scholarly journals XXIV.—Notice of Two Storms which swept over the British Islands during the last week of November 1838

1840 ◽  
Vol 14 (2) ◽  
pp. 467-487
Author(s):  
David Milne

Previously to the 25th and 26th November 1838, there had prevailed in Great Britain and Ireland, for more than a week, a steady wind from the NE., accompanied with frosts, a progressively rising barometer, and tolerably clear weather. The same sort of weather existed on the Continent, and over a large portion of northern Europe, both on sea and land.This state of things was changed, by the arrival of two storms from southern latitudes, which passed over the British isles during the last week of November. These two storms, until they reached this part of the globe, were separate. The first one reached the British seas, about thirty-six hours before the other. But the second moved with about double the velocity of the first, and overtook the first somewhere about the north of Ireland and south-west of Scotland. Accordingly, in the southern parts of England, there were distinct indicia of two different storms, each having its own period of arrival, veering, and cessation;—whilst towards the north, these indicia became gradually less distinguishable, and were at length significant of only a general gale.

2020 ◽  
Vol 221 (2) ◽  
pp. 1384-1401
Author(s):  
A Licciardi ◽  
R W England ◽  
N Piana Agostinetti ◽  
K Gallagher

SUMMARY We present a new Moho depth model of the British Isles and surrounding areas from the most up-to-date compilation of Moho depth estimates obtained from refraction, reflection and receiver function data. We use a probabilistic, trans-dimensional and hierarchical approach for the surface reconstruction of Moho topography. This fully data-driven approach allows for adaptive parametrization, assessment of relative importance between different data-types and uncertainties quantification on the reconstructed surface. Our results confirm the first order features of the Moho topography obtained in previous work such as deeper Moho (29–36 km) in continental areas (e.g. Ireland and Great Britain) and shallower Moho (12–22 km) offshore (e.g. in the Atlantic Ocean, west of Ireland). Resolution is improved by including recent available data, especially around the Porcupine Basin, onshore Ireland and Great Britain. NE trending features in Moho topography are highlighted above the Rockall High (about 28 km) and the Rockall Trough (with a NE directed deepening from 12 to about 20 km). A perpendicular SE oriented feature (Moho depth 26–28 km) is located between the Orkney and the Shetland, extending further SW in the North Sea. Onshore, our results highlight the crustal thinning towards the N in Ireland and an E–W oriented transition between deep (34 km) and shallow (about 28 km) Moho in Scotland. Our probabilistic results are compared with previous models showing overall differences around ±2 km, within the posterior uncertainties calculated with our approach. Bigger differences are located where different data are used between models or in less constrained areas where posterior uncertainties are high.


1853 ◽  
Vol 20 (2) ◽  
pp. 211-217
Author(s):  
James D. Forbes

The following remarks, being the result of a careful examination of a small district of country characteristic of the relations of the trap formations, are perhaps worthy of being recorded; although the general features of the county of Roxburgh have been very clearly stated in a paper by Mr Milne, published in the 15th volume of the Edinburgh Transactions.The outburst of porphyritic trap forming the conspicuous small group of the Eildon Hills, may be stated to be surrounded by the characteristic greywacke of the south of Scotland. It forms an elongated patch on the map, extending from the west end of Bowden Muir in the direction of the town of Selkirk, and running from west-south-west to east-north-east (true) towards Bemerside Hill, on the north bank of the Tweed. The breadth is variable, probably less than is generally supposed; but it cannot be accurately ascertained, owing to the accumulated diluvium which covers the whole south-eastern slope of this elevated ridge. On this account, my observations on the contact of rocks have been almost entirely confined to the northern and western boundaries of the trap, although the other side was examined with equal care.


1944 ◽  
Vol 43 (4) ◽  
pp. 229-240 ◽  
Author(s):  
A. Stanley Griffith ◽  
W. T. Munro

