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East Burra
East Burra ( sco, East Burra; Old Norse: "Barrey"Anderson, Joseph (Ed.) (1893) ''Orkneyinga Saga''. Translated by Jón A. Hjaltalin & Gilbert Goudie. Edinburgh. James Thin and Mercat Press (1990 reprint). ) is one of the Scalloway Islands, a subgroup of the Shetland Islands in Scotland. It is connected by a bridge to West Burra. With an area of it is the twelfth largest of the Shetland Islands. East Burra has a much smaller population than West Burra and no substantial settlement; rather, there are a few hamlets and a scattering of individual croft houses. It is known for its Neolithic remains including a burnt mound, and for sea caves. The roofless, plain, Old Haa (manor or laird's house) of Houss is a prominent feature. From Houss, it is possible to walk the two kilometres or so to the cliffs at the southern end of the island. From there, the island of South Havra, nowadays home only to sheep and seabirds, can be clearly seen. East Burra is linked to the Shetland Mainl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Australia
South Australia (commonly abbreviated as SA) is a state in the southern central part of Australia. It covers some of the most arid parts of the country. With a total land area of , it is the fourth-largest of Australia's states and territories by area, and second smallest state by population. It has a total of 1.8 million people. Its population is the second most highly centralised in Australia, after Western Australia, with more than 77 percent of South Australians living in the capital Adelaide, or its environs. Other population centres in the state are relatively small; Mount Gambier, the second-largest centre, has a population of 33,233. South Australia shares borders with all of the other mainland states, as well as the Northern Territory; it is bordered to the west by Western Australia, to the north by the Northern Territory, to the north-east by Queensland, to the east by New South Wales, to the south-east by Victoria, and to the south by the Great Australian Bight.M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Cave
A sea cave, also known as a littoral cave, is a type of cave formed primarily by the wave action of the sea. The primary process involved is erosion. Sea caves are found throughout the world, actively forming along present coastlines and as relict sea caves on former coastlines. Some of the largest wave-cut caves in the world are found on the coast of Norway, but are now 100 feet or more above present sea level. These would still be classified as littoral caves. By contrast, in places like Thailand's Phang Nga Bay, solutionally formed caves in limestone have been flooded by the rising sea and are now subject to littoral erosion, representing a new phase of their enlargement. Some of the best-known sea caves are European. Fingal's Cave, on the island of Staffa in Scotland, is a spacious cave some 70 m long, formed in columnar basalt. The Blue Grotto of Capri, although smaller, is famous for the apparent luminescent quality of its water, imparted by light passing through underwater ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Broch
A broch is an Iron Age drystone hollow-walled structure found in Scotland. Brochs belong to the classification "complex Atlantic roundhouse" devised by Scottish archaeologists in the 1980s. Their origin is a matter of some controversy. Origin and definition The word ''broch'' is derived from Lowland Scots 'brough', meaning (among other things) fort. In the mid-19th century Scottish antiquaries called brochs 'burgs', after Old Norse ', with the same meaning. Place names in Scandinavian Scotland such as Burgawater and Burgan show that Old Norse ' is the older word used for these structures in the north. Brochs are often referred to as ''duns'' in the west. Antiquarians began to use the spelling ''broch'' in the 1870s. A precise definition for the word has proved elusive. Brochs are the most spectacular of a complex class of roundhouse buildings found throughout Atlantic Scotland. The Shetland Amenity Trust lists about 120 sites in Shetland as candidate brochs, while the Royal C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burra, Shetland
Burra (Old Norse: ''Barrey'' ) is the collective name for two of the Shetland Islands, West (pop. 753) and East Burra (pop. 66), which are connected by bridge to one another, and to the Shetland Mainland via Trondra. In addition, Burra was an ancient Civil parish that included smaller additional islands such as South Havra, Little Havra, Papa and the tidal island West Head of Papa. The civil parish of Burra was merged into the civil parish of Lerwick, along with Quarff and Gulberwick, in 1891. It continues to exist as Quoad sacra parish of the Church of Scotland. ''Collins Encyclopedia of Scotland'' suggests that the name is a corruption of "Borgarey" (island of the broch),Keay, J. & Keay, J. (1994) ''Collins Encyclopaedia of Scotland''. London. HarperCollins. and while this is unlikely, and no broch is extant, the place name Brough, on West Burra West Burra is one of the Scalloway Islands, a subgroup of the Shetland Islands in Scotland. It is connected by bridge to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bridge
