A pottery group from Ayun, Chitrāl

1970 ◽  
Vol 33 (1) ◽  
pp. 1-4 ◽  
Author(s):  
F. R. Allchin
Keyword(s):  
Early Years ◽  
North West ◽  
The Past ◽  
The North ◽  
The Subject ◽  
Victoria And Albert Museum

The pots which form the subject of this note are among the Indian collections of the Victoria and Albert Museum. They were presented to the museum in 1921 by Lt.-Col. F. C. S. Lamborne-Palmer, C.B.E., and a note in the accessions register recalls that they were discovered during the digging of the foundations of a house in the early years of the century, at Owin (Ayun) in the Chitrāl valley, now in West Pakistan. What was striking from the outset about at least one of the three vessels was its resemblance to a form of jug occurring in early contexts in Iran. But when my attention was first directed to the collection, in the early 1950's, enough was not known of the prehistory of the North-West Frontier to allow any further evaluation. During the past decade several new and interesting discoveries have been made, and one may now draw more confident inferences regarding the collection. There are three pots only.

scholarly journals Ensemble models on palaeoclimate to predict India's groundwater challenge

2013 ◽  
Vol 2 (3) ◽  
Author(s):  
Partha Sarathi Datta
Keyword(s):  
Climate Change ◽  
Climate Models ◽  
Global Climate ◽  
Global Climate Models ◽  
Humid Climate ◽  
Ensemble Models ◽  
North West ◽  
The Past ◽  
The North ◽  
14C Age

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.

Some Actuarial Aspects of Unemployment Insurance

1929 ◽  
Vol 60 (2) ◽  
pp. 103-160
Author(s):  
J. G. Kyd ◽  
G. H. Maddex
Keyword(s):  
Unemployment Insurance ◽  
Public Interest ◽  
Early Years ◽  
Royal Commission ◽  
Poor Laws ◽  
The Past ◽  
The Poor ◽  
National Insurance ◽  
The Subject ◽  
The Government

Judged by the amount of space devoted to the subject in the Journal of the Institute, Unemployment Insurance has received but little attention from actuaries in the past Public interest in the problem of relieving distress due to unemployment became pronounced in the early years of the present century and led to the appointment in 1904 of a Royal Commission on the Poor Laws and, eventually, to the passing in 1911 of the first Unemployment Insurance Act. These important events found a somewhat pallid reflection in our proceedings in the form of reprints of extracts from Sir H. Llewellyn Smith's address on Insurance against Unemployment to the British Association in 1910 (J.I.A., vol. xliv, p. 511) and of Mr. Ackland's report on Part II of the National Insurance Bill (J.I.A., vol. xlv, p. 456). At a later date, when the scope of the national scheme was very greatly widened, the Government Actuary's report on the relevant measure—the Unemployment Insurance Bill 1919—was reprinted in the Journal (J.I.A., vol. lii, page 72).

II.—Notes on the Pleistocene of the North-West Territories of Canada, North-West and West of Hudson Bay

1894 ◽  
Vol 1 (9) ◽  
pp. 394-399 ◽  
Author(s):  
J. Burr Tyrrell
Keyword(s):  
Geological Survey ◽  
Hudson Bay ◽  
North West ◽  
The Past ◽  
North Shore ◽  
The North ◽  
South West ◽  
North West Territories

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

III.—The Pre-Cambrian Rocks of Wales

1893 ◽  
Vol 10 (9) ◽  
pp. 396-401
Author(s):  
Henry Hicks
Keyword(s):  
Recent Article ◽  
British Isles ◽  
The West ◽  
British Geological Survey ◽  
England And Wales ◽  
North West ◽  
The Past ◽  
The North ◽  
History Of ◽  
Lithological Character

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.

