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Wadi Hammamat
Wadi Hammamat ( en, Valley of Many Baths, ''India way; gateway to India'') is a dry river bed in Egypt's Eastern Desert, about halfway between Al-Qusayr and Qena. It was a major mining region and trade route east from the Nile Valley in ancient times, and three thousand years of rock carvings and graffiti make it a major scientific and tourist site today. Trade route Hammamat became the major route from Thebes to the Red Sea and then to the Silk Road that led to Asia, or to Arabia and the horn of Africa. This 200 km journey was the most direct route from the Nile to the Red Sea, as the Nile bends toward the coast at the western end of the wadi. The Hammamat route ran from Qift (or Coptos), located just north of Luxor, to Al-Qusayr on the coast of the Red Sea. Qift was an important center for administration, religion, and commerce. The cities at both ends of the route were established by the First Dynasty, although evidence of predynastic occupation also has been found ...
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Egypt Ancient Detail Wadi Hammamat
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, urban ...
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Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ...
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Graffiti
Graffiti (plural; singular ''graffiti'' or ''graffito'', the latter rarely used except in archeology) is art that is written, painted or drawn on a wall or other surface, usually without permission and within public view. Graffiti ranges from simple written words to elaborate wall paintings, and has existed Graffito (archaeology), since ancient times, with examples dating back to ancient Egypt, ancient Greece, and the Roman Empire. Graffiti is a controversial subject. In most countries, marking or painting property without permission is considered by property owners and civic authorities as defacement and vandalism, which is a punishable crime, citing the use of graffiti by street gangs to mark territory or to serve as an indicator of gang-related activities. Graffiti has become visualized as a growing urban "problem" for many cities in industrialized nations, spreading from the New York City Subway nomenclature, New York City subway system and Philadelphia in the early 1970s to ...
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Turin Papyrus Map
The Turin Papyrus Map is an ancient Egyptian map, generally considered the oldest surviving map of topographical interest from the ancient world. It is drawn on a papyrus reportedly discovered at Deir el-Medina in Thebes, collected by Bernardino Drovetti (known as Napoleon's Proconsul) in Egypt sometime before 1824 AD and now preserved in Turin's Museo Egizio. The map was drawn about 1150 BC by the well-known Scribe-of-the-Tomb Amennakhte, son of Ipuy. It was prepared for Ramesses IV's quarrying expedition to the Wadi Hammamat in the Eastern Desert, which exposes Precambrian rocks of the Arabian-Nubian Shield. The purpose of the expedition was to obtain blocks of ''bekhen''-stone (metagraywacke sandstone) to be used for statues of the king. Description The map shows a 15-kilometre stretch of Wadi Hammamat and has depictions of this wadi's confluence with wadis Atalla and el-Sid, the surrounding hills, the ''bekhen''-stone quarry, and the gold mine and settlement at Bir Umm Fawa ...
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Geological Map
A geologic map or geological map is a special-purpose map made to show various geological features. Rock units or geologic strata are shown by color or symbols. Bedding planes and structural features such as faults, folds, are shown with strike and dip or trend and plunge symbols which give three-dimensional orientations features. Stratigraphic contour lines may be used to illustrate the surface of a selected stratum illustrating the subsurface topographic trends of the strata. Isopach maps detail the variations in thickness of stratigraphic units. It is not always possible to properly show this when the strata are extremely fractured, mixed, in some discontinuities, or where they are otherwise disturbed. Symbols Lithologies Rock units are typically represented by colors. Instead of (or in addition to) colors, certain symbols can be used. Different geologic mapping agencies and authorities have different standards for the colors and symbols to be used for rocks of diff ...
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Senusret I
Senusret I (Middle Egyptian: z-n-wsrt; /suʀ nij ˈwas.ɾiʔ/) also anglicized as Sesostris I and Senwosret I, was the second pharaoh of the Twelfth Dynasty of Egypt. He ruled from 1971 BC to 1926 BC (1920 BC to 1875 BC), and was one of the most powerful kings of this Dynasty. He was the son of Amenemhat I. Senusret I was known by his prenomen, Kheperkare, which means "the Ka of Re is created." He expanded Egypt that allowed him to rule over an age of prosperity. He continued his father's aggressive expansionist policies against Nubia by initiating two expeditions into this region in his 10th and 18th years and established Egypt's formal southern border near the second cataract where he placed a garrison and a victory stele. He also organized an expedition to a Western Desert oasis. Senusret I established diplomatic relations with some rulers of towns in Syria and Canaan. He also tried to centralize the country's political structure by supporting nomarchs who were loyal to him. ...
