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Ħal Ä inwi Temple
The Ħal Ä inwi temple () was a prehistoric megalithic temple site located southeast of Å»ejtun, Malta dating back to the Ä gantija phase (3600–3200 BCE). The site is located in an area bearing the same name, or alternatively Ħal Ä ilwi, which is known for its archaeological remains, and lies around one kilometre from the Tas-SilÄ¡ multi-period sanctuary and archaeological site. History Remains of the temple at Ħal Ä inwi were found in the vicinity of San Niklaw chapel, to the right of the main road from Å»ejtun to Marsaxlokk, between Å»ejtun and the Tas-SilÄ¡ temple. The site is today represented by a few ashlar blocks still visible in a field wall. More remains may survive beneath the soil, since its excavation was superficial. The site was originally excavated by Albert V. Laferla in 1917. Architect Albert E. Vassallo drew the site during Laferla’s archaeological excavations. Themistocles Zammit, however, interpreted the remains as a possible domestic dwelling. J ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Architect
An architect is a person who plans, designs and oversees the construction of buildings. To practice architecture means to provide services in connection with the design of buildings and the space within the site surrounding the buildings that have human occupancy or use as their principal purpose. Etymologically, the term architect derives from the Latin ''architectus'', which derives from the Greek (''arkhi-'', chief + ''tekton'', builder), i.e., chief builder. The professional requirements for architects vary from place to place. An architect's decisions affect public safety, and thus the architect must undergo specialized training consisting of advanced education and a ''practicum'' (or internship) for practical experience to earn a Occupational licensing, license to practice architecture. Practical, technical, and academic requirements for becoming an architect vary by jurisdiction, though the formal study of architecture in academic institutions has played a pivotal role in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Largest Monoliths
This is a list of monoliths organized according to the size of the largest block of stone on the site. A monolith is a large stone which has been used to build a structure or monument, either alone or together with other stones. In this list at least one colossal stone over ten tons has been moved to create the structure or monument. In most cases ancient civilizations had little, if any, advanced technology that would help them move these monoliths. The most notable exception is that of the ancient Greeks and Romans, who had cranes and treadwheels to help lift colossal stones (see list of ancient Greek and Roman monoliths). This article also includes a list of modern experimental archaeology efforts to move colossal stones using technologies available to the respective ancient civilizations. Most of these weights are based on estimates by published scholars; however, there have been numerous false estimates of many of these stones presented as fact. To help recognize exaggerat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lipari
Lipari (; scn, Lìpari) is the largest of the Aeolian Islands in the Tyrrhenian Sea off the northern coast of Sicily, southern Italy; it is also the name of the island's main town and ''comune'', which is administratively part of the Metropolitan City of Messina. Its population is 12,821, but during the May to September tourist season, the total population may reach up to 20,000. Geography Lipari is the largest of a chain of islands in a volcanic archipelago situated in between Vesuvius and Etna. The island has a surface area of 37.6 km2 and is 30 km from Sicily. Besides the main town, most of the year-round population resides in one of the four main villages: Pianoconte is almost due west across the island, Quattropani in the northwest, Acquacalda along the northern coast, whereas Canneto is on the eastern shore north of Lipari town. The highest point on the island is Monte Chirica at 602 m (1975 ft). Geology Geologists agree on the fact that Lipari was created by a suc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Filicudi
Filicudi () is one of seven islands that make up the Aeolian archipelago, situated northeast of the island of Sicily, southern Italy. It is a ''frazione'' of the ''comune'' of Lipari. Geography Its total area is . There are several small villages on the island, which include Pecorini Mare and Valdichiesa. Filicudi's lands are capable of producing wine, olive oil, grain, and vegetables. In 1997, three quarters, approximately of Filicudi was turned into a Natural Reserve. The highest point is Monte Fossa Felci at . Other points include ''Monte Montagnola'' at and ''Monte Terrione'' at . At Capo Graziano are the remains of a Bronze Age village dating back to the second millennium BCE. Off the coast, the volcanic finger-like rock of La Canna rises about above the sea. History The modern name of "Filicudi" is a corruption of the ancient Greek name for the island, ''Phoenicusa'' (Phoenician island). The island, like the other Aeolian Islands, was settled since the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chert
Chert () is a hard, fine-grained sedimentary rock composed of microcrystalline or cryptocrystalline quartz, the mineral form of silicon dioxide (SiO2). Chert is characteristically of biological origin, but may also occur inorganically as a precipitation (chemistry), chemical precipitate or a diagenesis, diagenetic replacement, as in petrified wood. Chert is typically composed of the petrified remains of siliceous ooze, the biogenic sediment that covers large areas of the deep ocean floor, and which contains the silicon skeletal remains of diatoms, Dictyochales, silicoflagellates, and radiolarians. Precambrian cherts are notable for the presence of fossil cyanobacteria. In addition to Micropaleontology, microfossils, chert occasionally contains macrofossils. However, some chert is devoid of any fossils. Chert varies greatly in color (from white to black), but most often manifests as gray, brown, grayish brown and light green to rusty redW.L. Roberts, T.J. Campbell, G.R. Rapp Jr. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and start fires. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill'' Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along s and |
