scholarly journals The English Occupation of Tangier (1661–1683)

1905 ◽  
Vol 19 ◽  
pp. 61-78 ◽  
Author(s):  
Enid Routh

When Charles II. announced his impending marriage with Catharine of Portugal, the inclusion of Tangier in the Princess's dowry was the most popular clause of the marriage treaty.English hopes ran even higher round the little African port than over the companion gift of Bombay, for Tangier, situated almost on the north-west point of Morocco, lay in the direct trade route from the Levant to Western Europe. The English Consul at Lisbon pointed out that it might from its position become a magazine for all the Levant, a port which would be used by the Spanish West India fleet homeward bound to Seville or Cadiz, in order to avoid the high duties imposed by the Crown of Spain in its own ports—valuable asset this in case of war with Holland, Spain, or France.

Author(s):  
Anne Haour

This chapter explains the coverage of this book, which is about the comparison of rulers, warriors, traders, and clerics on the central Sahel and the North Sea region. It argues that there was more similarity between north-western Europe and the central Sahel in the few centuries either side of AD 1001 than has hitherto been recognised, and maintains that the nature of the sources has obscured these formative times and left them in the shadow of organised structures. It discusses the interconnectedness of central Sahel and north-west Europe through contacts and shared pre-industrial nature.


2020 ◽  
Author(s):  
Gerard van der Schrier ◽  
Antonello Squintu ◽  
Else van den Besselaar ◽  
Eveline van der Linden ◽  
Enrico Scoccimarro ◽  
...  

<p>The comparison of simulated climate with observed daily values allows to assess their reliability and the soundness of their projections on the climate of the future. Frequency and amplitude of extreme events are fundamental aspects that climate simulations need to reproduce. In this work six models developed within the High Resolution Model Intercomparison Project are compared over Europe with the homogenized version of the observational E-OBS gridded dataset. This is done by comparing averages, extremes and trends of the simulated summer maximum temperature and winter minimum temperatures with the observed ones.</p><p>Extreme values have been analyzed making use of indices based on the exceedances of percentile-based thresholds. Winter minimum temperatures are generally underestimated by models in their averages (down to -4 deg. C of difference over Italy and Norway) while simulated trends in averages and extreme values are found to be too warm on western Europe and too cold on eastern Europe (e.g. up to a difference of -4% per decade on the number of Cold Nights over Spain). On the other hand the models tend to underestimate summer maximum temperatures averages in Northern Europe and overestimate them in the Mediterranean areas (up to +5 deg. C over the Balkans). The simulated trends are too warm on the North West part and too cold on the South East part of Europe (down to -3%/dec. on the number of Warm Days over Italy and Western Balkans).</p><p>These results corroborate the findings of previous studies about the underestimation of the warming trends of summer temperatures in Southern Europe, where these are more intense and have more impacts.  A comparison of the high resolution models  with the corresponding version in CMIP5 has been performed comparing the absolute biases of extreme values trends. This has shown a slight improvement for the simulation of winter minimum temperatures, while no signs of significant progresses have been found for summer maximum temperatures.</p>


1988 ◽  
Vol 41 (02) ◽  
pp. 149-173 ◽  
Author(s):  
K. F. Woodman ◽  
J. Juleff ◽  
R. A. Allen

A mainly theoretical study has been undertaken to demonstrate how the extent of cover from a hyperbolic navigation system chain can be evaluated. The impetus for the study was the need to assess how Loran-C could be extended over Western Europe, particularly in the South western Approaches, North Sea, English Channel and Bay of Biscay sea areas.The technique described in this article leads to an accurate determination of the electric field strength at a distance from each transmitting site and takes into account the complexities of the ground-wave propagation path. This field-strength contour is combined with the geometric effects of station siting (expansion factors) to yield a constant S/N contour (–10 dB) which defines the ¼n.m. error and hence the limit of cover for the hyperbolic chain under study.In order to exercise the analytical methods a hypothetical Loran-C chain was studied comprising a master station at Lessay (France), with secondary stations at Soustons (also in France), at Sylt (dual rated; off the North Sea coast of Germany, near the Danish border) and at a fourth station located in north-west Britain on the Hebridean island of Barra. The study indicated that such a hypothetical chain would significantly improve Loran-C cover over much of western Europe.


