scholarly journals XXIII. An observation of the lights seen in the air, an Aurora Australis, on March 18. 1738-9. at London,

1740 ◽  
Vol 41 (461) ◽  
pp. 839-840
Keyword(s):  
The City ◽  

On Sunday evening, March 18. 1738-9. about half an hour past seven, the sky to the north was very clear, and the stars shone bright; to the south and south-east, as I was in the skirt of the town on the north-west side, the sky looked obscured, partly from a mist, partly from the smoak of the city.

1913 ◽  
Vol 10 (5) ◽  
pp. 205-215 ◽  
Author(s):  
A. R. Horwood

Although the Rhætic beds are not exposed continuously along the eastern boundary of the Keuper outcrop, they have been proved at many points from the River Trent in the north on the Nottinghamshire border to Glen Parva in the south. South of this point there is so much drift, and borings within the Liassic outcrop have been so isolated or shallow, that there is a gap in our knowledge of the intervening ground between the last point and the Rugby district. The Countesthorpe boring, carried to a depth of over 600 feet, encountered Upper Keuper beneath the Drift, with no intervening Rhætics. Commencing in the north in the Gotham district the two outliers are capped above the Red Marl and Tea-green Marl with Rhætic beds, and Lower Lias Limestone (Ps. planorbe zone) above. At Ash Spinney at the south end of the southern outlier, and at the east end of Crownend Wood, Black Shales with Avicula contorta crop out; and on the west side septaria are seen. On the north-west side of the northern outlier at Cottager's Hill Protocardium phillipianum has been found in a well-section near the lane. Rhætic shales are seen in the shafts driven for gypsum works about Gotham.


2018 ◽  
Vol 1 (123) ◽  
pp. 45-62
Author(s):  
Ahmed Abbas

The QADIS survey project is a joint initiative of the Alma Mater Studiorum - University of Bologna and the State Board of Antiquities and Heritage (SBAH). The findings presented here were analyzed in the frame of the EU funded project "EDUU - Educational and Cultural Heritage Enhancement for Social Cohesion in Iraq" (EuropeAid CSO-LA/2016/382-631). The first, second and third field seasons took place in January and October 2016 and in January 2017 respectively. We report here on the general survey activities of the first two seasons, providing detailed information on 40 sites newly identified in addition to Adams 1981. The survey area (Fig. 1) follows the administrative borders of the region of Qadisiyah to the South and East (including part of the Delmej basin), and it stops around the town of Afak to the North-West.1


2001 ◽  
Vol 23 (1) ◽  
pp. 71 ◽  
Author(s):  
PM Johnson ◽  
MDB Eldridge ◽  
V Kiernan ◽  
RJ Cupitt

IN 1982, the Queensland subspecies of the blackfooted rock-wallaby Petrogale lateralis purpureicollis was reported to occur around Mt Isa and south to around Dajarra (Briscoe et al. 1982). During 1991, the known range of this taxon was extended 300 km to the north-west when an adult female P. l. purpureicollis was collected from ?Ridgepole Waterhole? in the Musselbrook Resource Reserve near Lawn Hill National Park (Eldridge et al. 1993). In 1994 the range was further extended when P. l. purpureicollis was recorded from the Constance Ranges and the upper reaches of Stockyard and Elizabeth Creeks; around the town of Cloncurry and the following distances from the town: 85 km north west; 60 and 87 km west; 4, 23, 28 and 35 km south and 15 km east (Bell et al. 1995). Approaches by the Cannington Mining operation to the southwest of McKinley in October 1999 to confirm the presence of rock-wallabies on nearby Glenholme Station established the presence of P. l. purpureicollis; a 75 km range extension to the south-east.


1865 ◽  
Vol 1 (2) ◽  
pp. 247-286
Author(s):  
J. Dowson

In the year 1837, Dr. A. Burn transmitted to Mr. James Prinsep, then Secretary of the Asiatic Society of Bengal, transcripts and facsimiles of four Copper Plate Inscriptions. “These plates,” he said, “were found in the town of Kaira, about ten years ago. The river Watrua runs close to the walls on the north-west side, and was the cause of the discovery, by washing down the walls and earth. They had been handed about the country among the natives for translation, it being supposed they were connected with some deposit of treasure. At last they were brought to me by a fakir, of whom I purchased them.”


Author(s):  
Stephen Burt ◽  
Tim Burt

This chapter provides a brief introduction to the City of Oxford, its location, topography, climate and history. It provides a context for the weather observations presented in the rest of the book. Oxford, the county town of Oxfordshire, is located in the south Midlands of England. It lies just under 100 km west-north-west of London and 40 km north-west of Reading. The Radcliffe Observatory was built on the northern edge of the city in the 1770s. Since then, there has been extensive suburban development to the north. The city stands on a low-lying river terrace of the Thames, close to the present floodplain; this will influence certain aspects of the microclimate such as the incidence of fog.


