1.
Giza
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Giza, is the third-largest city in Egypt. It is located on the west bank of the Nile,5 km southwest of central Cairo, along with Cairo Governorate, Shubra El-Kheima, Helwan, 6th October City and Obour, the five form Greater Cairo metropolis. The city of Giza is the capital of the Giza Governorate and it is located right on the banks of the River Nile. The citys population was 2,681,863 in the 2006 national census and its large population made it the worlds second largest suburb in 2006, tied with Incheon, South Korea and Quezon City, Philippines, second only to Yokohama, Japan. Giza has always been a point in Egypts history due to its location close to Memphis. Its St. George cathedral is the see of the Coptic Catholic Eparchy of Giza. The Great Pyramid of Giza at one time was advocated as the location for the Prime Meridian, a reference point used for determining a base longitude. Mn Nefer, which means the wall in the ancient Egyptian language. Gizas most famous site, the Giza Plateau, holds some major monuments of Egyptian history. Once thriving with the Nile that flowed right into the Giza Plateau, the Giza Plateau is also home to Egyptian monuments such as the tomb of Pharaoh Djet of the First Dynasty, as well as that of Pharaoh Ninetjer of the Second Dynasty. The area in what is now Giza served as the necropolis of several pharaohs who ruled ancient Egypt, Three of these tombs, in the form of giant pyramids, are what is now the famed Three Pyramids of Giza. As ancient Egypt passed under several conquests under the Persians, Greeks, Romans and Byzantines, a Byzantine village named Teresa, located south of Giza, existed before the Muslim conquest of the region. A year later in 642 AD, they founded the city of Giza and its name, al-Jizzah in Arabic, means the valley or the plateau, pertaining to the areas topography. Giza has seen changes over time. Giza is a centre of Egyptian culture and is quite heavily populated, with many facilities. Giza saw much attention in particular to its vast amount of ancient Egyptian monuments found on the Giza Plateau, gizas infrastructure saw much attention from both the British government prior to the 1952 coup détat, as well as the current Egyptian government due to the citys importance in tourism. The city hosts the first zoo on the entire African continent and one of the oldest in the Mediterranean region, in addition, there are several parks, the most famous among them is Orman Park, which means Forest Park in the Turkish language. Giza has advanced level of medical care just like its elder twin Cairo, a list of famous hospitals in Giza, Agooza in Agouza district
2.
Pyramid
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A pyramid is a structure whose outer surfaces are triangular and converge to a single point at the top, making the shape roughly a pyramid in the geometric sense. The base of a pyramid can be trilateral, quadrilateral, or any polygon shape, as such, a pyramid has at least three outer triangular surfaces. The square pyramid, with base and four triangular outer surfaces, is a common version. A pyramids design, with the majority of the closer to the ground. This distribution of weight allowed early civilizations to create stable monumental structures and it has been demonstrated that the common shape of the pyramids of antiquity, from Egypt to Central America, represents the dry-stone construction that requires minimum human work. Pyramids have been built by civilizations in many parts of the world, khufus Pyramid is built mainly of limestone, and is considered an architectural masterpiece. It contains over 2,000,000 blocks ranging in weight from 2.5 tonnes to 15 tonnes and is built on a base with sides measuring about 230 m. Its four sides face the four cardinal points precisely and it has an angle of 52 degrees and it is still the tallest pyramid. The largest pyramid by volume is the Great Pyramid of Cholula, the Mesopotamians built the earliest pyramidal structures, called ziggurats. In ancient times, these were painted in gold/bronze. Since they were constructed of sun-dried mud-brick, little remains of them, ziggurats were built by the Sumerians, Babylonians, Elamites, Akkadians, and Assyrians for local religions. Each ziggurat was part of a complex which included other buildings. The precursors of the ziggurat were raised platforms that date from the Ubaid period during the fourth millennium BC, the earliest ziggurats began near the end of the Early Dynastic Period. The latest Mesopotamian ziggurats date from the 6th century BC, built in receding tiers upon a rectangular, oval, or square platform, the ziggurat was a pyramidal structure with a flat top. Sun-baked bricks made up the core of the ziggurat with facings of fired bricks on the outside, the facings were often glazed in different colors and may have had astrological significance. Kings sometimes had their names engraved on these glazed bricks, the number of tiers ranged from two to seven. It is assumed that they had shrines at the top, but there is no evidence for this. Access to the shrine would have been by a series of ramps on one side of the ziggurat or by a ramp from base to summit
3.
