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Long Meg And Her Daughters
Long Meg and Her Daughters is a Neolithic stone circle situated north-east of Penrith near Little Salkeld in Cumbria, North West England. One of around 1,300 stone circles in the British Isles and Brittany, it was constructed as a part of a megalithic tradition that emerged during Neolithic, and continued into the Early Bronze Age. Burl 2000. p. 13. The stone circle is the third widest in England, behind Avebury in Wiltshire, and only slightly smaller than Stanton Drew in Somerset. It consists of 59 stones (of which 27 remain upright) set in an east/west oval configuration measuring 340 ft (106 m) on its long axis. There may originally have been as many as 70 stones. Long Meg herself is a 12 ft (3.6 m) high monolith of red sandstone 80 ft (25 m) to the southwest of the circle made by her Daughters. Long Meg is marked with examples of megalithic art including a cup and ring mark, a spiral, and rings of concentric circles. Infra-red aerial photography has identi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Salkeld
Little Salkeld is a small village and former civil parish, now in the parish of Hunsonby, in the Eden district of Cumbria, England, a few miles to the north east of Penrith. In 1931 the civil parish had a population of 91. History The manor at Little Salkeld was confirmed by King Edward I in 1292. It is believed to be the original home of the Salkeld family of landowners. Little Salkeld was formerly a township in Addingham parish, from 1866 Little Salkeld was a civil parish in its own right until it was abolished on 1 April 1934 and merged with Hunsonby and Winskill to create Hunsonby. Places of interest ''Little Salkeld Watermill'', built in 1745, is a traditional English 18th-century water mill. It is Cumbria's only watermill still in full operation. Salkeld Hall is the village's largest house; built in the 16th century incorporating earlier walls. It is privately owned. The village contains a vicarage but no church - it was built for Addingham parish church one mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mayburgh Henge
Mayburgh Henge is a large prehistoric monument in the county of Cumbria in northern England. The henge is in the care of English Heritage and is a Scheduled Ancient Monument. It is 400 metres from King Arthur's Round Table Henge. Location The Ordnance Survey grid reference for Mayburgh Henge is . The henge is situated on a knoll just outside the village of Eamont Bridge close to the confluence of the Rivers Eamont and Lowther around 1 mile south of Penrith, just a few hundred yards from the M6 motorway. The henge sites are "to be seen as components in a landscape dominated by steep sided valleys and fast flowing streams...focused on a spring which lay between Mayburgh and King Arthur's Round Table, and which connected them to the River Eamont...on the other side of the Eamont are two less well known burial mounds." (The presence of the spring was noted by William Stukeley). The main communication routes of the time – "from Shap, from the Upper Eden, and down the Pet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratics
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhyolite
Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture, but may be porphyritic, containing larger mineral crystals ( phenocrysts) in an otherwise fine-grained groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase. It is the extrusive equivalent to granite. Rhyolitic magma is extremely viscous, due to its high silica content. This favors explosive eruptions over effusive eruptions, so this type of magma is more often erupted as pyroclastic rock than as lava flows. Rhyolitic ash-flow tuffs are among the most voluminous of continental igneous rock formations. Rhyolitic tuff has been extensively used for construction. Obsidian, which is rhyolitic volcanic glass, has been used for tools from prehistoric times to the present day because it can be shaped to an extremely sharp edge. Rhyolitic pumice finds use as an abrasive, in concrete, and as a soil amendment. Description Rhyolite i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lazonby
Lazonby is a village and civil parish in the Lower Eden Valley of Cumbria; it is located about north north-east of Penrith and 24 miles (38 km) south of the Scottish Borders. The total population of the ward of Lazonby, which also includes the nearby villages of North Dykes, Great Salkeld and Salkeld Dykes, was 1,425 at the time of the 2001 UK Census; this figure included 1,011 people between the ages of 16 and 74, of whom 675 were in employment. At the time of the 2011 Census, the population had decreased to 976. Description The village has one church, one chapel, two pubs (the Midland Hotel and the Joiner's Arms), a primary school, retained fire station, a Lakes & Dales Co-operative supermarket and post office, livestock auction mart, swimming pool and campsit Lazonby and Kirkoswald railway station, railway station (part of the Settle-Carlisle line) and the Bell's of Lazonby bakery complex. There is also an independent wooden toy shop, Croglin Toys & Designs (www.cr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thornborough Henges
The Thornborough Henges are an unusual ancient monument complex that includes the three aligned henges that give the site its name. The complex is located near the village of Thornborough, close to the town of Masham in North Yorkshire, England. The complex includes many large ancient structures including a cursus, henges, burial grounds and settlements. They are thought to have been part of a Neolithic and Bronze Age 'ritual landscape' comparable to Salisbury Plain and date from between 3500 and 2500 BC. This monument complex has been called 'The Stonehenge of the North'. Historic England considers its landscape comparable in ceremonial importance to better known sites such as Stonehenge, Avebury, and Orkney. In recent decades, there has been public concern about the impact on the ritual landscape of quarrying by Tarmac. Cursus The cursus is the oldest and largest ancient monument at Thornborough. It is almost a mile in extent and runs from Thornborough village, und ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Lowther
