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Forteviot Bronze Age Tomb
Forteviot Bronze Age tomb is a Bronze Age burial chamber discovered in 2009 at Forteviot near Perth, Scotland. The Bronze Age tomb is one of a number of archaeological digs at the site that Co-directors of the excavation, Dr. Gordon Noble of the University of Aberdeen, and professor Stephen Driscoll and Dr Kenneth Brophy, both of the University of Glasgow, are currently conducting. The excavation at Forteviot is part of a long-term collaborative study by the Strathearn Environs and Royal Forteviot (SERF) project – funded by Historic Scotland and the Perth and Kinross Heritage Trust – to study the archaeology of the former Pictish royal centre in the Strathearn region of what later became Central Scotland. Discovery and finds in Burial Chamber A high-status four-ton slab, forty centimetres thick and measuring two metres by two metres, was unearthed by archaeologists excavating at the site of a major Pictish Royal centre. Using a giant crane to remove the slab, known a ...
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Forteviot
Forteviot ( gd, Fothair Tabhaicht) (Ordnance Survey ) is a village in Strathearn, Scotland on the south bank of the River Earn between Dunning and Perth. It lies in the council area of Perth and Kinross. The population in 1991 was 160. The present village was rebuilt in the 1920s by John Alexander Dewar, 1st Baron Forteviot of the Dewar's whisky family. Early Bronze Age On 11 August 2009 archaeologists announced that they had discovered a royal tomb from the early Bronze Age at Forteviot. Along with the remains of the ancient ruler were found burial treasures which include a bronze and gold dagger, a wooden bowl and a leather bag. Archaeologists from Glasgow University and Aberdeen University continue to investigate the finds. The Pictish palace of Forteviot Forteviot is known to have been inhabited in the 9th century. King Cináed mac Ailpín (Kenneth mac Alpin or Kenneth I of Scotland) (d. 858), is said to have died in the 'palace' (''palacio'') there. The palace former ...
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Grave Goods
Grave goods, in archaeology and anthropology, are the items buried along with the body. They are usually personal possessions, supplies to smooth the deceased's journey into the afterlife or offerings to the gods. Grave goods may be classed as a type of votive deposit. Most grave goods recovered by archaeologists consist of inorganic objects such as pottery and stone and metal tools but organic objects that have since decayed were also placed in ancient tombs. The grave goods were to be useful to the deceased in the afterlife; therefore their favorite foods or everyday objects were left with them. Often times social status played a role in what was left and how often it was left. Funerary art is a broad term but generally means artworks made specifically to decorate a burial place, such as miniature models of possessions including slaves or servants for "use" in the afterlife. Although, in ancient Egypt they would sometimes bury the real servants with the deceased. Where grave ...
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Stonehenge
Stonehenge is a prehistoric monument on Salisbury Plain in Wiltshire, England, west of Amesbury. It consists of an outer ring of vertical sarsen standing stones, each around high, wide, and weighing around 25 tons, topped by connecting horizontal lintel stones. Inside is a ring of smaller bluestones. Inside these are free-standing trilithons, two bulkier vertical sarsens joined by one lintel. The whole monument, now ruinous, is aligned towards the sunrise on the summer solstice. The stones are set within earthworks in the middle of the densest complex of Neolithic and Bronze Age monuments in England, including several hundred ''tumuli'' (burial mounds). Archaeologists believe that Stonehenge was constructed from around 3000 BC to 2000 BC. The surrounding circular earth bank and ditch, which constitute the earliest phase of the monument, have been dated to about 3100 BC. Radiocarbon dating suggests that the first bluestones were raised between 2400 and 2200 BC, although ...
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Henge
There are three related types of Neolithic earthwork that are all sometimes loosely called henges. The essential characteristic of all three is that they feature a ring-shaped bank and ditch, with the ditch inside the bank. Because the internal ditches would have served defensive purposes poorly, henges are not considered to have been defensive constructions (cf. circular rampart). The three henge types are as follows, with the figure in brackets being the approximate diameter of the central flat area: # Henge (> ). The word ''henge'' refers to a particular type of earthwork of the Neolithic period, typically consisting of a roughly circular or oval-shaped bank with an internal ditch surrounding a central flat area of more than in diameter. There is typically little if any evidence of occupation in a henge, although they may contain ritual structures such as stone circles, timber circles and coves. Henge monument is sometimes used as a synonym for henge. Henges sometimes, but ...
