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Stirling Castle
Stirling Castle, located in Stirling, is one of the largest and most important castles in Scotland, both historically and architecturally. The castle sits atop Castle Hill, an intrusive crag, which forms part of the Stirling Sill geological formation. It is surrounded on three sides by steep cliffs, giving it a strong defensive position. Its strategic location, guarding what was, until the 1890s, the farthest downstream crossing of the River Forth, has made it an important fortification in the region from the earliest times. Most of the principal buildings of the castle date from the fifteenth and sixteenth centuries. A few structures remain from the fourteenth century, while the outer defences fronting the town date from the early eighteenth century. Before the union with England, Stirling Castle was also one of the most used of the many Scottish royal residences, very much a palace as well as a fortress. Several Scottish Kings and Queens have been crowned at Stirling, in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Historic Environment Scotland
Historic Environment Scotland (HES) ( gd, Àrainneachd Eachdraidheil Alba) is an executive non-departmental public body responsible for investigating, caring for and promoting Scotland's historic environment. HES was formed in 2015 from the merger of government agency Historic Scotland with the Royal Commission on the Ancient and Historical Monuments of Scotland (RCAHMS). Among other duties, Historic Environment Scotland maintains more than 300 properties of national importance including Edinburgh Castle, Skara Brae and Fort George. History The responsibilities of HES were formerly split between Historic Scotland, a government agency responsible for properties of national importance, and the Royal Commission on the Ancient and Historical Monuments of Scotland (RCAHMS), which collected and managed records about Scotland's historic environment. Under the terms of a Bill of the Scottish Parliament published on 3 March 2014, the pair were dissolved and their functions transferred ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Scottish Monarchs
The monarch of Scotland was the head of state of the Kingdom of Scotland. According to tradition, the first King of Scots was Kenneth I MacAlpin (), who founded the state in 843. Historically, the Kingdom of Scotland is thought to have grown out of an earlier "Kingdom of the Picts" (and later the Kingdom of Strathclyde that was conquered in the 11th century, becoming part of the new Kingdom of Scotland) though in reality the distinction is a product of later medieval myth and confusion from a change in nomenclature i.e. ('King of the Picts') becomes (King of Alba) under Donald II when annals switched from Latin to vernacular around the end of the 9th century, by which time the word in Scottish Gaelic had come to refer to the Kingdom of the Picts rather than Britain (its older meaning). The Kingdom of the Picts just became known as the Kingdom of Alba in Scottish Gaelic, which later became known in Scots and English as ''Scotland''; the terms are retained in both langua ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Penda Of Mercia
Penda (died 15 November 655)Manuscript A of the ''Anglo-Saxon Chronicle'' gives the year as 655. Bede also gives the year as 655 and specifies a date, 15 November. R. L. Poole (''Studies in Chronology and History'', 1934) put forward the theory that Bede began his year in September, and consequently November 655 would actually fall in 654; Frank Stenton also dated events accordingly in his ''Anglo-Saxon England'' (1943). 1 Others have accepted Bede's given dates as meaning what they appear to mean, considering Bede's year to have begun on 25 December or 1 January (see S. Wood, 1983: "Bede's Northumbrian dates again"). The historian D. P. Kirby suggested the year 656 as a possibility, alongside 655, in case the dates given by Bede are off by one year (see Kirby's "Bede and Northumbrian Chronology", 1963). The ''Annales Cambriae'' gives the year as 657Annales Cambriae at Fordham University/ref> was a 7th-century king of Mercia, the Anglo-Saxon kingdom in what is today the Midland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manaw Gododdin
Manaw Gododdin was the narrow coastal region on the south side of the Firth of Forth, part of the Brythonic-speaking Kingdom of Gododdin in the post-Roman Era. It is notable as the homeland of Cunedda prior to his conquest of North Wales, and as the homeland of the heroic warriors in the literary epic '' Y Gododdin''. Pressed by the Picts expanding southward and the Northumbrians expanding northward, it was permanently destroyed in the 7th century and its territory absorbed into the then-ascendant Kingdom of Northumbria. The lands both south and north of the Firth of Forth were known as 'Manaw', but from the post-Roman Era forward, only the southern side is referred to as Manaw Gododdin, the Manaw associated with the people of Gododdin. Manaw Gododdin was adjacent to – and possibly included in – Eidyn, the region surrounding modern Edinburgh. Though Manaw Gododdin was located within the territory of modern Scotland, as a part of ''Yr Hen Ogledd'' ( en, The Old North) it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maeatae
The Maeatae were a confederation of tribes that probably lived beyond the Antonine Wall in Roman Britain. The historical sources are vague as to the exact region they inhabited, but an association is thought to be indicated in the names of two hills with fortifications. Near the summit of Dumyat hill in the Ochils, overlooking Stirling, there are remains of a fort and the name of the hill (in Gaelic ''Dùn Mhèad'') is believed to derive from name meaning the hill of the Maeatae. The prominent hill fort may have marked their northern boundary, but Myot Hill, near Fankerton, plausibly marks their southern limits. A discussion of two views of the importance of Dumyat and Myot Hill is given in Wainwright. Cassius Dio describes them in detail in his ''Roman History'' (Book LXXVII), and is later quoted by Joseph Ritson and others. John Rhys seems convinced that they occupied the land between the Firth of Forth and the Firth of Tay or parts of what is now Clackmannanshire, Fife and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Doune
