Pyramid Of Sahure
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Pyramid Of Sahure
The pyramid of Sahure () is a pyramid complex built in the late 26th to 25th century BC for the Egyptian pharaoh Sahure of the Fifth Dynasty. It introduced a period of pyramid building by Sahure's successors in Abusir, on a location earlier used by Userkaf for his sun temple. The site was first thoroughly excavated by Ludwig Borchardt between March 1907 and 1908, who wrote the standard work () between 1910 and 1913. The pyramid complex's layout was adopted by succeeding kings of the Fifth and Sixth Dynasties, marking a milestone in pyramid complex construction. Compared to the preceding Fourth Dynasty, the immensity of the constructions was dramatically reduced but, in tandem, the decorative programme proliferated and temples were augmented by enlarged storeroom complexes. The complex is estimated to have had of finely carved relief adorning its walls, of which has been preserved. Some of these reliefs are considered unparalleled in Egyptian art, such as the by (4.2 × 1. ...
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Sahure
Sahure (also Sahura, meaning "He who is close to Re") was a pharaoh of ancient Egypt and the second ruler of the Fifth Dynasty (c. 2465 – c. 2325 BC). He reigned for about 13 years in the early 25th century BC during the Old Kingdom Period. Sahure's reign marks the political and cultural high point of the Fifth Dynasty. He was probably the son of his predecessor Userkaf with Queen NeferhetepesII, and was in turn succeeded by his son Neferirkare Kakai. During Sahure's rule, Egypt had important trade relations with the Levantine coast. Sahure launched several naval expeditions to modern-day Lebanon to procure cedar trees, slaves and exotic items. His reign may have witnessed the flourishing of the Egyptian navy, which included a high-seas fleet as well as specialized racing boats. Relying on this, Sahure ordered the earliest attested expedition to the land of Punt, which brought back large quantities of myrrh, malachite and electrum. Sahure is shown celebrating the success o ...
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Art Of Ancient Egypt
Ancient Egyptian art refers to art produced in ancient Egypt between the 6th millennium BC and the 4th century AD, spanning from Prehistoric Egypt until the Christianization of Roman Egypt. It includes paintings, sculptures, drawings on papyrus, faience, jewelry, ivories, architecture, and other art media. It is also very conservative: the art style changed very little over time. Much of the surviving art comes from tombs and monuments, giving more insight into the ancient Egyptian afterlife beliefs. The ancient Egyptian language had no word for "art". Artworks served an essentially functional purpose that was bound with religion and ideology. To render a subject in art was to give it permanence. Therefore, ancient Egyptian art portrayed an idealized, unrealistic view of the world. There was no significant tradition of individual artistic expression since art served a wider and cosmic purpose of maintaining order (Ma'at). Art of Pre-Dynastic Egypt (6 ...
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Khafre
Khafre (also read as Khafra and gr, Χεφρήν Khephren or Chephren) was an ancient Egyptian King (pharaoh) of the 4th Dynasty during the Old Kingdom. He was the son of Khufu and the successor of Djedefre. According to the ancient historian Manetho, Khafre was followed by king Bikheris, but according to archaeological evidence he was instead followed by king Menkaure. Khafre was the builder who made the second largest pyramid of Giza. The view held by modern Egyptology at large continues to be that the Great Sphinx was built in approximately 2500 BC for Khafre. Not much is known about Khafre, except from the reports of Herodotus, writing 2,000 years after his life. Family Khafre was a son of king Khufu and the brother and successor of Djedefre. Khafre is thought by some to be the son of Queen Meritites I due to an inscription where he is said to honor her memory. Kings-wife, his beloved, devoted to Horus, Mertitytes. King's-wife, his beloved, Mertitytes; beloved of ...
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Sarcophagus
A sarcophagus (plural sarcophagi or sarcophaguses) is a box-like funeral receptacle for a corpse, most commonly carved in stone, and usually displayed above ground, though it may also be buried. The word ''sarcophagus'' comes from the Greek σάρξ ' meaning "flesh", and φαγεῖν ' meaning "to eat"; hence ''sarcophagus'' means "flesh-eating", from the phrase ''lithos sarkophagos'' ( λίθος σαρκοφάγος), "flesh-eating stone". The word also came to refer to a particular kind of limestone that was thought to rapidly facilitate the decomposition of the flesh of corpses contained within it due to the chemical properties of the limestone itself. History of the sarcophagus Sarcophagi were most often designed to remain above ground. The earliest stone sarcophagi were used by Egyptian pharaohs of the 3rd dynasty, which reigned from about 2686 to 2613 B.C. The Hagia Triada sarcophagus is a stone sarcophagus elaborately painted in fresco; one style of later A ...
