In archaeology, the Epipalaeolithic or Epipaleolithic is a period occurring between the Upper Paleolithic and Neolithic during the Stone Age. Mesolithic also falls between these two periods, and the two are sometimes confused or used as synonyms. More often, they are distinct, referring to approximately the same period of time in different geographic areas. Epipaleolithic always includes this period in the Levant and, often, the rest of the Near East. It sometimes includes parts of Southeast Europe, where Mesolithic is much more commonly used. Mesolithic very rarely includes the Levant or the Near East; in Europe, Epipalaeolithic is used, though not very often, to refer to the early Mesolithic.
Several species of humans have intermittently occupied Great Britain for almost a million years. The earliest evidence of human occupation around 900,000 years ago is at Happisburgh on the Norfolk coast, with stone tools and footprints probably made by Homo antecessor. The oldest human fossils, around 500,000 years old, are of Homo heidelbergensis at Boxgrove in Sussex. Until this time Britain had been permanently connected to the Continent by a chalk ridge between South East England and northern France called the Weald-Artois Anticline, but during the Anglian Glaciation around 425,000 years ago a megaflood broke through the ridge, and Britain became an island when sea levels rose during the following Hoxnian interglacial.
Moorland or moor is a type of habitat found in upland areas in temperate grasslands, savannas, and shrublands and montane grasslands and shrublands biomes, characterised by low-growing vegetation on acidic soils. Moorland, nowadays, generally means uncultivated hill land, but also includes low-lying wetlands. It is closely related to heath, although experts disagree on what precisely distinguishes these types of vegetation. Generally, moor refers to highland and high rainfall zones, whereas heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats mostly occur in tropical Africa, northern and western Europe, and neotropical South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely high. Moorland also bears a relationship to tundra, appearing as the tundra and the natural tree zone. The boundary between tundra and moorland constantly shifts with climatic change.
Archaeology and geology continue to reveal the secrets of prehistoric Scotland, uncovering a complex past before the Romans brought Scotland into the scope of recorded history. Successive human cultures tended to be spread across Europe or further afield, but focusing on this particular geographical area sheds light on the origin of the widespread remains and monuments in Scotland, and on the background to the history of Scotland.
Lincolnshire, England derived from the merging of the territory of the ancient Kingdom of Lindsey with that controlled by the Danelaw borough Stamford. For some time the entire county was called 'Lindsey', and it is recorded as such in the Domesday Book. Later, Lindsey was applied to only the northern core, around Lincoln; it was defined as one of the three 'Parts of Lincolnshire', along with Holland in the south-east and Kesteven in the south west.
Tom Turner is an English landscape architect, garden designer and garden historian teaching at the University of Greenwich in London. He is the author of books and articles on landscape and gardens and is the editor of the Garden History Reference Encyclopedia. Educated at the Universities of St Andrews and Edinburgh, he studied landscape architecture under Frank Clark.
Environmental history is the study of human interaction with the natural world over time, emphasising the active role nature plays in influencing human affairs and vice versa.
The Britons, also known as Celtic Britons or Ancient Britons, were an indigenous Celtic people who inhabited Great Britain from at least the British Iron Age until the High Middle Ages, at which point they diverged into the Welsh, Cornish, and Bretons. They spoke Common Brittonic, the ancestor of the modern Brittonic languages.
Natural history of Scotland concerns the flora, fauna and mycota of Scotland.
Sir Martin Wyatt Holdgate is an English biologist and environmental scientist.
Steven Mithen, is an archaeologist. He is noted for his work on the evolution of language, music and intelligence, prehistoric hunter-gatherers, and the origins of farming. He is professor of early prehistory at the University of Reading.
This timeline of prehistoric Scotland is a chronologically ordered list of important archaeological sites in Scotland and of major events affecting Scotland's human inhabitants and culture during the prehistoric period. The period of prehistory prior to occupation by the genus Homo is part of the geology of Scotland. Prehistory in Scotland ends with the arrival of the Romans in southern Scotland in the 1st century AD and the beginning of written records. The archaeological sites and events listed are the earliest examples or among the most notable of their type.
Inchyra is a hamlet in the Carse of Gowrie in Scotland. It lies on the northern bank of the River Tay near Perth and is notable particularly for a number of archaeological finds made in the immediate vicinity.
Prehistoric Shetland refers to the prehistoric period of the Shetland archipelago of Scotland, when it was first occupied by humans. The period prior to human settlement in Shetland is known as the geology of Scotland. Prehistory in Shetland does not end until the beginning of the Early Medieval Period in Scotland, around AD 600. More than 5,000 archaeological sites have been recorded in the Shetland Islands.
The geography of Scotland in the Middle Ages covers all aspects of the land that is now Scotland, including physical and human, between the departure of the Romans in the early fifth century from what are now the southern borders of the country, to the adoption of the major aspects of the Renaissance in the early sixteenth century. Scotland was defined by its physical geography, with its long coastline of inlets, islands and inland lochs, high proportion of land over 60 metres above sea level and heavy rainfall. It is divided between the Highlands and Islands and Lowland regions, which were subdivided by geological features including fault lines, mountains, hills, bogs and marshes. This made communications by land problematic and raised difficulties for political unification, but also for invading armies.
Mynydd Maendy is a hilltop and moorland, near Gilfach Goch, in the County Borough of Rhondda Cynon Taf in south Wales, to the southwest of Tonyrefail. As with the Maindee district of Newport, the name derives from the Welsh maen dy meaning "stone house".
The demographic history of Scotland includes all aspects of population history in what is now Scotland. The earliest surviving archaeological evidence of human settlement is of Mesolithic hunter-gatherer encampments. These suggest a highly mobile boat-using people, probably with a very low density of population. Neolithic farming brought permanent settlements dating from 3500 BC, and greater concentrations of population. Evidence of hillforts and other buildings suggest a growing settled population. Changes in the scale of woodland indicates that the Roman invasions from the first century AD had a negative impact on the native population.
Prehistoric art in Scotland is visual art created or found within the modern borders of Scotland, before the departure of the Romans from southern and central Britain in the early fifth century CE, which is usually seen as the beginning of the early historic or Medieval era. There is no clear definition of prehistoric art among scholars and objects that may involve creativity often lack a context that would allow them to be understood.
Agriculture in prehistoric Scotland includes all forms of farm production in the modern boundaries of Scotland before the beginning of the early historic era. Scotland has between a fifth and a sixth of the arable or good pastoral land of England and Wales, mostly in the south and east. Heavy rainfall encouraged the spread of acidic blanket peat bog, which with wind and salt spray, made most of the western islands treeless. Hills, mountains, quicksands and marshes made internal communication and agriculture difficult.
Peter J. Atkins is emeritus professor of geography at Durham University. He is a specialist in food history and the geography of food.
