1.
Federation of Damanhur
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The Federation of Damanhur, often called simply Damanhur, is a commune, ecovillage, and spiritual community situated in the Piedmont region of northern Italy about 30 miles north of the city of Turin. It is located in the foothills of the Alps in the Chiusella Valley, the community has its own constitution and currency, the Credito. Damanhur is named after the Egyptian city of Damanhur which was the site of a dedicated to Horus. It was founded in 1975 by Oberto Airaudi with around 24 followers, the group holds a mix of New Age and neopagan beliefs. They gained fame in 1992 through the disclosure of their excavation of an extensive underground temple, the Temples of Humankind. The Italian authorities ordered construction work to stop because it had been constructed without planning approval, damanhurs supporters claim the growth and activity of the community has revitalized the local area. The Federation of Damanhur has centers in Europe, America, the constitution began with 3 bodies of Damanhur, The School of Meditation Social and The Game of Life. A fourth body was added, Technarcate. Citizens participate in one of 4 levels, depending on their involvement, A, B, C. Class A citizens share all resources and live on site full-time, class B citizens contribute to financial goals and live on site a minimum of 3 days a week. Class C and D citizens live anywhere, class A & B citizens participate fully in The School of Meditation, Social, and the Game of Life. Class C citizens participate fully in The School of Meditation, citizens participate in one of several ways, depending on their personal nature. Ways include the Way of the Oracle, the Way of the Monk, the Way of the Knight, the Way of Health, the Way of the Word, the Way of Art & Work, and many others. Most citizens live in houses of 10-20 people each, federated together into the Federation of Damanhur, marriage works on a renewal basis, for a period of so many years before renewal. Conception is timed for auspicious birthdays of children, Damanhur, The Story of the Extraordinary Italian Artistic Community. Atlantis in the Mountains of Italy, archived from the original on 2010-08-21
2.
Egypt
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Egypt, officially the Arab Republic of Egypt, is a transcontinental country spanning the northeast corner of Africa and southwest corner of Asia by a land bridge formed by the Sinai Peninsula. Egypt is a Mediterranean country bordered by the Gaza Strip and Israel to the northeast, the Gulf of Aqaba to the east, the Red Sea to the east and south, Sudan to the south, and Libya to the west. Across the Gulf of Aqaba lies Jordan, and across from the Sinai Peninsula lies Saudi Arabia, although Jordan and it is the worlds only contiguous Afrasian nation. Egypt has among the longest histories of any country, emerging as one of the worlds first nation states in the tenth millennium BC. Considered a cradle of civilisation, Ancient Egypt experienced some of the earliest developments of writing, agriculture, urbanisation, organised religion and central government. One of the earliest centres of Christianity, Egypt was Islamised in the century and remains a predominantly Muslim country. With over 92 million inhabitants, Egypt is the most populous country in North Africa and the Arab world, the third-most populous in Africa, and the fifteenth-most populous in the world. The great majority of its people live near the banks of the Nile River, an area of about 40,000 square kilometres, the large regions of the Sahara desert, which constitute most of Egypts territory, are sparsely inhabited. About half of Egypts residents live in areas, with most spread across the densely populated centres of greater Cairo, Alexandria. Modern Egypt is considered to be a regional and middle power, with significant cultural, political, and military influence in North Africa, the Middle East and the Muslim world. Egypts economy is one of the largest and most diversified in the Middle East, Egypt is a member of the United Nations, Non-Aligned Movement, Arab League, African Union, and Organisation of Islamic Cooperation. Miṣr is the Classical Quranic Arabic and modern name of Egypt. The name is of Semitic origin, directly cognate with other Semitic words for Egypt such as the Hebrew מִצְרַיִם, the oldest attestation of this name for Egypt is the Akkadian
3.
Governorates of Egypt
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Governorates are the first-level of the subdivisions. Egypt is divided, for administrative purposes, into twenty-seven governorates, egyptian governorates are the top tier of the countrys jurisdiction hierarchy. A governorate is administered by a governor, who is appointed by the President of Egypt, most governorates have a population density of more than one thousand per km², while the three largest have a population density of less than two per km². Governorates are either fully urban or else a mixture of urban, the official distinction between urban and rural is reflected in the lower tiers, i. e. fully urban governorates have no regions, as the markaz is, natively, a conglomeration of villages. Moreover, governorates may comprise just one city, as in the case of Cairo Governorate or Alexandria Governorate, hence, these one-city governorates are only divided into districts. Cairo Governorate consists of 41 districts, Alexandria Governorate consists of 7, two new governorates were created in April 2008, Helwan and 6th of October. In April 2011, however, the 6th of October and Helwan governorates were again incorporated into the Cairo and Giza Governorates, respectively. Luxor was created in December 2009, to be the 29th governorate of Egypt, but with the abolition of the 6th of October and Helwan governorates, before 1979, local government traditionally enjoyed limited power in Egypts highly centralized state. Under the central government, there were twenty-six governorates and these were subdivided into regions, each of which was further subdivided into towns or villages. At each level, there was a structure that combined representative councils and government-appointed executive organs headed by governors, district officers. Governors were appointed by the president, and they, in turn, the coercive backbone of the state apparatus ran downward from the Ministry of Interior through the governors executive organs to the district police station and the village headman. Before the 1952 revolution, state penetration of the areas was limited by the power of local notables. However, under Nasser, land reform reduced their socioeconomic dominance, the extension of officials into the countryside permitted the regime to bring development and services to the village. State penetration did not retreat under Sadat and Mubarak, the earlier effort to mobilize peasants and deliver services disappeared as the local party and cooperative withered, but administrative controls over the peasants remained intact. The local power of the old families and the headmen revived, the district police station balanced the notables, and the system of local government integrated them into the regime. Sadat took several measures to decentralize power to the provinces and towns, governors acquired more authority under Law Number 43 of 1979, which reduced the administrative and budgetary controls of the central government over the provinces. The elected councils acquired, at least formally, the right to approve or disapprove the local budget, in an effort to reduce local demands on the central treasury, local government was given wider powers to raise local taxes. Local representative councils became vehicles of pressure for government spending, under Mubarak decentralization and local autonomy became more of a reality, and local policies often reflected special local conditions
4.
Beheira Governorate
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Beheira Governorate is a coastal governorate in Egypt. Located in the part of the country in the Nile Delta. Beheira Governorate enjoys an important strategical place, west of the Rosetta branch of the Nile and it comprises four important highways, namely the Cairo-Alexandria desert road, the Cairo agricultural road, the international road and the circular road. Beheira Governorate is also home to a number of the most important Coptic monasteries in Wadi El Natrun, beheira consists of 13 centers and 14 cities, and contains important industries such as cotton, chemicals, carpets, electricity and fishing. In 2017, Egyptian President Abdel Fattah al-Sissi appointed the first female governor in the history for Beheiras Governorate. According to population estimates from 2015 the majority of residents in the live in rural areas. Out of an estimated 5,804,262 people residing in the governorate,4,674,346 people live in areas as opposed to only 1,129,916 in urban areas
5.
Eastern European Time
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Eastern European Time is one of the names of UTC+02,00 time zone,2 hours ahead of Coordinated Universal Time. The zone uses daylight saving time, so that it uses UTC+03,00 during the summer, a number of African countries use UTC+02,00 all year long, where it is called Central Africa Time, although Egypt and Libya also use the term Eastern European Time. The following countries, parts of countries, and territories use Eastern European Time all year round, Egypt, since 21 April 2015, used EEST from 1988–2010, Kaliningrad Oblast, since 26 October 2014, also used EET in years 1945 and 1991–2011. Libya, since 27 October 2013, switched from Central European Time, used year-round EET from 1980–1981, 1990–1996 and 1998–2012. Belarus, in years 1922–30 and 1990–2011 In Poland this time was used in years 1918–22, in time of World War II, Germany implemented MET in east occupied territories. Republic of Crimea and Sevastopol used EET as part of Ukraine in years 1991-94 and 1996-2014 Turkey, used EET in years 1910-1978, now uses year round DST timezone called Further-eastern European Time or Turkey Time. The Turkish Republic of Northern Cyprus also uses FET, sometimes, due to its use on Microsoft Windows, FLE Standard Time or GTB Standard Time are used to refer to Eastern European Time. Since political, in addition to geographical, criteria are used in the drawing of time zones. The EET time zone, were it drawn by purely geographical terms, the easternmost part of the Republic of Macedonia, including the city of Strumica. The absolutely easternmost part of Serbia, in the Pirot District, the easternmost town in Norway, Vardø, lies at 30°51 E, which is located east of even of the central meridian of UTC+2, i. e. east of Istanbul and Alexandria. The Norwegian-Russian border is the place where CET borders Moscow time. There is a point at the Norway-Finland-Russia tripoint, near the town of Rayakoski. Belarus is located between 23°11′E and 32°47′E and is fully located with the physical UTC+2 area, but it uses UTC+3 year around. This also includes the city of Anapa, at the westernmost tip of the Krasnodar Krai near the entrance to the Sea of Azov, the Norway–Russia–Finland tri-zone point at Muotkavaara is surrounded by three different times in winter, two in summer. It had three time zones year-around before 2014, two of the four tripoints of Belarus and the tripoint of the Kaliningrad Region are surrounded by three different times in winter
6.
Egyptian language
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The language spoken in ancient Egypt was a branch of the Afroasiatic language family. The earliest known complete sentence in the Egyptian language has been dated to about 2690 BCE, making it one of the oldest recorded languages known. Egyptian was spoken until the seventeenth century in the form of Coptic. The national language of modern Egypt is Egyptian Arabic, which gradually replaced Coptic as the language of life in the centuries after the Muslim conquest of Egypt. Coptic is still used as the language of the Coptic Orthodox Church of Alexandria. It has several hundred fluent speakers today, the Egyptian language belongs to the Afroasiatic language family. Of the other Afroasiatic branches, Egyptian shows its greatest affinities with Semitic, in Egyptian, the Proto-Afroasiatic voiced consonants */d z ð/ developed into pharyngeal ⟨ꜥ⟩ /ʕ/, e. g. Eg. Afroasiatic */l/ merged with Egyptian ⟨n⟩, ⟨r⟩, ⟨ꜣ⟩, and ⟨j⟩ in the dialect on which the language was based. Original */k g ḳ/ palatalize to ⟨ṯ j ḏ⟩ in some environments and are preserved as ⟨k g q⟩ in others, Egyptian has many biradical and perhaps monoradical roots, in contrast to the Semitic preference for triradical roots. Egyptian probably is more archaic in this regard, whereas Semitic likely underwent later regularizations converting roots into the triradical pattern, scholars group the Egyptian language into six major chronological divisions, Archaic Egyptian language Old Egyptian language Middle Egyptian language, characterizing Middle Kingdom. Demotic Coptic The earliest Egyptian glyphs date back to around 3300 BC and these early texts are generally lumped together under the general term Archaic Egyptian. They record names, titles and labels, but a few of them show morphological and syntactic features familiar from later, more complete, Old Egyptian is dated from the oldest known complete sentence, found in the tomb of Seth-Peribsen and dated to around 2690 BCE. It reads, dmḏ. n. f t3wj n z3. f nswt-bjt pr-jb. snj He has united the Two Lands for his son, extensive texts appear from about 2600 BCE. Demotic first appears about 650 BCE and survived as a written language until the fifth century CE and it probably survived in the Egyptian countryside as a spoken language for several centuries after that. Bohairic Coptic is still used by the Coptic Churches, Old, Middle, and Late Egyptian were all written using hieroglyphs and hieratic. Demotic was written using a script derived from hieratic, its appearance is similar to modern Arabic script and is also written from right to left. Coptic is written using the Coptic alphabet, a form of the Greek alphabet with a number of symbols borrowed from Demotic for sounds that did not occur in ancient Greek. Arabic became the language of Egypts political administration soon after the early Muslim conquests in the seventh century, today, Coptic survives as the sacred language of the Coptic Orthodox Church of Alexandria and the Coptic Catholic Church
7.