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Seti I
Menmaatre Seti I (or Sethos I in Greek) was the second pharaoh of the Nineteenth Dynasty of Egypt during the New Kingdom period, ruling c.1294 or 1290 BC to 1279 BC. He was the son of Ramesses I and Sitre, and the father of Ramesses II. The name 'Seti' means "of Set", which indicates that he was consecrated to the god Set (also termed "Sutekh" or "Seth"). As with most pharaohs, Seti had several names. Upon his ascension, he took the prenomen "mn-m3't-r' ", usually vocalized in Egyptian as ''Menmaatre (''Established is the Justice of Re). His better known nomen, or birth name, is transliterated as "''sty mry-n-ptḥ"'' or ''Sety Merenptah'', meaning "Man of Set, beloved of Ptah". Manetho incorrectly considered him to be the founder of the 19th Dynasty, and gave him a reign length of 55 years, though no evidence has ever been found for so long a reign. Reign After the enormous social upheavals generated by Akhenaten's religious reform, Horemheb, Ramesses I and Seti I's ...
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Narmer Palette
The Narmer Palette, also known as the Great Hierakonpolis Palette or the Palette of Narmer, is a significant Egyptian archeological find, dating from about the 31st century BC, belonging, at least nominally, to the category of cosmetic palettes. It contains some of the earliest Egyptian hieroglyphs, hieroglyphic inscriptions ever found. The tablet is thought by some to depict the unification of Upper Egypt, Upper and Lower Egypt under the king Narmer. Along with the Scorpion Macehead and the Narmer Maceheads, also found together in the main deposit at Nekhen, the Narmer Palette provides one of the earliest known depictions of an Egyptian king. On one side, the king is depicted with the bulbed Hedjet, White Crown of Upper (southern) Egypt, and the other side depicts the king wearing the level Deshret, Red Crown of Lower (northern) Egypt, which also makes it the earliest known example of a king wearing both types of headdress. The Palette shows many of the classic conventions of Anci ...
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Quartz
Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral defining the val ...
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University Of Toledo
The University of Toledo (UToledo or UT) is a public research university in Toledo, Ohio. It is the northernmost campus of the University System of Ohio. The university also operates a Health Science campus, which includes the University of Toledo Medical Center, in the West Toledo neighborhood of Toledo; a satellite campus in the Scott Park neighborhood of Toledo; the Center for the Visual Arts is located in downtown Toledo at the Toledo Museum of Art; and a research and education facility, known as the Lake Erie Center, at Maumee Bay State Park. The university was founded in 1872 in downtown Toledo as the Toledo University of Arts and Trades. It closed after six years. The city of Toledo took it over, reopening it in 1884 as the Toledo Manual Training School. The vocational school was developed as a university through the late 1800s. In 1931 the university moved to its current location in the Ottawa neighborhood. Since its establishment, the university has physically exp ...
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Cosmetic Palette
Cosmetic palettes are archaeological Artifact (archaeology), artifacts, originally used in predynastic Egypt, predynastic ancient Egypt, Egypt to grind and apply ingredients for facial or body cosmetics. The decorative palettes of the late 4th millennium BC, 4th millennium BCE appear to have lost this function and became commemorative, ornamental, and possibly ceremonial. They were made almost exclusively out of siltstone with a few exceptions. The siltstone originated from quarries in the Wadi Hammamat. Many of the palettes were found at Hierakonpolis, a centre of power in Predynastic Egypt, pre-dynastic Upper Egypt. After the unification of the country, the palettes ceased to be included in tomb assemblages. Notable palettes Notable decorative palettes are: * The Cosmetic palette in the form of a Nile tortoise * The Narmer Palette, often thought to depict the unification of Upper and Lower Egypt under the pharaoh Narmer, Egyptian Museum, Cairo * Libyan Palette, Egyptian Museum, ...
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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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