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Promontory Fort
A promontory fort is a defensive structure located above a steep cliff, often only connected to the mainland by a small neck of land, thus using the topography to reduce the ramparts needed. Although their dating is problematic, most seem to date to the Iron Age. They are mainly found in Brittany, Ireland, the Orkney Islands, the Isle of Man, Devon, the Channel Islands and Cornwall. Ireland Only a few Irish promontory forts have been excavated and most date to the Iron Age, though some, like Dunbeg Fort (County Kerry) might have originated in the Bronze Age. Others, like Dalkey Island (County Dublin) contain imported Eastern Mediterranean pottery and have been reoccupied and changed in the early medieval period. Some, like Doonmore (near Dingle, County Kerry) are associated with the Middle Ages. Dunbeg contains an early medieval corbelled stone hut (clochán). Isle of Man On the Isle of Man, promontory forts are found particularly on the rocky slate headlands of the south. F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Medieval
In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the Post-classical, post-classical period of World history (field), global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern history, modern period. The medieval period is itself subdivided into the Early Middle Ages, Early, High Middle Ages, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralized authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Penwith
Penwith (; kw, Pennwydh) is an area of Cornwall, England, United Kingdom, located on the peninsula of the same name. It is also the name of a former Non-metropolitan district, local government district, whose council was based in Penzance. The area is named after one of the ancient administrative hundreds of Cornwall which derives from two Cornish language, Cornish words, ''penn'' meaning 'headland' and ''wydh'' meaning 'at the end'. Natural England have designated the peninsula as national character area 156 and named it West Penwith. It is also known as the Land's End Peninsula. Geography The Penwith peninsula sits predominantly on granite bedrock that has led to the formation of a rugged coastline with many fine beaches. The contact between the granite and the adjoining sedimentary rock (mostly shales) is most clearly seen forming the cliffs at Land's End, the most westerly point in the district and this geology has resulted in the mining that has made Cornwall famous. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Promontory Forts Of Cornwall
Cornish promontory forts, commonly known in Cornwall as cliff castles, are coastal equivalents of the hill forts and Cornish "rounds" found on Cornish hilltops and slopes. Similar coastal forts are found on the north–west European seaboard, in Normandy, Brittany and around the coastlines of the British Isles, especially in Wales, Scotland and Ireland. Many are known in southwest England, particularly in Cornwall and its neighbouring county, Devon. Two have been identified immediately west of Cornwall, in the Isles of Scilly. A promontory fort is a coastal headland, isolated from the mainland by one stone, turf or earthen rampart (a univallate fort), or more than one (a multivallate fort). Some promontory forts also have ditches, created by the excavation of material to form the rampart. British promontory forts were constructed during the Iron Age, and remained in more-or-less continuous use into the early Roman period. Their function remains uncertain. They would have off ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Rumps - Geograph
''The'' () is a grammatical article in English, denoting persons or things already mentioned, under discussion, implied or otherwise presumed familiar to listeners, readers, or speakers. It is the definite article in English. ''The'' is the most frequently used word in the English language; studies and analyses of texts have found it to account for seven percent of all printed English-language words. It is derived from gendered articles in Old English which combined in Middle English and now has a single form used with pronouns of any gender. The word can be used with both singular and plural nouns, and with a noun that starts with any letter. This is different from many other languages, which have different forms of the definite article for different genders or numbers. Pronunciation In most dialects, "the" is pronounced as (with the voiced dental fricative followed by a schwa) when followed by a consonant sound, and as (homophone of pronoun ''thee'') when followed by a v ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peel, Isle Of Man
Peel ( gv, Purt ny h-Inshey – Port of the Island) is a seaside town and small fishing port in the Isle of Man, in the historic parish of German but administered separately. Peel is the third largest town in the island after Douglas and Ramsey but the fourth largest settlement, as Onchan has the second largest population but is classified as a village. Until 2016 (when it was merged with Glenfaba) Peel was also a House of Keys constituency, electing one Member of the House of Keys (MHK), who, from September 2015, was Ray Harmer. Peel has a ruined castle on St Patrick's Isle, and a cathedral, seat of the Diocese of Sodor and Man (the diocese was founded when Mann was ruled by the Norse). Geography Peel is on the west coast of the Isle of Man, on the east side of the mouth of the River Neb. To the north west is St Patrick's Isle, connected to the mainland by a causeway, and to the west across the river is Peel Hill. The A1 road connects Peel with Douglas. The A4 and A3 roads c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
