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Mount Pentelicus
Mount Pentelicus or Pentelikon (, or ) is a mountain in Attica, Greece, situated northeast of Athens and southwest of Marathon. Its highest point is the peak ''Pyrgari'', with an elevation of 1,109 m. The mountain is covered in large part with forest (about 60 or 70%), and can be seen from southern Athens (Attica), the Pedia plain, Parnitha, and the southern part of the northern suburbs of Athens. Houses surround the mountain, especially in Vrilissia, Penteli, Ekali, Dionysos and north of Gerakas. Marble from Mount Pentelicus is of exceptionally high quality and was used to construct much of the Athenian Acropolis. Later, Pentelic marble was exported to Rome, where it was used in construction and in sculptures. In ancient times it was also called Brilissos or Brilittos (, ) which is the origin of the name of the nearby suburb of Vrilissia. Mountain Mount Pentelicus has been famous for its marble since antiquity. Pentelic marble was used for the construction of buildings in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Penteli, Greece
Penteli ( el, Πεντέλη) is a village and a municipality in the North Athens regional unit, Attica, Greece. It belongs to the Athens rural area. It takes its name from Mount Pentelicus. Municipality The municipality Penteli was formed at the 2011 local government reform by the merger of the following 3 former municipalities, that became municipal units: *Melissia *Nea Penteli *Penteli Geography Penteli is situated on the southern slopes of the limestone Penteli mountains. The municipality has an area of 36.064 km2, the municipal unit Penteli 28.878 km2. It is 14 km northeast of central Athens. Some of the neighbourhoods of Penteli are Agia Triada, Agios Dimitrios, Daou and Kallithea. History The bones of prehistoric animals - mastodons, rhinoceros, antelope, and giraffe, along with giant turtles, hyenas and other animals no longer extant in the area - have been found among the limestone crags of the mountain that looms over the present suburb of Athens. The Penteli moun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Acropolis Restoration Project
An acropolis was the settlement of an upper part of an ancient Greek city, especially a citadel, and frequently a hill with precipitous sides, mainly chosen for purposes of defense. The term is typically used to refer to the Acropolis of Athens, yet every Greek city had an acropolis of its own. Acropoloi were used as religious centers and places of worship, forts, and places in which the royal and high-status resided. Acropolises became the nuclei of large cities of classical ancient times, and served as important centers of a community. Some well-known acropoloi have become the centers of tourism in present-day, and, especially, the Acropolis of Athens has been a revolutionary center for the studies of ancient Greece since the Mycenaean period. Many of them have become a source of revenue for Greece, and represent some great technology during the period. Origin An acropolis is defined by the Greek definition of ἀκρόπολις, akropolis; from akros (άκρος) or (άκ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Markopoulo Mesogaias
Markopoulo Mesogaias ( el, Μαρκόπουλο Μεσογαίας) is a suburban town and a municipality in East Attica, Greece. The municipality has an area of . Geography The municipality Markopoulo Mesogaias is situated in the Mesogaia plain, in the eastern part of the Attica peninsula, and touches the Aegean Sea coast in the east, where the port town Porto Rafti is located. The town Markopoulo is in the western part of the municipality, at about elevation. It is north of Kalyvia Thorikou, east of Koropi and southeast of Athens city centre. Greek National Road 89 (Gerakas - Koropi - Lavrio - Sounio) passes through Markopoulo. Athens International Airport is north of the town. Markopoulo had a railway station on the Athens–Lavrion Railway, which closed for passenger traffic in 1957. Settlements *Agía Triáda (2011 census pop. 218) *Vravróna, ancient Brauron (pop. 195) - located in the northeast by the Aegean Sea *Chamoliá (pop. 185) *Koulidás (pop. 243) *Markópo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keratea
