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Khaba Fort
Khaba (also read as Hor-Khaba) was a pharaoh of Ancient Egypt, active during the 3rd Dynasty of the Old Kingdom period. The exact time during which Khaba ruled is unknown but may have been around 2670 BC,Thomas Schneider: ''Lexikon der Pharaonen''. Albatros, Düsseldorf 2002, , p. 97. and almost definitely towards the end of the dynasty. King Khaba is considered to be difficult to assess as a figure of ancient Egypt. His name is archaeologically well-attested by stone bowls and mud seal impressions. Khaba's reign is securely dated to the Third Dynasty. Because of the contradictions within Ramesside king lists and the lack of contemporary, festive inscriptions, his exact chronological position within the dynasty remains disputed. These problems originate in part from contradictory king lists, which were all compiled long after Khaba's death, especially during the Ramesside era (which is separated from the Third Dynasty by 1,400 years). It is also a matter of debate as to wh ...
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Sedjes
Sedjes is an ancient Egyptian cartouche "name" for a king (pharaoh), who is said to have ruled during the 3rd Dynasty ( Old Kingdom period). The lexeme appears only once in the Abydos King List as cartouche No. 18, presented as if it were the name of the direct follower of king Sekhemkhet (here named ''Teti'') and the direct predecessor of king Neferkara I. In the 19th century it was thought by Egyptologists and historians to be the name of a king, because the scribes had placed the word ''sedjes'' inside a royal cartouche. But as knowledge about Ancient Egyptian phrasing and grammars advanced, scholars realized its true meaning: ''sedjes'' means "omitted" or "missing" with the scribes using the word as a pseudonym, replacing a now illegible name of a king. They encircled it with a royal cartouche to mark it as a king's name, but following generations of scribes erroneously took it as the actual birth name of the to-be listed king. A similar case can be observed with the ominous ...
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Nineteenth Dynasty Of Egypt
The Nineteenth Dynasty of Egypt (notated Dynasty XIX), also known as the Ramessid dynasty, is classified as the second Dynasty of the Ancient Egyptian New Kingdom of Egypt, New Kingdom period, lasting from 1292 BC to 1189 BC. The 19th Dynasty and the 20th Dynasty furthermore together constitute an era known as the ''Ramesside period''. This Dynasty was founded by Vizier (Ancient Egypt), Vizier Ramesses I, whom Pharaoh Horemheb chose as his successor to the throne. History Background The warrior kings of the early Eighteenth Dynasty of Egypt, 18th Dynasty had encountered only little resistance from neighbouring kingdoms, allowing them to expand their realm of influence easily, but the international situation had changed radically towards the end of the dynasty. The Hittites had gradually extended their influence into Syria and Canaan to become a major power in international politics, a power that both Seti I and his son Ramesses II would confront in the future. 19th Dynasty ...
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Ancient Egyptian Royal Titulary
The royal titulary or royal protocol is the standard naming convention taken by the pharaohs of ancient Egypt. It symbolised worldly power and holy might, also acting as a sort of mission statement for the duration of a monarch's reign (although sometimes it even changed during the reign). The full titulary, consisting of five names, did not come into standard usage until the Middle Kingdom but remained in use as late as the Roman Empire. Origins In order that the pharaoh, who held divine office, could be linked to the people and the gods, special epithets were created for them at their accession to the throne. These titles also served to demonstrate one's qualities and link them to the terrestrial realm. The five names were developed over the centuries beginning with the Horus name. This name identified the figure as a representative of the god Horus. The Nebty name was the second part of the royal titular of Upper and Lower Egypt. This name placed the king under the protection o ...
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London
London is the Capital city, capital and List of urban areas in the United Kingdom, largest city of both England and the United Kingdom, with a population of in . London metropolitan area, Its wider metropolitan area is the largest in Western Europe, with a population of 14.9 million. London stands on the River Thames in southeast England, at the head of a tidal estuary down to the North Sea, and has been a major settlement for nearly 2,000 years. Its ancient core and financial centre, the City of London, was founded by the Roman Empire, Romans as Londinium and has retained its medieval boundaries. The City of Westminster, to the west of the City of London, has been the centuries-long host of Government of the United Kingdom, the national government and Parliament of the United Kingdom, parliament. London grew rapidly 19th-century London, in the 19th century, becoming the world's List of largest cities throughout history, largest city at the time. Since the 19th cen ...
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Petrie Museum
The Petrie Museum of Egyptian and Sudanese Archaeology in London is part of University College London Museums and Collections. The museum contains over 80,000 objects, making it one of the world's largest collections of Egyptian and Sudanese material. It is designated under the Arts Council England Designation Scheme as being of "national and international importance". History The museum was established as a teaching resource for the Department of Egyptology, Egyptian Archaeology and Philology at University College at the same time as the department was established in 1892. The initial collection was donated by the writer Amelia Edwards. The first Edwards Professor, William Matthew Flinders Petrie, conducted many important excavations, and in 1913 he sold his collections of Egyptian antiquities to University College, creating the Flinders Petrie Collection of Egyptian Antiquities, and transforming the museum into one of the leading collections outside Egypt. The collection wa ...
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Elephantine
Elephantine ( ; ; ; ''Elephantíne''; , ) is an island on the Nile, forming part of the city of Aswan in Upper Egypt. The archaeological site, archaeological digs on the island became a World Heritage Site in 1979, along with other examples of Upper Egyptian architecture, as part of the "Nubian Monuments from Abu Simbel to Philae" (despite Elephantine being neither Nubian, nor between Abu Simbel and Philae temple complex, Philae). The island has been studied through excavation sites. Aramaic Papyrus, papyri and Ostracon, ostraca have been collected to study what life was like on Elephantine during the time of ancient Egypt. There have been studies about the Elephantine Triad and the Jews, Jewish presence that formulated on the island. The standard reference collection of the Aramaic documents of the Elephantine papyri and ostraca, Elephantine Papyri and Ostraca is the ''Textbook of Aramaic Documents from Ancient Egypt''. Geography Elephantine, or what ancient Egyptians called ...
