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Mastabet El-Fara'un
The Mastabat al-Fir’aun ( ar, مصطبة الفرعون, d=Maṣṭabat al-Firʿawn, also referred to in Egyptological literature as the ''Mastaba el-Faraun'', ''Mastabat el-Faraun'' or ''Mastabat Faraun'', and meaning "Bench of the Pharaoh") is the grave monument of the ancient Egyptian king Shepseskaf (reign ''circa'' 2510–2503 BC), the last king of the Fourth Dynasty documented to date. It is located in South Saqqara halfway between the Pyramid of Djoser at Saqqara and the pyramids of Sneferu, the founder of the Fourth Dynasty, at Dahshur. The structure is located close to the pyramid of Pepi II, a ruler of the Sixth Dynasty. The stone quarry for the structure is located west of the Red Pyramid of Sneferu. The Mastaba of Shepseskaf Discovery The Mastabat al-Fir’aun was described for the first time by[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shepseskaf
Shepseskaf (meaning "His Ka is noble") was a pharaoh of ancient Egypt, the sixth and probably last ruler of the fourth dynasty during the Old Kingdom period. He reigned most probably for four but possibly up to seven years in the late 26th to mid-25th century BC. Shepseskaf's relation to his predecessor Menkaure is not entirely certain; he might have been his son or possibly his brother. The identity of his mother is highly uncertain as she could have been one of Menkaure's consorts or queen Khentkaus I or Neferhetepes. Similarly, Shepseskaf's relation to his probable successor on the throne, Userkaf, is not known although in the absence of clear indication of strife at the transition between the fourth and fifth dynasties, Userkaf could well have been his son or his brother. If Shepseskaf was succeeded directly by Userkaf rather than by Thampthis as claimed by some historical sources, then his death marks the end of the fourth dynasty. The transition to the fifth dynasty se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karl Richard Lepsius
Karl Richard Lepsius ( la, Carolus Richardius Lepsius) (23 December 181010 July 1884) was a pioneering Prussian Egyptologist, linguist and modern archaeologist. He is widely known for his magnum opus ''Denkmäler aus Ägypten und Äthiopien''. Early life Karl Richard Lepsius was the son of Karl Peter Lepsius, a classical scholar from Naumburg, and his wife Friederike (née Gläser), who was the daughter of composer Carl Ludwig Traugott Gläser. The family name was originally "Leps" and had been Latinized to "Lepsius" by Karl's paternal great-grandfather Peter Christoph Lepsius. He was born in Naumburg on the Saale, Saxony. He studied Greek and Roman archaeology at the University of Leipzig (1829–1830), the University of Göttingen (1830–1832), and the Frederick William University of Berlin (1832–1833). After receiving his doctorate following his dissertation ''De tabulis Eugubinis'' in 1833, he travelled to Paris, where he attended lectures by the French classicist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rainer Stadelmann
Dr. Rainer Stadelmann (24 October 1933 – 14 January 2019) was a German Egyptologist. He was considered an expert on the archaeology of the Giza Plateau. Biography After studying in Neuburg an der Donau in 1933, he studied Egyptology, orientalism, and archaeology at the University of Munich. He participated in 1955 and 1956 in the excavations of the sun temple of the 5th Dynasty pharaoh Userkaf at Abusir. He continued his studies at the University of Heidelberg, where in 1960 he wrote his doctoral thesis on the Syrian-Palestinian deities in Egypt. He was a technical assistant in Heidelberg until 1967, after which he became scientific director at the German Archaeological Institute in Cairo, where he served from 1989 to 1998. Since 1975, he has been honorary professor at the University of Heidelberg. He has participated in numerous excavations at Elephantine, Thebes, and Dahshur, the latter of which he explored and wrote about the Bent Pyramid and the valley temple of King Snef ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Causeway
A causeway is a track, road or railway on the upper point of an embankment across "a low, or wet place, or piece of water". It can be constructed of earth, masonry, wood, or concrete. One of the earliest known wooden causeways is the Sweet Track in the Somerset Levels, England, which dates from the Neolithic age. Timber causeways may also be described as both boardwalks and bridges. Etymology When first used, the word ''causeway'' appeared in a form such as "causey way" making clear its derivation from the earlier form "causey". This word seems to have come from the same source by two different routes. It derives ultimately, from the Latin for heel, ''calx'', and most likely comes from the trampling technique to consolidate earthworks. Originally, the construction of a causeway utilised earth that had been trodden upon to compact and harden it as much as possible, one layer at a time, often by enslaved bodies or flocks of sheep. Today, this work is done by machines. The s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greywacke
