Neolithic

The Neolithic ⁱ/ˌniːəˈlɪθɪk/Age, Era, or Period, from νέος (néos, "new") and λίθος (líthos, "stone"), or New Stone Age, was a period in the development of human technology, beginning about 10,200 BC, according to the ASPRO chronology, in some parts of the Middle East, and later in other parts of the world and ending between 4,500 and 2,000 BC.

Traditionally considered the last part of the Stone Age, the Neolithic followed the terminal Holocene Epipaleolithic period and commenced with the beginning of farming, which produced the "Neolithic Revolution". It ended when metal tools became widespread (in the Copper Age or Bronze Age; or, in some geographical regions, in the Iron Age). The Neolithic is a progression of behavioral and cultural characteristics and changes, including the use of wild and domestic crops and of domesticated animals.

The beginning of the Neolithic culture is considered to be in the Levant (Jericho, modern-day West Bank) about 10,200 – 8,800 BC. It developed directly from the Epipaleolithic Natufian culture in the region, whose people pioneered the use of wild cereals, which then evolved into true farming. The Natufian period was between 12,000 and 10,200 BC, and the so-called "proto-neolithic" is now included in the Pre-Pottery Neolithic (PPNA) between 10,200 and 8,800 BC. As the Natufians had become dependent on wild cereals in their diet, and a sedentary way of life had begun among them, the climatic changes associated with the Younger Dryas are thought to have forced people to develop farming.

Bronze Age

The Bronze Age is a time period characterized by the use of bronze, proto-writing, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age Stone-Bronze-Iron system, as proposed in modern times by Christian Jürgensen Thomsen, for classifying and studying ancient societies.

An ancient civilization is defined to be in the Bronze Age either by smelting its own copper and alloying with tin, arsenic, or other metals, or by trading for bronze from production areas elsewhere. Copper-tin ores are rare, as reflected in the fact that there were no tin bronzes in western Asia before trading in bronze began in the third millennium BC. Worldwide, the Bronze Age generally followed the Neolithic period, but in some parts of the world, the Copper Age served as a transition from the Neolithic to the Bronze Age. Although the Iron Age generally followed the Bronze Age, in some areas, the Iron Age intruded directly on the Neolithic from outside the region.

Social science

Social science is a major category of academic disciplines, concerned with society and the relationships among individuals within a society. It in turn has many branches, each of which is considered a "social science". The main social sciences include economics, political science, human geography, demography and sociology. In a wider sense, social science also includes some fields in the humanities such as anthropology, archaeology, jurisprudence, psychology, history, and linguistics. The term is also sometimes used to refer specifically to the field of sociology, the original 'science of society', established in the 19th century.

Positivist social scientists use methods resembling those of the natural sciences as tools for understanding society, and so define science in its stricter modern sense. Interpretivist social scientists, by contrast, may use social critique or symbolic interpretation rather than constructing empirically falsifiable theories, and thus treat science in its broader sense. In modern academic practice, researchers are often eclectic, using multiple methodologies (for instance, by combining the quantitative and qualitative techniques). The term social research has also acquired a degree of autonomy as practitioners from various disciplines share in its aims and methods.

University of Southampton

The University of Southampton (abbreviated as Soton in post-nominal letters) is a public research university located in Southampton, England. Southampton is a research intensive university and a founding member of the Russell Group of elite British universities.

The origins of the university date back to the founding of the Hartley Institution in 1862 following a legacy to the Corporation of Southampton by Henry Robinson Hartley. In 1902, the Institution developed into the Hartley University College, with degrees awarded by the University of London. On 29 April 1952, the institution was granted a Royal Charter to give the University of Southampton full university status. It is a member of the European University Association, the Association of Commonwealth Universities and is an accredited institution of the Worldwide Universities Network.

In the 2014 Research Excellence Framework Southampton was ranked 8th for research intensity. Besides being recognised as one of the leading research universities in the UK, Southampton has also achieved consistently high scores for its teaching and learning activities. It additionally has one of the highest proportions of income derived from research activities in Britain, and is regularly ranked in the top 100 universities in the world. As of 2015 Southampton is one of the few universities to achieve a top 20 UK position in the most established national and international rankings (along Cambridge, Oxford, Imperial, UCL, LSE and Warwick). In the 2016 edition of U.S. News & World Report, Southampton is placed in the top 10 of British Universities.

Skara Brae

Skara Brae /ˈskærə ˈbreɪ/ is a stone-built Neolithic settlement, located on the Bay of Skaill on the west coast of Mainland, the largest island in the Orkney archipelago of Scotland. It consists of eight clustered houses, and was occupied from roughly 3180 BC–2500 BC. Europe's most complete Neolithic village, Skara Brae gained UNESCO World Heritage Site status as one of four sites making up "The Heart of Neolithic Orkney." Older than Stonehenge and the Great Pyramids, it has been called the "Scottish Pompeii" because of its excellent preservation.

Discovery and early exploration

In the winter of 1850, a severe storm hit Scotland, causing widespread damage and over 200 deaths. In the Bay of Skaill, the storm stripped the earth from a large irregular knoll known as "Skerrabra". When the storm cleared, local villagers found the outline of a village, consisting of a number of small houses without roofs. William Watt of Skaill, the local laird, began an amateur excavation of the site, but after four houses were uncovered, the work was abandoned in 1868. The site remained undisturbed until 1913, when during a single weekend the site was plundered by a party with shovels who took away an unknown quantity of artifacts. In 1924, another storm swept away part of one of the houses and it was determined the site should be made secure and more seriously investigated. The job was given to University of Edinburgh's Professor Vere Gordon Childe who travelled to Skara Brae for the first time in mid-1927.