Virgil's Location of Corythus

1976 ◽  
Vol 26 (2) ◽  
pp. 293-295
Author(s):  
E. L. Harrison
Keyword(s):  
Recent Article ◽  
Careful Examination ◽  
North West ◽  
The North ◽  
The Subject

In a recent article JRS (1973), 68 f. Nicholas Horsfall sought to demonstrate that Corythus, which Virgil makes the original home of Dardanus (Aen. iii, 167 f.), should be identified with Tarquinii, some 50 miles north-west of Rome, on the coast of Etruria, rather than with Cortona, roughly twice as far away, to the north, and inland. In doing so he expressed surprise that the Virgilian evidence should have been completely ignored by previous writers on the subject (p. 68): and, using the Aeneid as the main source on which his own argument was based, he supported his conclusion with a careful examination of several other aspects of the problem.

scholarly journals Words Don't Come Easy: How Male Prisoners' Difficulties Identifying and Discussing Feelings Relate to Suicide and Violence

2020 ◽  
Vol 11 ◽  
Author(s):  
Laura Hemming ◽  
Peer Bhatti ◽  
Jennifer Shaw ◽  
Gillian Haddock ◽  
Daniel Pratt
Keyword(s):  
Lived Experience ◽  
Harm Minimization ◽  
Open Communication ◽  
Cultural Shift ◽  
North West ◽  
The Past ◽  
The North ◽  
External Pressures ◽  
The Uk ◽  
Male Prisoners

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.

The verb in northern Najdi Arabic

1979 ◽  
Vol 42 (3) ◽  
pp. 467-499 ◽  
Author(s):  
Peter F. Abboud
Keyword(s):  
Saudi Arabia ◽  
North West ◽  
The North ◽  
Phonological Features ◽  
Najdi Arabic ◽  
The Subject ◽  
Object Pronouns

The dialects spoken in the Najd of Saudi Arabia have striking features which not only are unknown or unreported in other dialects but also retain some characteristics of the 'Arabiyya and of ancient dialects of the peninsula reported by the Arab grammarians. On both these counts, they are of paramount importance for synchronic, comparative and historical dialectology. Yet little is known of them and published materials remain scanty. It is the purpose of this article to describe in some detail the morphology of the verb, i.e., the stem, the subject markers and the object pronouns, and in the process, present phonological features and processes, in a dialect spoken in the North of the Najd, specifically that of Hāyil. This is an important town on the edge of the Jabal Shammar mountains just south of the Nafud, and some 350 miles to the north-west of Riyādh. Although the dialect manifests features which are typically Najdi, in the sense that investigation shows them to exist in other dialects of the Najd, it also possesses peculiarities all its own.

On Heptaphyllum, a New Genus of Carboniferous Coral

1924 ◽  
Vol 61 (9) ◽  
pp. 416-423 ◽  
Author(s):  
Arthur E. Clark
Keyword(s):  
New Genus ◽  
Growth Stages ◽  
Lower Carboniferous ◽  
North West ◽  
The North ◽  
Rugose Corals ◽  
The Subject ◽  
The Way ◽  
West Of Ireland

A few years ago Mr. Carruthers described an aberrant coral, Cryptophyllum hibernicum, from the Lower Carboniferous of Bundoran, Donegal. Cryptophyllum occurred in the Lower Calp shales, which are considered to be about at the horizon of Vaughan's C2 to S1 beds. Another aberrant genus, Heptaphyllum, also from the north-west of Ireland—Lower Carboniferous shales, Sligo—forms the subject of this paper. Cryptophyllum is remarkable, first for the manner in which the earlier major septa appear—irregularly, and nearly simultaneously, instead of regularly, and in consecutive pairs, as is typical for Rugose Corals; and also in the development of only five septa instead of the normal six in the earliest growth stages. Heptaphyllum, as its name implies, develops seven septa in the young corallum. It resembles Cryptophyllum in having an early aseptate corallum, and in the way in which the earlier septa appear.

Intermontane-basin development in the past 4 Myr in the north-west Himalaya

Nature ◽  
1982 ◽  
Vol 298 (5873) ◽  
pp. 432-436 ◽  
Author(s):  
Douglas W. Burbank ◽  
Gary D. Johnson
Keyword(s):  
North West ◽  
Intermontane Basin ◽  
The Past ◽  
The North ◽  
Basin Development ◽  
West Himalaya

The Roman Military Occupation of North-West Spain

1976 ◽  
Vol 66 ◽  
pp. 45-66 ◽  
Author(s):  
R. F. J. Jones
Keyword(s):  
Archaeological Site ◽  
Second Century ◽  
Military Force ◽  
Extensive Literature ◽  
Main Text ◽  
Gold Mines ◽  
North West ◽  
The North ◽  
History Of ