIONAL EXPLORATIWWTS Om sparsrs to have been sutured onto the Brazilian Shield near MEETlNQ-NO~~R14,laMJ the end of the Paleozoic. There is considerable controverav concerning is origin and original Iffietion, as well as the THOMAS E. O'CONNOR-Biographical Sketch nature of the suturina of the two maasifa. ~h~~..F nTnnnnr ie Asaocisted withthe Brazilian Shield ars two marine Vice President of Aminoil Paleozoic basins in the northern portion of the country. The Internationel, Incorporated. Tarija Basin is largely represented in BollrEa where it is the developing international ex- cemer of considerable exploration for and prdwtion of ptoration opportunltiea. Tom natural gas. Farther east is the large, imacmtonlc Cham- overviews three production Parena Basin which extends wuthweatdy from Paraguay areas (Indonesia, North Sea and Brazil. To date it has proved to be WenBf hydrocarbons. and Argentine) and directdl Along the western and southern margins of thesnlarged the exploration activity in lulesozoic continental mass of Argentina ie a saries of marina nine exploration contract basins which were present prior to We EoHloian and onset of areas. He received a B.S. subduction of the PeciPicplataduriw(hp Ladr hawob/Early degree ingedogyfromSfan- Tertiary. These western, leading kjnawere wiginally ford University in 1968 and simple in format end structural sQde untll zheowrpfimdf the an M.S. degree in geology Andean Orogeny and associated -rd-verging over- from the University of thrusts deformed their wastern margins. To varying degrees. Colorado in 1961. Since all of the marginal cretonic beaina have proved lo be hydro- 1983. he has been Adjunct Research Professor in the Earth carbon-bearing, inclwlingrecentdiawverieain the Megallanas/ Sciences and Resources Institute at the University of South Malvinas area. -
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. -
Policy Brief Clingendael Policy Brief
JUNE 2021 ‘A careful foot can step anywhere’ Policy Brief The UAE and China in the Horn of Africa: Implications for EU engagement Over the last decade, the UAE and China have vastly expanded their economic, political and military footprint in the Horn of Africa, and their actions now have the potential to shape developments in the region. Room for cooperation between Abu Dhabi and Beijing exists on issues such as maritime security, regional stability, and economic development. Moreover, the two countries’ interaction could lead to improvements in the Horn’s underdeveloped infrastructure by triggering a race to investment. Yet, development and stability in the region might suffer if the strategic interests of external players take precedence over local ones, or if local elites (mis)use external support for narrow domestic political calculations. The EU and its member states have high stakes in the Horn’s stability. To optimise their engagement, European policymakers should be aware of the implications of the Emirati and Chinese presence, and they should strive Jos Meester & Guido Lanfranchi MeesterJos & Guido to improve cooperation among the wide range of external players active in the Horn. Introduction Over the last decade, the Horn of Africa also significant from a security perspective, has become an increasingly contested as it allows swift naval transit across different geopolitical space.1 For observers of operational theatres (the Mediterranean, the the region, this trend may not come as Middle East, eastern Africa and the Indian a surprise. The Horn lays along one of Ocean) where several regional and global the world’s most important maritime powers are militarily engaged. -
Part Ii; Self Defense and the New Law of the Sea Regimes
PART II; SELF DEFENSE AND THE NEW LAW OF THE SEA REGIMES INTRODUCTION Admiral Bruce Harlow, USN Retired! Poulsbo, Washington It is a distinct pleasure for me to be here this afternoon to introduce a distinguished panel to you. I think the papers, commen- taries, aad discussion will be stimulating and will be of interest to all of you. I' ve had the pleasure of a personal association with the Law of the Sea Institute since its inception in Rhode Island in 1966. Believe me, that year is etched in my memory because as a somewhat idealistic lieutenant commander I presented a paper that damn near got me fired. Several weeks ago I reviewed the proceedings of that session for two reasons, One, I wanted to see the rate of survivorship of the charter members. I'm happy to report that membership does aot endanger your health, as evidenced by the large number of old fogies around here. The second reason to review the proceedings of that first meeting was to see if there was any relevance to the organization. I was frankly surprised when I looked at those proceedings to see how raaay of the thoughts and discussion points raised and reported in the pro- ceedings found their way into emerging customary law and indeed into provisions of the 1982 Convention. I think it is safe to say that over the years the Law of the Sea Institute has been one of the focal points for the discussion, albeit informal but authorititative, of important law of the sea issues. -
