The Stone Knight, the Sphinx and the Hare: New Aspects of Early Figural Celtic Art

1998 ◽  
Vol 64 ◽  
pp. 1-14 ◽  
Author(s):  
Otto-Herman Frey
Keyword(s):  
Early Development ◽  
Belief Systems ◽  
Human Form ◽  
Population Movements ◽  
North East ◽  
Mediterranean World ◽  
The Alps ◽  
Relationship Of ◽  
The Relationship ◽  
Complex Question

The paper re-examines arguments concerning the early development of early Celtic (La Tène A) art and its relations with the Mediterranean world. Taking as a focus the recent spectacular discoveries below the hillfort of the Glauberg north-east of Frankfurt, the Celtic approaches to representations of the human form are analysed and the complex question of meaning and the relationship of early Celtic art to contemporary belief systems discussed. As a brief coda, the striking changes which took place in many parts of the early Celtic world after c. 400 BC are referred to in the context of the major population movements of the time, notably those which brought settlers from north of the Alps to Italy.

Stone Orientation and Other Structural Features of Tills in East Yorkshire

1967 ◽  
Vol 104 (4) ◽  
pp. 344-360 ◽  
Author(s):  
L. F. Penny ◽  
J. A. Catt
Keyword(s):  
Ice Sheet ◽  
Structural Features ◽  
Coastal Areas ◽  
North East ◽  
South West ◽  
Direction Of Movement ◽  
Relationship Of ◽  
The Relationship

AbstractMacrofabric (stone orientation) and microfabric studies of the four tills exposed in the coastal areas of East Yorkshire indicate that the regional direction of ice movement during both the Saale and Weichsel Glaciations was from north-east to south-west. The Saale (Basement) Till was considerably modified by the advance of ice during the Weichsel Glaciation; in particular, the stones in the Basement were reorientated so that their long axes now lie at right angles to the direction of movement of the Weichsel ice sheet. The fabrics of the three Weichsel tills (Drab, Purple and Hessle) are alike, and it is suggested that all three were deposited from one composite ice sheet. The relationship of vertical joints in the Basement and Drab Tills to directions of ice movement is discussed; those in the Basement possibly originated as ac tension joints inherited from the parent ice, whereas some of those in the Drab are probably conjugate shear joints formed during post-depositional deformation of the till.

Globally Speaking

2008 ◽  
Vol 13 (2) ◽  
pp. 137-140 ◽  
Author(s):  
Trevor Wishart
Keyword(s):  
Electroacoustic Music ◽  
Digital Recording ◽  
Recording Equipment ◽  
High Quality ◽  
Cultural Experience ◽  
North East ◽  
The North ◽  
Local Sound ◽  
Relationship Of ◽  
The Relationship

AbstractCheaply available high-quality digital recording equipment, and the ubiquity of computer music tools and the Internet make the creation of electroacoustic music in diverse localities, and its dissemination around the globe, extremely easy. This raises important questions about the relationship of local sound worlds and cultural experience to a potentially global audience. This quandary is examined through the compositions Globalalia (which deals explicitly with speech material from many languages) and Fabulous Paris – a virtual oratorio whcih uses speech in different ways to contrast our relationship to the local and personal with our relationship to the mass experience of the globalised mega-city. The problems in relating to both a local and a global audience are considered in relation to the composer's current project recording speech materials in local communities in the North East of England.

D. W. W. on D. W. W.

2016 ◽  
pp. 35-48
Author(s):  
Donald W. Winnicott
Keyword(s):  
Early Development ◽  
Independent Group ◽  
Transitional Objects ◽  
Relationship Of ◽  
The Relationship

In January 1967, four years before his death, Winnicott was asked to address the 1952 Club (a society of senior British independent group analysts who meet informally for discussion of ideas) on the relationship of his theory to other formulations of early development, an exercise he called ‘D.W.W. on D.W.W’. Winnicott chronologically reviews the development of his ideas and speaks of those whose work had influenced him. He elaborates on his own work on psychoanalysis as an investigative method, on delinquency, on the environment, on dependence, on transitional objects and phenomena, on the psyche soma, on madness, on sublimation and on regression. This paper includes both the extract Winnicott handed out with spaces left to be filled in as the audience thought appropriate and a transcription of the recording of the actual talk.