Keratea ( el, Κερατέα) is a town in East Attica, Greece. Since the 2011 local government reform it is part of the municipality Lavreotiki, of which it is a municipal unit. The municipal unit has an area of 129.864 km2. It is part of Athens metropolitan area. Geography Keratea is situated in the hills in the southeastern part of the Attica peninsula, 6 km west of the Aegean Sea coast, at about 200 m elevation. It lies at the northern foot of . It is 5 km southeast of Kalyvia Thorikou, 12 km northwest of Lavrio and 29 km southeast of Athens city centre. Greek National Road 89 (Gerakas - Koropi - Lavrio - Sounio) passes through Keratea. In antiquity, the area of present Keratea was part of the deme Cephale, of the phyle Acamantis in Mesogeia area of Ancient Athens. Historical population The town has historically been an Arvanites, Arvanite settlement. Historical monuments The church of St. Athanasius (Kronizes). A wall painting monument (1744 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drafi
Drafi ( el, Ντράφι) is a residential settlement located in a semi-mountainous slopped region in the municipal unit of Pikermi, in the municipality Rafina–Pikermi, East Attica, Greece. It is situated east of Athens city center, on the slopes of the Penteliko Mountain. It was initially developed as a housing project for the Agricultural Worker Cooperarative "Pan" . It is bordering Pikermi, Dioni, Penteli, Anthousa and Pallini. Drafi is considered a middle-scale residential area, with many detached houses and luxury mansions. Its developmental stage peaked during 2000-2004, when large scale infrastructure works in East Attica, such as the new international airport in Spata, increased interest for new residences in the wider area. The road network is highly slopped and not fully developed, although Drafi offers a few wider roads than its neighbouring Dioni, such as Achaion St, connecting Drafi with Penteli and Anthousa. Drafi is also well connected towards the center of Pik ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anixi
Anoixi ( el, Άνοιξη, meaning "spring") is a suburban town in East Attica, Greece. Since the 2011 local government reform it is part of the municipality Dionysos, of which it is a municipal unit. The municipal unit has an area of 4.582 km2. Geography Anoixi is situated in the hills in the northeastern part of the Athens conurbation, at about 370 m elevation. It lies east of the Parnitha mountains and northwest of the Penteliko Mountain. It is 1 km south of Agios Stefanos, 9 km west of Marathon and 20 km northeast of Athens city centre. Its built-up area is continuous with those of the neighbouring suburbs Agios Stefanos, Drosia and Stamata. Motorway 1 (Athens - Lamia - Thessaloniki) and the railway from Athens to Thessaloniki pass west of the town. Greek National Road 83 (Athens - Marathon - Rafina) passes through Anoixi. Historical population See also *List of municipalities of Attica A ''list'' is any set of items in a row. List or lists may ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elgin Marbles
The Elgin Marbles (), also known as the Parthenon Marbles ( el, Γλυπτά του Παρθενώνα, lit. "sculptures of the Parthenon"), are a collection of Classical Greek marble sculptures made under the supervision of the architect and sculptor Phidias and his assistants. They are original parts of the Parthenon and other sacred and ceremonial structures built on the Acropolis of Athens in the 5th century BCE. The collection is on display in the British Museum, in the purpose-built Duveen Gallery. The presence of the Elgin Marbles in the British Museum is the subject of international controversy. From 1801 to 1812, agents of Thomas Bruce, 7th Earl of Elgin removed about half of the surviving sculptures of the Parthenon, as well as sculptures from the Propylaea and Erechtheion,''Encyclopædia Britannica'', "Elgin Marbles", 2008, O.Ed. and had them transported by sea to Britain. Elgin argued as his authority for this that he had obtained an official decree (a firman) fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Δ18O
In geochemistry, paleoclimatology and paleoceanography ''δ''18O or delta-O-18 is a measure of the ratio of stable isotope The term stable isotope has a meaning similar to stable nuclide, but is preferably used when speaking of nuclides of a specific element. Hence, the plural form stable isotopes usually refers to isotopes of the same element. The relative abundanc ...s oxygen-18 (18O) and oxygen-16 (16O). It is commonly used as a measure of the temperature of precipitation (meteorology), precipitation, as a measure of groundwater/mineral interactions, and as an indicator of processes that show isotope fractionation, isotopic fractionation, like methanogenesis. In paleosciences, 18O:16O data from corals, foraminifera and ice cores are used as a proxy (climate), proxy for temperature. The definition is, in "per mil" (‰, parts per thousand): :\delta \ce = \left( \frac - 1 \right) \times 1000 ‰ where the standard has a known isotopic composition, such as Vienna Standard ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Δ13C