Archaeologia ◽  
1887 ◽  
Vol 50 (2) ◽  
pp. 421-438
Author(s):  
G.L. Gomme

In the north-west of Wilts is a district which contains some remarkable reminiscences of the two dominant races who have influenced the history of this country. In tracing out the history of this district, as it has come down to us by the traditions and records of early chronicle writers, we arrive at an important epoch when for the first time is brought into strongly marked prominence the outline of the community which had settled there. This community, known to us later under the local name of Malmesbury, is one of the most perfect types of the primitive village which has survived in England, and to the elucidation of its chief characteristics it is proposed to devote some little attention. Keeping before us the outline made known from early records we shall see how this is gradually filled in from facts, which though gleaned from later and modern records, are nevertheless stamped as belonging to the earliest stages of history. And when this local mosaic is completely pieced in we shall be able, I think, to satisfy ourselves that what has so persistently clung to locality in later days originally belonged to a social group, types of which are still to be found in Eastern Europe and India, where society is in a state of arrested progress and has not advanced along the lines which mark its development in Western Europe.


2019 ◽  
Vol 33 (0) ◽  
pp. 34
Author(s):  
Katharina Herlofson ◽  
Svein Olav Daatland ◽  
Marijke Veenstra

The article addresses the strength and character of family responsibility norms in Eastern and Western Europe. The strength is measured by the level of support for filial and parental responsibilities (i.e., adult children’s obligations towards older parents and vice-versa) and the character is indicated by the priority given to the older or the younger generation. For the analyses, we employ data from thirteen Eastern and Western European countries participating in the Generations and Gender Survey. In general, family norms are stronger in the East than in the West, but it is difficult to establish where to draw a dividing line. The contrast between the two extremes, Norway and Sweden in the north-west and Georgia in the south-east, is striking. The remaining countries line up quite close along the geographical diagonal (from Scandinavia to Georgia). The character of the norms is less clearly distributed – whereas almost all countries in Eastern Europe give priority to the older generation, the picture in the West is more mixed. The results partly confirm earlier conclusions about east-west differences in family responsibility norms, but adding more countries to the analyses has revealed a more complex and ambiguous picture than presented in previous studies.


1912 ◽  
Vol 2 ◽  
pp. 201-214 ◽  
Author(s):  
F. Haverfield

It is a commonplace that Britain is an island. The further truth, that it is an island which is very closely tied to the continent lying east of it, is a good deal less familiar. Geographical writers are apt, even for historical purposes, to emphasise instead those two features of the island which Mr. Mackinder in his admirable volume has called its insularity and its universality, its separation, that is, from Europe, and its central position in the world. I feel, however, that both students of ancient history, and also modern men at this particular moment, are more concerned with the peculiar relation of Britain to Europe. It is not the insularity of the island but its dependence on the continent which really matters. This dependence dates from days long before the first appearance of man; it is due, indeed, to the configuration of western Europe in remote geological periods. In those dateless days the seas which now divide our southern coast from France, and our eastern coast from the Low Countries and from Germany, were river valleys which took the drainage of a vast area extending from Wales and the Pennine hills on the north-west, to the Eifel, the Vosges and the Cevennes on the south-east. The rivers have long vanished, but their valleys, vast almost as the valley of a Missouri or a Mississippi, can still be traced in the configuration of the British and continental coasts. On each side of the sea the main rivers flow down to face each other, the main harbours of each land lie vis-à-vis and the natural entrances by which trader or soldier might wish to enter Britain open on to the main exits by which he might wish to start from the continent. Nor is it merely a matter of entrances or exits. That part of Britain which faces the continent is the lower-lying part of the great valley which I have mentioned. It is therefore fairly flat, and it offers no strategic obstacle to invaders. Its only features, its forests and its fens, are hardly large enough even to divert the march of armies and have been over-rated by writers like the late Dr. Guest and Mr. J. R. Green. The really difficult regions of Britain, the tangled uplands of Wales and west Yorkshire and the north, lie far away from the path of European aggressors. They might assist the rulers of Britain in checking an Irish invasion; they do not protect it from European influences. Britain is a land which was made to be invaded from the continent.