Ancient Greek
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Ancient Greek includes the forms of Greek used in ancient Greece and the ancient world from around the 9th century BC to the 6th century AD. It is often divided into the Archaic period, Classical period. It is antedated in the second millennium BC by Mycenaean Greek, the language of the Hellenistic phase is known as Koine. Koine is regarded as a historical stage of its own, although in its earliest form it closely resembled Attic Greek. Prior to the Koine period, Greek of the classic and earlier periods included several regional dialects, Ancient Greek was the language of Homer and of fifth-century Athenian historians, playwrights, and philosophers. It has contributed many words to English vocabulary and has been a subject of study in educational institutions of the Western world since the Renaissance. This article primarily contains information about the Epic and Classical phases of the language, Ancient Greek was a pluricentric language, divided into many dialects. The main dialect groups are Attic and Ionic, Aeolic, Arcadocypriot, some dialects are found in standardized literary forms used in literature, while others are attested only in inscriptions. There are also several historical forms, homeric Greek is a literary form of Archaic Greek used in the epic poems, the Iliad and Odyssey, and in later poems by other authors. Homeric Greek had significant differences in grammar and pronunciation from Classical Attic, the origins, early form and development of the Hellenic language family are not well understood because of a lack of contemporaneous evidence. Several theories exist about what Hellenic dialect groups may have existed between the divergence of early Greek-like speech from the common Proto-Indo-European language and the Classical period and they have the same general outline, but differ in some of the detail. The invasion would not be Dorian unless the invaders had some relationship to the historical Dorians. The invasion is known to have displaced population to the later Attic-Ionic regions, the Greeks of this period believed there were three major divisions of all Greek people—Dorians, Aeolians, and Ionians, each with their own defining and distinctive dialects. Often non-west is called East Greek, Arcadocypriot apparently descended more closely from the Mycenaean Greek of the Bronze Age. Boeotian had come under a strong Northwest Greek influence, and can in some respects be considered a transitional dialect, thessalian likewise had come under Northwest Greek influence, though to a lesser degree. Most of the dialect sub-groups listed above had further subdivisions, generally equivalent to a city-state and its surrounding territory, Doric notably had several intermediate divisions as well, into Island Doric, Southern Peloponnesus Doric, and Northern Peloponnesus Doric. The Lesbian dialect was Aeolic Greek and this dialect slowly replaced most of the older dialects, although Doric dialect has survived in the Tsakonian language, which is spoken in the region of modern Sparta. Doric has also passed down its aorist terminations into most verbs of Demotic Greek, by about the 6th century AD, the Koine had slowly metamorphosized into Medieval Greek
8.
Cairo
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Cairo is the capital and largest city of Egypt. Cairo has long been a center of the political and cultural life. Cairo has the oldest and largest film and music industries in the Arab world, as well as the worlds second-oldest institution of higher learning, Al-Azhar University. Many international media, businesses, and organizations have regional headquarters in the city, with a population of 6.76 million spread over 453 square kilometers, Cairo is by far the largest city in Egypt. An additional 9.5 million inhabitants live in proximity to the city. Cairo, like many other mega-cities, suffers from high levels of pollution, Cairos metro, one of only two in Africa, ranks among the fifteen busiest in the world, with over 1 billion annual passenger rides. The economy of Cairo was ranked first in the Middle East in 2005, Egyptians often refer to Cairo as Maṣr, the Egyptian Arabic name for Egypt itself, emphasizing the citys importance for the country. In Coptic the city is known as Kahire, meaning Place of the Sun, possibly referring to the ancient city of Heliopolis, the location of the ancient city is the suburb of Ain Shams. The ancient Egyptian name for the area is thought to be Khere-Ohe, The Place of Combat, sometimes the city is informally referred to as Kayro. The area around present-day Cairo, especially Memphis, had long been a point of Ancient Egypt due to its strategic location just upstream from the Nile Delta. However, the origins of the city are generally traced back to a series of settlements in the first millennium. Around the turn of the 4th century, as Memphis was continuing to decline in importance and this fortress, known as Babylon, remained the nucleus of the Roman, and, later, the Byzantine, city and is the oldest structure in the city today. It is also situated at the nucleus of the Coptic Orthodox community, many of Cairos oldest Coptic churches, including the Hanging Church, are located along the fortress walls in a section of the city known as Coptic Cairo. Following the Muslim conquest in 640 AD the conqueror Amr ibn As settled to the north of the Babylon in an area became known as al-Fustat. Originally a tented camp Fustat became a permanent settlement and the first capital of Islamic Egypt, in 750, following the overthrow of the Ummayad caliphate by the Abbasids, the new rulers created their own settlement to the northeast of Fustat which became their capital. This was known as al-Askar as it was laid out like a military camp, a rebellion in 869 by Ahmad ibn Tulun led to the abandonment of Al Askar and the building of another settlement, which became the seat of government. This was al-Qattai, to the north of Fustat and closer to the river, Al Qattai was centred around a palace and ceremonial mosque, now known as the Mosque of ibn Tulun. In 905 the Abbasids re-asserted control of the country and their returned to Fustat
9.
Alexandria
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Alexandria is the second largest city and a major economic centre in Egypt, extending about 32 km along the coast of the Mediterranean Sea in the north central part of the country. Its low elevation on the Nile delta makes it vulnerable to rising sea levels. Alexandria is Egypts largest seaport, serving approximately 80% of Egypts imports and exports and it is an important industrial center because of its natural gas and oil pipelines from Suez. Alexandria is also an important tourist destination, Alexandria was founded around a small Ancient Egyptian town c.331 BC by Alexander the Great. Alexandria was the second most powerful city of the ancient world after Rome, Alexandria is believed to have been founded by Alexander the Great in April 331 BC as Ἀλεξάνδρεια. Alexanders chief architect for the project was Dinocrates, Alexandria was intended to supersede Naucratis as a Hellenistic center in Egypt, and to be the link between Greece and the rich Nile valley. The city and its museum attracted many of the greatest scholars, including Greeks, Jews, the city was later plundered and lost its significance. Just east of Alexandria, there was in ancient times marshland, as early as the 7th century BC, there existed important port cities of Canopus and Heracleion. The latter was rediscovered under water. An Egyptian city, Rhakotis, already existed on the shore also and it continued to exist as the Egyptian quarter of the city. A few months after the foundation, Alexander left Egypt and never returned to his city, after Alexanders departure, his viceroy, Cleomenes, continued the expansion. Although Cleomenes was mainly in charge of overseeing Alexandrias continuous development, the Heptastadion, inheriting the trade of ruined Tyre and becoming the center of the new commerce between Europe and the Arabian and Indian East, the city grew in less than a generation to be larger than Carthage. In a century, Alexandria had become the largest city in the world and and it became Egypts main Greek city, with Greek people from diverse backgrounds. Alexandria was not only a center of Hellenism, but was home to the largest urban Jewish community in the world. The Septuagint, a Greek version of the Tanakh, was produced there, in AD115, large parts of Alexandria were destroyed during the Kitos War, which gave Hadrian and his architect, Decriannus, an opportunity to rebuild it. On 21 July 365, Alexandria was devastated by a tsunami, the Islamic prophet, Muhammads first interaction with the people of Egypt occurred in 628, during the Expedition of Zaid ibn Haritha. He sent Hatib bin Abi Baltaeh with a letter to the king of Egypt and Alexandria called Muqawqis In the letter Muhammad said, I invite you to accept Islam, Allah the sublime, shall reward you doubly. But if you refuse to do so, you bear the burden of the transgression of all the Copts
10.
Nile Delta
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The Nile Delta is the delta formed in Northern Egypt where the Nile River spreads out and drains into the Mediterranean Sea. It is one of the worlds largest river deltas—from Alexandria in the west to Port Said in the east, from north to south the delta is approximately 160 kilometres in length. The Delta begins slightly down-river from Cairo, from north to south, the delta is approximately 160 kilometres in length. From west-to-east, it covers some 240 kilometres of coastline, the delta is sometimes divided into sections, with the Nile dividing into two main distributaries, the Damietta and the Rosetta, flowing into the Mediterranean at port cities with the same name. In the past, the delta had several distributaries, but these have been lost due to flood control, one such defunct distributary is Wadi Tumilat. The Suez Canal runs to the east of the delta, entering the coastal Lake Manzala in the north-east of the delta, to the north-west are three other coastal lakes or lagoons, Lake Burullus, Lake Idku and Lake Maryut. The Nile is considered to be a delta, as it resembles a triangle or flower when seen from above. The outer edges of the delta are eroding, and some coastal lagoons have seen increasing salinity levels as their connection to the Mediterranean Sea increases, topsoil in the delta can be as much as 70 feet in depth. People have lived in the Delta region for thousands of years, the Delta River used to flood on an annual basis, but this ended with the construction of the Aswan Dam. The Rosetta Stone was found in the Nile Delta in 1799 in the city of Rosetta. The delta was a constituent of Lower Egypt. The Biblical Land of Goshen was located in an area on the west bank of the Pelusiac distributary. There are many sites in and around the Nile Delta. About 39 million people live in the Delta region, outside of major cities, population density in the delta averages 1,000 persons/km² or more. Alexandria is the largest city in the delta with a population of more than 4.5 million. Other large cities in the delta include Shubra al Khaymah, Port Said, El-Mahalla El-Kubra, El Mansura, Tanta, during autumn, parts of the Nile River are red with lotus flowers. The Lower Nile and the Upper Nile have plants that grow in abundance, the Upper Nile plant is the Egyptian lotus, and the Lower Nile plant is the Papyrus Sedge, although it is not nearly as plentiful as it once was, and is becoming quite rare. Several hundred thousand birds winter in the delta, including the world’s largest concentrations of little gulls
11.
