Palaeomagnetic investigations in Great Britain

Positions on the globe are given by the colatitude (θ) and the longitude (∅), measured from the north geographical pole and from the Greenwich meridian eastwards, respectively.The declination of the geomagnetic field or a palaeomagnetic direction (D ) is measured from the geographical meridian eastwards and the inclination (I) (the term * angle of dip ’ is not used here because of possible confusion with the term ‘geological dip’) is measured from the horizontal plane, positive if the north-seeking pole is below the horizon, negative if it is above.

Archaeologia ◽  
1817 ◽  
Vol 18 ◽  
pp. 340-343
Author(s):  
Edward Daniel Clarke

It is not attaching too high a degree of importance to the study of Celtic antiquities, to maintain, that, owing to the attention now paid to it in this country, a light begins to break in upon that part of ancient history, which, beyond every other, seemed to present a forlorn investigation. All that relates to the aboriginal inhabitants of the north of Europe, would be involved in darkness but for the enquiries now instituted respecting Celtic sepulchres. From the information already received, concerning these sepulchres, it may be assumed, as a fact almost capable of actual demonstration, that the mounds, or barrows, common to all Great Britain, and to the neighbouring continent, together with all the tumuli fabled by Grecian and by Roman historians as the tombs of Giants, are so many several vestiges of that mighty family of Titan-Celts who gradually possessed all the eastern shores of the Mediterranean, and who extended their colonies over all the countries where Cyclopéan structures may be recognized; whether in the walls of Crotona, or the temple at Stonehénge; in the Cromlechs of Wales, or the trilithal monuments of Cimbrica Chersonesus; in Greece, or in Asia-Minor; in Syria, or in Egypt. It is with respect to Egypt alone, that an exception might perhaps be required; but history, while it deduces the origin of the worship of Minerva, at Sais, from the Phrygians, also relates of this people, that they were the oldest of mankind. The Cyclopéan architecture of Egypt may therefore be referred originally to the same source; but, as in making the following Observations brevity must be a principal object, it will be necessary to divest them of every thing that may seem like a Dissertation; and confine the statement, here offered, to the simple narrative of those facts, which have led to its introduction.


1906 ◽  
Vol 10 (40) ◽  
pp. 50-51

No fewer than seven nations tried to win the Gordon Bennett Cup in the race which started from the Tuileries Gardens, in Paris, on September 30th. But the wind was in an unfavourable direction for the accomplishment of a long distance record. To some, the English Channel barred the way, to some, the North Sea.The cup offered for the greatest distance covered has been accorded to the American aeronaut, Mr. Frank P. Lahm, who descended 15 miles north of Scarborough.It will be seen in another part of this Journal that in December next, Members of the Aëronautical Society of Great Britain will hear an account of the Gordon-Bennett race from Colonel J. E. Capper, who took part in the race, having accompanied Mr. Rolls in the “ Britannia.” In this account, therefore, it will suffice to merely tabulate the competitors and results.


1954 ◽  
Vol 6 (4) ◽  
pp. 163-168 ◽  
Author(s):  
K. M. CREER ◽  
E. IRVING ◽  
S. K. RUNCORN

1982 ◽  
Vol 14 (10) ◽  
pp. 1389-1404 ◽  
Author(s):  
A R Townsend

The severe downturn in the British economy in 1980 is apparent in regional data for employment (provisional), redundancies, and unemployment. Five shift-share analyses are used here to explore the data on employment and redundancies, three of them conducted at ‘minimum list heading’ level. The period 1976 to 1979 is one of poor performance by regions of traditional policy interest, whereas the events of 1980 are seen as essentially a national phenomenon. However, bias in the industrial composition of the recession towards manufacturing in general and towards certain individual products is sufficient to focus its very worst effects on Wales, the West Midlands, and the North West.


1945 ◽  
Vol 82 (6) ◽  
pp. 267-273 ◽  
Author(s):  
W. Anderson

Formerly there were several surface brine springs in the North-East Coalfield; to-day there are none. From the many accounts of their occurrence nothing has been learned of their exact position, and very little of the composition of their waters. The earliest record, made in 1684, described the Butterby spring (Todd, 1684), and then at various times during the next two centuries brine springs at Framwellgate, Lumley, Birtley, Walker, Wallsend, Hebburn, and Jarrow were noted. In particular the Birtley salt spring is often mentioned, and on the 6-in. Ordnance map, Durham No. 13, 1862 edition, it is sited to the south-east of the village. Although no record has been found there must have been either a brine spring or well at Gateshead, for the name of the present-day suburb, Saltwell, is very old, and brine springs are still active in the coal workings of that area.


1906 ◽  
Vol 20 ◽  
pp. 79-107
Author(s):  
J. F. Chance

The policy pursued by George I. in the north of Europe in the first years of his reign has not received much attention from historians, at least in England. The few paragraphs which authors of such merit as Lord Mahon or J. R. Green allot to the subject show that they did not think it worth while, or were not able, to inform themselves of the facts. They record, rightly enough, that George's own principal purpose was to add the Swedish provinces of Bremen and Verden to his electoral dominions, and they attribute to Charles XII. the design of invading Great Britain in revenge, with the object of placing James III. upon the throne. Though he does not appear to have ever seriously contemplated such a thing, the belief that he held it in view was, after the Jacobite rebellion, genuine and general. But nothing is said of the pressing importance to Great Britain of the Baltic commerce, with which Charles interfered and Peter the Great seemed likely to interfere. This it was solely that gave George I. the services of a British squadron in the Baltic in 1715, and this the principal cause of the estrangement between Great Britain and Russia, which lasted for over twenty years. The object of the present paper is to present a narrative of events up to the death of Charles XII., from which conclusions may be drawn. Details may be avoided, as these have appeared in papers by the author published in the ‘English Historical Review.’


Author(s):  
Lubomír Hampl

The translation from Latin and Czech into Polish of an entire important, but still little-known work (Latin Dedicatio ad tria regna – Czech Dedikace třem královstvím – English Dedication to the three Kingdoms) introduces us to a large extent to the subject matter of the “i m p r o v e m e n t o f human affairs”. The translation of this manuscript fills a large gap in Polish comeniology. In the work translated into Polish, we can see how John Amos Comenius persistently and decisively pursued the honorable goal he had set for himself – that is, the pansophic improvement of all human affairs. The Polish-speaking reader will finally be able to “fully” read this work in their native language, in which there are also important elements related not only to pedagogical and educational topics, but above all to socio-philosophical issues and theological-biblical comparative references, centered around the domain of interdisciplinary research. The so-called “Portrait sketch” is also presented, or what hopes Comenius linked to the three described countries, strictly speaking the kingdoms of the North, i.e. Poland, Sweden and Great Britain, during the period of significant changes in seventeenth-century Europe.


1976 ◽  
Vol 13 (4) ◽  
pp. 563-578 ◽  
Author(s):  
D. K. Bingham ◽  
M. E. Evans

Paleomagnetic results from 55 sampling sites throughout the Stark Formation are reported. The known stratigraphic sequence of these sites enables the behaviour of the geomagnetic field in these remote times (1750 m.y.) to be elucidated. Two polarity reversals are identified and these represent potentially useful correlative features in strata devoid of index fossils. One of these is investigated in detail and indicates that behaviour of the geomagnetic field during polarity reversals was essentially the same in the early Proterozoic as it has been over the last few million years. The pole position (145°W, 15°S, dp = 3.5, dm = 6.9) lies far to the west of that anticipated from earlier results, implying further complexity of the North American polar wander curve. Possible alternatives to this added complexity are discussed.


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