The River Lowther is a small river which flows through limestone rock in Cumbria, England. It is a tributary of the River Eamont which in turn is a tributary of the River Eden which flows into the Solway Firth near Carlisle. The Lowther begins with the confluence of the Keld Gill and the Keld Dub near the village of Keld. It flows north-west until it passes between Bampton and Bampton Grange, before turning north until it flows into the River Eamont close to Penrith. It is the main spawning area for Eden spring salmon, but is primarily a trout fishery. The river is held back by the Wet Sleddale dam, and so flows at a fairly consistent level (between 0.33 m and 1.8 m for 90% of monitoring time), with the highest level ever recorded at the River Lowther (2.93 m) occurring at Eamont Bridge, Beehive, on Sunday 6 December 2015. Its name is recorded about 1175 as ''Lauder''. It may come from Brittonic ''lǭwadr'', "a washing or bathing place", which would give it the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Eamont
The River Eamont is a river in Cumbria, England and one of the major tributaries of the River Eden. The name of the river is from Old English (ēa-gemōt) and is a back formation from Eamont Bridge which means the ''junction of streams.'' The river is formed by the outflow from Ullswater in the Lake District, later augmented by Dacre Beck from the west and the River Lowther which carries the water from Haweswater north to the Eamont at Penrith. It reaches the Eden east of Penrith. The river has flooded on numerous occasions, with the most recent being when Storm Desmond hit in December 2015. During the flooding, 300-year old Pooley Bridge was washed away and a temporary bridge had to be installed to reconnect the two halves of the village. The same storm caused damage to the grade I listed Eamont Bridge Eamont Bridge is a small village immediately to the south of Penrith, Cumbria, England. The village is named after the bridge over the River Eamont and straddles t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avenue (archaeology)
In prehistoric archaeology, an avenue is a long, parallel-sided strip of land, measuring up to about 30m in width, open at either end, with edges marked by stone or timber alignments and/or a low earth bank and ditch. The term is used for such features all over the British Isles but they are concentrated in the centre and south of England. Most are either short and straight (Type I, less than 800m long), or long and curving (Type II, up to 2.5 km). It has been noted that they often link stone circles with rivers. They are a common element to Bronze Age ritual landscapes. Avenues are identified through their earthworks or using aerial archaeology, as their parallel features can be seen stretching over some distance. In most examples, it is the association of the avenue with other contemporary monuments that provides diagnosis. Avenues differ from cursus monuments, in that the latter also have earthworks at their terminal ends and have no upright stone or timber alignment ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oddendale
Oddendale is a hamlet in Cumbria, England, near the large village of Shap. For transport there is the M6 motorway and the A6 road. History Oddendale stone circle Oddendale has a stone circle nearby, (), part of the complex of cairns, stone circles and standing stones that includes the ' Shap Stone Avenue' of monuments. The site has benefitted from an extensive and relatively recent (1997) excavation that revealed various stages in the monument's history: firstly, two concentric circles of oak wooden posts (dating to the Neolithic, c. 2,872–2,350 BC); followed by their removal and replacement with stone cappings of pink granite; followed by an Early Bronze Age ring cairn built over the inner circle surfaced with blue/gray stones and yellow/white pieces of flat limestone, with cremated bone, pottery and other 'token' grave goods; and then a fourth stage which saw the addition of a pink granite platform on to the side of the cairn, which itself had a kerb of red stones around it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shap Stone Avenue
The Shap Stone Avenue (an unofficial name) is a megalithic complex near Shap in Cumbria, England, comprising stone circles, a two-mile avenue (actually two avenues) of stones, and burial mounds. Location Shap Stone Avenue is one of three major complexes of megalithic monuments to be found in east Cumbria. The stone circles, henges, cairns and other standing stones in the area are often grouped at nodes of communication routes - the monuments around Shap form an 'avenue' running to the east of the River Lowther along a main route to the north; the Long Meg complex runs alongside the River Eden; Mayburgh Henge and the other henges run alongside the River Eamont near its confluence with the River Lowther. The OS grid reference of the Shap Avenue site can be given as , but the actual boundaries of the complex remain in doubt. Some stones have been lost, some natural erratics may have been added to the monument in historical times, and the various early accounts of the setting by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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