scholarly journals VII. Observations of the aurora borealis made in England by Andr. Celsius, F. R. S. and Secr. R. S. of Upsal in Sweden

1735 ◽  
Vol 39 (441) ◽  
pp. 241-244 ◽  

Sept . 13, 1735, in the Town of Woodford , six Miles to the North East of London , at 11½ h.

1925 ◽  
Vol 15 (3) ◽  
pp. 257-271 ◽  
Author(s):  
James Hendrick ◽  
George Newlands

1. Previous investigations showed that certain Scottish soils were of glacial drift origin, that they were comparatively rich in unweathered silicates and therefore in reserves of plant-food, that they showed considerable variation in such silicates and were capable of classification accordingly. Some indication was also shown that the glacial drift, and hence the resulting soil, was sometimes of local origin, its character being determined by the underlying rock. In the present investigation a more extensive survey of Scottish soils has been made in order to discover to what extent these preliminary findings might be applicable generally.2. For this purpose soils have been collected from various localities in the north, north-east, west and south of Scotland, and have been analysed mechanically and the “fine sand” fraction examined mineralogically.


1936 ◽  
Vol 16 (1) ◽  
pp. 1-7
Author(s):  
F. Cottrill

Excavations made in June 1935 for the foundations of a new sub-station of the London Passenger Transport Board at Trinity Place, Trinity Square, E.C., brought to light some remains of the Roman town wall of London. A large portion of the medieval superstructure is still standing on the east side of Trinity Place, and to the north of this the Inner Circle Railway runs in a cutting under the roadway. The construction of this cutting involved the removal of a length of 73 ft. of the wall in 1882 (R.C.H.M. Roman London, 83). The site of the discoveries to be described here was immediately behind the southern retaining wall of the cutting. Both faces of the Roman wall were exposed at this point, and could be examined in detail, and against the external face was a fragment of one of the later Roman bastions (pl. 1). These remains were investigated by the writer on behalf of this Society, and the Passenger Transport Board kindly granted all necessary facilities, and rendered every possible assistance.


2021 ◽  
pp. 102452942110113
Author(s):  
Luke Telford

Based on 52 qualitative interviews with working-class individuals, this paper explores the social and economic decline of a coastal locale referred to as High Town in Teesside in the North East of England. First, the paper outlines how the locality expanded as a popular seaside resort under capitalism’s post-war period. It then assesses how the seaside existed together with industrial work, offering stable employment opportunities, economic security and a sense of community. Next, the article documents the shift to neoliberalism in the 1980s, specifically the decline of High Town’s seaside resort, the deindustrialization process and therefore the 2015 closure of High Town’s steelworks. It explicates how this exacerbated the locale’s economic decline through the loss of industrial work’s ‘job for life’, its diminishing popularity as a coastal area and the further deterioration of the town centre. The paper concludes by suggesting that High Town has lost its raison d’être under neoliberalism and faces difficulties in revival.


Archaeologia ◽  
1779 ◽  
Vol 5 ◽  
pp. 95-97
Author(s):  
Pegge

Rudston, a village in the East-Riding of Yorkshire, on the Wolds, near Burlington, is thus noticed in bishop Gibson's edition of Camden, col. 901. “More inward into the “land, is Ruston, where, in the church-yard, is a kind of “pyramidal stone of great height. Whether the name of the “town may not have some relation to it, can be known only “from the private history of the place; but if the stone bear “any resemblance to a cross, rod in Saxon doth imply so much.” This cross, as the bishop calls it, and I think not improperly, is a very curious monument; and, no doubt, of very remote antiquity. I am not aware that it has ever been engraved, and therefore I here present the Society with an accurate drawing* of it, which I received A. 1769, from the friendly hand of Mr. Willan, whose account I shall take the liberty to subjoin. “This stone stands about four yards from the North East “corner of Rudston church, which is situated on a high hill. “Its depth under ground equal to its height above, as appeared “from an experiment made by the late Sir William Strickland. “All the four sides are a little convex, and the whole covered “with moss. No tradition in this country of any authorrity, either concerning the time, manner, or occasion of its “erection.”


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.


