Abu Rawash
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Abu Rawash
Abu Rawash (also spelled ''Abu Roach'', Abu Roash; ar, ابو رواش  , , , "flesh of sensual pleasures"), north of Giza, is the site of Egypt's most northerly pyramid, also known as the lost pyramid – the mostly ruined Pyramid of Djedefre, the son and successor of Khufu. Originally, it was thought that this pyramid had never been completed, but the current archaeological consensus is that not only was it completed, but that it was built about the same size as the Pyramid of Menkaure – the third largest of the Giza pyramids. It is the location of the northernmost pyramid in Egypt (known as Lepsius Number One), the pyramid of Djedefre (also known as Radjedef) and around fifty mastabas (located one and a half kilometres from Djedefre’s pyramid). Location Its location adjacent to a major crossroads made it an easy source of stone. Quarrying, which began in Roman times, has left little apart from a few courses of stone superimposed upon the natural hillock ...
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Pyramid Of Djedefre 01
A pyramid (from el, πυραμίς ') is a structure whose outer surfaces are triangular and converge to a single step at the top, making the shape roughly a pyramid in the geometric sense. The base of a pyramid can be trilateral, quadrilateral, or of any polygon shape. As such, a pyramid has at least three outer triangular surfaces (at least four faces including the base). The square pyramid, with a square base and four triangular outer surfaces, is a common version. A pyramid's design, with the majority of the weight closer to the ground and with the pyramidion at the apex, means that less material higher up on the pyramid will be pushing down from above. This distribution of weight allowed early civilizations to create stable monumental structures. Civilizations in many parts of the world have built pyramids. The largest pyramid by volume is the Great Pyramid of Cholula, in the Mexican state of Puebla. For thousands of years, the largest structures on Earth were pyramids ...
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Rudist
Rudists are a group of extinct box-, tube- or ring-shaped marine heterodont bivalves belonging to the order Hippuritida that arose during the Late Jurassic and became so diverse during the Cretaceous that they were major reef-building organisms in the Tethys Ocean, until their complete extinction at the close of the Cretaceous. Shell description The Late Jurassic forms were elongate, with both valves being similarly shaped, often pipe or stake-shaped, while the reef-building forms of the Cretaceous had one valve that became a flat lid, with the other valve becoming an inverted spike-like cone. The size of these conical forms ranged widely from just a few centimeters to well over a meter in length. Their "classic" morphology consisted of a lower, roughly conical valve that was attached to the seafloor or to neighboring rudists, and a smaller upper valve that served as a kind of lid for the organism. The small upper valve could take a variety of interesting forms, including: a ...
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List Of Ancient Egyptian Sites
This is a list of ancient Egyptian sites, throughout all of Egypt and Nubia. Sites are listed by their classical name whenever possible, if not by their modern name, and lastly with their ancient name if no other is available. Nomes A nome is a subnational administrative division of Ancient Egypt. Lower Egypt * Nome 1: White Walls *Nome 2: Cow's thigh *Nome 3: West *Nome 4: Southern Shield *Nome 5: Northern Shield * Nome 6: Mountain bull *Nome 7: West harpoon *Nome 8: East harpoon *Nome 9: Andjety *Nome 10: Black bull *Nome 11: Heseb bull *Nome 12: Calf and Cow * Nome 13: Prospering Scepter *Nome 14: Eastmost *Nome 15: Fish *Nome 16: Djehuti *Nome 17: The Throne *Nome 18: Prince of the South *Nome 19: Prince of the North *Nome 20: Plumed Falcon Upper Egypt * Nome 1: Land of the bow * Nome 2: Throne of Horus * Nome 3: The Shrine *Nome 4: The sceptre * Nome 5: The two falcons * Nome 6: The crocodile *Nome 7: Sistrum * Nome 8: Great lands *Nome 9: Minu (Min) * Nome 10: Cob ...
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List Of Ancient Egyptian Towns And Cities
This is a list of known ancient Egyptian towns and cities.
http://www.ucl.ac.uk/. Retrieved on 2016-03-05. The list is for sites intended for permanent settlement and does not include fortresses and other locations of intermittent habitation. Use Ctrl + F and enter the town's name or alternative name for convenience.