Modernization of Universities through Greater Interaction with Small Firms

1999 ◽  
Vol 13 (2) ◽  
pp. 119-126 ◽  
Author(s):  
Fiona Tilley ◽  
David Johnson
Keyword(s):  
Higher Education ◽  
Small Firms ◽  
Best Practice ◽  
Business Sector ◽  
North East ◽  
The North ◽  
The Uk ◽  
Political Economic ◽  
Relationship Of ◽  
The Relationship

This paper explores the ‘best practice’ interactions between universities and small firms in the UK. The purpose is to identify ways in which a university can build stronger and more effective links with small firms. The relationship between universities and small firms is of growing importance. There are political, economic and educational pressures which influence the behaviour and relationship of higher education toward the business sector, and small firms in particular. The wider context of the changes taking place within higher education are discussed. This is followed by the initial findings from a recently completed research project for the Council for Industry and Higher Education which investigated the foremost components in ‘best practice’ interactions and linkages between small firms and universities in the North East of England. Some preliminary ideas are suggested on how best practice can be further facilitated. These proposals are then interpreted in terms of the operational implications for universities and other strategic organizations involved in building linkages with small firms.

Serpentinites in the North-East Ox Mountains, Eire

1966 ◽  
Vol 103 (2) ◽  
pp. 124-137 ◽  
Author(s):  
G. G. Lemon
Keyword(s):  
Fracture Zone ◽  
Additional Information ◽  
North East ◽  
The North ◽  
Relationship Of ◽  
Boundary Fracture ◽  
First Time ◽  
The Relationship

AbstractSix serpentinites occur in the Moinian granulites of the North-East Ox Mountains. Four have been known for some time and have been previously described. Additional information on these and the associated vermiculite deposits is provided. The remaining two serpentinites are described for the first time. A pyroxenite vein associated with one of these may have been produced by meta-morphic regeneration.The relationship of some of these serpentinites to the probable position of the Highland Boundary Fracture-zone in Eire is also discussed. Brief comparison is made with serpentinites occurring in the Scottish Moinian.

scholarly journals Paleoecology of Late Eocene-Oligocene foraminiferal assemblages in a two-well transect across the North-East Newfoundland shelf

1991 ◽  
Vol 10 (1) ◽  
pp. 57-67
Author(s):  
F. C. Thomas
Keyword(s):  
North Sea ◽  
Late Eocene ◽  
Western Boundary ◽  
Late Oligocene ◽  
North East ◽  
The North ◽  
Early Oligocene ◽  
The North Sea ◽  
Relationship Of ◽  
The Relationship

Abstract. Core samples from the Paleogene of the Bonavista C-99 well on the northeast Newfoundland shelf and cuttings from downdip Blue H-28 contain foraminiferal assemblages which enable reconstruction of paleoenvironments along a downslope transect in Eocene through Late Oligocene-Miocene time. Comparison with coeval assemblages in North Sea wells with respect to structure and grain size of agglutinated taxa between the two areas reveal inter-basin differences.Reconstruction of the paleobathymetry derived from foraminiferal analysis, confirms seismic evidence for shallowing at the Bonavista site beginning in the Early Oligocene. The relationship of the Bonavista assemblages to contour currents is explored with reference to modern regional analogues. Species such as Reticulophragmium amplectens, Haplophragmoides walteri, Eponides umbonatus and Uvigerina ex. gr. miozea-nuttalli persist stratigraphically higher in the deeper Blue site.The paleoslope of this two-well transect is determined as approximately 0.48° during the Middle to Late Eocene and 0.68° during the Late Oligocene-Early Miocene. The bottom water hydrography of the transect can be evaluated by reference to these assemblages and a comparison to flysch-type agglutinated assemblages from a transect in the North Sea. The presence of an Upper Eocene-Middle Miocene hiatus at the Blue site contrasting with apparently continuous Tertiary deposition at Bonavista places a theoretical upper limit of 500–1000 m on the depth of the early Cenozoic western boundary undercurrent.

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