A bridge is a structure built to span a physical obstacle (such as a body of water, valley, road, or rail) without blocking the way underneath. It is constructed for the purpose of providing passage over the obstacle, which is usually something that is otherwise difficult or impossible to cross. There are many different designs of bridges, each serving a particular purpose and applicable to different situations. Designs of bridges vary depending on factors such as the function of the bridge, the nature of the terrain where the bridge is constructed and anchored, and the material used to make it, and the funds available to build it. The earliest bridges were likely made with fallen trees and stepping stones. The Neolithic people built boardwalk bridges across marshland. The Arkadiko Bridge (dating from the 13th century BC, in the Peloponnese) is one of the oldest arch bridges still in existence and use. Etymology The '' Oxford English Dictionary'' traces the origin of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trondra
Trondra ( sco, Trondra) is one of the Scalloway Islands, a subgroup of the Shetland Islands in Scotland. It shelters the harbour of Scalloway and has an area of . History Trondra was becoming rapidly depopulated until 1970, when road bridges were built to neighbouring Burra (West and East) and to the southern peninsula of the Shetland Mainland. Since then the population has recovered from a low of 20 in 1961. A local community hall was opened in 1986. Composition Settlements on the island include: *Burland - Burland houses one of Shetland's most popular tourist attractions - the Burland Croft Trail. * Cauldhame * Cutts *Glendale * Scarfataing Geology Trondra is made up of steeply inclined dalradian rocks; mainly quartz and mica rich schists but with some crystalline limestone in the north which provide fertile soils around Cauldhame and Cutts. The hills are covered in grass and heather, with trees being few and far between, much like the rest of the Shetland Islands. Wildl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shetland Mainland
The Mainland is the main island of Shetland, Scotland. The island contains Shetland's only burgh, Lerwick, and is the centre of Shetland's ferry and air connections. Geography It has an area of , making it the third-largest Scottish island and the fifth largest of the British Isles after Great Britain, Ireland, Lewis and Harris and Skye. Mainland is the second most populous of the Scottish islands (only surpassed by Lewis and Harris), and had 18,765 residents in 2011 compared to 17,550 in 2001. The mainland can be broadly divided into four sections: *The long southern peninsula, south of Lerwick, has a mixture of moorland and farmland and contains many important archaeological sites. **Bigton, Cunningsburgh, Sandwick, Scalloway, and Sumburgh *The Central Mainland has more farmland and some woodland plantations. *The West Mainland **Aith, Walls, and Sandness *The North Mainland – in particular the large Northmavine peninsula, connected to Mainland by a narrow isthmus at Mav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Havra
South Havra ( sco, Sooth Haevra; non, Hafrey), formerly Hevera, is an uninhabited island in the Scalloway Islands, Shetland, Scotland. Geography and geology South Havra lies south of Burra and west of the southern peninsula of the Mainland. The island's rock is "epidiotic syenite with undifferentiated schist and gneiss." The soil is fairly fertile, but the lack of running water meant that, unusually for Shetland, the islanders resorted to building a windmill to grind corn. Geological features on the island include caves and natural arches. Little Havra is to its west. History Olaf Sinclair, foud (a kind of magistrate) of all Shetland lived here in the 16th century. The island's ruined windmill is an unusual sight in the Shetland Islands, especially as some have pointed out, that the Dutch Dutch commonly refers to: * Something of, from, or related to the Netherlands * Dutch people () * Dutch language () Dutch may also refer to: Places * Dutch, West Virginia, a comm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burnt Mound
A burnt mound is an archaeological feature consisting of a mound of shattered stones and charcoal, normally with an adjacent hearth and trough. The trough could be rock-cut, wood-lined or clay-lined to ensure it was watertight. Radiocarbon dates vary quite widely, the earliest being late Neolithic, with clusters of dates between 1900 and 1500 BC and 1200–800 BC, with some outliers in the Iron Age. There are also some dates that go into the Early Middle Ages. The technology used at burnt mounds has much greater antiquity and is found from the Palaeolithic onwards. Description and creation The shattered rock fragments are thought to be the remains of stones heated in fires, which were used to heat water. The shattering of the rock appears to have been the result of thermal shock when the heated stones were dropped into liquid, normally believed to be water. The mound is assumed to result from the periodic clearing out of the trough, with the stone fragments and charcoal be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mainland, Shetland
The Mainland is the main island of Shetland, Scotland. The island contains Shetland's only burgh, Lerwick, and is the centre of Shetland's ferry and air connections. Geography It has an area of , making it the third-largest Scottish island and the fifth largest of the British Isles after Great Britain, Ireland, Lewis and Harris and Skye. Mainland is the second most populous of the Scottish islands (only surpassed by Lewis and Harris), and had 18,765 residents in 2011 compared to 17,550 in 2001. The mainland can be broadly divided into four sections: *The long southern peninsula, south of Lerwick, has a mixture of moorland and farmland and contains many important archaeological sites. **Bigton, Cunningsburgh, Sandwick, Scalloway, and Sumburgh *The Central Mainland has more farmland and some woodland plantations. *The West Mainland **Aith, Walls, and Sandness *The North Mainland – in particular the large Northmavine peninsula, connected to Mainland by a narrow isthmus at ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
