Callanish II
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Callanish II
The Callanish II stone circle ( gd, Cnoc Ceann a' Gharaidh) is one of many megalithic structures around the better-known (and larger) Calanais I on the west coast of the Isle of Lewis, in the Outer Hebrides, Scotland. Description Callanish II is situated on a ridge just 90 metres from the waters of Loch Roag. It is just a few hundred metres from the Callanish III stone circle. See also Callanish IV, Callanish VIII and Callanish X for other minor sites. The stone circle consists of thin standing stones arranged in the shape of an ellipse measuring 21.6 by 18.9 metres. Five of the stones are standing and two have fallen. The stones vary from 2 to 3.3 metres in height. A slab, 1.4 metres long, lies in front of the western stone, pointing towards the centre of the circle. The stone circle surrounds a cairn with a diameter of 8.5 metres. When 3 feet (1 metre) of peat was removed from the site in 1848, four holes were noticed, three grouped in an arc at the northwest, a fourth at the ...
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Isle Of Lewis
The Isle of Lewis ( gd, Eilean Leòdhais) or simply Lewis ( gd, Leòdhas, ) is the northern part of Lewis and Harris, the largest island of the Western Isles or Outer Hebrides archipelago in Scotland. The two parts are frequently referred to as if they were separate islands. The total area of Lewis is . Lewis is, in general, the lower-lying part of the island: the other part, Harris, is more mountainous. Due to its larger area and flatter, more fertile land, Lewis contains three-quarters of the population of the Western Isles, and the largest settlement, Stornoway. The island's diverse habitats are home to an assortment of flora and fauna, such as the golden eagle, red deer and seal, and are recognised in a number of conservation areas. Lewis has a Presbyterian tradition and a rich history. It was once part of the Norse Kingdom of the Isles. Today, life is very different from elsewhere in Scotland, with Sabbath observance, the Scottish Gaelic language and peat cutting retainin ...
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Callanish IV
The Callanish IV stone circle ( gd, Ceann Hulavig) is one of many megalithic structures around the better-known (and larger) Calanais I on the west coast of the Isle of Lewis, in the Outer Hebrides (Western Isles), Scotland. It is a scheduled monument and its official name is Sron a'Chail. The site was first surveyed and recorded by RCAHMS in 1914 and again in 2009, with another survey in the 1970s by other archaeologists, but no known archaeological excavations have taken place at the stones. Description Callanish IV is around two miles southeast of the Callanish Stones, about 180 metres west of the unfenced B8011 road. The nearest settlement is Garynahine to its northeast. The stone circle forms a pronounced oval measuring 13.3 by 9.5 metres. Only five stones currently stand, but there could have been as many as thirteen. The stones range in size from 2 to 2.7 metres. In the centre is a dilapidated cairn. A small slab, 60 centimetres high, is set on edge within the cair ...
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Archaeological Sites In The Outer Hebrides
Archaeology or archeology is the scientific study of human activity through the recovery and analysis of material culture. The archaeological record consists of artifacts, architecture, biofacts or ecofacts, sites, and cultural landscapes. Archaeology can be considered both a social science and a branch of the humanities. It is usually considered an independent academic discipline, but may also be classified as part of anthropology (in North America – the four-field approach), history or geography. Archaeologists study human prehistory and history, from the development of the first stone tools at Lomekwi in East Africa 3.3 million years ago up until recent decades. Archaeology is distinct from palaeontology, which is the study of fossil remains. Archaeology is particularly important for learning about prehistoric societies, for which, by definition, there are no written records. Prehistory includes over 99% of the human past, from the Paleolithic until the advent of ...
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Charcoal
Charcoal is a lightweight black carbon residue produced by strongly heating wood (or other animal and plant materials) in minimal oxygen to remove all water and volatile constituents. In the traditional version of this pyrolysis process, called charcoal burning, often by forming a charcoal kiln, the heat is supplied by burning part of the starting material itself, with a limited supply of oxygen. The material can also be heated in a closed retort. Modern "charcoal" briquettes used for outdoor cooking may contain many other additives, e.g. coal. This process happens naturally when combustion is incomplete, and is sometimes used in radiocarbon dating. It also happens inadvertently while burning wood, as in a fireplace or wood stove. The visible flame in these is due to combustion of the volatile gases exuded as the wood turns into charcoal. The soot and smoke commonly given off by wood fires result from incomplete combustion of those volatiles. Charcoal burns at a higher temper ...
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Peat
Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficient carbon sink on the planet, because peatland plants capture carbon dioxide (CO2) naturally released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of , which is the average depth of the boreal orthernpeatlands", which store around 415 gigatonnes (Gt) of carbon (about 46 times 2019 global CO2 emissions). Globally, peat stores up to 550 Gt of carbon, 42% of all soil carbon, which exceeds the carbon stored in all other vegetation types, including the world's forests, although it covers just 3% of the land's surface. ''Sphagnum'' moss, also called peat moss, is one of th ...
