A chambered cairn is a burial monument, usually constructed during the Neolithic, consisting of a sizeable chamber around and over which a cairn of stones was constructed. Some chambered cairns are also passage-graves. They are found throughout Britain and Ireland, with the largest number in Scotland.
Maeshowe is a Neolithic chambered cairn and passage grave situated on Mainland Orkney, Scotland. It was probably built around 2800 BC. In the archaeology of Scotland, it gives its name to the Maeshowe type of chambered cairn, which is limited to Orkney.
A passage grave or passage tomb consists of one or more burial chambers covered in earth or stone and having a narrow access passage made of large stones. These structures usually date from the Neolithic Age and are found largely in Western Europe. When covered in earth, a passage grave is a type of burial mound which are found in various forms all over the world. When a passage grave is covered in stone, it is a type of cairn.
Newgrange is a prehistoric monument in County Meath in Ireland, located on a rise overlooking the River Boyne, eight kilometres west of the town of Drogheda. It is an exceptionally grand passage tomb built during the Neolithic Period, around 3200 BC, making it older than Stonehenge and the Egyptian pyramids. Newgrange is the main monument in the Brú na Bóinne complex, a World Heritage Site that also includes the passage tombs of Knowth and Dowth, as well as other henges, burial mounds and standing stones.
The court cairn or court tomb is a megalithic type of chambered cairn or gallery grave. During the period, 3900–3500 BC, more than 390 court cairns were built in Ireland and over 100 in southwest Scotland. The Neolithic monuments are identified by an uncovered courtyard connected to one or more roofed and partitioned burial chambers. Many monuments were built in multiple phases in both Ireland and Scotland and later re-used in the Early Bronze Age.
A gallery grave is a form of megalithic tomb built primarily during the Neolithic Age in Europe in which the main gallery of the tomb is entered without first passing through an antechamber or hallway. There are at least four major types of gallery grave, and they may be covered with an earthen mound or rock mound.
Dowth is a Neolithic passage tomb near the River Boyne in County Meath, Ireland. It is one of the three main tombs of the Brú na Bóinne World Heritage Site, along with Newgrange and Knowth. Its features align it with the other passage tombs, which date from around 3200 BC. Unlike its bigger neighbours, Dowth has mostly been left as a ruin, although its smaller inner chambers are largely intact. The Royal Irish Academy carried out a botched excavation in 1847, leaving a large crater in the mound that has never been repaired.
Carrowmore is a large group of megalithic monuments on the Coolera Peninsula to the west of Sligo, Ireland. They were built in the 4th millennium BC, during the Neolithic. There are thirty surviving tombs, making Carrowmore one of the largest clusters of megalithic tombs in Ireland, and one of the 'big four' along with Carrowkeel, Loughcrew and Brú na Bóinne. Carrowmore is the heart of an ancient ritual landscape which is dominated by the mountain of Knocknarea to the west. It is a protected National Monument.
The dolmens of Jersey are neolithic sites, including dolmens, in Jersey. They range over a wide period, from around 4800 BC to 2250 BC, these dates covering the periods roughly designated as Neolithic, or “new stone age”, to Chalcolithic, or “copper age”.
Megalithic monuments in Ireland typically represent one of several types of megalithic tombs: court cairns, passage tombs, portal tombs and wedge tombs. The remains of over 1,000 such megalithic tombs have been recorded around Ireland.
Gavrinis is a small island in the Gulf of Morbihan in Brittany, France. It contains the Gavrinis tomb, a Neolithic passage tomb built around 4200–4000 BC, making it one of the world's oldest surviving buildings. Stones inside the passage and chamber are covered in megalithic art. It is likened to other Neolithic passage tombs such as Barnenez in Brittany and Newgrange in Ireland.
Prehistoric Orkney refers only to the prehistory of the Orkney archipelago of Scotland that begins with human occupation. Although some records referring to Orkney survive that were written during the Roman invasions of Scotland, “prehistory” in northern Scotland is defined as lasting until the start of Scotland's Early Historic Period.
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Nordic megalith architecture is an ancient architectural style found in Northern Europe, especially Scandinavia and North Germany, that involves large slabs of stone arranged to form a structure. It emerged in northern Europe, predominantly between 3500 and 2800 BC. It was primarily a product of the Funnelbeaker culture. Between 1964 and 1974, Ewald Schuldt in Mecklenburg-Western Pomerania excavated over 100 sites of different types: simple dolmens, extended dolmens, passage graves, great dolmens, unchambered long barrows, and stone cists. In addition, there are polygonal dolmens and types that emerged later, for example, the Grabkiste and Röse. This nomenclature, which specifically derives from the German, is not used in Scandinavia where these sites are categorised by other, more general, terms, as dolmens, passage graves and stone cists.
The architecture of Scotland in the prehistoric era includes all human building within the modern borders of Scotland, before the arrival of the Romans in Britain in the first century BCE. Stone Age settlers began to build in wood in what is now Scotland from at least 8,000 years ago. The first permanent houses of stone were constructed around 6,000 years ago, as at Knap of Howar, Orkney and settlements like Skara Brae. There are also large numbers of chambered tombs and cairns from this era, particularly in the west and north. In the south and east there are earthen barrows, often linked to timber monuments of which only remnants remain. Related structures include bank barrows, cursus monuments, mortuary enclosures and timber halls. From the Bronze Age there are fewer new buildings, but there is evidence of crannogs, roundhouses built on artificial islands and of Clava cairns and the first hillforts. From the Iron Age there is evidence of substantial stone Atlantic roundhouses, which include broch towers, smaller duns. There is also evidence of about 1,000 hillforts in Scotland, most located below the Clyde-Forth line.
Unchambered long cairns are found in Scotland and Northern England, and form a group of non- or semi-megalithic monuments. There are about 28 long cairns in north Scotland and 21 in south Scotland that show no evidence of internal stone chambers. However, proving the existence of wooden chambers under a cairn is not possible without excavation work. The exact classification of this group of monuments is therefore not easy. Three particularly noteworthy examples of these cairns are:
British megalith architecture is the study of those ancient cultures that built megalithic sites on the British Isles, including the research and documentation of these sites. The classification sometimes used of these cultures based on geological criteria is problematic.
Fourknocks Passage Tomb is a passage grave and National Monument located in County Meath, Ireland.
Huntersquoy chambered cairn is a Neolithic chambered cairn located on the island of Eday, in Orkney, Scotland. The monument dates from the 3rd millennium BC and is an Orkney–Cromarty type chambered cairn. Huntersquoy is a distinctive two-story burial monument with overlapping chambers. Historic Environment Scotland established the site as a scheduled monument in 1936.
Wideford Hill chambered cairn is a Neolithic chambered cairn on Mainland, Orkney in Scotland. The tomb dates to around 2000 BC, and is similar in design to the Maeshowe chambered cairn on Orkney. Historic Environment Scotland established the site as a scheduled monument in 1994.