House Of Manannan
The House of Manannan is a museum in Peel in the Isle of Man. It is named after the "great mythological sea god" Manannan and covers the island's Celtic, Viking, and Maritime history. History The museum is located in the former Peel railway station. The original building was built in 1873 and closed in September 1968 with the closure of the Peel line between Douglas and Peel. In 1979 it was used to house '' Odin's Raven''. In 1997 the building was then repurposed and expanded to suit the needs of the museum at a cost of £5.5 million. Exhibitions The museum has several permanent exhibitions depicting the Celtic period of the Isle of Man to the modern era, such as a life size reconstruction of a Celtic roundhouse, as well as other attractions based from the 19th century, like a replication of a Peel street. Sea stories are also shared with visitors. One of its most notable attractions is ''Odin's Raven'', a recreation of a Viking longboat in two-thirds scale. Odin's Raven w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norsemen
The Norsemen (or Norse people) were a North Germanic ethnolinguistic group of the Early Middle Ages, during which they spoke the Old Norse language. The language belongs to the North Germanic branch of the Indo-European languages and is the predecessor of the modern Germanic languages of Scandinavia. During the late eighth century, Scandinavians embarked on a large-scale expansion in all directions, giving rise to the Viking Age. In English-language scholarship since the 19th century, Norse seafaring traders, settlers and warriors have commonly been referred to as Vikings. Historians of Anglo-Saxon England distinguish between Norse Vikings (Norsemen) from Norway who mainly invaded and occupied the islands north and north-west of Britain, Ireland and western Britain, and Danish Vikings, who principally invaded and occupied eastern Britain. Modern descendants of Norsemen are the Danes, Icelanders, Faroe Islanders, Norwegians, and Swedes, who are now generally referred to as "Sc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cronk Ny Merriu
''Cronk ny Merriu'' ( en, Hill of the Dead) is one of the remains of promontory forts in the Isle of Man. Close to Port Grenaugh, this site dates back almost 2,000 years. The bank and ditch of Iron Age date created a defensive promontory fort at ''Cronk ny Merriu''. Later, a rectangular building of Norse style and layout stood here, part of a system of coastal lookout posts. Several of the lookout posts, especially in Santon, where ''Cronk ny Merriu'' is situated, can be visited using the coastal footpath. All of the posts have a rampart on their vulnerable landward side, and excavations have shown that access to the fort was via a strongly built gate. The Scandinavians who arrived in Mann in the eighth and ninth centuries sometimes re-used these Iron Age promontory forts, often obliterating the old domestic quarters with their characteristic rectangular houses; the fine example at ''Cronk ny Merriu'' has been used as the basis of the reconstruction in the House of Manannan. Et ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raad Ny Foillan
' ( en, The Way of the Gull) is a coastal long distance footpath in the Isle of Man. Because it is a closed loop around the coast, it can be walked in either a clockwise or an anti-clockwise direction. Route and history The ' starts and finishes at the Millennium Bridge over Douglas Harbour. The path, which is in length, forms a complete loop around the Manx coast, waymarked with signs showing a gull on a blue background. The walk was created to mark the Island's "Heritage Year" celebrations in 1986 and generally follows the coast, passing through terrain varying from shingle beaches at the Ayres to over hills and cliffs. The route comprises the following sections: *Douglas to Castletown, including the Langness peninsula * Castletown to Port St Mary, *Port St Mary to Port Erin, *Port Erin to Peel, (this section can be shortened by leaving out Bradda Head and the Niarbyl) * Peel to Kirk Michael, *Kirk Michael to Jurby, *Jurby to Point of Ayre, *Point of Ayre to Rams ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Santon (parish)
Santon ( gv, Stondane), historically Santan, is one of the seventeen historic parishes of the Isle of Man. It is located in the south-east of the island (part of the traditional ''South Side'' division) in the sheading of Middle. Settlements in the parish include Newtown. Local government For the purposes of local government, the whole of the historic parish forms a single parish district with commissioners. The Captain of the Parish (since 2003) is Donald James Gelling, CBE. Politics Santon parish is part of the Middle constituency, which elects two members to the House of Keys. From 1986 until 2016 it was in the Malew and Santon constituency. Geography It has an area of approximately and is the island's smallest parish. The parish is now popularly known as Santon instead of the older Santan. Currently the Captain of the Parish is Mr Donald Gelling. To the north of the parish is Newtown and the recently built estate of Mount Murray where the northern border along th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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