Khufu
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Khufu, originally Khnum-Khufu, is the birth name of an ancient Egyptian pharaoh, who ruled during the Fourth Dynasty in the first half of the Old Kingdom period. Khufu was the pharaoh of the 4th dynasty, he followed his possible father, king Sneferu. He is generally accepted as having commissioned the Great Pyramid of Giza, one of the Seven Wonders of the Ancient World, the only completely preserved portrait of the king is a three-inch high ivory figurine found in a temple ruin of later period at Abydos in 1903. All other reliefs and statues were found in fragments and many buildings of Khufu are lost, everything known about Khufu comes from inscriptions in his necropolis at Giza and later documents. For example, Khufu is the actor of the famous Papyrus Westcar from the 13th dynasty. Most documents that mention king Khufu were written by ancient Egyptian, thanks to these documents, an obscure and critical picture of Khufus personality persists. Khufus name was dedicated to the earth deity Khnum, which point to an increase of Khnums popularity. Khufu may have viewed himself as a creator, a role that was already given to Khnum. As a consequence, the king connected Khnums name with his own, interestingly, the pharaoh officially used two versions of his birth name, Khnum-khuf and Khufu. The first version clearly exhibits Khufus religious loyalty to Khnum, the version does not. It is unknown as to why the king would use a shortened version, since it hides the name of Khnum. It might be possible though, that the name wasnt meant to be connected to any god at all. Khufu is well known under his Hellenized name Khêops or Cheops and less well known under another Hellenized name, a rare version of the name of Khufu, used by Josephus, is Sofe. Arab historians, who wrote stories about Khufu and the Giza pyramids. The royal family of Khufu was quite large and it is uncertain if Khufu was actually the biological son of Sneferu. Mainstream Egyptologists believe Sneferu was Khufus father, but only because it was handed down by historians that the eldest son or a selected descendant would inherit the throne. In 1925 the tomb of queen Hetepheres I, G 7000x, was found east of Khufus pyramid and it contained many precious grave goods, and several inscriptions give her the title Mut-nesut, together with the name of king Sneferu. Therefore, it seemed clear at first that Hetepheres was the wife of Sneferu, more recently, however, some have doubted this theory, because Hetepheres is not known to have borne the title Hemet-nesut, a title indispensable to confirm a queens royal status
4.
Pyramid of Menkaure
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The Pyramid of Menkaure, located on the Giza Plateau in the southwestern outskirts of Cairo, Egypt, is the smallest of the three main Pyramids of Giza. It is thought to have built to serve as the tomb of the fourth dynasty Egyptian Pharaoh Menkaure. Menkaures pyramid had a height of 65.5 metres and was the smallest of the three major pyramids at the Giza Necropolis. It now stands at 61 m tall with a base of 108.5 m and its angle of incline is approximately 51°20′25″. It was constructed of limestone and granite, the first sixteen courses of the exterior were made of red granite. The upper portion was cased in the manner with Tura limestone. Part of the granite was left in the rough, incomplete projects such as this pyramid help archaeologists understand the methods used to build pyramids and temples. South of the pyramid of Menkaure are three pyramids that are each accompanied with a temple and have a substructure. The southernmost is the largest and a true pyramid and its casing is partly of granite, like the main pyramid, and is believed to have been completed due to the limestone pyramidion found close by. Neither of the two progressed beyond the construction of the inner core. In the mortuary temple the foundations and the core were made of limestone. The floors were begun with granite and granite facings were added to some of the walls, the foundations of the valley temple were made of stone. However both temples were finished with crude bricks and it was not unusual for a son or successor to complete a temple when a Pharaoh died, so it is not unreasonable to assume that Shepseskaf finished the temples with crude brick. There was an inscription in the temple that said he made it as his monument for his father. During excavations of the temples Reisner found a number of statues mostly of Menkaure alone. These were all carved in the style of the old kingdom with a high degree of detail evident. The pyramids date of construction is unknown, because Menkaures reign has not been accurately defined and it lies a few hundred meters southwest of its larger neighbors, the Pyramid of Khafre and the Great Pyramid of Khufu in the Giza necropolis. Richard William Howard Vyse, who first visited Egypt in 1835, discovered in the upper antechamber the remains of a wooden anthropoid coffin inscribed with Menkaures name, deeper into the pyramid, Vyse came upon a beautiful basalt sarcophagus, rich in detail with a bold projecting corniche
5.