Author(s):  
Roger Ling ◽  
Lesley Ling

We take the opportunity of modifying ideas presented in Volume I, and responding to queries raised by reviewers and other commentators. 1. Street fountains. It was claimed in Volume I (p. 252) that the cutting back of the fac¸ade of I.10.1 to create space round the fountain was almost without parallel in the city: the only other places where we could point to similar sacrifices being made, either for fountains or for the distribution tanks and watertowers which were an integral part of the distribution system provided to feed them, were at the southern tip of Insula VI.1 and the south-east corner of VI.14. We suggested, therefore, that the owner or occupier of I.10.1, rather than being subject to an expropriation order, may have yielded the space voluntarily. It is certainly true that street fountains and water-towers were as far as possible sited to avoid impinging upon existing buildings, even though the installations in question almost invariably ended up both encroaching upon the sidewalk and projecting into the carriageway. In some cases, as at the northeast corner of VI.8, there was no great problem, because there was suficient space for pedestrians and wheeled trafic to get past without dificulty. In other places, the street was closed to vehicles, so the fountain could project freely into the carriageway or even stand wholly within it: such was the case at the north-west corner of VI.13, where the lack of ruts and a strategically placed bollard at the south end conform that the Vico del Labirinto was for pedestrians only. The western stretch of the Via dell’Abbondanza, between the forum and the Via Stabiana crossing, was at least partially closed to vehicles, but there was, in any case, no shortage of space for the fountains at the south-east corners of VII.9 and VII.14. At the north end of the Via delle Scuole, closed off by the forum colonnade, it was even possible to site a fountain in the middle of the road. In other cases, however, accommodating the fountain presented serious difficulties. At the south-east corner of VII.4, for instance, the fountain jutted into the street so far as to leave only a narrow gap for wheeled trafic to squeeze through, and ultimately the street was closed.


1906 ◽  
Vol 3 (4) ◽  
pp. 171-176 ◽  
Author(s):  
Charles Davison

Pendleton lies on the north-west side of Manchester and within the borough of Salford, and is traversed by the well-known Pendleton or Irwell Valley fault, a fault which has been traced for more than twenty miles from the neighbourhood of Bolton to that of Poynton in Cheshire. The fault is still slowly growing, for, on February 10th, 1889, a slip near Bolton gave rise to an earthquake of intensity 6, felt over an area of about 2,500 square miles. Small superficial movements may also be taking place close to Pendleton, though here probably aided by mining operations. Within the last seven years there have been local shakes on three occasions, namely, February 27th, 1899, April 7th, 1900, and November 25th, 1905. The materials for the study of the first two of these shakes are not quite sufficient to determine the boundaries of their disturbed areas with accuracy. The areas appear, however, to have been approximately circular in form and about four or five miles in diameter. In both cases the intensity of the shock was 4, or nearly 5. In 1899 the centre of the disturbed area was about half a mile north of Pendleton and a short distance on the north-east or downthrow side of the Pendleton fault; in 1900 it lay a mile or two farther to the south or south-south-east of the former centre.


1921 ◽  
Vol 58 (5) ◽  
pp. 200-205
Author(s):  
J. E. A. Whealler

ABOUT twelve years ago Dr. R. H. Rastall and Mr. J. Romanes published an account of the Boulders of the Cambridge Drift. In this paper a list was given of the rock-types recognized at that time in the gravels of the Travellers' Rest Pit, situated about a mile north-west of the town of Cambridge on the Huntingdon Road. Since that time Professor Marr has paid much attention to this pit, among others, with special reference to the Palæolithic implements there found. He has embodied his results in two important papers. In the course of this work Professor Marr collected a number of interesting erratics, and the same pit has also been investigated by many geologists connected with the University, both members of the Sedgwick Club and others. During the last ten years, though the North Pit has been abandoned, the South Pit has been very actively worked for gravel, and has been greatly increased in size. In consequence of this a large amount of additional material has been collected, including many new types, while some of the older specimens, whose origin had been left indeterminate by Rastall and Romanes, have been now identified. Hence it is felt that the time has now arrived when these more recent results should be put on record.


1906 ◽  
Vol 38 (3) ◽  
pp. 553-580
Author(s):  
W. Vost

Do the Chinese pilgrims know two cities named Kapilavastu?Certain discords and bearings in the itineraries of the pilgrims are discussed in the Prefatory Note to Antiquities in the Tarai, Nepal, and from them it is inferred there were two cities named Kapilavastu; one the city visited by Fa-hsien, now represented by the ruins at Piprāhavā; the other that described by Yuan Chwang, of which the “royal precincts” are found in Tilaurā Koṭ, some ten miles to the north-west of Piprāhavā. Paltā Devī is held to mark the site of the town either of the Buddha Krakucandra or of the Buddha Koṇāgamana; or Sisaniā Pānḍe may represent the town of Koṇāgamana. Guṭihavā is believed to represent the site of the famous Nyagrodha grove.


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

This complex consists of an atrium-house from which a front room has been separated at a late stage to form an independent shop or workshop. Together they occupy the north-west corner of the insula, the house opening northwards and the shop westwards. Before the shop was separated from it, the house had a relatively broad facade (approx. 14 m.), but the oblique alignment of the insula boundary to the west resulted in a considerable contraction towards the rear. At the southern end of the roofed part of the house, coinciding with the south walls of rooms 10 and 12, the property is only 10 m. wide; and the garden beyond this, thanks primarily to a shift in the line of the eastern boundary becomes even narrower, contracting to less than 8.50 m. As in the Casa del Fabbro, the atrium (1) is set against one of the property boundaries, this time the west rather than the east; but, owing to the greater width of the house, it is broader (from 7.20 to 8.20 m.) and still allows space for a deep room on the east. The impluvium is centrally positioned in relation to the short (south) side. The fauces, however, enters the atrium somewhat off-centre, 3.80 m. from the northeast corner and 2.70 m. from the north-west, presumably in order to obtain three more or less equally sized rooms on the north facade. As the plot contracts toward the rear, this tripartite division becomes more difficult; the outlying rooms, on the west side particularly are uncomfortably narrow and cramped. Of the three rooms on the north front, the westernmost is the one which in the final period had become a shop with an independent entrance (I 10, 9); it had formerly been a corner room opening from the atrium via a doorway immediately adjacent to the fauces, but this doorway was blocked and a new entrance, 2.30 m. wide, quoined in opus listatum, was opened in the west wall (Pl 90). The lava threshold (Fig. 61) points to fittings typical of a shop: a separate pivoted door and vertical planks set overlapping in a groove.


Sign in / Sign up

Export Citation Format

Share Document