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Ħaġar Qim
Ħaġar Qim (; "Standing/Worshipping Stones") is a megalithic temple complex found on the Mediterranean island of Malta, dating from the Ġgantija phase (3600-3200 BC). The Megalithic Temples of Malta are among the most ancient religious sites on Earth, described by the World Heritage Sites committee as "unique architectural masterpieces." In 1992 UNESCO recognized Ħaġar Qim and four other Maltese megalithic structures as World Heritage Sites. V. Gordon Childe, Professor of Prehistoric European Archeology and director of the Institute of Archaeology in the University of London from 1946-1957 visited Ħaġar Qim. He wrote, "I have been visiting the prehistoric ruins all round the Mediterranean, from Mesopotamia to Egypt, Greece and Switzerland, but I have nowhere seen a place as old as this one." Ħaġar Qim's builders used globigerina limestone in the temple's construction. As a result of this, the temple has suffered from severe weathering and surface flaking ove ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qrendi
Qrendi ( mt, Il-Qrendi) is a village in the Southern Region of Malta, with a population of 2752 people as of March 2014. It is located close to Mqabba, Żurrieq and Siggiewi. Within its boundaries are two well-known Neolithic temples called Mnajdra and Ħaġar Qim. In this village two feasts are held annually. The feast of Our Lady of Lourdes is celebrated either on the last Sunday of June or on the first Sunday of July, with 15 August the titular feast of the Ascension of Our Lady. This feast is popularly known as the feast of Santa Maria. Although the majority of the village's old core buildings remain today, Qrendi has changed considerably in recent times. A bypass road has been built to divert through-traffic away from the village, modern suburb developments has been built and an open space with a bus terminus being created in front of the Parish Church by removing the walled grounds from an old villa. History Fossilized remains of animals dating back to the Quaternary ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
UCL Institute Of Archaeology
UCL's Institute of Archaeology is an academic department of the Social & Historical Sciences Faculty of University College London (UCL) which it joined in 1986 having previously been a school of the University of London. It is currently one of the largest centres for the study of archaeology, cultural heritage and museum studies in the world, with over 100 members of staff and 600 students housed in a 1950s building on the north side of Gordon Square in the Bloomsbury area of Central London. History The Institute of Archaeology had its origins in Mortimer Wheeler's vision of a centre for archaeological training in the United Kingdom, which he conceived in the 1920s. Wheeler and Tessa Verney Wheeler, his wife and an archaeologist in her own right, lobbied colleagues and gathered funds to open the institute. The Wheeler's ambitions were realised when the institute was officially opened in 1937, with Mortimer Wheeler as its first director. Among its early members of staff were s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apse
In architecture, an apse (plural apses; from Latin 'arch, vault' from Ancient Greek 'arch'; sometimes written apsis, plural apsides) is a semicircular recess covered with a hemispherical vault or semi-dome, also known as an ''exedra''. In Byzantine, Romanesque, and Gothic Christian church (including cathedral and abbey) architecture, the term is applied to a semi-circular or polygonal termination of the main building at the liturgical east end (where the altar is), regardless of the shape of the roof, which may be flat, sloping, domed, or hemispherical. Smaller apses are found elsewhere, especially in shrines. Definition An apse is a semicircular recess, often covered with a hemispherical vault. Commonly, the apse of a church, cathedral or basilica is the semicircular or polygonal termination to the choir or sanctuary, or sometimes at the end of an aisle. Smaller apses are sometimes built in other parts of the church, especially for reliquaries or shrines of saints. Hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Retaining Wall
Retaining walls are relatively rigid walls used for supporting soil laterally so that it can be retained at different levels on the two sides. Retaining walls are structures designed to restrain soil to a slope that it would not naturally keep to (typically a steep, near-vertical or vertical slope). They are used to bound soils between two different elevations often in areas of terrain possessing undesirable slopes or in areas where the landscape needs to be shaped severely and engineered for more specific purposes like hillside farming or roadway overpasses. A retaining wall that retains soil on the backside and water on the frontside is called a seawall or a bulkhead. Definition A wall for holding in place a mass of earth or the like, as at the edge of a terrace or excavation. A retaining wall is a structure designed and constructed to resist the lateral pressure of soil, when there is a desired change in ground elevation that exceeds the angle of repose of the soil. A basement ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forecourt
Forecourt may refer to: * a courtyard at the front of a building * in racket sports, the front part of the court * the area in a filling station A filling station, also known as a gas station () or petrol station (), is a facility that sells fuel and engine lubricants for motor vehicles. The most common fuels sold in the 2010s were gasoline (or petrol) and diesel fuel. Ga ... containing the fuel pumps * chamber tomb forecourt, Stone Age architectural element See also * Forecourt Fountain, former name of Keller Fountain, Portland, Oregon, United States * Forecourt Piers, 123 Mortlake High Street, Richmond upon Thames, United Kingdom {{dab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Megalithic Architectural Elements
This article describes several characteristic architectural elements typical of European megalithic (Stone Age) structures. Forecourt In archaeology, a forecourt is the name given to the area in front of certain types of chamber tomb. Forecourts were probably the venue for ritual practices connected with the burial and commemoration of the dead in the past societies that built these types of tombs. In European megalithic architecture, forecourts are curved in plan with the entrance to the tomb at the apex of the open semicircle enclosure that the forecourt creates. The sides were built up by either large upright stones or walls of smaller stones laid atop one another. Some also had paved floors and some had blocking stones erected in front of them to seal the tomb such as at West Kennet Long Barrow. Their shape, which suggests an attempt to focus attention on the tomb itself may mean that they were used ceremonially as a kind of open air auditorium during ceremonies. Excavation w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trilithon
A trilithon or trilith is a structure consisting of two large vertical stones (posts) supporting a third stone set horizontally across the top (lintel). It is commonly used in the context of megalithic monuments. The most famous trilithons are those of Stonehenge in England. The word ''trilithon'' is derived from the Greek "having three stones" (τρι- ''tri-'' "three" + λίθος ''líthos'' "stone") and was first used in its modern archaelogical sense by William Stukeley. Other famous trilithons include those found in the Megalithic temples of Malta (which like Stonehenge are a UNESCO World Heritage Site), the Osireion in Egypt, and the Haʻamonga ʻa Maui in Tonga, Polynesia. The term is also used to describes the groups of three stones in the Hunebed tombs of the Netherlands. See also * Dolmen * Standing stone * Henge * Megalithic architectural elements This article describes several characteristic architectural elements typical of European megalithic (Sto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geologic Time Scale
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective is to precisely define ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene Period. The Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Major changes during the Oligocene included a global expansion o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