Turonian
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The Turonian is, in the ICS geologic timescale, the second age in the Late Cretaceous epoch, or a stage in the Upper Cretaceous series. It spans the time between 93.9 ±0.8 Ma and 89.8 ±1 Ma, the Turonian is preceded by the Cenomanian stage and underlies the Coniacian stage. At the beginning of the Turonian an anoxic event took place which is called the Cenomanian-Turonian boundary event or the Bonarelli Event, the Turonian was defined by the French paleontologist Alcide dOrbigny in 1842. Orbigny named it after the French city of Tours in the region of Touraine, the base of the Turonian stage is defined as the place where the ammonite species Wutinoceras devonense first appears in the stratigraphic column. The official reference profile for the base of the Turonian is located in the Rock Canyon anticline near Pueblo, the top of the Turonian stage is defined as the place in the stratigraphic column where the inoceramid bivalve species Cremnoceramus rotundatus first appears. The Turonian is sometimes subdivided in Lower/Early, Middle and Upper/Late substages or subages, inoceramids are bivalve Mollusca related to todays mussels. & Smith, A. G.2004, A Geologic Time Scale 2004, & Cobban, W. A.2005, The Global Boundary Stratotype Section and Point for the base of the Turonian Stage of the Cretaceous, Pueblo, Colorado, U. S. A
6.
Intertidal zone
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The intertidal zone, also known as the foreshore and seashore and sometimes referred to as the littoral zone, is the area that is above water at low tide and under water at high tide. This area can include different types of habitats, with many types of animals, such as starfish, sea urchins. The well-known area also includes rocky cliffs, sandy beaches. The area can be a strip, as in Pacific islands that have only a narrow tidal range. Organisms in the zone are adapted to an environment of harsh extremes. The intertidal zone is home to many several species from different taxa including Porifera, Annelids, Coelenterates, Mollusks, crustaceans, Arthropods. Water is available regularly with the tides but varies from fresh with rain to highly saline, wave splash can dislodge residents from the littoral zone. With the intertidal zones high exposure to the sun, the range can be anything from very hot with full sun to near freezing in colder climates. Some microclimates in the zone are ameliorated by local features. Adaptation in the littoral zone allows the use of nutrients supplied in high volume on a basis from the sea. Edges of habitats, in this land and sea, are themselves often significant ecologies. Along most shores, the zone can be clearly separated into the following subzones, high tide zone, middle tide zone. The intertidal zone is one of a number of biomes or habitats, including estuaries, neritic, surface. Marine biologists divide the region into three zones, based on the overall average exposure of the zone. The low intertidal zone, which borders on the shallow subtidal zone, is exposed to air at the lowest of low tides and is primarily marine in character. The mid intertidal zone is exposed and submerged by average tides. The high intertidal zone is covered by the highest of the high tides. The high intertidal zone borders on the splash zone, on shores exposed to heavy wave action, the intertidal zone will be influenced by waves, as the spray from breaking waves will extend the intertidal zone
7.
Littoral zone
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The littoral zone is the part of a sea, lake or river that is close to the shore. In coastal environments the littoral zone extends from the water mark. It always includes this intertidal zone and is used to mean the same as the intertidal zone. However, the meaning of littoral zone can extend well beyond the intertidal zone, what is regarded as the full extent of the littoral zone, and the way the littoral zone is divided into subregions, varies in different contexts. The use of the term varies from one part of the world to another. For example, military commanders speak of the littoral in ways that are different from marine biologists. The adjacency of water gives a number of characteristics to littoral regions. The erosive power of water results in particular types of landforms, such as sand dunes, the natural movement of the littoral along the coast is called the littoral drift. Biologically, the availability of water enables a greater variety of plant and animal life. In addition, the local humidity due to evaporation usually creates a microclimate supporting unique types of organisms. The word littoral is used both as a noun and an adjective and it derives from the Latin noun litus, litoris, meaning shore. In oceanography and marine biology, the idea of the zone is extended roughly to the edge of the continental shelf. Starting from the shoreline, the zone begins at the spray region just above the high tide mark. From here, it moves to the region between the high and low water marks, and then out as far as the edge of the continental shelf. These three subregions are called, in order, the zone, the eulittoral zone and the sublittoral zone. The supralittoral zone is the area above the high tide line that is regularly splashed. Seawater penetrates these elevated areas only during storms with high tides, organisms here must cope also with exposure to fresh water from rain, cold, heat and predation by land animals and seabirds. At the top of this area, patches of dark lichens can appear as crusts on rocks, some types of periwinkles, Neritidae and detritus feeding Isopoda commonly inhabit the lower supralittoral
8.
