XXVI.—A Late-Celtic and Romano-British Cave-dwelling at Wookey-Hole, near Wells, Somerset

Archaeologia ◽  
1911 ◽  
Vol 62 (2) ◽  
pp. 565-592 ◽  
Author(s):  
H. E. Balch ◽  
R. D. R. Troup

The great cavern of Wookey-Hole is situated two miles to the north-west of the city of Wells, in the centre of Somerset, and immediately adjacent to the thriving- village which has taken the name of the cavern, and has depended for its prosperity on the existence of the copious and usually pellucid stream, which here bursts forth from Mendip's hidden reservoirs. This is the source of the Axe, which winds its way through the lower lands, and after uniting with the sister stream of Cheddar, flows into the sea near Weston-super-mare. From Wookey-Hole the southern slope of Mendip rises in an unbroken sweep till it reaches a thousand feet above the sea, commanding a magnificent view to the east, south, and west. It is not a limestone cave in the ordinary sense of the word, since every known cavity in the immediate vicinity is not in the Carboniferous Limestone, but in the Dolomitic Conglomerate, which here attains enormous thickness. To the north, the great mass of Carboniferous Limestone, receiving the water of innumerable springs from the Old Red Sandstone and Shales and from a generous rainfall, engulfs it in a countless number of swallets, many of which are insignificant, whilst some of the larger have been opened by our exploring parties during the past few years, and followed through unimagined beauties to profound depths.

Author(s):  
Partha Sarathi Datta

In many parts of the world, freshwater crisis is largely due to increasing water consumption and pollution by rapidly growing population and aspirations for economic development, but, ascribed usually to the climate. However, limited understanding and knowledge gaps in the factors controlling climate and uncertainties in the climate models are unable to assess the probable impacts on water availability in tropical regions. In this context, review of ensemble models on δ18O and δD in rainfall and groundwater, 3H- and 14C- ages of groundwater and 14C- age of lakes sediments helped to reconstruct palaeoclimate and long-term recharge in the North-west India; and predict future groundwater challenge. The annual mean temperature trend indicates both warming/cooling in different parts of India in the past and during 1901–2010. Neither the GCMs (Global Climate Models) nor the observational record indicates any significant change/increase in temperature and rainfall over the last century, and climate change during the last 1200 yrs BP. In much of the North-West region, deep groundwater renewal occurred from past humid climate, and shallow groundwater renewal from limited modern recharge over the past decades. To make water management to be more responsive to climate change, the gaps in the science of climate change need to be bridged.


1896 ◽  
Vol 3 (4) ◽  
pp. 167-174 ◽  
Author(s):  
Peter Macnair

In the following paper I propose to give an account of some observations upon the structure and succession of the rocks of the Southern Highlands. By the term Southern Highlands I mean that part of the Scottish Highlands lying immediately to the north-west of the great line of fault separating the older rocks of the former area from the younger Old Red Sandstone series of the low grounds.


1894 ◽  
Vol 1 (9) ◽  
pp. 394-399 ◽  
Author(s):  
J. Burr Tyrrell

In the extreme northernmost part of Canada, lying between North Latitudes 56° and 68° and West Longitudes 88° and 112°, is an area of about 400,000 square miles, which had up to the past two years remained geologically unexplored.In 1892 the Director of the Geological Survey of Canada sent the writer to explore the country north of Churchill River, and south-west of Lake Athabasca;in1893 the exploration was continued northward, along the north shore of Athabasca Lake


1886 ◽  
Vol 39 (239-241) ◽  
pp. 394-404

The question of the geological age of the yellow sandstones of the district lying to the north of the city of Elgin has been, as is well known, the subject of very animated discussions among geologists. Some have even gone so far as to assert that the evidence on the question, which has been adduced by palaeontologists, is absolutely incapable of reconciliation with that relied upon by stratigraphists.


Author(s):  
Anna K. Hodgkinson

Little is necessary in terms of an introduction, since Amarna is one of the best-known settlements of ancient Egypt. The city was founded by pharaoh Amenhotep IV, known from his fifth regal year as Akhenaten, on his move away from Thebes and Memphis to found a new religious and administrative capital city. Akhenaten reigned approximately between 1348 and 1331 BC, and his principal wife was Nefertiti. Akhenaten’s direct successor appears to have been a figure named Smenkhare (or Ankhkheperure) who was married to Akhenaten’s daughter Meritaten. Like Nefertiti, Smenkhare/Ankhkheperure held the throne name Nefernefruaten. For this reason it is uncertain whether this individual was Nefertiti, who may have reigned for some years after the death of Akhenaten, possibly even with a brief co-regency, or whether this was a son or younger brother of the latter. The rule of Smenkhare/Ankhkheperure was short, and he or she was eventually succeeded by Tutankhamun. The core city of Amarna was erected on a relatively flat desert plain surrounded by cliffs on the east bank of the Nile, in Middle Egypt, approximately 60km south of the modern city of Minia, surrounded by the villages et- Till to the north and el-Hagg Qandil to the south. The site was defined by at least sixteen boundary stelae, three of which actually stand on the western bank, past the edge of the modern cultivation. In total, the city measures 12.5km north–south on the east bank between stelae X and J, and c.8.2km west–east between the projected line between stelae X and J and stela S to the far east, which also indicates approximately the longitude of the royal tomb. The distance between stelae J and F, to the far south-west, measures c.20km, and between stelae X and A, to the far north-west 19.2km. The core city, which is the part of the settlement examined in this section, was erected along the Nile, on the east bank, and it is defined by the ‘Royal Road’, a major thoroughfare running through the entire core city north–south.


