Kamil Crater
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Kamil Crater
The Kamil Crater is a wide and deep (original depth, a part covered by sand at present) meteorite impact crater in the East Uweinat Desert in southwestern New Valley Governorate, Egypt, Only north of the border with the Sudan and above sea level. It was located in 2008 using Google Earth satellite imagery by Vincenzo de Michele (former curator of the Museo Civico di Storia Naturale di Milan in Milan, Italy). Studies The first geophysical study of the Kamil Crater was conducted during an Italian-Egyptian expedition undertaken in February 2010 as part of the 2009 Egyptian-Italian Science Year (EISY) and proved the meteoritic origin of the crater. It is estimated to be less than 5,000 years old and shows a well-preserved rayed structure. The crater was produced by an iron meteorite that has been given an official name after the closest topographic feature in the area, Gebel Kamil, and which fragmented into thousands of pieces upon impact with the sandstone bedrock. The ...
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Egypt
Egypt ( ar, مصر , ), officially the Arab Republic of Egypt, is a transcontinental country spanning the northeast corner of Africa and southwest corner of Asia via a land bridge formed by the Sinai Peninsula. It is bordered by the Mediterranean Sea to the north, the Gaza Strip of Palestine and Israel to the northeast, the Red Sea to the east, Sudan to the south, and Libya to the west. The Gulf of Aqaba in the northeast separates Egypt from Jordan and Saudi Arabia. Cairo is the capital and largest city of Egypt, while Alexandria, the second-largest city, is an important industrial and tourist hub at the Mediterranean coast. At approximately 100 million inhabitants, Egypt is the 14th-most populated country in the world. Egypt has one of the longest histories of any country, tracing its heritage along the Nile Delta back to the 6th–4th millennia BCE. Considered a cradle of civilisation, Ancient Egypt saw some of the earliest developments of writing, agriculture, ur ...
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Geophysics
Geophysics () is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term ''geophysics'' sometimes refers only to solid earth applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations and pure scientists use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial physics; and analogous problems associated with the Moon and other planets. Gutenberg, B., 1929, Lehrbuch der Geophysik. Leipzig. Berlin (Gebruder Borntraeger). Runcorn, S.K, (editor-in-chief), 1967, International ...
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Gebel Kamil (Meteorite)
Gebel may refer to: Places * Gebel Edmonstone, a flat-topped mesa * Gebel Elba, a peak in Egypt * Gebel el-Haridi, an archaeological site in Egypt * Gebel el-Silsila, an archaeological quarry site in Egypt * Gebel Ramlah, an archaeological site in Egypt * Ġebel San Pietru, a hill in Malta * Gebel Tingar, small mountain in Egypt * Gebel-al-Tarik (Mountain of Tarik), the Arabic name for Gibraltar * Tuna el-Gebel, the necropolis of Khmun Other * Gebel (surname), Turkish and German surname * Gebel el-Arak Knife, an ivory and flint knife * Gebel Kamil (meteorite) * Gebel, a fictional character in '' Bloodstained: Ritual of the Night'' and its companion game ''Bloodstained: Curse of the Moon'' See also * Jabal (other) Jabal, Jabel, Jebel or Jibal may refer to: People * Jabal (name), a male Arabic given name * Jabal (Bible), mentioned in the Hebrew Bible Places In Arabic, ''jabal'' or ''jebel'' (spelling variants of the same word) means 'mountain'. * Dzhebel, ...
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University Of Pisa
The University of Pisa ( it, Università di Pisa, UniPi), officially founded in 1343, is one of the oldest universities in Europe. History The Origins The University of Pisa was officially founded in 1343, although various scholars place its origins in the 11th century. It is certain, however, that from the middle of the 12th century Pisa had a “Universitas” in the original sense of the word, that is, a group of students who gathered around masters. It was during this period that Leonardo Fibonacci was born and worked. He was one of the greatest mathematicians in history who, through his work, synthesized the spirit and processes of Greek geometry and the tools of Arabic mathematics for the first time in Europe. The papal seal “In Supremae dignitatis”, issued by Pope Clement VI on 3 September 1343, granted the Studium in Pisa the title of Studium Generale with various exclusive privileges, making it universally recognised. In medieval times, the Studium Generale wa ...
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University Of Siena
The University of Siena ( it, Università degli Studi di Siena, abbreviation: UNISI) in Siena, Tuscany, is one of the oldest and first publicly funded universities in Italy. Originally called ''Studium Senese'', the institution was founded in 1240. It had around 20,000 students in 2006, nearly half of Siena's total population of around 54,000. In the academic year 2022–2023, it had a total undergraduate enrollment of 17,00 and graduate enrollment of 2,989. Today, the University of Siena is best known for its Schools of Law, Medicine, and Economics and Management. History The early ''studium'' The School of Humanities and Philosophy On December 26, 1240, Ildebrandino Cacciaconti, the then podestà of Siena, signed a decree imposing a tax on citizens of Siena who rented rooms to students of the local "''Studium Senese''". The money from this tax went to pay for the salaries of the ''maestri'' (teachers) of this new studium. The studium was further supported when, in 1252, ...
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Cairo
Cairo ( ; ar, القاهرة, al-Qāhirah, ) is the capital of Egypt and its largest city, home to 10 million people. It is also part of the largest urban agglomeration in Africa, the Arab world and the Middle East: The Greater Cairo metropolitan area, with a population of 21.9 million, is the 12th-largest in the world by population. Cairo is associated with ancient Egypt, as the Giza pyramid complex and the ancient cities of Memphis and Heliopolis are located in its geographical area. Located near the Nile Delta, the city first developed as Fustat, a settlement founded after the Muslim conquest of Egypt in 640 next to an existing ancient Roman fortress, Babylon. Under the Fatimid dynasty a new city, ''al-Qāhirah'', was founded nearby in 969. It later superseded Fustat as the main urban centre during the Ayyubid and Mamluk periods (12th–16th centuries). Cairo has long been a centre of the region's political and cultural life, and is titled "the city of a thousand m ...
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Egyptian Geological Museum
The Egyptian Geological Museum is a museum in Cairo, Egypt. The museum was established in 1901 as part of the Egyptian Geological Survey, which had been started in 1896 under the direction of the Khedive Ismail. The museum was the first of its kind in the Middle East and the African continent.Kamil, Jill"History in geological time", ''Al-Ahram Weekly'', October 7, 2004. Accessed October 3, 2008. Museum history The museum was initially housed in a Greco-Roman style building that was located in the gardens of the Ministry of Public Works in downtown Cairo; it was designed by Marcel Dourgnon, the French architect who had previously designed and constructed the Egyptian Museum (also known as the Museum of Egyptian Antiquities). This building had an exhibition hall with ceilings high in order to accommodate the reconstructed fossil skeletons of paleontological finds, which included a high ancestral elephant. The first Museum Keeper was William Andrews, a paleontologist from London's N ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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Meteoritical Society
The Meteoritical Society is a non-profit scholarly organization founded in 1933 to promote research and education in planetary science with emphasis on studies of meteorites and other extraterrestrial materials that further our understanding of the origin and history of the Solar System. Members The membership of the society comprises over 1,000 scientists and amateur enthusiasts from over 52 countries who are interested in a wide range of planetary science topics. Members interests include meteorites, cosmic dust, asteroids and comets, natural satellites, planets, impact events, and the origins of the Solar System. Activities The Meteoritical Society is the organization that records all known meteorites in its '' Meteoritical Bulletin''. The Society also publishes one of the world's leading planetary science journals, ''Meteoritics & Planetary Science'', and is a cosponsor with the Geochemical Society of the renowned journal ''Geochimica et Cosmochimica Acta''. The Society presen ...
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Gebel Kamil (meteorite)
Gebel Kamil is a meteorite that struck Egypt later than 3000 BC, leaving a crater surrounded by thousands of pieces of iron shrapnel with a total weight of about . History In February 2009 and 2010, meteorite fragments with masses ranging from < to , plus an specimen, were found in and around a radius from by an Italian-Egyptian geophysical team. About was recovered. The geophysical survey took place as part of the "2009 Italian-Egyptian Year of Science and Technology".