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Hierakonpolis
Nekhen (, ), also known as Hierakonpolis (; , meaning City of Hawks or City of Falcons, a reference to Horus; ) was the religious and political capital of Upper Egypt at the end of prehistoric Egypt ( 3200–3100 BC) and probably also during the Early Dynastic Period ( 3100–2686 BC). Located in Upper Egypt about 100 kilometers south of the modern-day city of Luxor, Nekhen has been the subject of extensive archeological research over the past one and half centuries, and has yielded a large number of artifacts that give a greater understanding to this period of ancient Egyptian history. The city was the center of cult worship of the god Horus, who is said to have his origins in Nekhen as its tutelary deity. Tombs, temples, breweries, houses, and other structures have all been discovered that date back to the predynastic era. The oldest known tomb with painted decoration, known as the Painted Tomb, is located in Nekhen and is thought to date to c. 3500–3200 BC. It shares disti ...
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Serekh
In Egyptian hieroglyphs, a serekh is a rectangular enclosure representing the niched or gated façade of a palace surmounted by (usually) the Horus falcon, indicating that the text enclosed is a royal name. The serekh was the earliest convention used to set apart the royal name in ancient Egyptian iconography, predating the later and better known cartouche by four dynasties and five to seven hundred years. Appearance A serekh was an ornamental vignette combining a view of a palace façade and a plan (top view) of the royal courtyard. The term ''serekh'' derives from the Egyptian word for "façade". Different serekhs on different types of object display countless variations of the façade decor in its complexity and detail. It seems that no strict artistic rules for the design of the serekh itself existed.Jürgen von Beckerath: ''Handbuch der ägyptischen Königsnamen''. Münchner Ägyptologische Studien. Bd. 49. Philipp von Zabern, Mainz 1999, , p. 7-9.Rolf Gundlach: ''Horus ...
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Abusir
Abusir (  ; Egyptian ''pr wsjr'' ' "the resting place of Osiris"; ) is the name given to an ancient Egyptian archaeological pyramid complex comprising the ruins of 4 kings' pyramids dating to the Old Kingdom period, and is part of the Pyramid Fields of the Memphis and its Necropolis UNESCO World Heritage Site. The pyramid complex is named after the neighbouring village of Abusir, in the markaz (county) of Badrashin, Giza. The Abusir pyramid complex is located on the Western Desert plateau at the edge of the cultivated plain, with the Giza Pyramids to its north, and Saqqara to its south, and served as one of the main elite cemeteries for the ancient Egyptian capital city of Memphis. Several other villages in northern and southern Egypt are named Abusir or Busiri. The locality of Abusir took its turn as the focus of the prestigious western burial rites operating out of the then-capital of Memphis during the Old Kingdom 5th Dynasty. As an elite cemetery, neighbou ...
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Diorite
Diorite ( ) is an intrusive rock, intrusive igneous rock formed by the slow cooling underground of magma (molten rock) that has a moderate content of silica and a relatively low content of alkali metals. It is Intermediate composition, intermediate in composition between low-silica (mafic) gabbro and high-silica (felsic) granite. Diorite is found in mountain-building belts (''orogens'') on the margins of continents. It has the same composition as the fine-grained volcanic rock, andesite, which is also common in orogens. Diorite has been used since prehistoric times as decorative stone. It was used by the Akkadian Empire of Sargon of Akkad for funerary sculptures, and by many later civilizations for sculptures and building stone. Description Diorite is an intrusive rock, intrusive igneous rock composed principally of the silicate minerals plagioclase feldspar (typically andesine), biotite, hornblende, and sometimes pyroxene. The chemical composition of diorite is Intermedia ...
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Travertine
Travertine ( ) is a form of terrestrial limestone deposited around mineral springs, especially hot springs. It often has a fibrous or concentric appearance and exists in white, tan, cream-colored, and rusty varieties. It is formed by a process of rapid precipitation of calcium carbonate, often at the mouth of a hot spring or in a limestone cave. In the latter, it can form stalactites, stalagmites, and other speleothems. Travertine is frequently used in Italy and elsewhere as a building material. Similar, but softer and extremely porous deposits formed from ambient-temperature water are known as ''tufa''. Definition Travertine is a sedimentary rock formed by the chemical precipitation of calcium carbonate minerals from fresh water, typically in springs, rivers, and lakes; that is, from surface and ground waters. In the broadest sense, travertine includes deposits in both hot and cold springs, including the porous, spongy rock known as tufa, and also the cave features known as ...
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Magnesite
Magnesite is a mineral with the chemical formula ( magnesium carbonate). Iron, manganese, cobalt, and nickel may occur as admixtures, but only in small amounts. Occurrence Magnesite occurs as veins in and an alteration product of ultramafic rocks, serpentinite and other magnesium rich rock types in both contact and regional metamorphic terrains. These magnesites are often cryptocrystalline and contain silica in the form of opal or chert. Magnesite is also present within the regolith above ultramafic rocks as a secondary carbonate within soil and subsoil, where it is deposited as a consequence of dissolution of magnesium-bearing minerals by carbon dioxide in groundwaters. Formation Magnesite can be formed via talc carbonate metasomatism of peridotite and other ultramafic rocks. Magnesite is formed via carbonation of olivine in the presence of water and carbon dioxide at elevated temperatures and high pressures typical of the greenschist facies. Magnesite can also be f ...
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