2008 ◽  

From the late Sixties on, industrial development in Italy evolved through the spread of small and medium sized firms, aggregated in district networks, with an elevated propensity to enterprise and the marked presence of owner-families. Installed within the local systems, the industrial districts tended to simulate large-scale industry exploiting lower costs generated by factors that were not only economic. The districts are characterised in terms of territorial location (above all the thriving areas of the North-east and Centre) and sector, since they are concentrated in the "4 As" (clothing-fashion, home-decor, agri-foodstuffs, automation-mechanics), with some overlapping with "Made in Italy". How can this model be assessed? This is the crucial question in the debate on the condition and prospects of the Italian productive system between the supporters of its capacity to adapt and the critics of economic dwarfism. A dispassionate judgement suggests that the prospects of "small is beautiful" have been superseded, but that the "declinist" view, that sees only the dangers of globalisation and the IT revolution for our SMEs is risky. The concept of irreversible crisis that prevails at present is limiting, both because it is not easy either to "invent", or to copy, a model of industrialisation, and because there is space for a strategic repositioning of the district enterprises. The book develops considerations in this direction, showing how an evolution of the district model is possible, focusing on: gains in productivity, scope economies (through diversification and expansion of the range of products), flexibility of organisation, capacity to meld tradition and innovation aiming at product quality, dimensional growth of the enterprises, new forms of financing, active presence on the international markets and valorisation of the resources of the territory. It is hence necessary to reactivate the behavioural functions of the entrepreneurs.


2010 ◽  
Vol 1 (1) ◽  
pp. 81 ◽  
Author(s):  
Rudy Ercek ◽  
Didier Viviers ◽  
Nadine Warzée

<p>The city of Itanos is situated in the North-East of Crete. Between 1994 and 2005, the French School of Archaeology at Athens (Efa) and the Center for Mediterranean Studies in Rethymnon carried out excavation campaigns during which a necropolis and an Archaic building have been explored by a team of the CReA. A very close collaboration between archeologists, engineers and computer graphic designers allowed the 3D reconstruction of these remains. The archeologist was able to directly verify his hypotheses during the reconstruction process. In summer 2007 and 2008, a 3D digitalization of Itanos was made in order to insert the 3D reconstructions into the actual landscape.</p>


Author(s):  
T. Hogue

The twin communities of Inangahua Camp and Inangahua Junction were rudely awakened at approximately 5.25 a.m.by a severe earthquake. About a minute before the quake all the birdlife suddenly stopped their noisy callingand an uncanny stillness settled over the area. The first movement of the earthquake was an upward displacement although a few argue that the initial displacement was to the north east. No longer than two seconds later the high frequency vibrating and confusion of noise enveloped the town, then came the jolting of no discriminate pattern as shock-waves started to rebound through the region. During the peak of the earthquake most people who. were by now fully awakened thought that "this was the end", any dissenters from this view acknowledged that it was "at least a beaut”.


Itinerario ◽  
2002 ◽  
Vol 26 (1) ◽  
pp. 107-125
Author(s):  
Rafael Ruiz

Historians have made in depth studies on the consequences of the Dutch incursions and invasion into the north and northwest of Brazil, for both the Spanish Empire and the United Provinces of the Dutch Republic. The purpose of this paper is to show that the war between Spain and the Dutch Republic also affected the south of Brazil and that it forced Spain to adopt measures that altered the policy of the Spanish Crown regarding Sao Paulo.


1974 ◽  
Vol 14 (1) ◽  
pp. 21 ◽  
Author(s):  
R. M. Bell ◽  
R. G. C. Jessop

The West Sulu Basin lies in the western portion of the Sulu Sea. Republic of the Philippines. It occupies an area in excess of 26,000 square miles (67,000 km2) and is bounded to the west and south by the cordilleran arc extending from the island of Palawan through Sabah and along the Sulu Archipelago to the island of Mindanao. To the north-east, the basin probably extends beyond the edge of the continental shelf in Philippine territorial waters.The basin may be broadly divided into a western platform and an eastern deep: the latter is subdivided by northeast-trending basement ridges into three sub-basins. Sediments deposited in these sub-basins are of Tertiary to Recent age and have been affected by several orogenies and by contemporaneous movements of fault-controlled blocks. This has resulted in truncation and the development of marked erosion surfaces and onlap within the Upper Tertiary section. Many anticlinal features mapped within the basin have resulted from drape over basement highs or from penecontemporaneous growth of these highs.Major unconformities associated with Upper Tertiary tectonic events have been recognized onshore. Extrapolation to offshore areas where these events can be seismically mapped has enabled an interpretative geologic model to be built up. Provisional identification of stratigraphic units and their nature have been made using this model.The Upper Tertiary section within the eastern deep is expected to consist of deltaic and paralic reservoir sands interbedded with, grading into and transgressed by deeper water shale and mudstone with good hydrocarbon source potential. Some limestone lenses may be present.The presence of Lower to Middle Miocene diapiric shale and Plio-Pleistocene intrusives coupled with data of variable quality makes seismic interpretation difficult in some areas. However, several large anticlinal features and a number of stratigraphic and combination traps have been located.A non-commercial discovery of oil and gas has been made in the basin.


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