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Cairn
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ...
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RCAHMS
The Royal Commission on the Ancient and Historical Monuments of Scotland (RCAHMS) was an executive non-departmental public body of the Scottish Government that was "sponsored" inanced and with oversightthrough Historic Scotland, an executive agency of the Scottish Government. As one of the country's National Collections, it was responsible for recording, interpreting and collecting information about the built and historic environment. This information, which relates to buildings, sites, and ancient monuments of archaeological, architectural and historical interest (including maritime sites and underwater constructions), as well as historical aspects of the landscape, was then made available to the public, mainly at no cost. It was established (shortly ahead of parallel commissions for Wales and England) by a Royal Warrant of 1908, which was revised in 1992. The RCAHMS merged with government agency Historic Scotland to form Historic Environment Scotland, a new executive no ...
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Callanish X
The Callanish X stone circle (or "Na Dromannan", "Druim Nan Eun") is one of many megalithic structures around the more well-known and larger Calanais I on the west coast of the isle of Lewis, in the Western Isles of the Outer Hebrides, Scotland Scotland (, ) is a country that is part of the United Kingdom. Covering the northern third of the island of Great Britain, mainland Scotland has a border with England to the southeast and is otherwise surrounded by the Atlantic Ocean to the .... External links Calanais Excavations - Na Dromannan Archaeological sites in the Outer Hebrides Isle of Lewis Scheduled monuments in Scotland {{Scotland-struct-stub ...
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Callanish VIII
The Callanish VIII stone setting is one of many megalithic structures around the better-known (and larger) Calanais I on the west coast of the Isle of Lewis, in the Outer Hebrides (Western Isles), Scotland. It is also known locally as Tursachan."Great Bernera, 'Tursachan', Barraglom"
RCAHMS. Retrieved 22 June 2008. This is a very unusual (and possibly unique) setting, with a semicircle of four large stones on the edge of a cliff on the south of the island of
Great Bernera Great Bernera (; gd, Beàrnaraigh Mòr), often known just as Bernera ( gd, Beàrnaraigh), is an island and community in the Outer Hebrides of Scotland. With an area of just over , ...
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Callanish III
The Callanish III stone circle ( gd, Cnoc Fillibhir Bheag) is one of many megalithic structures around the better-known (and larger) Calanais I on the west coast of the Isle of Lewis, in the Outer Hebrides, Scotland. Description The stone circle consists of two concentric ellipses. The outer ring measures about 13.7 by 13.1 metres. It contains 13 stones, of which eight are still standing and five have fallen. The inner ring is a pronounced oval measuring 10.5 by 6.6 metres. Only four stones remain in the inner circle, the tallest of which measures 2.1 metres. There is no sign of a central mound or cairn. It is just a few hundred metres from the Callanish II stone circle. See also Callanish IV, Callanish VIII and Callanish X The Callanish X stone circle (or "Na Dromannan", "Druim Nan Eun") is one of many megalithic structures around the more well-known and larger Calanais I on the west coast of the isle of Lewis, in the Western Isles of the Outer Hebrides, Scotland ... ...
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Stone Circle
A stone circle is a ring of standing stones. Most are found in Northwestern Europe – especially in Britain, Ireland, and Brittany – and typically date from the Late Neolithic and Early Bronze Age, with most being built from 3000 BC. The best known examples include those at the henge monument at Avebury, the Rollright Stones, and elements within the ring of standing stones at Stonehenge. Scattered examples exist from other parts of Europe. Later, during the Iron Age, stone circles were built in southern Scandinavia. Stone circles are usually grouped in terms of the shape and size of the stones, the span of their radius, and their population within the local area. Although many theories have been advanced to explain their use, usually related to providing a setting for ceremony or ritual, no consensus exists among archaeologists regarding their intended function. Their construction often involved considerable communal effort, including specialist tasks such as planning, quar ...
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Loch Roag
''Loch'' () is the Scottish Gaelic, Scots and Irish word for a lake or sea inlet. It is cognate with the Manx lough, Cornish logh, and one of the Welsh words for lake, llwch. In English English and Hiberno-English, the anglicised spelling lough is commonly found in place names; in Lowland Scots and Scottish English, the spelling "loch" is always used. Many loughs are connected to stories of lake-bursts, signifying their mythical origin. Sea-inlet lochs are often called sea lochs or sea loughs. Some such bodies of water could also be called firths, fjords, estuaries, straits or bays. Background This name for a body of water is Insular CelticThe current form has currency in the following languages: Scottish Gaelic, Irish, Manx, and has been borrowed into Lowland Scots, Scottish English, Irish English and Standard English. in origin and is applied to most lakes in Scotland and to many sea inlets in the west and north of Scotland. The word comes from Proto-Indo-Europea ...
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