1. This report summarizes the results of investigating 6963 cases of pulmonary tuberculosis in Great Britain.2. The tubercle bacilli in the sputum of each case were obtained in culture and their types determined.In Scotland out of 2769 cases 2609 yielded strains of human type (2564 eugonic and 45 dysgonic) and 160 (5·8 %) yielded strains of bovine type.In England tubercle bacilli of the human type were demonstrated in 3592 cases and of the bovine type in seventy-nine cases. Dysgonic human strains were found in seven cases, four of which occurred in the only series of English cases, namely 680, which were systematically examined for strains of this variety; dysgonic human strains were therefore proportionately less frequent in England than in Scotland. Of the seventy-nine bovine cases fifty-four occurred among 3422 unselected cases and twenty-five among a series of selected cases.In Wales 203 cases were examined and two were found to be bovine infections.In Eire no bovine infections were found in a series of 320 cases.3. The total number of cases of pulmonary tuberculosis shown to be expectorating bacilli of the bovine type of the sputum was 241, but twenty-five of them, occurring as they did among selected cases, are not used in the following percentages.The proportional frequencies of bovine infections were higher in all regions of Scotland than in England, the percentage being highest in the Orkney Islands (25·8%). The rural districts of the mainland of north-east Scotland follow with 9·1% and then those of the rest of Scotland with 5·2%. The City of Aberdeen gave 4·4% of bovine infections, but many of these had been infected in the country. In England the highest percentages were recorded in the north and middle regions, namely 2·0%, the southern part yielding only 0·6%.4. The strains from 232 of the 241 cases were fully virulent and from nine they showed varying degrees of attenuation.5. In six cases the bovine bacilli were associated with tubercle bacilli of another type, five times with eugonic human strains and once with a strain which could not be cultivated.6. The anatomical evidence (previous cervical and abdominal glandular and bone and joint tuberculosis) in about a third of the cases in Scotland and in a quarter of those in England was strongly in favour of the digestive tract as the channel of entry of the bacilli.7. Autopsies have been made on fourteen cases. In one case the lungs only were examined. In nine autopsies the anatomical evidence indicated the alimentary canal as the route of infection. In four autopsies the anatomical evidence was inconclusive.8. A history of tuberculosis was obtained in seven families in each of which two cases of pulmonary tuberculosis occurred. But bacteriological investigations in each of two families showed human in one affected person and bovine tubercle bacilli in the other and therefore disproved human to human infection. All the ten patients in five families yielded cultures of bovine tubercle bacilli. We concluded from the evidence that in one family both cases were of alimentary origin. Human to human infection was presumptive in the remaining four families. No autopsies were made in the last cases.9. Twenty-five patients were associated in their employment with cattle. Autopsies were made on two of them but the anatomical evidence as to the channel of entry of the bacilli was inconclusive.10. Of the 241 persons, forty-eight were known to be married and had 120 children. Bovine strains were obtained from two children (two families). Bacteriological evidence disproved infection from the parents in one case but was in favour of it having taken place in the other.11. One probable instance of infection with bovine bacilli spreading from man to cattle is quoted.12. A case of tuberculosis of the lungs due to bovine tubercle bacilli is indistinguishable clinically, radiologically and by post-mortem examination from one due to human tubercle bacilli.


1934 ◽  
Vol 7 (3) ◽  
pp. 366-372 ◽  
Author(s):  
J. P. T. Burchell

In 1931 I described two newly-discovered stone age industries of post-glacial age situated in north-east Ireland which had been made by myself and worked in conjunction with my friend C. Blake Whelan: the one from the Lower Estuarine Clay on Islandmagee, and the other from what is probably a fluviatile gravel intercalated between the Upper and Lower Estuarine Clays in the raised-beach formation at Cushendun.The former of these cultures has its counterpart in the blade industry beneath alluvium in the Orwell Estuary at Ipswich, Suffolk; whilst the latter finds its parallel in the raised-beach at Campbeltown in Argyllshire, Scotland. Adopting the familiar culture-sequence of Central Europe I had previously designated these two groups as phases of the Magdalenian period, but, in order to avoid confusion between the time-periods and the nomenclature of continental cultures, I have decided to base my chronology of the north Irish industries upon the natural changes of climate revealed by a study of the deposits in which they were found. The industries to be described below were contemporary with the Mesolithic Forest Cultures distinguished by Childe and Clark over the plain of northern Europe.


1963 ◽  
Vol 29 ◽  
pp. 326-356 ◽  
Author(s):  
John M. Coles

One of the features of the Irish Late Bronze Age is the appearance of wind instruments, commonly called ‘Trumpets’, often found in groups and only rarely in association with other material. Being conical and curved, these are therefore members of the horn family, to which the other large musical group of the Bronze Age, the north Europeanlurer, also belong.The Irish horns have attracted the attention of antiquarians for over 100 years, with the principal collection and listing of these beginning in 1860. Evans devoted a section of his 1881 book to the ‘trumpets’, and was followed by Day, Allen and Coffey. The latest treatment, which brought together most of the previous lists of horns, was by MacWhite in 1945. All of these later works were primarily concerned with the typology of the horns, and attention was paid neither to their actual production nor to their music. In the present study, all previously published horns have been examined where possible, as well as a number of unpublished finds, and an attempt will be made not only (i) to describe the typological variations and dating of the horns, but also (ii) to discuss their production as objects from Late Bronze Age workshops and (iii) to consider for the first time their musical potential.