Oil Rights in the Gulf of Suez Richard A
Louisiana Law Review Volume 38 | Number 4 Summer 1978 Oil Rights in the Gulf of Suez Richard A. Curry Repository Citation Richard A. Curry, Oil Rights in the Gulf of Suez, 38 La. L. Rev. (1978) Available at: https://digitalcommons.law.lsu.edu/lalrev/vol38/iss4/4 This Comment is brought to you for free and open access by the Law Reviews and Journals at LSU Law Digital Commons. It has been accepted for inclusion in Louisiana Law Review by an authorized editor of LSU Law Digital Commons. For more information, please contact [email protected]. OIL RIGHTS IN THE GULF OF SUEZ International law recognizes that coastal nations have the right to exploit natural resources found in continental shelf areas beneath adja- cent water bodies. In most situations the coastal nation entitled to this right is easily identified as the sovereign in actual control of the land immediately adjacent to the water body. However, the nation in physi- cal control of such land may not be the sovereign thereof. In such a case, both the nation having actual control and the nation claiming sov- ereignty may assert the right to exploit natural resources in the adjacent continental shelf. Such a situation currently exists in the Gulf of Suez. When Israel invaded the Sinai in 1967 it acquired the possession but not the sovereignty of that territory. Now, both Egypt, as sovereign, and Israel, as occupant, claim the right to drill for oil in the adjacent conti- nental shelf. The Gulf of Suez is a semi-enclosed body of water which opens into the Red Sea at the south and narrows into the Suez Canal at the north. -
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. -
Page 1 of 7 Location the Nation of Libya Is Located in North Africa And
Libya Location The nation of Libya is located in North Africa and covers approximately one million seven hundred fifty square kilometers, which is slightly larger than the United State’s Alaska. It is one of the largest countries in Africa. Libya lies in the geographic coordinates 25°N and 17°E. It is bordered in the north by the Mediterranean Sea and by Niger and Chad in the south. Libya’s western border connects to Algeria and Tunisia, and connects to Egypt and Sudan in the east. Geography The highest point in Libya is the Bikku Bitti, also known as Bette Peak, which stands at seven thousand four hundred and thirty eight feet at its highest point. It is located in the Tibesti Mountains in southern Libya near the Chadian border. The Sahara, an immense North African desert, covers most of Libya. Much of the country’s land consists of barren, rock-strewn plains and sand sea, with flat to underlying plains, plateaus, and depressions. Two small areas of hills ascend in the northwest and northeast, and the Tibesti mountains rise near the southern border. There are no permanent rivers or streams in Libya. The coastline is sunken near the center by the Gulf of Sidra, where barren desert reaches the Mediterranean Sea. Libya is divided into three natural regions. The first and largest, to the east of the Gulf of Sidra, is Cyrenaica, which occupies the plateau of Jabal al Akhdar. The majority of the area of Cyrenaica is covered with sand dunes, especially along the border with Egypt. -
Africa Command: U.S
Order Code RL34003 Africa Command: U.S. Strategic Interests and the Role of the U.S. Military in Africa Updated July 6, 2007 Lauren Ploch Analyst in African Affairs Foreign Affairs, Defense, and Trade Division Africa Command: U.S. Strategic Interests and the Role of the U.S. Military in Africa Summary On February 6, 2007, the Bush Administration announced its intention to create a new unified combatant command, U.S. Africa Command or AFRICOM, to promote U.S. national security objectives in Africa and its surrounding waters. U.S. military involvement on the continent is currently divided among three commands: U.S. European Command (EUCOM), U.S. Central Command (CENTCOM), and U.S. Pacific Command (PACOM). As envisioned by the Administration, the command’s area of responsibility (AOR) would include all African countries except Egypt. In recent years, analysts and U.S. policymakers have noted Africa’s growing strategic importance to U.S. interests. Among those interests are Africa’s role in the Global War on Terror and the potential threats posed by ungoverned spaces; the growing importance of Africa’s natural resources, particularly energy resources; and ongoing concern for the continent’s many humanitarian crises, armed conflicts, and more general challenges, such as the devastating effect of HIV/AIDS. In 2006, Congress authorized a feasibility study on the creation of a new command for Africa. As defined by the Department of Defense (DOD), AFRICOM’s mission will be to promote U.S. strategic objectives by working with African states and regional organizations to help strengthen stability and security in the region through improved security capability, military professionalization, and accountable governance.