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Kenneth MacAlpin
Kenneth MacAlpin ( mga, Cináed mac Ailpin, label= Medieval Gaelic, gd, Coinneach mac Ailpein, label=Modern Scottish Gaelic; 810 – 13 February 858) or Kenneth I was King of Dál Riada (841–850), King of the Picts (843–858), and the King of Alba (843–858) of likely Gaelic origin. He inherited the throne of Dál Riada from his father Alpín mac Echdach, founder of the Alpínid dynasty. Kenneth I conquered the kingdom of the Picts in 843–850 and began a campaign to seize all of Scotland and assimilate the Picts, for which he was posthumously nicknamed ''An Ferbasach'' ("The Conqueror"). Forteviot became the capital of his kingdom, and he also fought the Britons of the Kingdom of Strathclyde and the invading Vikings from Scandinavia. Kenneth also relocated relics including the Stone of Scone from an abandoned abbey on Iona to his new domain. Kenneth I is traditionally considered the founder of Scotland, which was then known as Alba, although like his immediate ...
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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 lan ...
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List Of Kings Of The Picts
The list of kings of the Picts is based on the Pictish Chronicle king lists. These are late documents and do not record the dates when the kings reigned. The various surviving lists disagree in places as to the names of kings, and the lengths of their reigns. A large portion of the lists, not reproduced here, belongs with the Caledonian or Irish mythology. The latter parts of the lists can largely be reconciled with other sources. Pictish kings Pictish kings ruled in northern and eastern Scotland. In 843 tradition records the replacement of the Pictish kingdom by the Kingdom of Alba, although the Irish annals continue to use ''Picts'' and ''Fortriu'' for half a century after 843. The king lists are thought to have been compiled in the early 8th century, probably by 724, placing them in the reigns of the sons of Der-Ilei, Bridei and Nechtan.Woolf, "Pictish matriliny reconsidered", p. 153. Irish annals (the Annals of Ulster, Annals of Innisfallen) refer to some kings as ''k ...
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Prehistory
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron A ...
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Radiocarbon Test
Radiocarbon dating (also referred to as carbon dating or carbon-14 dating) is a method for determining the age of an object containing organic material by using the properties of radiocarbon, a radioactive isotope of carbon. The method was developed in the late 1940s at the University of Chicago by Willard Libby. It is based on the fact that radiocarbon () is constantly being created in the Earth's atmosphere by the interaction of cosmic rays with atmospheric nitrogen. The resulting combines with atmospheric oxygen to form radioactive carbon dioxide, which is incorporated into plants by photosynthesis; animals then acquire by eating the plants. When the animal or plant dies, it stops exchanging carbon with its environment, and thereafter the amount of it contains begins to decrease as the undergoes radioactive decay. Measuring the amount of in a sample from a dead plant or animal, such as a piece of wood or a fragment of bone, provides information that can be us ...
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Filipendula Ulmaria
''Filipendula ulmaria'', commonly known as meadowsweet or mead wort, is a perennial herbaceous plant in the family Rosaceae that grows in damp meadows. It is native throughout most of Europe and Western Asia (Near east and Middle east). It has been introduced and naturalised in North America. Meadowsweet has also been referred to as queen of the meadow, pride of the meadow, meadow-wort, meadow queen, lady of the meadow, dollof, meadsweet, and bridewort. Description The stems, growing up to 120 cm, are tall, erect and furrowed, reddish to sometimes purple. The leaves are dark-green on the upper side and whitish and downy underneath, much divided, interruptedly pinnate, having a few large serrate leaflets and small intermediate ones. Terminal leaflets are large, 4–8 cm long, and three- to five-lobed. Meadowsweet has delicate, graceful, creamy-white flowers clustered close together in irregularly-branched cymes, having a very strong, sweet smell redolent of antisep ...
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Birch Bark
Birch bark or birchbark is the bark of several Eurasian and North American birch trees of the genus ''Betula''. The strong and water-resistant cardboard-like bark can be easily cut, bent, and sewn, which has made it a valuable building, crafting, and writing material, since pre-historic times. Today, birch bark remains a popular type of wood for various handicrafts and arts. Birch bark also contains substances of medicinal and chemical interest. Some of those products (such as betulin) also have fungicidal properties that help preserve bark artifacts, as well as food preserved in bark containers. Collection and storage Removing birch bark from live trees is harmful to tree health and should be avoided. Instead, it can be removed fairly easily from the trunk or branches of dead wood, by cutting a slit lengthwise through the bark and pulling or prying it away from the wood. The best time for collection is spring or early summer, as the bark is of better quality and most easi ...
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Quartz
Quartz is a hard, crystalline mineral composed of silica ( silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral definin ...
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