Author(s):  
Roger Ling ◽  
Paul Arthur ◽  
Georgia Clarke ◽  
Estelle Lazer ◽  
Lesley A. Ling ◽  
...  

The casa degli amanti (house of the lovers), at the south-west corner of the insula, falls into two fairly distinct halves: the atrium complex, oriented on the street to the west, and the peristyle with its surrounding rooms, oriented on the street to the south and on the property boundary to the east. In the atrium complex, the atrium is misplaced to the south of the central axis, allowing space for two large rooms to the north, one of which was possibly a shop or workshop (5.50 m. × 4.70 m.), with a separate entry from the street (I 10, 10), while the other (5.80 m. × 4.50 m.), decorated with mythological wallpaintings and provided with a wide opening on to the peristyle, must have been a dining-room or oecus (room 8). Each of these had a segmental vault rising from a height of about 3.50 m. at the spring to slightly over 4 m. at the crown. In the first the vault is missing, but the holes for some of its timbers are visible in the east wall and a groove along the north wall marks the seating for the planking attached to them; at a higher level, in the north and south walls, are the remains of beam-holes for the joists of the upper floor or attic (see below). The arrangements in room 8 are now obscured by the modern vault constructed to provide a surface for the reassembled fragments of the ceiling-paintings; but the shape of the vault is confirmed by the surviving plaster of the lunettes, while a beam-hole for the lowest of the vault-timbers is visible above the corner of the western lunette in an early photograph (Superintendency neg. C 1944). The shop I 10, 10 had a small window high in the street wall to the south of Its entrance; whether there were any additional windows above the entrance, it is impossible to say, since this part of the wall is a modern reconstruction. Room 8 was lit by a splayed window cut in the angle of the vault and the eastern lunette, opening into the upper storey of the peristyle.


1876 ◽  
Vol 3 (4) ◽  
pp. 145-150 ◽  
Author(s):  
G. Linnarsson

In a paper on “The Physical Conditions under which the Cambrian and Lower Silurian Rocks were probably deposited over the European Area,” Mr. Hicks has recently put forth some opinions on the lowest fossiliferous rocks of Scandinavia and Russia, and their relations, as to age and stratigraphical characters, to those of Britain, which I think ought to be somewhat modified. The chief assertions in Mr. Hicks's paper are, that at the Pre-Cambrian period a large continent existed in Europe; that a subsidence began in the south-western part, and gradually extended to the north-eastern, which was not submerged until the Tremadoc group had been deposited over the western areas; and, finally, that the marine faunas migrated from the south-west. In order to prove these generalizations, Mr. Hicks makes a comparison between the most important Cambrian districts of Europe. He thinks that the British Cambrian rocks are the oldest, that the lowest Swedish beds are probably equivalent to the British Menevian group, and that the Russian are not older than the Arenig. Though the scantiness of the organic remains in some instances makes it very difficult, or, indeed, impossible to parallelize with certainty the oldest deposits of the various countries, it seems, however, from the palæontological facts already known, quite unquestionable that the lowest rocks of Scandinavia and Russia are older than Mr. Hicks has supposed them to be in comparison to those of Britain.


1959 ◽  
Vol 79 ◽  
pp. 132-148 ◽  
Author(s):  
James J. Tierney

It has long been recognised as a puzzling fact that in Ptolemy's map of the British Isles Great Britain is turned abruptly to the east from about latitude 55° north (corresponding roughly to the area of Scotland) so as to make a right angle approximately with the southern part of the country. It may be of interest to review briefly various tentative explanations of this peculiar fact which have been advanced during the last three-quarters of a century, and to add yet another to the list.In 1885 H. Bradley suggested that either Ptolemy or one of his predecessors had before him three sectional maps representing respectively England, Scotland, and Ireland, and that in fitting the three maps together Ptolemy or his predecessor fell into the mistake of turning the oblong map of Scotland the wrong way. T. G. Rylands next put forward his view that the error was due to a faulty observation of a lunar eclipse at Duncansby Head causing an error of longitude, together with a faulty gnomonic observation at the same place causing an error of latitude. In 1894 H. Kiepert was clearly getting nearer the truth when he wrote: ‘The only coherent, though often deficient source for the knowledge of the [British] islands that has come down to us from the most flourishing period of the Empire, is the map of Ptolemy, the result of a combination of the lines of roads and of the coasting expeditions during the first century of Roman occupation. One great fault, however, has crept into the map by his having made use also of a totally different source, namely the astronomical fixations of latitude executed by Pytheas in the time of the earliest Greek mercantile expeditions to these regions of high latitudes.’ In a footnote to this observation he added: ‘These fixations stop at a borderline at the highest point reached in the north, which according to the itinerary sources would have been crossed in a northward direction, and thus the Alexandrian scholar was forced to give the northern half of the island a bend towards the east, the only possible direction, in consequence of which all the localities of Caledonia have been shifted from their proper positions by about a quarter of a circle.’


