The Mesolithic settlement at Morton lies some six miles north-north-west of St. Andrews in Fife, Scotland (fig. 1). The area around the site, north-eastern Fife, is surrounded on three sides by water, and projects as a blunt peninsula into the North Sea. The river Eden and the Firth of Tay serve as southern and northern boundaries of this peninsula, which consists today principally of the wind-deposited sands of Tentsmuir. The area of Tentsmuir, now afforested, is one of the relatively few regions in Britain where land is building up into the North Sea, and this process has been in action for many centuries (Sissons, 1967).The Tentsmuir Sands are a prolific source of later prehistoric and early historic finds, the earliest yet known being of the late third millennium B.C. In February 1957, while searching for such material on Tentsmuir, Mr R. Candow of Tayport collected some flints from molehills and other exposures on the high ground of the ‘Old Quarry’ field at Morton Farm (National Grid Reference NO 467257). Surface collections continued to be made until 1963 when excavations of the site were undertaken by Mr Candow in collaboration with Dundee Museum and Art Gallery (Candow, 1966). A total of 41 trenches were excavated between May 1963 and April 1967, and these are shown on the plan of site A (fig. 4, no. 1–41). In November 1967, site B in the same field was discovered and partially excavated (fig. 29, no. 51), before work was suspended and the writer was invited to continue the investigations.
The start-up of the Large Hadron Collider (LHC) at CERN, Geneva, presents a huge challenge in processing and analysing the vast amounts of scientific data that will be produced. The architecture of the worldwide grid that will handle 15 PB of particle physics data annually from this machine is based on a hierarchical tiered structure. We describe the development of the UK component (GridPP) of this grid from a prototype system to a full exploitation grid for real data analysis. This includes the physical infrastructure, the deployment of middleware, operational experience and the initial exploitation by the major LHC experiments.
This paper is primarily concerned with the large series of Bronze Age shields known in central, north and western Europe, but, for purposes which will become apparent, some attention has also been paid to certain shields of the Mediterranean world. The first part will be devoted to a culture-historical study of the shields and the second to the methods used in their production.
The so-called Dansaren rock carving at Järrestad, southern Sweden, is one of the largest rock carving sites in that country. This paper presents a detailed description and re-analysis of the carvings, examining not only the images themselves but also their topographical location, groupings and position in relation to the available rock surface and possible viewpoints of the observer. The history of research at the site is described together with the methods used for recording. The motifs are described and discussed and it is noted that the various types of images, including footsoles, feet, horsemen, cupmarks, and boats occur in particular combinations and are distributed on the rock surface in such a manner that discrete panels are apparent, delineated by natural cracks in the rock which form an integral part of the design. The location and distribution of other monuments and rock carvings in the region are discussed and a social and symbolic context within the later Bronze Age presented for the Dancer and its associated carvings.
The peat deposits in the Somerset Levels have yielded many finds of prehistoric and early historic age, ranging from flint and metal artefacts to roadways and other structures. These finds have been a source of interest to archaeologists for many years, and the work here described represents only one aspect of the early occupation of the region. The Levels themselves lie between the major uplands of the Quantock Hills and the Mendip Hills (fig. 1), but within the Levels are extensive ridges of limestone (including the Polden Hills and the Wedmore Ridge), smaller and lower areas of limestone (such as Westhay and Meare), and patches of sands (Burtle Beds) all of which provided dry ground for occupation or other activities. We are concerned in this paper with the earliest wooden roads and tracks of Neolithic age which were built to allow communication between the Westhay ridge and the largest Burtle Bed north of the Polden Hills (pl. XIV).
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