Doune (; from Scottish Gaelic: ''An Dùn'', meaning 'the fort') is a burgh within Perthshire. The town is administered by Stirling Council. Doune is assigned Falkirk postcodes starting "FK". The village lies within the parish of Kilmadock and mainly within the area surrounded by the River Teith and Ardoch Burn. In the 2001 Scottish census, 2.75% residents of Doune could speak Scottish Gaelic. Doune has a small primary school with 183 pupils on the roll (June 2016), drawn from a catchment area which extends outside the town, especially to the north. It is located on the site of Doune Roman fort. Gaelic is taught in Primary 1–7 and Spanish is now taught from P5 upwards . History The town is dominated by Doune Castle, built in the late 14th century. Architecturally it is a mixture of fortress and manor house. Bonnie Prince Charlie passed through Doune in 1745. Doune was also famous for its manufacture of pistols, but this eventually ceased due to the competition of manufa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roman Britain
Roman Britain was the period in classical antiquity when large parts of the island of Great Britain were under occupation by the Roman Empire. The occupation lasted from AD 43 to AD 410. During that time, the territory conquered was raised to the status of a Roman province. Julius Caesar invaded Britain in 55 and 54 BC as part of his Gallic Wars. According to Caesar, the Britons had been overrun or culturally assimilated by other Celtic tribes during the British Iron Age and had been aiding Caesar's enemies. He received tribute, installed the friendly king Mandubracius over the Trinovantes, and returned to Gaul. Planned invasions under Augustus were called off in 34, 27, and 25 BC. In 40 AD, Caligula assembled 200,000 men at the Channel on the continent, only to have them gather seashells ('' musculi'') according to Suetonius, perhaps as a symbolic gesture to proclaim Caligula's victory over the sea. Three years later, Claudius directed f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hill Fort
A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roman period. The fortification usually follows the contours of a hill and consists of one or more lines of earthworks, with stockades or defensive walls, and external ditches. Hillforts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC, and were used in many Celtic areas of central and western Europe until the Roman conquest. Nomenclature The spellings "hill fort", "hill-fort" and "hillfort" are all used in the archaeological literature. The ''Monument Type Thesaurus'' published by the Forum on Information Standards in Heritage lists ''hillfort'' as the preferred term. They all refer to an elevated site with one or more ramparts made of earth, stone and/or wood, with an external ditch. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crag And Tail
A crag (sometimes spelled cragg, or in Scotland craig) is a rocky hill or mountain, generally isolated from other high ground. Origin Crags are formed when a glacier or ice sheet passes over an area that contains a particularly resistant rock formation (often granite, a volcanic plug or some other volcanic structure). The force of the glacier erodes the surrounding softer material, leaving the rocky block protruding from the surrounding terrain. Frequently the crag serves as a partial shelter to softer material in the wake of the glacier, which remains as a gradual fan or ridge forming a tapered ramp (called the tail) up the leeward side of the crag. In older examples, or those latterly surrounded by the sea, the tail is often missing, having been removed by post-glacial erosion. Examples Examples of crag and tail formations include: * Castle Rock (the crag, site of Edinburgh Castle) and the Royal Mile (the tail), in Edinburgh, Scotland * Salisbury Crags and Arthur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciation
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 pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartz-dolerite
Quartz dolerite or quartz diabase is an intrusive rock similar to dolerite (also called diabase), but with an excess of quartz. Dolerite is similar in composition to basalt, which is volcanic, and gabbro, which is plutonic. The differing crystal sizes are due to the different rate of cooling, basalt cools quickly and has a very fine structure, while gabbro cools very slowly, at great depth, and large crystals develop. Dolerite is intermediate. Quartz dolerite is very common in central Scotland, in intrusive formations, sills and dykes, and is widely quarried for roadstone. It was used with some success for making millstones at one time, the Millstone Grit part of the carboniferous strata not being present in Scotland, but it is no longer used for this purpose, and would probably be illegal now due to the formation of small quartz and other silicate particles, which could cause the serious respiratory disease silicosis Silicosis is a form of occupational lung disease caused ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scheduled Ancient Monument
In the United Kingdom, a scheduled monument is a nationally important archaeological site or historic building, given protection against unauthorised change. The various pieces of legislation that legally protect heritage assets from damage and destruction are grouped under the term "designation." The protection provided to scheduled monuments is given under the Ancient Monuments and Archaeological Areas Act 1979, which is a different law from that used for listed buildings (which fall within the town and country planning system). A heritage asset is a part of the historic environment that is valued because of its historic, archaeological, architectural or artistic interest. Only some of these are judged to be important enough to have extra legal protection through designation. There are about 20,000 scheduled monuments in England representing about 37,000 heritage assets. Of the tens of thousands of scheduled monuments in the UK, most are inconspicuous archaeological sites, but s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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