Moon Phases 2019 – Lunar Calendar for Nouakchott, Mauritania
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Recent discoveries of offshore gas reserves by Kosmos have increased production forecasts. Mauritania and Senegal, with BP and Kosmos Energy, announced in December that they reached a final investment decision for the Grand Tortue project. In addition to a national EITI, focal points were designated in each municipal council in to support greater outreach, dissemination as well as collection of information. The three main taxes and fees imposed on companies operating in the mining sector include unique annual royalties, dividends from state participation and contributions to the state budget, a new fee introduced in
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The geology of Mauritania is built on more than two billion year old Archean crystalline basement rock in the Reguibat Shield of the West African Craton , a section of ancient and stable continental crust. Mobile belts and the large Taoudeni Basin formed and filled with sediments in the connection with the Pan-African orogeny mountain building event million years ago and a subsequent orogeny created the Mauritanide Belt.
In the last million years, Mauritania has accumulated additional sedimentary rocks during periods of marine transgression and sea level retreat. The extremely old crystalline basement rock of the shield is almost entirely Neoarchean age and metamorphosed to hornblende or granulite grade in the metamorphic facies sequence. These Saouda Series rocks include gneiss , with different endmembers enriched in leptynite garnet , hypersthene and sillimanite garnet, as well as pyroxene amphibolite , magnetite quartzites and marble.
The Saouda Series is intruded by younger basalts , anorthosite and gabbros along with serpentinite. Saouda Series rocks appear to be restite , the residual material left at a location after in situ granite production through intense metamorphism and are part of a larger group of anatectic and magmatic granites in the Rag el Abiod complex. In Mauritania, metamorphic and igneous crystalline basement rock is exposed as the Kenieba and Kayes inliers, sections of older rock surrounded by younger rock.
They show signs of multiple phases of deformation and intrusion by tectonic and post-tectonic granites, dated at 2. Geologists have found pebbles within microsyenites and microgranites , in a folded conglomerate , that form part of a metasedimentary unit, which may be the remnants of even older Archean rocks. In the Neoproterozoic , the Pan-African orogeny began to form mobile belts across Africa. Also known as the Bove Basin further south, the Taoudeni Basin is a slightly dipping sag basin filled with two to three kilometers of clastic sedimentary rocks.
The rocks are grouped into three sequences. Sequence 1 deposited in the Middle Neoproterozoic and includes sandstones and carbonates formed from stromatolites. Supergroup 2 also dates to the Neoproterozoic and contains dolomite rich in barite , basal tillite , marine chert and sandstones. The deposition of Supergroup 2 continued with the formation of sandstones containing brachiopod fossils, in the Cambrian and Ordovician , followed by Late Ordovician tillites, graptolite Silurian sandstones and shales, as well as Devonian shales with reef limestones.
The Mauritanide Belt formed in an orogeny between to million years ago that is allochthonous , lying on top of the Reguibat Shield crystalline basement rocks and the sedimentary rocks of the Taoudeni Basin. The Mauritanide Belt was thrust on top of the Taoudeni Basin during the Hercynian orogeny , which also folded and fractured the edge of the basin. It is one of several West African fold belts along with the Bassarides and Rokelides.
Mauritania is part of the Senegal Basin and its Mesozoic sedimentary sequence begins with Late Jurassic dolomite formed in a shallow marine environment. Offshore research has found Early Cretaceous detrital sediments lying atop Early Jurassic evaporites. The ocean receded in the region in the Maastrichtian near the end of the Cretaceous, followed by a large marine transgression in the early Cenozoic. The country’s sedimentary rocks interfinger between continental sediments and silicate marine sediments in the west.
Mauritania has two interconnected groundwater systems, the Continental Terminal coastal system and the interior Taoudeni Basin. Most groundwater flow happens in porous sedimentary rock, although some moves through fractured crystalline basement rock. The Continental Terminal system have very limited recharge, while the Taoudeni Basin has three main areas of recharge on the northwest edge of the shield, in tillites in the south and in the vicinity of Tidjikdja.
Fresh groundwater discharges east into Mali and saltwater intrusions affect the coastal areas of Mauritania. Iron ore mining plays an important role in the economy of Mauritania. Mining began 25 kilometers north of Zouerate, as part of the Guelb project in the mids. Dust storms and problems at the site’s mill have limited production.