Shoal
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Often it 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 and or present sedimentary and hydrographic processes are referred to as a shoal complex. The term shoal is also used in a number of ways that can be similar or quite different from how it is used in the geologic, geomorphic. Shoals are characteristically long and narrow ridges and they can develop where a stream, river, or ocean current promotes deposition of sediment and granular material, resulting in localized shallowing of the water. Marine shoals also develop either by the in place drowning of barrier islands as the result of sea level rise or by the erosion. Shoals can appear as a coastal landform in the sea, where they are classified as a type of bank, or as fluvial landforms in rivers, streams. A shoal–sandbar may seasonally separate a smaller body of water from the sea, such as, Marine lagoons Brackish water estuaries Freshwater seasonal stream and river mouths and deltas. They are typically composed of sand, although they could be of any matter that the moving water has access to and is capable of shifting around. Wave shoaling is the process when surface waves move towards shallow water, such as a beach, they slow down, their wave height increases and this behavior is called shoaling, and the waves are said to shoal. The waves may or may not build to the point where they break, depending on how large they were to begin with, in particular, waves shoal as they pass over submerged sandbanks or reefs. This can be treacherous for boats and ships, shoaling can also diffract waves, so the waves change direction. For example, if waves pass over a bank which is shallower at one end than the other. Thus the wave fronts will refract, changing direction like light passing through a prism, refraction also occurs as waves move towards a beach if the waves come in at an angle to the beach, or if the beach slopes more gradually at one end than the other. Sandbars, also known as a trough bars, form where the waves are breaking, sometimes this occurs seaward of a trough. Sand carried by the moving bottom current is deposited where the current reaches the wave break. Other longshore bars may lie further offshore, representing the point of even larger waves. A harbor or river bar is a sedimentary deposit formed at an entrance or river mouth by. Where beaches are suitably mobile, or the river’s suspended and/or bed loads are large enough, deposition can build up a sandbar that completely blocks a river mouth and damming the river
9.
Beni Suef
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Beni Suef, is the capital city of the Beni Suef Governorate in Egypt. Beni Suef is an important agricultural center, which grew from a village at the turn of the century. It was famous for its manufacturing in the Middle Ages. It is also known for its alabaster, quarried in the nearby hills, Beni Suef is located about 115 km south of Cairo. The Meidum Pyramid and Fayum Oasis are nearby, Beni Suef is known for its large mansions, including the Ismail Mansion, owned by General Ahmed Mamdouh Ismail. Beni Suef University and the private Al Nahda University are located in Beni Suef, Beni Suef has a hot desert climate in Köppen-Geiger classification, as does all of Egypt. It has very hot summers and warm winters with cool nights, a train accident in 1995 near Beni Suef left 75 people dead. The Beni Suef Cultural Palace Fire, on September 5,2005, berlenti Abdul Hamid, actress Telephonat Bani Sweif football team has been promoted for the first time in the Egyptian Premier League for the 2011/2012 season. Sannur Cave national park Bishop Athanasius The Daughters of St. Mary Falling Rain Genomics, Inc
10.
Memphis, Egypt
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Memphis was the ancient capital of Aneb-Hetch, the first nome of Lower Egypt. Its ruins are located near the town of Mit Rahina,20 km south of Giza, according to legend related by Manetho, the city was founded by the pharaoh Menes. Capital of Egypt during the Old Kingdom, it remained an important city throughout ancient Mediterranean history and it occupied a strategic position at the mouth of the Nile delta, and was home to feverish activity. Its principal port, Peru-nefer, harboured a high density of workshops, factories, during its golden age, Memphis thrived as a regional centre for commerce, trade, and religion. Memphis was believed to be under the protection of the god Ptah and its great temple, Hut-ka-Ptah, was one of the most prominent structures in the city. The name of temple, rendered in Greek as Aί γυ πτoς by the historian Manetho, is believed to be the etymological origin of the modern English name Egypt. The history of Memphis is closely linked to that of the country itself and its eventual downfall is believed to be due to the loss of its economic significance in late antiquity, following the rise of coastal Alexandria. Its religious significance also diminished after the abandonment of the ancient religion following the Edict of Thessalonica, the ruins of the former capital today offer fragmented evidence of its past. They have been preserved, along with the complex at Giza. The site is open to the public as an open-air museum, Memphis has had several names during its history of almost four millennia. Its Ancient Egyptian name was Inbu-Hedj, because of its size, the city also came to be known by various other names that were actually the names of neighbourhoods or districts that enjoyed considerable prominence at one time or another. For example, according to a text of the First Intermediate Period, it was known as Djed-Sut, the city was also at one point referred to as Ankh-Tawy, stressing the strategic position of the city between Upper and Lower Egypt. This name appears to date from the Middle Kingdom, and is found in ancient Egyptian texts. At the beginning of the New Kingdom, the city known as Men-nefer. The name Memphis is the Greek adaptation of this name, which was originally the name of the pyramid of Pepi I, in the Bible, Memphis is called Moph or Noph. The city of Memphis is 20 km south of Cairo, on the west bank of the Nile. The modern cities and towns of Mit Rahina, Dahshur, Abusir, Abu Gorab, the city was also the place that marked the boundary between Upper and Lower Egypt. The island of the city is today uninhabited, the closest settlement is the town of Mit Rahina