1881 ◽  
Vol 13 (2) ◽  
pp. 183-207
Author(s):  
William Simpson

On leaving for India to accompany the army into Afghanistan in 1878, Colonel Yule, among other hints of places of interest of an archæological character to be looked out for, mentioned Nagarahara, the capital of the Jelalabad Valley in the Buddhist period. In the time of Hiouen-Thsang the district bore the same name as the capital, and it had no king of its own, but belonged to Kapisa, a city situated somewhere in the direction of Kabul. The district of Nagarahara extended to about 600 Chinese Li, from east to west, which would be over 100 miles. This might reach from about Jugduluck to the Khyber, so that in this last direction it would thus border on Gandara, and on the other extremity would touch Kapisa, which was also the name of the district as well as the capital of that name. The Valley of Jelalabad is small in comparison to that of the province which formerly belonged to it. From Darunta on the west to Ali-Boghan on the east is fifteen miles, but, on the left bank of the Kabul River, the flat land of Kamah extends the valley on that side, about five or six miles further to the east. The termination of the Valley at this place is called Mirza Kheyl, a white rocky ridge comes down close to the river, and there are remains of Buddhist masonry on it, with caves in the cliff below. On the right bank opposite Mirza Kheyl is Girdi Kas, which lies in a small valley at the northern end of a mass of hills which terminates the Jelalabad Valley on that side at Ali-Boghan, separating it from the Chardeh Plain, which again extends as far as Basawul. I got a kind of bird's-eye view of this one day from a spur of the Sufaid Koh, 8,000 feet high, near to Gundumuck, and the Jelalabad Valley and the Chardeh Plain seemed to be all one, the hills at Girdi Kas appearing at this distance to be only a few slight mounds lying in the middle of this space, which would be altogether about 40 miles in extent. When in the Jelalabad Valley, the Girdi Kas hills are undoubtedly the eastern barrier, while the Siah Koh Range is the western. The Siah Koh Range trends to the south-west, and then turns due west, forming a distinct barrier on the north till it is lost at Jugduluck; there are only some low-lying ridges between Futteeabad and Gundumuck, but they are so small that it might be said to be a continuous valley all the way from Ali-Boghan to the plain of Ishpan. The eastern end of the Siah Koh Range terminates at Darunta, which is the north-west corner of the Jelalabad Valley. The Kabul River, instead of going round the extreme end of this range, has, by some curious freak, found a way through the rocky ridge so close to the extremity, that it leaves only what might be called one vertebra of this stony spine beyond. The river here has formed for itself a narrow gorge through perpendicular cliffs, in which it flows, from the district of Lughman, into the level plain of the Jelalabad Valley. The Surkhab pours down from the Sufaid Koh, starting close to Sikaram, the highest point of the range, which our surveyors found to be 15,600 feet above the sea. It passes over the western end of the Ishpan plain, towards the Siah Koh Range, and it then keeps to the contour of its base all the way to the Jelalabad Valley, and joins the Kabul River about two miles below Darunta.


1898 ◽  
Vol 4 ◽  
pp. 95-100
Author(s):  
Duncan Mackenzie

From the modern town of Kos, on the site of the ancient capital at the north-east extremity of the island, to the village of Kephalos at the southwest end is a ride of eight hours.The village stands on a chalky plateau which beyond the isthmus marks the beginning of the mountain district of south-west Kos. This in turn is a repetition on a smaller scale of the mountain region, at the other end of the island, which forms the lofty termination to the long central tableland. The highest points of the mountain district are towards the south-east where the fall to the sea is very rapid. The highest neighbouring peak, Mount Ziní, is about an hour distant from the village in a south-easterly direction, while all that lies to the north-west of the main range is high pastoral country with many torrent beds.


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