Lower Egypt


Upper Egypt

}) , tȝ mȝy Sbk nb Pay pȝ nṯr ʿȝ , , - , Tepihu ( Aphroditopolis) , , , 22nd , (cult center during Greek period) , , Petpeh
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Den (pharaoh)
Den, also known as Hor-Den, Dewen and Udimu, is the Horus name of a pharaoh of the Early Dynastic Period who ruled during the First Dynasty of Egypt. He is the best archaeologically-attested ruler of this period. Den is said to have brought prosperity to his realm and numerous innovations are attributed to his reign. He was the first to use the title "King of Upper and Lower Egypt", and the first depicted as wearing the double crown (red and white). The floor of his tomb at Umm El Qa'ab near Abydos is made of red and black granite, the first time in Egypt this hard stone was used as a building material. During his long reign he established many of the customs of court ritual and royalty used by later rulers and he was held in high regard by his immediate successors. Length of reign The Ancient Egyptian historian Manetho called him “Oúsaphaîdos” and credited him with a reign of 20 years,William Gillan Waddell: ''Manetho (The Loeb Classical Library, Volume 350)''. Harvard U ...
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Hor-Aha
Hor-Aha (or Aha or Horus Aha) is considered the second pharaoh of the First Dynasty of Egypt by some Egyptologists, while others consider him the first one and corresponding to Menes. He lived around the 31st century BC and is thought to have had a long reign. Identity Name The commonly used name ''Hor-Aha'' is a rendering of the pharaoh's Horus-name, an element of the royal titulary associated with the god Horus, and is more fully given as ''Horus-Aha'' meaning ''Horus the Fighter''. Manetho's record ''Aegyptiaca'' (translating to History of Egypt) lists his Greek name as Athothis, or "Athotís". For the Early Dynastic Period, the archaeological record refers to the pharaohs by their Horus-names, while the historical record, as evidenced in the Turin and Abydos king lists, uses an alternative royal titulary, the ''nebty''-name. The different titular elements of a pharaoh's name were often used in isolation, for brevity's sake, although the choice varied according to c ...
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First Dynasty Of Egypt
The First Dynasty of ancient Egypt (Dynasty I) covers the first series of Egyptian kings to rule over a unified Egypt. It immediately follows the unification of Upper and Lower Egypt, possibly by Narmer, and marks the beginning of the Early Dynastic Period, a time at which power was centered at Thinis. The date of this period is subject to scholarly debate about the Egyptian chronology. It falls within the early Bronze Age and is variously estimated to have begun anywhere between the 34th and the 30th centuriesBC. In a 2013 study based on radiocarbon dates, the beginning of the First Dynasty—the accession of Narmer (commonly known as Menes)—was placed at 3100BC give or take a century (3218–3035, with 95% confidence). The dynasty Information about this dynasty is derived from a few monuments and other objects bearing royal names, the most important being the Narmer Palette and Narmer Macehead, as well as Den and Qa'a king lists. No detailed records of the first two dynas ...
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Beni Suef
Beni Suef ( ar, بني سويف, Baniswēf the capital city of the Beni Suef Governorate in Egypt. Beni Suef is the location of Beni Suef University. An important agricultural trade centre on the west bank of the Nile River, the city is located 110 km (70 miles) south of Cairo. Etymology The modern name of the town is a corruption of its original name ''Manfiswayh'' (), which itself comes from a Coptic toponymic construction ⲡ-ⲙⲁ-ⲛ-... ("the place of..."); however, its exact etymology is unknown. History From the early Pharaonic era to the Roman period, the area was home to the city of Heracleopolis, 10 miles west of the modern city. which also served as the capital of Lower and Middle Egypt during the 9th and 10th dynasties. The modern city rose to prominence during the Middle Ages, when it was renowned for its linen manufacturing, which continues to the present day through the city's carpet making and cotton spinning industries. Beni Suef became the chief town of ...
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Shoals
In oceanography, geomorphology, and geoscience, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material and rises from the bed of a body of water to near the surface. It often refers to those submerged ridges, banks, or bars that rise near enough to the surface of a body of water as to constitute a danger to navigation. Shoals are also known as sandbanks, sandbars, or gravelbars. Two or more shoals that are either separated by shared troughs or interconnected by past or present sedimentary and hydrographic processes are referred to as a shoal complex.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. The term ''shoal'' is also used in a number of ways that can be either similar or quite different from how it is used in geologic, geomorphic, and oceanographic literature. Sometimes, this term refers ...
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Facies
In geology, a facies ( , ; same pronunciation and spelling in the plural) is a body of rock with specified characteristics, which can be any observable attribute of rocks (such as their overall appearance, composition, or condition of formation), and the changes that may occur in those attributes over a geographic area. A facies encompasses all of the characteristics of a rock including its chemical, physical, and biological features that distinguish it from adjacent rock. The term facies was introduced by the Swiss geologist Amanz Gressly in 1838 and was part of his significant contribution to the foundations of modern stratigraphy, which replaced the earlier notions of Neptunism. Types of facies Sedimentary facies Ideally, a Sedimentary structures, sedimentary facies is a distinctive rock unit that forms under certain conditions of sedimentation, reflecting a particular process or environment. Sedimentary facies are either descriptive or interpretative. Sedimentary facies ...
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Subtidal
The neritic zone (or sublittoral zone) is the relatively shallow part of the ocean above the drop-off of the continental shelf, approximately in depth. From the point of view of marine biology it forms a relatively stable and well-illuminated environment for marine life, from plankton up to large fish and corals, while physical oceanography sees it as where the oceanic system interacts with the coast. Definition (marine biology), context, extra terminology In marine biology, the neritic zone, also called coastal waters, the coastal ocean or the sublittoral zone, refers to that zone of the ocean where sunlight reaches the ocean floor, that is, where the water is never so deep as to take it out of the photic zone. It extends from the low tide mark to the edge of the continental shelf, with a relatively shallow depth extending to about 200 meters (660 feet). Above the neritic zone lie the intertidal (or eulittoral) and supralittoral zones; below it the continental slope begi ...
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