In geochemistry, paleoclimatology, and paleoceanography ''δ''13C (pronounced "delta c thirteen") is an isotopic signature, a measure of the ratio of stable isotopes 13C : 12C, reported in parts per thousand (per mil, ‰). The measure is also widely used in archaeology for the reconstruction of past diets, particularly to see if marine foods or certain types of plants were consumed The definition is, in per mil: :\delta \ce = \left( \frac - 1 \right) \times 1000 ‰ where the standard is an established reference material. ''δ''13C varies in time as a function of productivity, the signature of the inorganic source, organic carbon burial, and vegetation type. Biological processes preferentially take up the lower mass isotope through kinetic fractionation. However some abiotic processes do the same, methane from hydrothermal vents can be depleted by up to 50%. Reference standard The standard established for carbon-13 work was the Pee Dee Belemnite (PDB) and was based on a Cr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clastic Rock
Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock. A clast is a fragment of geological detritus,Essentials of Geology, 3rd Ed, Stephen Marshak, p. G-3 chunks, and smaller grains of rock broken off other rocks by physical weathering.Essentials of Geology, 3rd Ed, Stephen Marshak, p. G-5 Geologists use the term clastic to refer to sedimentary rocks and particles in sediment transport, whether in suspension or as bed load, and in sediment deposits. Sedimentary clastic rocks Clastic sedimentary rocks are rocks composed predominantly of broken pieces or ''clasts'' of older weathered and eroded rocks. Clastic sediments or sedimentary rocks are classified based on grain size, clast and cementing material (matrix) composition, and texture. The classification factors are often useful in determining a sample's environment of deposition. An example of clastic environment would be a river system in which the full range of grains being transported by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calcite
Calcite is a Carbonate minerals, carbonate mineral and the most stable Polymorphism (materials science), polymorph of calcium carbonate (CaCO3). It is a very common mineral, particularly as a component of limestone. Calcite defines hardness 3 on the Mohs scale of mineral hardness, based on Scratch hardness, scratch hardness comparison. Large calcite crystals are used in optical equipment, and limestone composed mostly of calcite has numerous uses. Other polymorphs of calcium carbonate are the minerals aragonite and vaterite. Aragonite will change to calcite over timescales of days or less at temperatures exceeding 300 °C, and vaterite is even less stable. Etymology Calcite is derived from the German ''Calcit'', a term from the 19th century that came from the Latin word for Lime (material), lime, ''calx'' (genitive calcis) with the suffix "-ite" used to name minerals. It is thus etymologically related to chalk. When applied by archaeology, archaeologists and stone trade pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Accessory Mineral
In geology and mineralogy, a mineral or mineral species is, broadly speaking, a solid chemical compound with a fairly well-defined chemical composition and a specific crystal structure that occurs naturally in pure form.John P. Rafferty, ed. (2011): Minerals'; p. 1. In the series ''Geology: Landforms, Minerals, and Rocks''. Rosen Publishing Group. The geological definition of mineral normally excludes compounds that occur only in living organisms. However, some minerals are often biogenic (such as calcite) or are organic compounds in the sense of chemistry (such as mellite). Moreover, living organisms often synthesize inorganic minerals (such as hydroxylapatite) that also occur in rocks. The concept of mineral is distinct from rock, which is any bulk solid geologic material that is relatively homogeneous at a large enough scale. A rock may consist of one type of mineral, or may be an aggregate of two or more different types of minerals, spacially segregated into distinct ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