A Neoproterozoic carbonate unit, part of a synformal nappe overturned in the Paleozoic, now forms a major copper deposit kilometers northeast of Nouakchott in the Mauritanides Belt. The one kilometer, meter wide deposit spans the West and East Moghrein Guelb hills. Forty meters below the deposit is a secondary deposit of cuprite , azurite , malachite and tenorite , with an additional 2. In the s, mining at the site had mostly ceased except for gold mining in the tailings pile.
Gypsum is extracted from the N’Drahamcha quarry, 50 kilometers northeast of Nouakchott, used to produce concrete blocks and plaster. From Wikipedia, the free encyclopedia. Geology portal Mauritania portal. Geological Atlas of Africa. Geology of Africa. Sahrawi Arab Democratic Republic Somaliland. Retrieved from ” https: Geology of Mauritania Geology by country. Hidden categories: Commons category link from Wikidata Commons category link is on Wikidata using P Portal templates with redlinked portals.
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Located in the Sahelian and Saharan zones, Mauritania has one of the poorest agricultural bases in West Africa. Most important to the rural economy has been the livestock subsector. Between and , herding engaged up to 70 percent of the population, and sedentary farmers constituted about 20 percent of the population. The vast majority of the population lived in the southern one-third of the country, where rainfall levels were high enough to sustain cattle herding.
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Convention concerning the State frontier line established between the Islamic Republic of Mauritania and the Kingdom of Morocco, 14 April entry into force: Mail to: The Division for Ocean Affairs and the Law of the Sea of the Office of Legal Affairs of the United Nations makes every effort to provide the most up-to-date information available to it at this website.
Stops Reset. Departure from Bengaluru Reset. Arrival at Nouakchott Reset. Doha DOH 03 hrs 15 mins Layover. Nouakchott 28 May Flight Details. Dubai DXB 19 hrs 10 mins Layover. Conakry CKY 01 hr 30 mins Layover. Dakar DSS 01 hr 55 mins Layover. Dubai DXB 18 hrs 40 mins Layover.
Dating in Zreïf el Azra
Nestled on the edge of the Atlantic Ocean, along a beautiful coast kilometres long, Mauritania is lined to the south-west by the Senegal River. Characterised by warm temperatures and a record level of sunshine throughout the year, Mauritania offers a mild climate during a large part of the year from November to July. The ocean with its endless sandy beaches, embraces wonderful bays and lagoons. It is in this background between ocean, sand and sunshine that you can discover one of the most fascinating marvels: With a history that stretches over a millennium, a few cities in the middles of the desert and a famous archaeological sites lies nowadays a priceless treasures for visitors. Founded between the 9th and 13th centuries, the cities of Ouadane , Chinguetti , Tichitt and Oualata were mainly developed through the Saharan trade roads and strengthened later with the Muslim conquest, abandoned by the caravan and invaded by the sand, they have been deserted by some of their inhabitants fleeing drought.
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Moon Phases 2019 – Lunar Calendar for Nouakchott, Mauritania
The geology of Mauritania is built on more than two billion year old Archean crystalline basement rock in the Reguibat Shield of the West African Craton , a section of ancient and stable continental crust. Mobile belts and the large Taoudeni Basin formed and filled with sediments in the connection with the Pan-African orogeny mountain building event million years ago and a subsequent orogeny created the Mauritanide Belt. In the last million years, Mauritania has accumulated additional sedimentary rocks during periods of marine transgression and sea level retreat. The extremely old crystalline basement rock of the shield is almost entirely Neoarchean age and metamorphosed to hornblende or granulite grade in the metamorphic facies sequence. These Saouda Series rocks include gneiss , with different endmembers enriched in leptynite garnet , hypersthene and sillimanite garnet, as well as pyroxene amphibolite , magnetite quartzites and marble.
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Sign Up for our Newsletters. Mauritania is rich in rock art sites, particularly in the south eastern parts such as Guilemsi which occurs on a sandstone ridge in the Tagant District. Paintings are found in the walled shelters and on stonewall banks of a dry river. Images include camels, horsemen, cattle, wild animals and a few geometric designs belonging to the fourth and third millennia. More recent images include human figures in red riding horses or cattle with some holding weapons.