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Tora, Egypt
Tura ( arz, طرة '  , , ) was the primary quarry for limestone in ancient Egypt. The site, which was known by the ancient Egyptians as ''Troyu'' or ''Royu'', is located about halfway between modern-day Cairo and Helwan. Its ancient Egyptian name was misinterpreted by the ancient Greek geographer Strabo, who thought it meant it was inhabited by Trojans, thus the Hellenistic city was named Troia. The site is located by the modern town of ''Tora'' in the Cairo Governorate. Ancient mining town The limestone from Tura was the finest and whitest of all the Egyptian quarries, so it was used for facing stones for the richest tombs, as well as for the floors and ceilings of mastabas, which were otherwise made of mudbrick. It was used during the Old Kingdom and was the source of the limestone used for the "Rhomboidal Pyramid" or Bent Pyramid of Sneferu, the Great Pyramid of Khufu, the sarcophagi of many Old Kingdom nobles, the pyramids of the Middle Kingdom, and certain temples ...
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Mortar (masonry)
Mortar is a workable paste which hardens to bind building blocks such as stones, bricks, and concrete masonry units, to fill and seal the irregular gaps between them, spread the weight of them evenly, and sometimes to add decorative colors or patterns to masonry walls. In its broadest sense, mortar includes pitch, asphalt, and soft mud or clay, as those used between mud bricks, as well as cement mortar. The word "mortar" comes from Old French ''mortier'', "builder's mortar, plaster; bowl for mixing." (13c.). Cement mortar becomes hard when it cures, resulting in a rigid aggregate structure; however, the mortar functions as a weaker component than the building blocks and serves as the sacrificial element in the masonry, because mortar is easier and less expensive to repair than the building blocks. Bricklayers typically make mortars using a mixture of sand, a binder, and water. The most common binder since the early 20th century is Portland cement, but the ancient binder lim ...
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Limestone Block
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limestone co ...
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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 ...
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Alabaster
Alabaster is a mineral or rock that is soft, often used for carving, and is processed for plaster powder. Archaeologists and the stone processing industry use the word differently from geologists. The former use it in a wider sense that includes varieties of two different minerals: the fine-grained massive type of gypsum and the fine-grained banded type of calcite.''More about alabaster and travertine'', brief guide explaining the different use of these words by geologists, archaeologists, and those in the stone trade. Oxford University Museum of Natural History, 2012/ref> Geologists define alabaster only as the gypsum type. Chemically, gypsum is a Water of crystallization, hydrous sulfur, sulfate of calcium, while calcite is a carbonate of calcium. The two types of alabaster have similar properties. They are usually lightly colored, translucent, and soft stones. They have been used throughout history primarily for carving decorative artifacts."Grove": R. W. Sanderson and Francis ...
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Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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Great Pyramid Of Giza
The Great Pyramid of Giza is the biggest Egyptian pyramid and the tomb of Fourth Dynasty pharaoh Khufu. Built in the early 26th century BC during a period of around 27 years, the pyramid is the oldest of the Seven Wonders of the Ancient World, and the only one to remain largely intact. As part of the Giza pyramid complex, it borders present-day Giza in Greater Cairo, Egypt. Initially standing at , the Great Pyramid was the tallest man-made structure in the world for more than 3,800 years. Over time, most of the smooth white limestone casing was removed, which lowered the pyramid's height to the present . What is seen today is the underlying core structure. The base was measured to be about square, giving a volume of roughly , which includes an internal hillock. The dimensions of the pyramid were high, a base length of , with a seked of palms (a slope of 51°50'40"). The Great Pyramid was built by quarrying an estimated 2.3 million large blocks weighing 6 million tonnes ...
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Miroslav Verner
Miroslav Verner (born October 31, 1941 in Brno) is a Czech egyptologist, who specializes in the history and archaeology of Ancient Egypt of the Old Kingdom and especially of the Fifth Dynasty of Egypt. Biography Verner was the director of the Czechoslovak and later Czech Institute of Egyptology at the Faculty of Arts, Charles University in Prague for twenty-five years, and led the Czech excavations at Abusir. He has also been associated with the Universities of Vienna and Hamburg as well as the Charles University in Prague and the American University in Cairo. Verner has been active in archaeological work since 1964, and he has been excavating at Abusir since 1976. In 1998, the tomb of Iufaa Iufaa was an Egyptian priest and administer of palaces who lived around 500 BC. His mummy was discovered in an unmolested tomb by Czech archaeologists under the direction of Ladislav Bareš and Miroslav Verner in February 1998. The discovery of an ..., an Egyptian priest and administer of ...
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