Mineralogy

'''' The Gebel Kamil meteorite contains the minerals



Iron Meteorite
Iron meteorites, also known as siderites, or ferrous meteorites, are a type of meteorite that consist overwhelmingly of an iron–nickel alloy known as meteoric iron that usually consists of two mineral phases: kamacite and taenite. Most iron meteorites originate from cores of planetesimals, with the exception of the IIE iron meteorite group The iron found in iron meteorites was one of the earliest sources of usable iron available to humans, due to the malleability and ductility of the meteoric iron, before the development of smelting that signaled the beginning of the Iron Age. Occurrence Although they are fairly rare compared to the stony meteorites, comprising only about 5.7% of witnessed falls, iron meteorites have historically been heavily over-represented in meteorite collections. This is due to several factors: * They are easily recognized as unusual even by laymen, as opposed to stony meteorites. Modern-day searches for meteorites in deserts and Antarctica yield a muc ...
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Ray System
A ray system comprises radial streaks of fine '' ejecta'' thrown out during the formation of an impact crater, looking somewhat like many thin spokes coming from the hub of a wheel. The rays may extend for lengths up to several times the diameter of their originating crater, and are often accompanied by small secondary craters formed by larger chunks of ejecta. Ray systems have been identified on the Moon, Earth ( Kamil Crater), Mercury, and some moons of the outer planets. Originally it was thought that they existed only on planets or moons lacking an atmosphere, but more recently they have been identified on Mars in infrared images taken from orbit by '' 2001 Mars Odyssey''s thermal imager. Rays appear at visible, and in some cases infrared wavelengths, when ejecta are made of material with different reflectivity (i.e., albedo) or thermal properties from the surface on which they are deposited. Typically, visible rays have a higher albedo than the surrounding surface. More rarel ...
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