Ancient Egypt
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Ancient Egypt was a civilization of ancient Northeastern Africa, concentrated along the lower reaches of the Nile River in what is now the modern country of Egypt. It is one of six civilizations to arise independently, Egyptian civilization followed prehistoric Egypt and coalesced around 3150 BC with the political unification of Upper and Lower Egypt under the first pharaoh Narmer. In the aftermath of Alexander the Greats death, one of his generals, Ptolemy Soter and this Greek Ptolemaic Kingdom ruled Egypt until 30 BC, when, under Cleopatra, it fell to the Roman Empire and became a Roman province. The success of ancient Egyptian civilization came partly from its ability to adapt to the conditions of the Nile River valley for agriculture, the predictable flooding and controlled irrigation of the fertile valley produced surplus crops, which supported a more dense population, and social development and culture. Its art and architecture were widely copied, and its antiquities carried off to far corners of the world and its monumental ruins have inspired the imaginations of travelers and writers for centuries. The Nile has been the lifeline of its region for much of human history, nomadic modern human hunter-gatherers began living in the Nile valley through the end of the Middle Pleistocene some 120,000 years ago. By the late Paleolithic period, the climate of Northern Africa became increasingly hot and dry. In Predynastic and Early Dynastic times, the Egyptian climate was less arid than it is today. Large regions of Egypt were covered in treed savanna and traversed by herds of grazing ungulates, foliage and fauna were far more prolific in all environs and the Nile region supported large populations of waterfowl. Hunting would have been common for Egyptians, and this is also the period when many animals were first domesticated. The largest of these cultures in upper Egypt was the Badari, which probably originated in the Western Desert, it was known for its high quality ceramics, stone tools. The Badari was followed by the Amratian and Gerzeh cultures, which brought a number of technological improvements, as early as the Naqada I Period, predynastic Egyptians imported obsidian from Ethiopia, used to shape blades and other objects from flakes. In Naqada II times, early evidence exists of contact with the Near East, particularly Canaan, establishing a power center at Hierakonpolis, and later at Abydos, Naqada III leaders expanded their control of Egypt northwards along the Nile. They also traded with Nubia to the south, the oases of the desert to the west. Royal Nubian burials at Qustul produced artifacts bearing the oldest-known examples of Egyptian dynastic symbols, such as the crown of Egypt. They also developed a ceramic glaze known as faience, which was used well into the Roman Period to decorate cups, amulets, and figurines. During the last predynastic phase, the Naqada culture began using written symbols that eventually were developed into a system of hieroglyphs for writing the ancient Egyptian language. The Early Dynastic Period was approximately contemporary to the early Sumerian-Akkadian civilisation of Mesopotamia, the third-century BC Egyptian priest Manetho grouped the long line of pharaohs from Menes to his own time into 30 dynasties, a system still used today
12.
Nome (Egypt)
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A nome was a subnational administrative division of Ancient Egypt. Todays use of the Greek νομή, nomé rather than the Egyptian term sepat came about during the Ptolemaic period, the availability of Greek records on Egypt influenced the adoption of Greek terms by later historians. The division of ancient Egypt into nomes can be traced back to the Predynastic Period and these nomes originally existed as autonomous city-states, but later began to unify. According to ancient tradition, the ruler Menes completed the final unification, not only did the division into nomes remain in place for more than three millennia, the areas of the individual nomes and their ordering remained remarkably stable. Some, like Xois in the Delta or Khent in Upper Egypt, were first mentioned on the Palermo stone, the names of a few, like the nome of Bubastis, appeared no earlier than the New Kingdom. Under the system that prevailed for most of pharaonic Egypts history, lower Egypt, from the Old Kingdom capital Memphis to the Mediterranean Sea, comprised 20 nomes. The first was based around Memphis, Saqqara, and Giza, the nomes were numbered in a more or less orderly fashion south to north through the Nile delta, first covering the territory on the west before continuing with the higher numbers to the east. Thus, Alexandria was in the Third Nome, Bubastis was in the Eighteenth, Upper Egypt was divided into 22 nomes. The first of these was centered on Elephantine close to Egypts border with Nubia at the First Cataract – the area of modern-day Aswan, from there the numbering progressed downriver in an orderly fashion along the narrow fertile strip of land that was the Nile valley. Waset was in the Fourth Nome, Amarna in the Fourteenth, some nomes were added or renamed during the Graeco-Roman occupation of Egypt. For example, the Ptolemies renamed the Crocodilopolitan nome to Arsinoe, hadrian created a new nome, Antinoopolites, for which Antinoopolis was the capital. The nomes survived into Roman times, under Roman rule, individual nomes minted their own coinage, the so-called nome coins, which still reflect individual local associations and traditions. The nomes of Egypt retained their importance as administrative units until the fundamental rearrangement of the bureaucracy during the reigns of Diocletian. From AD 307/8, their place was taken by units called pagi. Eventually powerful local officials arose who were called pagarchs, through whom all patronage flowed, the pagarchs essential role was as an organizer of tax-collection. Later the pagarch assumed some military functions as well, the pagarchs were often wealthy landowners who reigned over the pagi from which they originated. For most of the history, each nome was headed by a nomarch, the position of the nomarch was at times hereditary, while at others they were appointed by the pharaoh. Generally, when the government was stronger, nomarchs were the kings appointed governors
13.
Mareotis
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Lake Mariout, also spelled Maryut or Mariut, is a brackish lake in northern Egypt. The lake area covered 200 km² and had a canal at the beginning of the 20th century. The name derives from Mareotis or Marea, the name of the lake in ancient times and it is separated from the Mediterranean Sea by the narrow isthmus on which the city of Alexandria was built. The lake shore is home to fisheries and saltworks, as far back as the early 1900s, it was documented that salt was being refined from the western part of the lake. Some of the areas around the lake have been reclaimed for new building as the city grows. According to some records, a homonymous nome was located on the shores of this lake, the diocese was nominally restored in 1933 as Titular bishopric of Mareotes / Mareotes / Mareoten. Although technically a Latin titular see, it has had several Eastern Catholic incumbents, in 2015 a stele, resembling the Rosetta Stone and dating back some 2,200 years, was discovered in ancient ruins called Taposiris Magna Temple site at Lake Mariout. Measuring 41 inches by 25.6 inches by 7 inches, there are ancient tombs located on the shores of the lake. The fish species Nile perch lives in the lake, although it principally needs fresh water to live in, in 1939, a small lake, called the Nozha Hydrodrome was isolated from Lake Mariout and this allowed for the Nile perch to flourish there. List of Catholic dioceses in Egypt GCatholic Bishopric of Mareotes
14.
Canopus, Egypt
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Canopus, also known as Canobus, was an Ancient Egyptian coastal town, located in the Nile Delta. Its site is in the outskirts of modern-day Alexandria, around 25 kilometers from the center of that city. Canopus was located on the bank at the mouth of the westernmost branch of the Delta – known as the Canopic or Heracleotic branch. It belonged to the seventh Egyptian Nome, known as Menelaites and it was the principal port in Egypt for Greek trade before the foundation of Alexandria, along with Naucratis and Heracleion. Its ruins lie near the present Egyptian village of Abu Qir, the settlements Egyptian name was Peguat or Pikuat. The Greeks called it Canopus after a commander of the era of the Trojan War supposedly buried there. The English form of the name derives from the Latinized form used under Roman rule, Canopus was the site of a temple to the Egyptian god Serapis. The name of Canopus appears in the first half of the 6th century BC in a poem by Solon, the exact date of the foundation of Canopus is unknown, but Herodotus refers to it as an ancient port. Homeric myth claims that it was founded by Menelaus, and named after Canopus, the pilot of his ship, legend describes how Menelaus built a monument to his memory on the shore, around which the town later grew up. The real origin of the name Canopus is said to be Ancient Egyptian Kah Nub, there is unlikely to be any connection with canopy. A temple to Osiris was built by Pharaoh Ptolemy The Good, but, according to Herodotus, very near to Canopus was an older shrine, Osiris was worshipped at Canopus under a peculiar form, that of a vase with a human head. In Ptolemy III Euergetes ninth regnal year, an assembly of priests at Canopus passed an honorific decree that, inter alia, conferred various new titles on the king and his consort. This was the earliest of the series of inscriptions of the Rosetta Stone Series. There are three such Decrees altogether, the town had a large trade in henna. In Roman times, the town was notorious for its dissoluteness, juvenals Satire VI referred to the debauchery that prevailed there. The emperor Hadrian built a villa at Tivoli,18 miles away from Rome, one of these was borrowed from Canopus. The Egyptian city of Abu Qir, honoring two Christian martyrs, is located a few miles away from the ruins of Canopus and it is a village, at the end of a little peninsula north-east of Alexandria. It has a trade in quails, which are caught in nets hung along the shore, off Aboukir on 1 August 1798, the French Mediterranean fleet was destroyed within the roads by British Admiral Horatio Nelson on 25 July 1799
15.
Nile
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The Nile is a major north-flowing river in northeastern Africa. It is generally regarded as the longest river in the world, in particular, the Nile is the primary water source of Egypt and Sudan. The Nile has two tributaries, the White Nile and Blue Nile. The White Nile is considered to be the headwaters and primary stream of the Nile itself, the Blue Nile, however, is the source of most of the water and silt. The White Nile is longer and rises in the Great Lakes region of central Africa and it flows north through Tanzania, Lake Victoria, Uganda and South Sudan. The Blue Nile begins at Lake Tana in Ethiopia and flows into Sudan from the southeast, the two rivers meet just north of the Sudanese capital of Khartoum. The northern section of the river flows north almost entirely through the Sudanese desert to Egypt, then ends in a large delta, Egyptian civilization and Sudanese kingdoms have depended on the river since ancient times. Most of the population and cities of Egypt lie along those parts of the Nile valley north of Aswan, in the ancient Egyptian language, the Nile is called Ḥpī or Iteru, meaning river. In Coptic, the words piaro or phiaro meaning the river come from the ancient name. The English name Nile and the Arabic names en-Nîl and an-Nîl both derive from the Latin Nilus and the Ancient Greek Νεῖλος, beyond that, however, the etymology is disputed. One possible etymology derives it from a Semitic Nahal, meaning river, the standard English names White Nile and Blue Nile, to refer to the rivers source, derive from Arabic names formerly applied only to the Sudanese stretches which meet at Khartoum. Above Khartoum, the Nile is also known as the White Nile, at Khartoum the river is joined by the Blue Nile. The White Nile starts in equatorial East Africa, and the Blue Nile begins in Ethiopia, both branches are on the western flanks of the East African Rift. The drainage basin of the Nile covers 3,254,555 square kilometers, the source of the Nile is sometimes considered to be Lake Victoria, but the lake has feeder rivers of considerable size. It is either the Ruvyironza, which emerges in Bururi Province, Burundi, or the Nyabarongo, the two feeder rivers meet near Rusumo Falls on the Rwanda-Tanzania border. Gish Abay is reportedly the place where the water of the first drops of the Blue Nile develop. The Nile leaves Lake Nyanza at Ripon Falls near Jinja, Uganda and it flows north for some 130 kilometers, to Lake Kyoga. For the remaining part it flows westerly through the Murchison Falls until it reaches the very northern shores of Lake Albert where it forms a significant river delta
16.
Horus
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Horus is one of the most significant ancient Egyptian deities. He was worshipped from at least the late prehistoric Egypt until the Ptolemaic Kingdom, different forms of Horus are recorded in history and these are treated as distinct gods by Egyptologists. He was most often depicted as a falcon, most likely a falcon or peregrine falcon. In another tradition Hathor is regarded as his mother and sometimes as his wife, Horus served many functions, most notably being a god of the sky, war and hunting. Horus is recorded in Egyptian hieroglyphs as ḥr. w Falcon, additional meanings are thought to have been the distant one or one who is above, over. As the language changed over time, it appeared in Coptic dialects variously as hoːɾ or ħoːɾ and was adopted into ancient Greek as Ὧρος Hōros and it also survives in Late Egyptian and Coptic theophoric names such as Har-si-ese Horus, Son of Isis. Nekheny may have been another falcon god worshipped at Nekhen, city of the falcon, Horus may be shown as a falcon on the Narmer Palette, dating from about the 31st century BC. In early Egypt, Horus was the brother of Isis, Osiris, Set, as different cults formed, he became the son of Isis and Osiris. Isis remained the sister of Osiris, Set and Nephthys, the Pyramid Texts describe the nature of the pharaoh in different characters as both Horus and Osiris. The pharaoh as Horus in life became the pharaoh as Osiris in death, New incarnations of Horus succeeded the deceased pharaoh on earth in the form of new pharaohs. The lineage of Horus, the product of unions between the children of Atum, may have been a means to explain and justify pharaonic power. The gods produced by Atum were all representative of cosmic and terrestrial forces in Egyptian life, the notion of Horus as the pharaoh seems to have been superseded by the concept of the pharaoh as the son of Ra during the Fifth Dynasty. Once Isis knew she was pregnant with Horus, she fled to the Nile Delta marshlands to hide from her brother Set, who jealously killed Osiris, there Isis bore a divine son, Horus. Since Horus was said to be the sky, he was considered to contain the sun. It became said that the sun was his eye and the moon his left, and that they traversed the sky when he. Later, the reason that the moon was not as bright as the sun was explained by a tale, known as the The Contendings of Horus and Seth. As Horus was the victor he became known as ḥr. w wr Horus the Great. In the struggle, Set had lost a testicle, explaining why the desert, Horus left eye had also been gouged out, then a new eye was created by part of Khonsu, the moon god, and was replaced
17.
Hermes
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Hermes is an Olympian god in Greek religion and mythology, the son of Zeus and the Pleiad Maia, and the second youngest of the Olympian gods. Hermes is considered a god of transitions and boundaries and he is described as quick and cunning, moving freely between the worlds of the mortal and divine. He is also portrayed as an emissary and messenger of the gods and he has been viewed as the protector and patron of herdsmen, thieves, oratory and wit, literature and poetry, athletics and sports, invention and trade, roads, boundaries and travelers. In some myths, he is a trickster and outwits other gods for his own satisfaction or for the sake of humankind and his attributes and symbols include the herma, the rooster, the tortoise, satchel or pouch, winged sandals, and winged cap. His main symbol is the Greek kerykeion or Latin caduceus, which appears in a form of two snakes wrapped around a staff with carvings of the other gods. The earliest form of the name Hermes is the Mycenaean Greek *hermāhās, most scholars derive Hermes from Greek ἕρμα herma, prop, heap of stones, boundary marker, from which the word hermai also derives. The etymology of ἕρμα itself is unknown, R. S. P. Beekes rejects the connection with herma and suggests a Pre-Greek origin. Scholarly speculation that Hermes derives from a primitive form meaning one cairn is disputed. In Greek, a find is a hermaion. It is also suggested that Hermes is a cognate of the Vedic Sarama, homer and Hesiod portrayed Hermes as the author of skilled or deceptive acts and also as a benefactor of mortals. In the Iliad, he is called the bringer of luck, guide and guardian. He was an ally of the Greeks against the Trojans. However, he did protect Priam when he went to the Greek camp to retrieve the body of his son Hector and he also rescued Ares from a brazen vessel where he had been imprisoned by Otus and Ephialtes. In the Odyssey, Hermes helps his son, the protagonist Odysseus, by informing him about the fate of his companions. Hermes instructed Odysseus to protect himself by chewing a magic herb, when Odysseus killed the suitors of his wife, Hermes led their souls to Hades. Hermes was then instructed to take her as wife to Epimetheus, aesop featured him in several of his fables, as ruler of the gate of prophetic dreams, as the god of athletes, of edible roots, and of hospitality. He also said that Hermes had assigned each person his share of intelligence, Hermes, as an inventor of fire, is a parallel of the Titan Prometheus. In addition to the lyre, Hermes was believed to have invented many types of racing and the sports of wrestling and boxing, in 1820 Shelley translated this hymn
18.
Thoth
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Thoth or Djehuti was one of the deities of the Egyptian pantheon. In art, he was depicted as a man with the head of an ibis or a baboon. His feminine counterpart was Seshat, and his wife was Maat, Thoths chief temple was located in the city of Khmun, later called Hermopolis Magna during the Greco-Roman era and Shmounein in the Coptic rendering, and was partially destroyed in 1826 CE. In that city, he led the Ogdoad pantheon of eight principal deities and he also had numerous shrines within the cities of Abydos, Hesert, Urit, Per-Ab, Rekhui, Ta-ur, Sep, Hat, Pselket, Talmsis, Antcha-Mutet, Bah, Amen-heri-ab, and Ta-kens. Thoth played many vital and prominent roles in Egyptian mythology, such as maintaining the universe, the final -y may even have been pronounced as a consonant, not a vowel. According to Theodor Hopfner, Thoths Egyptian name written as ḏḥwty originated from ḏḥw, the addition of -ty denotes that he possessed the attributes of the ibis. Hence his name means He who is like the ibis, Djehuty is sometimes alternatively rendered as Jehuti, Jehuty, Tahuti, Tehuti, Zehuti, Techu, or Tetu. Greek versions Thot, Thout and Thoth are derived from the letters ḏḥwty, not counting differences in spelling, Thoth had many names and titles, like other goddesses and gods. Among the names used are A, Sheps, Lord of Khemennu, Asten, Khenti, Mehi, Hab, in addition, Thoth was also known by specific aspects of himself, for instance the moon god Iah-Djehuty, representing the Moon for the entire month. The Greeks related Thoth to their god Hermes due to his similar attributes, One of Thoths titles, Thrice great was translated to the Greek τρισμέγιστος, making Hermes Trismegistus. Thoth has been depicted in many ways depending on the era, usually, he is depicted in his human form with the head of an ibis. In this form, he can be represented as the reckoner of times, when depicted as a form of Shu or Ankher, he was depicted to be wearing the respective gods headdress. Sometimes he was seen in art to be wearing the Atef crown or the United Crowns of Upper and Lower Egypt. When not depicted in this form, he sometimes takes the form of the ibis directly. He also appears as a baboon or a man with the head of a baboon when he is Aan. In the form of Aah-Djehuty he took a more human-looking form and these forms are all symbolic and are metaphors for Thoths attributes. The Egyptians did not believe these gods actually looked like humans with animal heads, for example, Maat is often depicted with an ostrich feather, the feather of truth, on her head, or with a feather for a head. Thoths roles in Egyptian mythology were many and he served as a mediating power, especially between good and evil, making sure neither had a decisive victory over the other
19.
Stephanus of Byzantium
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Stephen of Byzantium, also known as Stephanus Byzantinus, was the author of an important geographical dictionary entitled Ethnica. Of the dictionary itself only meagre fragments survive, but we possess an epitome compiled by one Hermolaus, not otherwise identified. Nothing is known about the life of Stephanus, except that he was a grammarian at Constantinople, and lived after the time of Arcadius and Honorius, even as an epitome, the Ethnica is of enormous value for geographical, mythological, and religious information about ancient Greece. Nearly every article in the epitome contains a reference to some ancient writer, Stephanus cites Artemidorus, Polybius, Aelius Herodianus, Herodotus, Thucydides, Xenophon, Strabo and other writers. The chief fragments remaining of the work are preserved by Constantine Porphyrogennetos, De administrando imperio, ch.23 and De thematibus. 10, the latter includes a passage from the comic poet Alexis on the Seven Largest Islands, another respectable fragment, from the article Δύμη to the end of Δ, exists in a manuscript of the Fonds Coislin, the library formed by Pierre Séguier. The first modern printed edition of the work was published by the Aldine Press in Venice,1502. The complete standard edition is still that of Augustus Meineke, and by convention, a new completely revised edition in German is in preparation, however, edited by B. Zubler, M. Billerbeck, J. F. Gaertner,2006 onwards, google Books Guilielmus Xylander,1568, Στέφανος. Google Books Claudius Salmasius and Abraham van Berkel,1688, Στεφάνου Βυζαντίου Ἐθνικὰ κατ ἐπιτομήν Περὶ πόλεων = Stephani Byzantini Gentilia per epitomen, google Books Lucas Holstenius,1692, Notae & castigationes in Stephanum Byzantium De urbibus. Google Books Thomas de Pinedo,1725, Stephanus de urbibus, google Books Karl Wilhelm Dindorf,1825, Stephanus Byzantinus. Incorporating notes by L. Holsteinius, A. Berkelius, and T. de Pinedo, google Books Anton Westermann,1839, Stephani Byzantii ethnikon quae supersunt. Google Books Augustus Meineke,1849, Stephani Byzantii ethnicorum quae supersunt, google Books Margarethe Billerbeck et al. Berlin/New York, Walter de Gruyter, This article incorporates text from a now in the public domain, Chisholm, Hugh. Smith, W. Dictionary of Greek and Roman Biography and Mythology, diller, Aubrey 1938, The tradition of Stephanus Byzantius, Transactions of the American Philological Association 69, 333-48. Bunbury,1883, History of Ancient Geography, vol. i, Holstenius, L.1684, Lucae Holstenii Notae et castigationes postumae in Stephani Byzantii Ethnika, quae vulgo Peri poleōn inscribuntur. 1873, De Stephani Byzantii auctoribus Johannes Geffcken,1886, De Stephano Byzantio Whitehead, D.1994, From political architecture to Stephanus Byzantius, sources for the ancient Greek polis
20.
Strabo
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Strabo was a Greek geographer, philosopher, and historian who lived in Asia Minor during the transitional period of the Roman Republic into the Roman Empire. Strabo was born to an affluent family from Amaseia in Pontus, Strabos life was characterized by extensive travels. He journeyed to Egypt and Kush, as far west as coastal Tuscany and as far south as Ethiopia in addition to his travels in Asia Minor and the time he spent in Rome. Travel throughout the Mediterranean and Near East, especially for scholarly purposes, was popular during this era and was facilitated by the relative peace enjoyed throughout the reign of Augustus. He moved to Rome in 44 BC, and stayed there, studying and writing, in 29 BC, on his way to Corinth, he visited the island of Gyaros in the Aegean Sea. Around 25 BC, he sailed up the Nile until reaching Philae and it is not known precisely when Strabos Geography was written, though comments within the work itself place the finished version within the reign of Emperor Tiberius. Some place its first drafts around 7 BC, others around 17 or 18 AD, the latest passage to which a date can be assigned is his reference to the death in AD23 of Juba II, king of Maurousia, who is said to have died just recently. He probably worked on the Geography for many years and revised it steadily, on the presumption that recently means within a year, Strabo stopped writing that year or the next, when he died. The first of Strabos major works, Historical Sketches, written while he was in Rome, is completely lost. Strabo studied under several prominent teachers of various specialties throughout his life at different stops along his Mediterranean travels. His first chapter of education took place in Nysa under the master of rhetoric Aristodemus, Strabo was an admirer of Homers poetry, perhaps a consequence of his time spent in Nysa with Aristodemus. At around the age of 21, Strabo moved to Rome, where he studied philosophy with the Peripatetic Xenarchus, despite Xenarchuss Aristotelian leanings, Strabo later gives evidence to have formed his own Stoic inclinations. In Rome, he learned grammar under the rich and famous scholar Tyrannion of Amisus. Although Tyrannion was also a Peripatetic, he was more relevantly a respected authority on geography, the final noteworthy mentor to Strabo was Athenodorus Cananites, a philosopher who had spent his life since 44 BC in Rome forging relationships with the Roman elite. Athenodorus endowed to Strabo three important items, his philosophy, his knowledge, and his contacts, moreover, from his own first-hand experience, Athenodorus provided Strabo with information about regions of the empire which he would not otherwise have known. Strabo is most notable for his work Geographica, which presented a history of people. Although the Geographica was rarely utilized in its antiquity, a multitude of copies survived throughout the Byzantine Empire. It first appeared in Western Europe in Rome as a Latin translation issued around 1469, the first Greek edition was published in 1516 in Venice
21.
Ptolemy
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Claudius Ptolemy was a Greek writer, known as a mathematician, astronomer, geographer, astrologer, and poet of a single epigram in the Greek Anthology. He lived in the city of Alexandria in the Roman province of Egypt, wrote in Koine Greek, beyond that, few reliable details of his life are known. His birthplace has been given as Ptolemais Hermiou in the Thebaid in a statement by the 14th-century astronomer Theodore Meliteniotes. This is a very late attestation, however, and there is no reason to suppose that he ever lived elsewhere than Alexandria. Ptolemy wrote several treatises, three of which were of importance to later Byzantine, Islamic and European science. The first is the astronomical treatise now known as the Almagest, although it was entitled the Mathematical Treatise. The second is the Geography, which is a discussion of the geographic knowledge of the Greco-Roman world. The third is the treatise in which he attempted to adapt horoscopic astrology to the Aristotelian natural philosophy of his day. This is sometimes known as the Apotelesmatika but more known as the Tetrabiblos from the Greek meaning Four Books or by the Latin Quadripartitum. The name Claudius is a Roman nomen, the fact that Ptolemy bore it indicates he lived under the Roman rule of Egypt with the privileges and political rights of Roman citizenship. It would have suited custom if the first of Ptolemys family to become a citizen took the nomen from a Roman called Claudius who was responsible for granting citizenship, if, as was common, this was the emperor, citizenship would have been granted between AD41 and 68. The astronomer would also have had a praenomen, which remains unknown and it occurs once in Greek mythology, and is of Homeric form. All the kings after him, until Egypt became a Roman province in 30 BC, were also Ptolemies, abu Mashar recorded a belief that a different member of this royal line composed the book on astrology and attributed it to Ptolemy. The correct answer is not known”, Ptolemy wrote in Greek and can be shown to have utilized Babylonian astronomical data. He was a Roman citizen, but most scholars conclude that Ptolemy was ethnically Greek and he was often known in later Arabic sources as the Upper Egyptian, suggesting he may have had origins in southern Egypt. Later Arabic astronomers, geographers and physicists referred to him by his name in Arabic, Ptolemys Almagest is the only surviving comprehensive ancient treatise on astronomy. Ptolemy presented his models in convenient tables, which could be used to compute the future or past position of the planets. The Almagest also contains a catalogue, which is a version of a catalogue created by Hipparchus
22.
Antonine Itinerary
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The Antonine Itinerary is a famous itinerarium, a register of the stations and distances along various roads. Seemingly based on documents, possibly from a survey carried out under Augustus. Owing to the scarcity of other extant records of this type, almost nothing is known of its date or author. The British section is known as the Iter Britanniarum, and can be described as the map of Roman Britain. There are 15 such itineraries in the document applying to different geographic areas, the itinerary measures distances in Roman miles, where 1,000 Roman paces equals one Roman mile. A Roman pace was two steps, left plus right, Roman paces were not everywhere the same, and conversion to modern units is imprecise, but 1 Roman mile approximately equals 4,690 feet, or 1430 m. Below is the original Latin ablative forms for sites along route 13, a transcriber omitted an entry, so that the total number of paces does not equal the sum of paces between locations. Below is the original Latin for route 14 followed by a translation with a name for the modern site. Its authenticity was not seriously challenged until 1845, and it was cited as an authoritative source until the late nineteenth century. While the document is no longer cited, since its authenticity became indefensible, its data has not been removed from past. Some authors, such as Thomas Reynolds, without challenging the authenticity of the forgery, took care to note its discrepancies and this was not always so, even after the forgery was debunked. The Antonine Itinerary, Iter Britanniarum - The British Section Analysis of the Itinerary Itinerarium Antonini Augusti at SOLTDM. COM Roman Roads in Britain
23.
Roman Catholic
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The Catholic Church, also known as the Roman Catholic Church or the Universal Church, is the largest Christian church, with more than 1.28 billion members worldwide. As one of the oldest religious institutions in the world, it has played a prominent role in the history, headed by the Bishop of Rome, known as the Pope, the churchs doctrines are summarised in the Nicene Creed and the Apostles Creed. Its central administration is located in Vatican City, enclaved within Rome, the Catholic Church is notable within Western Christianity for its sacred tradition and seven sacraments. It teaches that it is the one church founded by Jesus Christ, that its bishops are the successors of Christs apostles. The Catholic Church maintains that the doctrine on faith and morals that it declares as definitive is infallible. The Latin Church, the Eastern Catholic Churches, as well as such as mendicant orders and enclosed monastic orders. Among the sacraments, the one is the Eucharist, celebrated liturgically in the Mass. The church teaches that through consecration by a priest the sacrificial bread and wine become the body, the Catholic Church practises closed communion, with only baptised members in a state of grace ordinarily permitted to receive the Eucharist. The Virgin Mary is venerated in the Catholic Church as Queen of Heaven and is honoured in numerous Marian devotions. The Catholic Church has influenced Western philosophy, science, art and culture, Catholic spiritual teaching includes spreading the Gospel while Catholic social teaching emphasises support for the sick, the poor and the afflicted through the corporal and spiritual works of mercy. The Catholic Church is the largest non-government provider of education and medical services in the world, from the late 20th century, the Catholic Church has been criticised for its doctrines on sexuality, its refusal to ordain women and its handling of sexual abuse cases. Catholic was first used to describe the church in the early 2nd century, the first known use of the phrase the catholic church occurred in the letter from Saint Ignatius of Antioch to the Smyrnaeans, written about 110 AD. In the Catechetical Discourses of Saint Cyril of Jerusalem, the name Catholic Church was used to distinguish it from other groups that call themselves the church. The use of the adjective Roman to describe the Church as governed especially by the Bishop of Rome became more widespread after the Fall of the Western Roman Empire and into the Early Middle Ages. Catholic Church is the name used in the Catechism of the Catholic Church. The Catholic Church follows an episcopal polity, led by bishops who have received the sacrament of Holy Orders who are given formal jurisdictions of governance within the church. Ultimately leading the entire Catholic Church is the Bishop of Rome, commonly called the pope, in parallel to the diocesan structure are a variety of religious institutes that function autonomously, often subject only to the authority of the pope, though sometimes subject to the local bishop. Most religious institutes only have male or female members but some have both, additionally, lay members aid many liturgical functions during worship services
24.
Ahmed Zewail
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Ahmed Hassan Zewail was an Egyptian-American scientist, known as the father of femtochemistry. He was awarded the 1999 Nobel Prize in Chemistry for his work on femtochemistry, Ahmed Hassan Zewail was born on February 26,1946, in Damanhour, Egypt, and was raised in Desouk. After completing his PhD, Zewail did postdoctoral research at the University of California, Berkeley, following this, he was awarded a faculty appointment at the California Institute of Technology in 1976, and he was made the first Linus Pauling Chair in Chemical Physics. He became a citizen of the United States on 5 March 1982. Zewail was the director of the Physical Biology Center for Ultrafast Science, zewails key work was as a pioneer of femtochemistry —i. e. the study of chemical reactions across femtoseconds. Using a rapid ultrafast laser technique, the allows the description of reactions on very short time scales – short enough to analyse transition states in selected chemical reactions. Zewail became known as the father of femtochemistry, in a speech at Cairo University on June 4,2009, US President Barack Obama announced a new Science Envoy program as part of a new beginning between the United States and Muslims around the world. In January 2010, Ahmed Zewail, Elias Zerhouni, and Bruce Alberts became the first US science envoys to Islam, when asked about rumors that he might contest the 2011 Egyptian presidential election, Ahmed Zewail said, I am a frank man. I have no political ambition, as I have stressed repeatedly that I only want to serve Egypt in the field of science, during the 2011 Egyptian protests he announced his return to the country. Zewail said that he would join a committee for constitutional reform alongside Ayman Nour, Mubaraks rival at the 2005 presidential elections, in 1999, Zewail became the first Egyptian and the first Arab to receive a science Nobel Prize when he was awarded the Nobel Prize in Chemistry. Zewail gave his Nobel Lecture on Femtochemistry, Atomic-Scale Dynamics of the Chemical Bond Using Ultrafast Lasers, in 1999, he received Egypts highest state honor, the Grand Collar of the Nile. Zewail was elected a Foreign Member of the Royal Society in 2001 and he was awarded an honorary doctorate from Heriot-Watt University in 2002. He was awarded a doctorate by Lund University in Sweden in May 2003 and was made a Foreign Member of the Royal Swedish Academy of Sciences. Cambridge University awarded him an honorary Doctor of Science in 2006, in May 2008, Zewail received an honorary doctorate from Complutense University of Madrid. In February 2009, Zewail was awarded a doctorate in arts. In May 2010, he gave the commencement address at Southwestern University, on 3 October 2011 he was awarded an honorary doctorate in science from the University of Glasgow. On 19 May 2014, he was awarded a degree from Yale University. The Zewail city of science and technology, established in 2000, Zewail married his wife Dema Faham in 1989
25.
Nobel Prize in Chemistry
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The Nobel Prize in Chemistry is awarded annually by the Royal Swedish Academy of Sciences to scientists in the various fields of chemistry. It is one of the five Nobel Prizes established by the will of Alfred Nobel in 1895, awarded for outstanding contributions in chemistry, physics, literature, peace, and physiology or medicine. This award is administered by the Nobel Foundation and awarded by Royal Swedish Academy of Sciences on proposal of the Nobel Committee for Chemistry which consists of five elected by Academy. The award is presented in Stockholm at a ceremony on December 10. The first Nobel Prize in Chemistry was awarded in 1901 to Jacobus Henricus van t Hoff, of the Netherlands, for his discovery of the laws of chemical dynamics and osmotic pressure in solutions. From 1901 to 2016, the award has been bestowed on a total of 174 individuals, though Nobel wrote several wills during his lifetime, the last was written a little over a year before he died, and signed at the Swedish-Norwegian Club in Paris on 27 November 1895. Nobel bequeathed 94% of his assets,31 million Swedish kronor, to establish. Due to the level of surrounding the will, it was not until April 26,1897 that it was approved by the Storting. The executors of his will were Ragnar Sohlman and Rudolf Lilljequist, the members of the Norwegian Nobel Committee that were to award the Peace Prize were appointed shortly after the will was approved. The prize-awarding organisations followed, the Karolinska Institutet on June 7, the Swedish Academy on June 9, the Nobel Foundation then reached an agreement on guidelines for how the Nobel Prize should be awarded. In 1900, the Nobel Foundations newly created statutes were promulgated by King Oscar II, according to Nobels will, The Royal Swedish Academy of Sciences were to award the Prize in Chemistry. The committee and institution serving as the board for the prize typically announce the names of the laureates in October. The prize is awarded at formal ceremonies held annually on December 10. The highlight of the Nobel Prize Award Ceremony in Stockholm is when each Nobel Laureate steps forward to receive the prize from the hands of His Majesty the King of Sweden, the Nobel Laureate receives three things, a diploma, a medal and a document confirming the prize amount. Later the Nobel Banquet is held in Stockholm City Hall, a maximum of three laureates and two different works may be selected. The award can be given to a maximum of three recipients per year and it consists of a gold medal, a diploma, and a cash grant. The Nobel Laureates in chemistry are selected by a committee that consists of five elected by the Royal Swedish Academy of Sciences. In its first stage, several people are asked to nominate candidates
26.
Apollo
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Apollo is one of the most important and complex of the Olympian deities in classical Greek and Roman religion and Greek and Roman mythology. The ideal of the kouros, Apollo has been recognized as a god of music, truth and prophecy, healing, the sun and light, plague, poetry. Apollo is the son of Zeus and Leto, and has a twin sister, Apollo is known in Greek-influenced Etruscan mythology as Apulu. As the patron of Delphi, Apollo was an oracular god—the prophetic deity of the Delphic Oracle. Medicine and healing are associated with Apollo, whether through the god himself or mediated through his son Asclepius, yet Apollo was also seen as a god who could bring ill-health and deadly plague. Amongst the gods custodial charges, Apollo became associated with dominion over colonists, as the leader of the Muses and director of their choir, Apollo functioned as the patron god of music and poetry. Hermes created the lyre for him, and the instrument became an attribute of Apollo. Hymns sung to Apollo were called paeans, Apollo and Helios/Sol remained separate beings in literary and mythological texts until the 3rd century CE. The name Apollo—unlike the related older name Paean—is generally not found in the Linear B texts, the etymology of the name is uncertain. The spelling Ἀπόλλων had almost superseded all other forms by the beginning of the common era and it probably is a cognate to the Doric month Apellaios, and the offerings apellaia at the initiation of the young men during the family-festival apellai. According to some scholars the words are derived from the Doric word apella, apella is the name of the popular assembly in Sparta, corresponding to the ecclesia. R. S. P. Beekes rejected the connection of the theonym with the noun apellai, several instances of popular etymology are attested from ancient authors. Thus, the Greeks most often associated Apollos name with the Greek verb ἀπόλλυμι, in the ancient Macedonian language πέλλα means stone, and some toponyms may be derived from this word, Πέλλα and Πελλήνη. The role of Apollo as god of plague is evident in the invocation of Apollo Smintheus by Chryses, the Hittite testimony reflects an early form *Apeljōn, which may also be surmised from comparison of Cypriot Ἀπείλων with Doric Ἀπέλλων. A Luwian etymology suggested for Apaliunas makes Apollo The One of Entrapment, Apollos chief epithet was Phoebus, literally bright. It was very commonly used by both the Greeks and Romans for Apollos role as the god of light, like other Greek deities, he had a number of others applied to him, reflecting the variety of roles, duties, and aspects ascribed to the god. However, while Apollo has a number of appellations in Greek myth. Aegletes, from αἴγλη, light of the sun Helius, literally sun Lyceus light, the meaning of the epithet Lyceus later became associated with Apollos mother Leto, who was the patron goddess of Lycia and who was identified with the wolf
27.
Arabic
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Arabic is a Central Semitic language that was first spoken in Iron Age northwestern Arabia and is now the lingua franca of the Arab world. Arabic is also the language of 1.7 billion Muslims. It is one of six languages of the United Nations. The modern written language is derived from the language of the Quran and it is widely taught in schools and universities, and is used to varying degrees in workplaces, government, and the media. The two formal varieties are grouped together as Literary Arabic, which is the language of 26 states. Modern Standard Arabic largely follows the standards of Quranic Arabic. Much of the new vocabulary is used to denote concepts that have arisen in the post-Quranic era, Arabic has influenced many languages around the globe throughout its history. During the Middle Ages, Literary Arabic was a vehicle of culture in Europe, especially in science, mathematics. As a result, many European languages have borrowed many words from it. Many words of Arabic origin are found in ancient languages like Latin. Balkan languages, including Greek, have acquired a significant number of Arabic words through contact with Ottoman Turkish. Arabic has also borrowed words from languages including Greek and Persian in medieval times. Arabic is a Central Semitic language, closely related to the Northwest Semitic languages, the Ancient South Arabian languages, the Semitic languages changed a great deal between Proto-Semitic and the establishment of the Central Semitic languages, particularly in grammar. Innovations of the Central Semitic languages—all maintained in Arabic—include, The conversion of the suffix-conjugated stative formation into a past tense, the conversion of the prefix-conjugated preterite-tense formation into a present tense. The elimination of other prefix-conjugated mood/aspect forms in favor of new moods formed by endings attached to the prefix-conjugation forms, the development of an internal passive. These features are evidence of descent from a hypothetical ancestor. In the southwest, various Central Semitic languages both belonging to and outside of the Ancient South Arabian family were spoken and it is also believed that the ancestors of the Modern South Arabian languages were also spoken in southern Arabia at this time. To the north, in the oases of northern Hijaz, Dadanitic and Taymanitic held some prestige as inscriptional languages, in Najd and parts of western Arabia, a language known to scholars as Thamudic C is attested
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Early Muslim conquests
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The early Muslim conquests also referred to as the Arab conquests and early Islamic conquests began with the Islamic Prophet Muhammad in the 7th century. He established a new unified polity in the Arabian Peninsula which under the subsequent Rashidun, the resulting empire stretched from the borders of China and the Indian subcontinent, across Central Asia, the Middle East, North Africa, Sicily, and the Iberian Peninsula, to the Pyrenees. The Muslim conquests brought about the collapse of the Sassanid Empire, the reasons for the Muslim success are hard to reconstruct in hindsight, primarily because only fragmentary sources from the period have survived. Most historians agree that the Sassanid Persian and Byzantine Roman empires were militarily and economically exhausted from decades of fighting one another, in the case of Byzantine Egypt, Palestine and Syria, these lands had only a few years before being reclaimed from the Persians. The estimates for the size of the Islamic Caliphate suggest it was more than thirteen million square kilometers, the last of these wars ended with victory for the Byzantines, Emperor Heraclius regained all lost territories, and restored the True Cross to Jerusalem in 629. According to George Liska, the unnecessarily prolonged Byzantine–Persian conflict opened the way for Islam, in late 620s Muhammad had already managed to conquer and unify much of Arabia under Muslim rule, and it was under his leadership that the first Muslim-Byzantine skirmishes took place. The province of Syria was the first to be wrested from Byzantine control, on the heels of their victory, the Arab armies took Damascus in 636, with Baalbek, Homs, and Hama to follow soon afterwards. However, other fortified towns continued to resist despite the rout of the army and had to be conquered individually. Jerusalem fell in 638, Caesarea in 640, while others held out until 641, the Byzantine province of Egypt held strategic importance for its grain production, naval yards, and as a base for further conquests in Africa. The Muslim general Amr ibn al-As began the conquest of the province on his own initiative in 639, nevertheless, the province was scarcely urbanized and the defenders lost hope of receiving reinforcements from Constantinople when the emperor Heraclius died in 641. The last major center to fall into Arab hands was Alexandria, according to Hugh Kennedy, Of all the early Muslim conquests, that of Egypt was the swiftest and most complete. Seldom in history can so massive a political change have happened so swiftly, after an Arab incursion into Sasanian territories, the energetic king Yazdgerd III, who had just ascended the Persian throne, raised an army to resist the invasion. However, the Persians suffered a defeat at the Battle of al-Qadisiyyah in 636. As a result, the Arab-Muslims gained control over the whole of Iraq, including Ctesiphon, the Persian forces withdrew over the Zagros mountains and the Arab army pursued them across the Iranian plateau, where the fate of the Sasanian empire was sealed at the Battle of Nahavand. In the aftermath of their victory over the army, the invaders still had to contend with a collection of militarily weak. It took decades to bring all under control of the caliphate. The rapidity of the early conquests has received various explanations, contemporary Christian writers conceived them as Gods punishment visited on their fellow Christians for their sins. Early Muslim historians viewed them as a reflection of religious zeal of the conquerors, according to Chase F. Robinson, it is likely that Muslim forces were often outnumbered, but, unlike their opponents, they were fast, well coordinated and highly motivated
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Northern coast of Egypt
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The Northern Coast of Egypt extends for about 1,050 km from Rafah, the easternmost city in the North Sinai Governorate to Sallum in the west on the Egyptian-Libyan border. It is one of the longest Mediterranean shores in North Africa, the city of Alexandria lies at the center of the Mediterranean Egyptian coastline, as chosen by Alexander the Great. It has been the hub of sea travel between the Mediterranean Sea and the Nile Delta for over 2,300 years and it is also characterised by the occurrence of Egypts five northernmost lakes. The region has typical Mediterranean flora and fauna on land and in life with the weather being between pleasant and hot during summer and mild in winter. The region receives the most rain in Egypt, hail and sleet fall rarely in winter, snowfalls occur in some inland towns and locations. Temperatures range between a monthly average of 9.5 °C in winter and 23 °C in summer. Egypts Mediterranean coast can be differentiated into 4 subregions, Western North Coast, higher altitude witnesses higher snowfalls and it is colder than the other 3 portions. It also has more shrubed and forested terrain, Yet with no lakes and this subregion faces Greece and Crete. It has cities, towns and villages like, Sallum a border town at Libyan borders, sidi Barrani a snowy town, and Egypts closest inhabited settlement towards Europe and Greece. Zawyet Umm El Rakham a village with archeological sites, marsa Matruh the main seaport on Egypts Western Mediterranean coast. Fuka a village famous for excellent Mediterranean fruits and touristic beaches, sidi Abdel Rahman a new touristic seaport town. Central North Coast, The southernmost Mediterranean shoreline in Egypt, forming a big gulf and this subregion faces the West of Turkey. Sidi Kreir a major town and municipality Borg El Arab a major city Alexandria the main Mediterranean city, at the center of the entire Medi coastline and the second largest city in Egypt. Deltas North Coast, Which is settled by larger populations and hosts larger cities -With exception of Alexandria- and it has Nile Delta which features hail and sleet in winters. Sometime frost and frozen ground during winter nights destroy the crops,3 of Egypts Northern Lakes are located there, Lake Mariout, Edko Lake and Lake Burullus. Its cities, towns and villages are like, Rosetta a historic western Nile delta city where Rashids Nile branch and it is colder on its eastern part than its other part. 2 Northern lakes of Egypt are found in this subregion as well, Lake Manzala and this subregion faces Cyprus and Turkey. Red Sea Riviera Turkish Riviera Italian Riviera French Riviera New Homes in Egypt North Coast Compounds in Egypt
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Desert climate
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An area that features this climate usually experiences from 25 to 200 mm per year of precipitation and in some years may experience no precipitation at all. Averages may be even less such as in Arica, Chile, there are usually two or three variations of a desert climate, a hot desert climate, a cold desert climate and, sometimes, a mild desert climate. To determine whether a location has a climate, the precipitation threshold is determined. If the areas precipitation is less than half the threshold. Hot desert climates are found under the subtropical ridge where there is largely unbroken sunshine for the whole year due to the stable descending air. These areas are located between 30 degrees south and 30 degrees north latitude, under the subtropical latitudes called the horse latitudes, hot desert climates are generally hot, sunny and dry year-round. Hot desert climates also reach similar latitudes in the Middle East, North Africa, hot desert climates usually feature hot, sometimes exceptionally hot, periods of the year. In many locations featuring a hot climate, maximum temperatures of over 40 °C are not uncommon in summer. The world absolute heat records, over 50 °C, are generally in the hot deserts, some desert locations consistently experience very high temperatures all year long, even during wintertime. These locations feature some of the highest annual average temperatures recorded on Earth and this last feature is seen in some parts of deserts of Africa and Arabia. During colder periods of the year, night-time temperatures can drop to freezing or below due to the radiation loss under the clear skies. However, very rarely do temperatures drop far below freezing, only one region in Europe has a hot desert climate, Province of Almeria, Province of Alicante and Province of Murcia in South Eastern Spain. Cold desert climates usually feature warm and dry summers, though summers typically are not quite as hot as summers in hot desert climates, unlike hot desert climates, cold desert climates tend to feature cold winters with rare snow. Cold desert climates are found at higher altitudes than hot desert climates. A cold desert climate is found in temperate zones, usually in the rain shadow of high mountains. A classic example of this is the Patagonian Desert in Argentina bounded by the Andes to its west, in the case of Central Asia, mountains restrict precipitation from the monsoon. The Gobi desert in Mongolia is an example of this. Though hot in summer, it shares the cold winters of the rest of Central Asia
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Mediterranean Sea
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The sea is sometimes considered a part of the Atlantic Ocean, although it is usually identified as a separate body of water. The name Mediterranean is derived from the Latin mediterraneus, meaning inland or in the middle of land and it covers an approximate area of 2.5 million km2, but its connection to the Atlantic is only 14 km wide. The Strait of Gibraltar is a strait that connects the Atlantic Ocean to the Mediterranean Sea and separates Gibraltar. In oceanography, it is called the Eurafrican Mediterranean Sea or the European Mediterranean Sea to distinguish it from mediterranean seas elsewhere. The Mediterranean Sea has a depth of 1,500 m. The sea is bordered on the north by Europe, the east by Asia and it is located between latitudes 30° and 46° N and longitudes 6° W and 36° E. Its west-east length, from the Strait of Gibraltar to the Gulf of Iskenderun, the seas average north-south length, from Croatia’s southern shore to Libya, is approximately 800 km. The Mediterranean Sea, including the Sea of Marmara, has an area of approximately 2,510,000 square km. The sea was an important route for merchants and travelers of ancient times that allowed for trade, the history of the Mediterranean region is crucial to understanding the origins and development of many modern societies. In addition, the Gaza Strip and the British Overseas Territories of Gibraltar and Akrotiri, the term Mediterranean derives from the Latin word mediterraneus, meaning amid the earth or between land, as it is between the continents of Africa, Asia and Europe. The Ancient Greek name Mesogeios, is similarly from μέσο, between + γη, land, earth) and it can be compared with the Ancient Greek name Mesopotamia, meaning between rivers. The Mediterranean Sea has historically had several names, for example, the Carthaginians called it the Syrian Sea and latter Romans commonly called it Mare Nostrum, and occasionally Mare Internum. Another name was the Sea of the Philistines, from the people inhabiting a large portion of its shores near the Israelites, the sea is also called the Great Sea in the General Prologue by Geoffrey Chaucer. In Ottoman Turkish, it has also been called Bahr-i Sefid, in Modern Hebrew, it has been called HaYam HaTikhon, the Middle Sea, reflecting the Seas name in ancient Greek, Latin, and modern languages in both Europe and the Middle East. Similarly, in Modern Arabic, it is known as al-Baḥr al-Mutawassiṭ, in Turkish, it is known as Akdeniz, the White Sea since among Turks the white colour represents the west. Several ancient civilisations were located around the Mediterranean shores, and were influenced by their proximity to the sea. It provided routes for trade, colonisation, and war, as well as food for numerous communities throughout the ages, due to the shared climate, geology, and access to the sea, cultures centered on the Mediterranean tended to have some extent of intertwined culture and history. Two of the most notable Mediterranean civilisations in classical antiquity were the Greek city states, later, when Augustus founded the Roman Empire, the Romans referred to the Mediterranean as Mare Nostrum
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Precipitation
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In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation include drizzle, rain, sleet, snow, graupel, Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and precipitates. Thus, fog and mist are not precipitation but suspensions, because the vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated, Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers, moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into clouds and rain. This process is active when freezing rain is occurring. A stationary front is often present near the area of freezing rain, provided necessary and sufficient atmospheric moisture content, the moisture within the rising air will condense into clouds, namely stratus and cumulonimbus. Eventually, the droplets will grow large enough to form raindrops. Lake-effect snowfall can be locally heavy, thundersnow is possible within a cyclones comma head and within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation, on the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. The movement of the trough, or intertropical convergence zone. Precipitation is a component of the water cycle, and is responsible for depositing the fresh water on the planet. Approximately 505,000 cubic kilometres of water falls as precipitation each year,398,000 cubic kilometres of it over the oceans and 107,000 cubic kilometres over land. Given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres, Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Precipitation may occur on celestial bodies, e. g. when it gets cold, Mars has precipitation which most likely takes the form of frost. Precipitation is a component of the water cycle, and is responsible for depositing most of the fresh water on the planet. Approximately 505,000 km3 of water falls as precipitation each year,398,000 km3 of it over the oceans, given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres. Mechanisms of producing precipitation include convective, stratiform, and orographic rainfall, Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice
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Winter
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Winter is the coldest season of the year in polar and temperate climates, between autumn and spring. Winter is caused by the axis of the Earth in that hemisphere being oriented away from the Sun, different cultures define different dates as the start of winter, and some use a definition based on weather. When it is winter in the Northern Hemisphere, it is summer in the Southern Hemisphere, in many regions, winter is associated with snow and freezing temperatures. The moment of winter solstice is when the elevation with respect to the North or South Pole is at its most negative value, meaning this day will have the shortest day. The English word winter comes from the Proto-Indo-European root wend, relating to water, the tilt of the Earths axis relative to its orbital plane plays a large role in the formation of weather. The Earth is tilted at an angle of 23. 44° to the plane of its orbit, when it is winter in the Northern Hemisphere, the Southern Hemisphere faces the Sun more directly and thus experiences warmer temperatures than the Northern Hemisphere. Conversely, winter in the Southern Hemisphere occurs when the Northern Hemisphere is tilted more toward the Sun, from the perspective of an observer on the Earth, the winter Sun has a lower maximum altitude in the sky than the summer Sun. During winter in either hemisphere, the altitude of the Sun causes the sunlight to hit that hemisphere at an oblique angle. In regions experiencing winter, the amount of solar radiation is spread out over a larger area. This effect is compounded by the distance that the light must travel through the atmosphere. Compared with these effects, the changes in the distance of the earth from the sun are negligible, the manifestation of the meteorological winter in the northerly snow–prone parallels is highly variable depending on elevation, position versus marine winds and the amount of precipitation. A case in point is Canada, a country associated with tough winters. Winnipeg on the Great Plains at a distance from large bodies of water has a January high of −11.3 °C. In comparison, Vancouver on the coast with an influence from moderating Pacific winds has a January low of 1.4 °C with days well above freezing at 6.9 °C. Both areas are on the 49th parallel north and in the western half of the continent. Winter is often defined by meteorologists to be the three months with the lowest average temperatures. This corresponds to the months of December, January and February in the Northern Hemisphere, the coldest average temperatures of the season are typically experienced in January or February in the Northern Hemisphere and in June, July or August in the Southern Hemisphere. Blizzards often develop and cause many transportation delays, diamond dust, also known as ice needles or ice crystals, forms at temperatures approaching −40 °F due to air with slightly higher moisture from aloft mixing with colder, surface based air
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Rain
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Rain is liquid water in the form of droplets that have condensed from atmospheric water vapor and then precipitated—that is, become heavy enough to fall under gravity. Rain is a component of the water cycle and is responsible for depositing most of the fresh water on the Earth. It provides suitable conditions for many types of ecosystems, as well as water for power plants. The major cause of production is moisture moving along three-dimensional zones of temperature and moisture contrasts known as weather fronts. If enough moisture and upward motion is present, precipitation falls from convective clouds such as cumulonimbus which can organize into narrow rainbands. On the leeward side of mountains, desert climates can exist due to the dry air caused by downslope flow which causes heating and drying of the air mass, the movement of the monsoon trough, or intertropical convergence zone, brings rainy seasons to savannah climes. The urban heat island effect leads to increased rainfall, both in amounts and intensity, downwind of cities, global warming is also causing changes in the precipitation pattern globally, including wetter conditions across eastern North America and drier conditions in the tropics. The globally averaged annual precipitation over land is 715 mm, climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Rainfall is measured using rain gauges, rainfall amounts can be estimated by weather radar. Rain is also known or suspected on other planets, where it may be composed of methane, neon, sulfuric acid, or even iron rather than water. Air contains water vapor, and the amount of water in a mass of dry air. The amount of moisture in air is commonly reported as relative humidity. How much water vapor a parcel of air can contain before it becomes saturated, warmer air can contain more water vapor than cooler air before becoming saturated. Therefore, one way to saturate a parcel of air is to cool it, the dew point is the temperature to which a parcel must be cooled in order to become saturated. There are four mechanisms for cooling the air to its dew point, adiabatic cooling, conductive cooling, radiational cooling. Adiabatic cooling occurs when air rises and expands, the air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain. Conductive cooling occurs when the air comes into contact with a surface, usually by being blown from one surface to another. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath, evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation
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Season
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A season is a division of the year marked by changes in weather, ecology and hours of daylight. Seasons result from the orbit of the Earth around the Sun. During May, June, and July, the northern hemisphere is exposed to direct sunlight because the hemisphere faces the sun. The same is true of the hemisphere in November, December. It is the tilt of the Earth that causes the Sun to be higher in the sky during the months which increases the solar flux. However, due to lag, June, July, and August are the hottest months in the northern hemisphere and December, January. In temperate and subpolar regions, four calendar-based seasons are recognized, spring, summer, autumn or fall. Ecologists often use a model for temperate climate regions, prevernal, vernal, estival, serotinal, autumnal. Many tropical regions have two seasons, the rainy, wet, or monsoon season and the dry season, some have a third cool, mild, or harmattan season. Seasons often held special significance for agrarian societies, whose lives revolved around planting and harvest times, in some parts of the world, some other seasons capture the timing of important ecological events such as hurricane season, tornado season, and wildfire season. The most historically important of these are the three seasons—flood, growth, and low water—which were previously defined by the annual flooding of the Nile in Egypt. The seasons result from the Earths axis of rotation being tilted with respect to its orbital plane by an angle of approximately 23.5 degrees, regardless of the time of year, the northern and southern hemispheres always experience opposite seasons. This is because during summer or winter, one part of the planet is directly exposed to the rays of the Sun than the other. For approximately half of the year, the northern hemisphere tips toward the Sun, for the other half of the year, the same happens, but in the southern hemisphere instead of the northern, with the maximum around December 21. The two instants when the Sun is directly overhead at the Equator are the equinoxes. Also at that moment, both the North Pole and the South Pole of the Earth are just on the terminator, and hence day and night are equally divided between the northern and southern hemispheres. Around the March equinox, the northern hemisphere will be experiencing spring as the hours of daylight increase, the effect of axial tilt is observable as the change in day length and altitude of the Sun at noon during a year. Between this effect and the daylight hours, the axial tilt of the Earth accounts for most of the seasonal variation in climate in both hemispheres
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Hail
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Hail is a form of solid precipitation. It is distinct from ice pellets, though the two are often confused and it consists of balls or irregular lumps of ice, each of which is called a hailstone. Ice pellets falls generally in cold weather while hail growth is inhibited during cold surface temperatures. Unlike graupel, which is made of rime, and ice pellets, the METAR reporting code for hail 5 mm or greater is GR, while smaller hailstones and graupel are coded GS. Hail is possible within most thunderstorms as it is produced by cumulonimbus, Hail formation requires environments of strong, upward motion of air with the parent thunderstorm and lowered heights of the freezing level. In the mid-latitudes, hail forms near the interiors of continents, while in the tropics, there are methods available to detect hail-producing thunderstorms using weather satellites and weather radar imagery. Severe weather warnings are issued for hail when the stones reach a size, as it can cause serious damage to human-made structures and, most commonly. Any thunderstorm which produces hail that reaches the ground is known as a hailstorm, Hail has a diameter of 5 millimetres or more. Hailstones can grow to 15 centimetres and weigh more than 0.5 kilograms, unlike ice pellets, hailstones are layered and can be irregular and clumped together. Although the diameter of hail is varied, in the United States, stones larger than 2 cm are usually considered large enough to cause damage. The Meteorological Service of Canada issues severe thunderstorm warnings when hail that size or above is expected, the US National Weather Service has a 2.5 cm or greater in diameter threshold, effective January 2010, an increase over the previous threshold of ¾-inch hail. Other countries have different thresholds according local sensitivity to hail, for grape growing areas could be adversely impacted by smaller hailstones. Hailstones can be large or very small, depending on how strong the updraft is. These types of strong updrafts can also indicate the presence of a tornado, the growth rate is maximized where air is near a temperature of −13 °C. Like other precipitation in clouds, hail begins as water droplets. As the droplets rise and the temperature goes below freezing, they become supercooled water, a cross-section through a large hailstone shows an onion-like structure. This means the hailstone is made of thick and translucent layers, alternating layers that are thin, white. Former theory suggested that hailstones were subjected to multiple descents and ascents, falling into a zone of humidity and this up and down motion was thought to be responsible for the successive layers of the hailstone
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Frost
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Frost is the coating or deposit of ice that may form in humid air in cold conditions, usually overnight. In temperate climates it most commonly appears as white crystals or frozen dew drops near the ground. Frost is composed of delicate branched patterns of ice crystals formed as the result of fractal process development, Frost is known to damage crops or reduce future crop yields, therefore farmers in those regions where frost is a problem often invest substantial means to prevent its formation. In most temperate countries such temperatures usually are the result of loss by radiation at night. The size of frost crystals varies depending on the time they have been building up, Frost crystals may be clear or translucent, but, like snow, a mass of frost crystals will scatter light in all directions, so that a coating of frost appears white. If a solid surface is chilled below the dew point of the humid air. If the water deposits as a liquid that freezes, it forms a coating that may look glassy, opaque, or crystalline. Depending on context, that also may be called atmospheric icing. The ice it produces differs in ways from crystalline frost. For desublimation to proceed the surface must be below the frost point of the air, the air must be humid, but not sufficiently humid to permit the condensation of liquid water, or icing will result instead of desublimation. The size of the crystals depends largely on the temperature, the amount of water vapor available, as a rule, except in conditions where supercooled droplets are present in the air, frost will form only if the deposition surface is colder than the surrounding air. For instance frost may be observed around cracks in cold wooden sidewalks when humid air escapes from the ground beneath. Other objects on which frost commonly forms are those with low specific heat or high thermal emissivity, such as blackened metals, the apparently erratic occurrence of frost in adjacent localities is due partly to differences of elevation, the lower areas becoming colder on calm nights. Where static air settles above an area of ground in the absence of wind, hoar frost refers to white ice crystals, deposited on the ground or loosely attached to exposed objects such as wires or leaves. They form on cold, clear nights when conditions are such that heat radiates out to the sky faster than it can be replaced from nearby sources such as wind or warm objects. Under suitable circumstances, objects cool to below the frost point of the surrounding air, such freezing may be promoted by effects such as flood frost or frost pocket. These occur when ground-level radiation losses cool air till it flows downhill and accumulates in pockets of cold air in valleys. Hoar frost may freeze in such low-lying cold air even when the air temperature a few feet above ground is well above freezing
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Holy Land
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The Holy Land is an area roughly located between the Jordan River and the Mediterranean Sea that also includes the Eastern Bank of the Jordan River. Traditionally, it is synonymous with both the biblical Land of Israel and historical Palestine, the term usually refers to a territory roughly corresponding to the modern State of Israel, the Palestinian territories, western Jordan, and parts of southern Lebanon and southwestern Syria. It is considered holy by Jews, Christians, and Muslims, many sites in the Holy Land have long been pilgrimage destinations for adherents of the Abrahamic religions, including Jews, Christians, Muslims, and Baháís. Pilgrims visit the Holy Land to touch and see physical manifestations of their faith, confirm their beliefs in the context with collective excitation. Jews do not commonly refer to the Land of Israel as Holy Land, the Tanakh explicitly refers to it as holy land in only one passage, in Zechariah 2,16. The holiness of the Land of Israel is generally implied in the Tanakh by the Land being given to the Israelites by God, that is, it is the promised land, an integral part of Gods covenant. In the Torah many mitzvot commanded to the Israelites can only be performed in the Land of Israel, for example, in the Land of Israel, no land shall be sold permanently. Shmita is only observed with respect to the land of Israel, according to Eliezer Schweid, The uniqueness of the Land of Israel is. geo-theological and not merely climatic. This is the land which faces the entrance of the spiritual world, Jerusalem, as the site of the Temple, is considered especially significant. Sacred burials are still undertaken for diaspora Jews who wish to lie buried in the soil of Israel. According to Jewish tradition, Jerusalem is Mount Moriah, the location of the binding of Isaac, the Hebrew Bible mentions the name Jerusalem 669 times, often because many mitzvot can only be performed within its environs. The name Zion, which refers to Jerusalem, but sometimes the Land of Israel. The Talmud mentions the religious duty of colonising Israel, so significant in Judaism is the act of purchasing land in Israel, the Talmud allows for the lifting of certain religious restrictions of Sabbath observance to further its acquisition and settlement. Rabbi Johanan said that one who walks a distance of 4 cubits in Israel may be confident of a share in the future world, a story says that when R. Eleazar b. Due to the Jewish population being concentrated in Israel, emigration was generally prevented, many Jews wanted Israel to be the place where they died. R. Anan said, To be buried in Israel is like being buried under the altar, the saying His land will absolve His people implies that burial in Israel will cause one to be absolved of all ones sins. Christian books, including editions of the Bible, often had maps of the Holy Land, for instance, the Itinerarium Sacrae Scripturae of Heinrich Bünting, a German Protestant pastor, featured such a map. As a geographic term, the description Holy Land loosely encompasses modern-day Israel, in the Quran, the term الأرض المقدسة is mentioned at least seven times, once when Moses proclaims to the Children of Israel, O my people
39.
Haaretz
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It was founded in 1918, making it the longest running newspaper currently still in print in Israel, and is now published in both Hebrew and English in Berliner format. The English edition is published and sold together with the International New York Times, both Hebrew and English editions can be read on the Internet. In North America, it out as a weekly newspaper. It is known for its left-wing and liberal stances on domestic, as of 2016, the newspaper had a weekday exposure rate of 3. 9% in Israel, significantly lower than the countrys other national newspapers. Haaretz was first published in 1918 as a newspaper sponsored by the British military government in Palestine, in 1919, it was taken over by a group of socialist-oriented Zionists, mainly from Russia. The newspaper was established on 18 June 1919 by a group of businessmen including prominent philanthropist Isaac Leib Goldberg, later, the name was shortened to Haaretz. The literary section of the paper attracted leading Hebrew writers of the time, the newspaper was initially published in Jerusalem. From 1919 to 1922, the paper was headed by a succession of editors and it was shut down briefly due to a budgetary shortfall and reopened in Tel Aviv at the beginning of 1923 under the editorship of Moshe Glickson, who held the post for 15 years. The Tel Aviv municipality granted the financial support by paying in advance for future advertisements. Salman Schocken, a wealthy German Jewish Zionist who owned a chain of department stores in Germany and his son, Gershom Schocken, became the chief editor in 1939 and held that position until his death in 1990. Until August 2006, the Schocken family owned 100% of the Haaretz Group, the deal was negotiated with the help of former Israeli ambassador to Germany, Avi Primor. This deal was seen as controversial in Israel as DuMont Schaubergs father, Kurt Neven DuMont, was member of the German Nazi party, while his publishing house promoted Nazi ideology. On 12 June 2011, it was announced that Russian-Israeli businessman Leonid Nevzlin had purchased a 20% stake in the Haaretz Group, buying 15% from the family and this means that the Schocken family now owns 60% and M. DuMont Schauberg and Leonid Nevzlin have 20% each. In October 2012, a union strike mobilized to protest planned layoffs by the Haaretz management, as a consequence, both the Haaretz newspaper and its TheMarker business supplement were not printed for one day. According to Israel Radio, it was the first time since 1965 that a newspaper did not go to press on account of a strike, the newspapers editorial policy was defined by Gershom Schocken, who was editor-in-chief from 1939 to 1990. Schocken was succeeded as editor-in-chief by Hanoch Marmari, in 2004 David Landau replaced Marmari and was succeeded by Dov Alfon in 2008. The current editor-in-chief of the newspaper is Aluf Benn, who replaced Alfon in August 2011, charlotte Halle became editor of the English Print Edition in February 2008. Haaretz describes itself as having a liberal outlook both on domestic issues and on international affairs
Egypt
"Damanhūr". Encyclopædia Britannica. 7 (11th ed.). 1911. p. 783.
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This article incorporates text from a publication now in the public domain: Smith, William, ed. (1854–1857). "article name needed". Dictionary of Greek and Roman Geography. London: John Murray.