Maltese Language
Maltese ( mt, Malti, links=no, also ''L-Ilsien Malti'' or ''''), is a Semitic language derived from late medieval Sicilian Arabic with Romance superstrata spoken by the Maltese people. It is the national language of Malta and the only official Semitic and Afro-Asiatic language of the European Union. Maltese is a latinised variety of spoken historical Arabic through its descent from Siculo-Arabic, which developed as a Maghrebi Arabic dialect in the Emirate of Sicily between 831 and 1091. As a result of the Norman invasion of Malta and the subsequent re-Christianisation of the islands, Maltese evolved independently of Classical Arabic in a gradual process of latinisation. It is therefore exceptional as a variety of historical Arabic that has no diglossic relationship with Classical or Modern Standard Arabic. Maltese is thus classified separately from the 30 varieties constituting the modern Arabic macrolanguage. Maltese is also distinguished from Arabic and other Semitic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tal-Qadi Temple
Tal-Qadi Temple is a megalithic temple in Salina, limits of Naxxar, Malta. It is in a very bad state of preservation, with only the temple's general outline still visible. Site The site of Tal-Qadi was possibly in use around 4000 BC, during the Ä gantija phase of Maltese prehistory, but the temple itself was built during the Tarxien phase between 3300 and 3000 BC. The temple continued to be used during the Tarxien Cemetery phase, since pottery sherds from that era have been found. Tal-Qadi is the only temple in Malta which is orientated to the north-east. Most other temples face the south or south-east, but in the case of Tal-Qadi this would not have been possible since there is a steep slope in that direction. Today, the temple is in poor condition, with few remains visible apart from its general outline. The remains of a central area and two apses can still be seen. The temple probably contained another two apses, giving it a four-apse shape which was typical of the late te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Megalith
A megalith is a large stone that has been used to construct a prehistoric structure or monument, either alone or together with other stones. There are over 35,000 in Europe alone, located widely from Sweden to the Mediterranean sea. The word was first used in 1849 by the British antiquarian Algernon Herbert in reference to Stonehenge and derives from the Ancient Greek words "mega" for great and " lithos" for stone. Most extant megaliths were erected between the Neolithic period (although earlier Mesolithic examples are known) through the Chalcolithic period and into the Bronze Age. At that time, the beliefs that developed were dynamism and animism, because Indonesia experienced the megalithic age or the great stone age in 2100 to 4000 BC. So that humans ancient tribe worship certain objects that are considered to have supernatural powers. Some relics of the megalithic era are menhirs (stone monuments) and dolmens (stone tables). Types and definitions While "megalith" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsaxlokk
Marsaxlokk () is a small, traditional fishing village in the South Eastern Region of Malta. It has a harbour, and is a tourist attraction known for its views, fishermen and history. As at March 2014, the village had a population of 3,534. The village is also known for the Marsaxlokk Market, which is mainly a large fish market which takes place along the seafront on Sundays, and a tourist market during all other days of the week. Inhabited and well-known since antiquity, Marsaxlokk was used as a port by Phoenicians, Carthaginians and also has the remains of a Roman-era harbour. Originally a part of the city of Żejtun, the fishing village became a separate parish in the late nineteenth century. Traditional luzzi and other larger and more modern vessels line the sheltered inner harbour. The village is also popular among locals and tourists alike for its walks around the coast and harbour, its restaurants, as well as for its swimming zones. Marsaxlokk Bay also includes a contain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Megalithic Temples Of Malta
The Megalithic Temples of Malta ( mt, It-Tempji MegalitiÄ‹i ta' Malta) are several prehistoric temples, some of which are UNESCO World Heritage Sites, built during three distinct periods approximately between 3600 BC and 2500 BC on the island country of Malta. They had been claimed as the oldest free-standing structures on Earth until the discovery of Göbekli Tepe. Archaeologists believe that these megalithic complexes are the result of local innovations in a process of cultural evolution. This led to the building of several temples of the Ä gantija phase (3600–3000 BC), culminating in the large Tarxien temple complex, which remained in use until 2500 BC. After this date, the temple-building culture disappeared. The Ä gantija temples were listed as a UNESCO World Heritage Site in 1980. In 1992, the UNESCO Committee further extended the existing listing to include five other megalithic temple sites. These are ĦaÄ¡ar Qim (in Qrendi), Mnajdra (in Qrendi), Ta' ĦaÄ¡rat Temples (in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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