Achaemenid Architecture
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Achaemenid Architecture
Achaemenid architecture includes all architectural achievements of the Achaemenid Persians manifesting in construction of spectacular cities used for governance and inhabitation (Persepolis, Susa, Ecbatana), temples made for worship and social gatherings (such as Zoroastrian temples), and mausoleums erected in honor of fallen kings (such as the burial tomb of Cyrus the Great). Achaemenid architecture was influenced by Mesopotamian, Assyrian, Egyptian, Elamite, Lydian, Greek and Median architecture. Boardman J. ''Persia and the West: An Archaeological Investigation of the Genesis of Achaemenid Art''. Thames & Hudson. 2000. p. 102-122. André-Salvini B. ''Forgotten Empire: The World of Ancient Persia''. University of California Press. 2005. p. 54. Talebian M. H. ''Persia and Greece: The role of cultural interactions in the architecture of Persepolis-Pasargadae''. 2008. The quintessential feature of Persian architecture was its eclectic nature with foreign elements, yet produc ...
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Persian Column
Persian columns or Persepolitan columns are the distinctive form of column developed in the Achaemenid architecture of ancient Persia, probably beginning shortly before 500 BCE. They are mainly known from Persepolis, where the massive main columns have a base, fluted shaft, and a double-animal capital, most with bulls. Achaemenid palaces had enormous hypostyle halls called apadana, which were supported inside by several rows of columns. The Throne Hall or "Hall of a Hundred Columns" at Persepolis, measuring 70 × 70 metres was built by the Achaemenid king Artaxerxes I. The apadana hall is even larger. These often included a throne for the king and were used for grand ceremonial assemblies; the largest at Persepolis and Susa could fit ten thousand people at a time. The Achaemenids had little experience of stone architecture, but were able to import artists and craftsmen from around their empire to develop a hybrid imperial style drawing on influences from Mesopotamia, Egypt ...
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Persepolis
, native_name_lang = , alternate_name = , image = Gate of All Nations, Persepolis.jpg , image_size = , alt = , caption = Ruins of the Gate of All Nations, Persepolis. , map = , map_type = Iran#West Asia , map_alt = , map_caption = , map_size = , altitude_m = , altitude_ref = , relief = yes , coordinates = , map_dot_label = , location = Marvdasht, Fars Province, Iran , region = , type = Settlement , part_of = , length = , width = , area = , volume = , diameter = , circumference = , height = , builder = , and , material = Limestone, mud-brick, cedar wood , built = 6th century BC , abandoned = , epochs = Achaemenid Empire , cultures = Persian , dependency_of = , occupants = , event = *Battle of the ...
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Ancient Greek Architecture
Ancient Greek architecture came from the Greek-speaking people (''Hellenic'' people) whose culture flourished on the Greek mainland, the Peloponnese, the Aegean Islands, and in colonies in Anatolia and Italy for a period from about 900 BC until the 1st century AD, with the earliest remaining architectural works dating from around 600 BC. Ancient Greek architecture is best known from its temples, many of which are found throughout the region, with the Parthenon regarded, now as in ancient times, as the prime example. Most remains are very incomplete ruins, but a number survive substantially intact, mostly outside modern Greece. The second important type of building that survives all over the Hellenic world is the open-air theatre, with the earliest dating from around 525–480 BC. Other architectural forms that are still in evidence are the processional gateway ('' propylon''), the public square (''agora'') surrounded by storied colonnade ('' stoa''), the town council building ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for lime ...
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