1893 ◽  
Vol 10 (9) ◽  
pp. 396-401
Author(s):  
Henry Hicks

In a recent article on the Pre-Cambrian Rocks of the British Isles in the Journal of Geology, vol. i., No. 1, Sir Archibald Geikie makes the following statement: “There cannot, I think, be now any doubt that small tracts of gneiss, quite comparable in lithological character to portions of the Lewisian rocks of the North-West of Scotland, rise to the surface in a few places in England and Wales. In the heart of Anglesey, for example, a tract of such rocks presents some striking external or scenic resemblance to the characteristic types of ground where the oldest gneiss forms the surface in Scotland and the West of Ireland.” To those who have followed the controversy which has been going on for nearly thirty years between the chiefs of the British Geological Survey and some geologists who have been working amongst the rocks in Wales, the importance of the above admission will be readily apparent; but as it is possible that some may be unable to realize what such an admission means in showing geological progress in unravelling the history of the older rocks in Wales during the past thirty years, a brief summary of the results obtained may possibly be considered useful.


2010 ◽  
Vol 75 (5) ◽  
pp. 703-715 ◽  
Author(s):  
Snezana Nenadovic ◽  
Ljiljana Matovic ◽  
Misko Milanovic ◽  
Sava Janicevic ◽  
Jasmina Grbovic-Novakovic ◽  
...  

In this paper, the impacts of some meteorological parameters on the SO2 concentrations in the City of Obrenovac are presented. The City of Obrenovac is located in the north-west part of Serbia on the banks of the River Sava. The observed source emission, the power plants TENT A and TENT B are situated on the bank of the Sava River in the vicinity of Obrenovac. During the period from January to November 2006, the concentrations of sulfur dioxide in the air at 4 monitoring sites in Obrenovac were measured. It was noticed that the maximal measured daily concentrations of sulfur dioxide ranged from 1 ?g/m3 (16th November, 2006) to 98 ?g/m3 (29th January 2006) and lie under the maximal allowed concentration value according to the Serbian Law on Environmental Protection. The measured sulfur dioxide concentrations mostly showed characteristics usual for a daily acidification sulfur dioxide cycle, excluding the specificities influenced by the measuring site itself. Sulfur dioxide transport was recorded at increased wind speeds, primarily from the southeast direction. Based on the impact of meteorological parameters on the sulfur dioxide concentration, a validation of the monitoring sites was also performed from the aspect of their representivity.


Urban History ◽  
2019 ◽  
Vol 47 (4) ◽  
pp. 671-688
Author(s):  
Katherine Fennelly

AbstractCities develop around industry, markets and transport links. Dublin in the nineteenth century was similar, but additionally the north-west of the city developed around the expansion of a complex of institutional buildings for the reception, confinement and welfare of the poor and sick. This article argues that these institutions were implicit in the development of the modern city in the same way as industry and commerce. The physical development of the buildings altered and defined both the streetscape and, over time, the social identities and historical communities in the locale, in the same way that industrial development defined urban areas.


2019 ◽  
Vol 10 (2) ◽  
pp. 255-270
Author(s):  
Caryn Abrahams ◽  
David Everatt

The city of Johannesburg offers insights into urban governance and the interesting interplay between managing the pressures in a rapidly urbanizing context, with the political imperatives that are enduring challenges. The metropolitan municipality of Johannesburg (hereafter Johannesburg), as it is known today, represents one of the most diverse cities in the African continent. That urbanization, however, came up hard against the power of the past. Areas zoned by race had been carved into the landscape, with natural and manufactured boundaries to keep formerly white areas ‘safe’ from those zoned for other races. Highways, light industrial plant, rivers and streams, all combined to ensure the Johannesburg landscape are spatially disfigured, and precisely because it is built into the landscape, the impact of apartheid has proved remarkably durable. Urban growth is concentrated in Johannesburg’s townships and much of it is class driven: the middle class (of all races) is increasingly being found in cluster and complexes in the north Johannesburg, while poor and working-class African and coloured communities in particular are densifying in the south. The racial and spatial divisions of the city continue to pose fundamental challenges in terms of governance, fiscal management and spatially driven service delivery.


2020 ◽  
Vol 11 ◽  
Author(s):  
Laura Hemming ◽  
Peer Bhatti ◽  
Jennifer Shaw ◽  
Gillian Haddock ◽  
Daniel Pratt

Suicide and violence are prevalent within male prisons in the UK. It has been suggested that alexithymia may be associated with both suicide and violence. Alexithymia can be defined as an inability to identify or discuss emotions. The present study aimed to qualitatively explore male prisoners' experiences of alexithymia and how these experiences may relate to suicide and violence. Fifteen male prisoners were recruited from two prisons in the North West of England. All participants had experienced suicidal and/or violent thoughts and/or behaviors in the past 3 months, and all screened positive on an established measure of alexithymia. Participants took part in a qualitative interview during which they were also given the opportunity to provide drawings of their emotions. Data were transcribed and analyzed using thematic analysis, with a collaborative approach taken between researchers and an individual with lived experience of residing in prison. The results indicated that male prisoners tended not to talk about their emotions with others, due to external pressures of residing in prison in addition to internal difficulties with recognizing and articulating emotions. Not discussing emotions with others was associated with a build-up of emotions which could result in either an emotional overload or an absence of emotions. Both experiences were perceived to be associated with hurting self or others, however, participants also identified a “safety valve” where it was acknowledged that using more adaptive approaches to releasing emotions could prevent harm to self and others. These findings suggest three main clinical implications; (1) a cultural shift in male prisons is needed which encourages open communication of emotions (2) individualized support is needed for those identified as experiencing a difficulty in recognizing and articulating emotions and (3) prison staff should encourage alternative ways of releasing emotions such as by using harm minimization or distraction techniques.


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