Greywacke or graywacke (German ''grauwacke'', signifying a grey, earthy rock) is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or lithic fragments set in a compact, clay-fine matrix. It is a texturally immature sedimentary rock generally found in Paleozoic strata. The larger grains can be sand- to gravel-sized, and matrix materials generally constitute more than 15% of the rock by volume. The term "greywacke" can be confusing, since it can refer to either the immature (rock fragment) aspect of the rock or its fine-grained (clay) component. The origin of greywacke was unknown until turbidity currents and turbidites were understood, since, according to the normal laws of sedimentation, gravel, sand and mud should not be laid down together. Geologists now attribute its formation to submarine avalanches or strong turbidity currents. These actions churn sediment and cause mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Portcullis
A portcullis (from Old French ''porte coleice'', "sliding gate") is a heavy vertically-closing gate typically found in medieval fortifications, consisting of a latticed grille made of wood, metal, or a combination of the two, which slides down grooves inset within each jamb of the gateway. Usage Portcullises fortified the entrances to many medieval castles, securely closing off the castle during time of attack or siege. Every portcullis was mounted in vertical grooves in the walls of the castle and could be raised or lowered quickly by means of chains or ropes attached to an internal winch. Portcullises had an advantage over gates in that they could be closed immediately at a time of crisis by a single guard. Often, two portcullises to the main entrance would be used. The one closer to the inside would be closed first, and then the one farther away. This was used to trap the enemy, and often, burning wood or fire-heated sand would be dropped onto them from the roof or murder-h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Early Dynastic Period (Egypt)
The Early Dynastic Period or Archaic Period, also known as the Thinite Period (from Thinis, the supposed hometown of its rulers), is the era of ancient Egypt that immediately follows the unification of Upper and Lower Egypt in . It is generally taken to include the First Dynasty and the Second Dynasty, lasting from the end of the archaeological culture of Naqada III until , or the beginning of the Old Kingdom. With the First Dynasty, the Egyptian capital moved from Thinis to Memphis, with the unified land being ruled by an Egyptian god-king. In the south, Abydos remained the major centre of ancient Egyptian religion; the hallmarks of ancient Egyptian civilization, such as Egyptian art, Egyptian architecture, and many aspects of Egyptian religion, took shape during the Early Dynastic Period. Before the unification of Egypt, the land was settled with autonomous villages. With the early dynasties, and for much of Egypt's history thereafter, the country came to be known as "The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fifth Dynasty
The Fifth Dynasty of ancient Egypt (notated Dynasty V) is often combined with Dynasties Third Dynasty of Egypt, III, Fourth Dynasty of Egypt, IV and Sixth Dynasty of Egypt, VI under the group title the Old Kingdom of Egypt, Old Kingdom. The Fifth Dynasty pharaohs reigned for approximately 150 years, from the early 25th century BC until the mid 24th century BC. Chronology The Fifth Dynasty of Egypt is a group of nine kings ruling Egypt for approximately 150 years in the 25th century BC, 25th and 24th century BC, 24th centuries BC. The relative succession of kings is not entirely secured as there are contradictions between historical sources and archaeological evidence regarding the reign of the shadowy Shepseskare. Rulers Known rulers in the Fifth Dynasty are listed below. Manetho assigns 248 years of rule to the Fifth Dynasty; however, the pharaohs of this dynasty more probably ruled for approximately 150 years. This estimate varies by both scholar and source. The Horus names a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Unas
Unas or Wenis, also spelled Unis ( egy, wnjs, hellenized form Oenas or Onnos), was a pharaoh, the ninth and last ruler of the Fifth Dynasty of Egypt during the Old Kingdom. Unas reigned for 15 to 30 years in the mid-24th century BC (circa 2345–2315 BC), succeeding Djedkare Isesi, who might have been his father. Little is known of Unas' activities during his reign, which was a time of economic decline. Egypt maintained trade relations with the Levantine coast and Nubia, and military action may have taken place in southern Canaan. The growth and decentralization of the administration in conjunction with the lessening of the king's power continued under Unas, ultimately contributing to the collapse of the Old Kingdom some 200 years later. Unas built a pyramid in Saqqara, the smallest of the royal pyramids completed during the Old Kingdom. The accompanying mortuary complex with its high and valley temples linked by a causeway was lavishly decorated with painted reliefs, whose ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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