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Jordanian Highlands
The Jordanian Highlands is a mountain range in Jordan. It extends north and south through the western portion of the country, between the Red Sea- Dead Sea depression to the west and a plateau to the east. The highlands are home to most of Jordan's population and large cities. Geography The Jordanian Highlands extend about 300 km north to south. The highlands are bounded on the north by the deeply-incised Yarmouk River valley, which forms part of the border between Jordan and Syria. They extend to south to Jordan's border with Saudi Arabia. From the plateau to the east the highlands appear as a series of hills. To the west the highlands drop steeply 1,000 meters or more to the Jordan Rift Valley, which contains the Jordan River and the Dead Sea, a saline lake with a surface below sea level.Wagner W. (2011) Northwestern Mountain and Rift Zone of the Northern Arabian Platform. In: Groundwater in the Arab Middle East. Springer, Berlin, Heidelberg. Elevation of the higher peaks ran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Nebo
Mount Nebo ( ar, جَبَل نِيبُو, Jabal Nībū; he, , Har Nəḇō) is an elevated ridge located in Jordan, approximately above sea level. Part of the Abarim mountain range, Mount Nebo is mentioned in the Bible as the place where Moses was granted a view of the Promised Land before his death. The view from the summit provides a panorama of the West Bank across the Jordan River valley. The city of Jericho is usually visible from the summit, as is Jerusalem on a very clear day. The biblical town of Nebo, now known as Khirbet al-Mukhayyat, is located 3.5 km away. Religious significance According to the Bible (Deuteronomy), Moses ascended Mount Nebo, in the land of Moab (today in Jordan), and from there he saw the Land of Canaan (the Promised Land), which God had said he would not enter; Moses then died there. The Bible () says Moses' burial place was unknown. A monument atop Mount Nebo commemorates Moses' death after seeing Canaan, across the Jordan valley. A purported ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Madaba
Madaba ( ar, مادبا; Biblical Hebrew: ''Mēḏəḇāʾ''; grc, Μήδαβα) is the capital city of Madaba Governorate in central Jordan, with a population of about 60,000. It is best known for its Byzantine and Umayyad mosaics, especially a large Byzantine-era mosaic map of the Holy Land. Madaba is located south-west of the capital Amman. History Madaba dates from the Middle Bronze Age. The town of Madaba was once a Moabite border city, mentioned in the Bible in Numbers 21:30 and Joshua 13:9. Control over the city changed back and forth between Israel and Moab, as mentioned in the Mesha Stele. During its rule by the Roman and Byzantine empires from the 2nd to the 7th centuries, the city formed part of the Provincia Arabia set up by the Roman Emperor Trajan to replace the Nabataean kingdom of Petra. The first evidence for a Christian community in the city, with its own bishop, is found in the Acts of the Council of Chalcedon in 451, where Constantine, Metropolit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arbutus Andrachne
''Arbutus'' is a genus of 12 accepted speciesAct. Bot. Mex no.99 Pátzcuaro abr. 2012.''Arbutus bicolor''/ref> of flowering plants in the family Ericaceae, native to warm temperate regions of the Mediterranean, western Europe, the Canary Islands and North America. The name ''Arbutus'' was taken from Latin, where it referred to ''Arbutus unedo''. Description ''Arbutus'' are small trees or shrubs with red flaking bark and edible red berries.Mabberley, D. J. 1997. ''The plant book: A portable dictionary of the vascular plants''. Cambridge University Press, Cambridge. Fruit development is delayed for about five months after pollination, so that flowers appear while the previous year's fruit are ripening. Peak flowering for the genus is in April with peak fruiting in October. History The smooth wood of the tree is mentioned by Theophrastus in his ''Enquiry into Plants'' (''Historia Plantarum'') as formerly being used to make weaving spindles. An article on Arbutus tree cultivatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quercus Aegilops
''Quercus macrolepis'', the Valonia oak, is a species of oak in the beech family, Fagaceae. Formerly, it was commonly treated as a subspecies of the closely related and sympatric mount Tabor oak. At present, however, it is mostly granted species-status. Geographical range It is found in the Balkans, and in the southern and eastern Mediterranean, including Albania, the Greek Islands, Turkey, Israel, and Morocco. Systematics Within the oak genus, Quercus macrolepis is classified in the subgenus ''Cerris'', section ''Cerris'', which includes the turkey oak and related species. It is most closely related to Mount Tabor oak (Quercus ithaburensis) and Brant's oak (Quercus brantii). Uses The cups, known as valonia, are used for tanning and dyeing as are the unripe acorns called camata or camatina. The ripe acorns are eaten raw or boiled. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quercus Infectoria
''Quercus infectoria'' or the Aleppo oak is a species of oak well known for producing galls (called manjakani in Malaysia, majuphal in India) that have been traditionally used for centuries in Asia medicinally while also used in softening leather and in making black dye and ink. Description ''Quercus infectoria'' is a small tree, growing to in height. The stems are crooked, shrubby looking with smooth and bright-green leaves borne on short petioles of long. The leaves are bluntly mucronate, rounded, smooth, unequal at the base and shiny on the upper side. The galls arise on young branches of the tree when gall wasps sting the oak tree and deposit their larvae. The chemical reaction causes an abnormality in the tree, causing hard balls to be formed. They are corrugated in appearance. Gall chemistry The galls from ''Quercus infectoria'' contain the highest naturally occurring level of tannin, approximately 50–70%, as well as syringic acid, β-sitosterol, amentoflavone, hexam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quercus Calliprinos
''Quercus calliprinos'' is an oak classified as part of the ''Ilex'' section of the genus growing in the Mediterranean climate zone, mainly on limestone, in mid-elevations, often dominating the flora, alongside terebinths (''Pistacia terebinthus'').Zohary, M. "The maquis of Quercus calliprinos in Israel, Palestine, and Jordan." Bulletin of the Research Council of Israel 9.2 (1960): 51-72.. It is native to eastern Mediterranean region and southwest Asia, and grows in the Levant, North Africa to Anatolia and further eastwards. In Israel it is called the common oak (, ) or the Palestine oak. ''Quercus calliprinos'' was described by Webb in 1838. The name ''calliprinos'' derives from Ancient Greek, and means ‘beautiful oak’: κάλλος (''kallos'') = beauty + πρῖνος (''prinos'') a name for Holm Oak (''Q. ilex''). The common name Sindian Oak derives from the local Palestinian name (Stapf 1920). Description ''Quercus calliprinos'' is a small to medium-sized tree or la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aleppo Pine
''Pinus halepensis'', commonly known as the Aleppo pine, also known as the Jerusalem pine, is a pine native to the Mediterranean region. Description ''Pinus halepensis'' is a small to medium-sized tree, tall, with a trunk diameter up to , exceptionally up to . The bark is orange-red, thick, and deeply fissured at the base of the trunk, and thin and flaky in the upper crown. The leaves ('needles') are very slender, long, distinctly yellowish green, and produced in pairs (rarely a few in threes). The cones are narrow conic, long and broad at the base when closed, green at first, ripening glossy red-brown when 24 months old. They open slowly over the next few years, a process quickened if they are exposed to heat such as in forest fires. The cones open wide to allow the seeds to disperse. The seeds are long, with a wing, and are wind- dispersed.Nahal, I. (1962). Le Pin d'Alep (''Pinus halepensis'' Miller). Étude taxonomique, phytogéographique, écologique et sylvicole. ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dana Nature - Panoramio (6)
Dana may refer to: People Given name * Dana (given name) Surname * Dana (surname) * Dana family of Cambridge, Massachusetts ** James Dwight Dana (1813–1895), scientist, zoological author abbreviation Dana Nickname or stage name * Dana International, stage name of singer Sharon Cohen * Dana Shum, the Shaw Brothers Hong Kong actress from 1973 to 1979 * Dana, stage name of Dana Rosemary Scallon (born 1951), Irish singer and former politician * Dana (South Korean singer) (born 1986), South Korean pop singer Places Ancient world * Ancient Dana or Tyana in Cappadocia, capital of a Neo-Hittite kingdom in the 1st millennium BC * Ancient Dana possibly associated with Tynna in Cappadocia Canada * CFS Dana, a former military radar installation in Saskatchewan, Canada * Dana Lake, a lake in Eeyou Istchee Baie-James, Quebec, Canada Ethiopia * Dana, Ethiopia, a village Iran * Dana County, an administrative subdivision of Iran * Dana Rural District, an administrative subdi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and 45 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arabian Plate
The Arabian Plate is a minor tectonic plate in the Northern and Eastern Hemispheres. It is one of the three continental plates (along with the African and the Indian Plates) that have been moving northward in geological history and colliding with the Eurasian Plate. That is resulting in a mingling of plate pieces and mountain ranges extending in the west from the Pyrenees, crossing Southern Europe to Iran, forming the Alborz and the Zagros Mountains, to the Himalayas and ranges of Southeast Asia. Lexicology The ''Arabian Plate'' is a designation of the region, and it is also sometimes referred to as the ''Arab Plate''. Borders The Arabian Plate consists mostly of the Arabian Peninsula; it extends westward to the Sinai Peninsula and the Red Sea and northward to the Levant. The plate borders are: *East, with the Indian Plate, at the Owen Fracture Zone *South, with the African Plate to the west and the Somali Plate and the Indian Plate to the east *West, a left lateral fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868). During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans (''Homo habilis'') appeared in Africa near the end of the period. Some continental movements took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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