Slavic Review ◽  
1966 ◽  
Vol 25 (3) ◽  
pp. 458-474 ◽  
Author(s):  
Thomas Esper

Historians have customarily treated two major periods of Russia's commercial relations with Western Europe (defined as Western Christendom) in the pre-Petrine period: (1) until 1494, the year in which Ivan III closed the Hanseatic establishment in Novgorod and which is generally viewed as the end of Hanseatic dominance in the Russian trade; and (2) from 1553, when the English first sailed around the North Cape to establish regular commercial relations with Russia via the northern route, or from 1558, when Ivan IV conquered the Baltic port of Narva (he then maintained direct trade with Western merchants there until he lost that port to the Swedes in 1581).


1918 ◽  
Vol 5 (8) ◽  
pp. 354-367 ◽  
Author(s):  
Henry H. Howorth

Some years ago I was allowed to publish in the Geological Magazine some papers on the recent geological history of the Baltic, in which I tried to bring before English readers the very important discoveries of the Northern geologists as affecting the general geology of the north-west of Europe and to extend their deductions. I was obliged to interrupt them for other work. Perhaps you will allow me to continue them some steps further, as we had reached a stage of some interest.


2013 ◽  
Vol 19 (1) ◽  
pp. 89-101 ◽  
Author(s):  
Bob Hancké

This article examines the problems of the single currency in light of the organization of labour relations in the Member States and their interaction with monetary policies. Continental (western) Europe consists of two very different systems of employment and labour relations, roughly coinciding with ‘coordinated market economies’ in the north-west of the continent, and ‘Mixed Market Economies’ in the south. These differences in employment relations and wage-setting systems implied that, against the background of a relatively restrictive one-size-fits-all monetary policy in place since 1999, the north-west of the continent systematically improved its competitiveness, while the south lost competitiveness in parallel. Small differences between the two groups of countries at the start of EMU thus were accentuated and, against the background of low growth and an almost closed E(M)U economy, the northern coordinated market economies accumulated current account surpluses while the GIIPS (Greece, Italy, Ireland, Portugal and Spain) ran into severe balance of payments problems in 2010 and 2011.


Author(s):  
Alain Demoulin

The present-day major relief features of western Europe are to a great extent determined by the underlying geological structures, either passively or actively. To get a comprehensive picture of their morphological evolution and interrelations, this chapter provides an overview of the spatial and temporal characteristics of the larg-escale tectonic framework of the continent. After having described the west European landscape at the end of the Palaeozoic, to which time the oldest preserved landforms date back, an outline of the Mesozoic and Cenozoic history of the major tectonic domains follows. Finally, some denudation estimates highlighting the relationship between tectonics, erosion, and the resulting relief, will be discussed. The three main influences on the present-day topographic patterns are those of the Alpine orogeny, the Cenozoic West European rifting, and the imprint of Variscan structures. They combine within a regional stress field determined by the Africa–Eurasia collision and the Alpine push as well as the mid-Atlantic ridge push. Since the end of the Miocene, this stress field is characterized by a fan-shaped distribution of SHmax along the northern border of the Alpine arc. This gives way to a more consistent NW–SE to NNW–SSE direction of compression further from the chain (Bergerat 1987; Müller et al. 1992). Topographically, western Europe may be roughly divided into a series of belts parallel to the Alpine chain. The Alpine chain culminates in a number of peaks exceeding 4,000 m in elevation (4,810 m at Mont Blanc) but the average altitude is in the order of 2,000 m. To the north, the mountainous Alps are bordered by the Molasse foredeep basin whose surface makes an inclined plane descending northwards from c.1,000 m to c.300 m near the Donau River in the Regensburg-Passau area. To the north-west, the Molasse basin narrows between the Alps and the Jura Mountains and is occupied by several extended lakes inherited from Quaternary glacial activity. Next to the Molasse basin in the north and west is a wide belt of recently more or less uplifted areas between 200 and 1,000 m in elevation (and locally in excess of 1,000 m in the French Massif Central and the Bohemian massif).


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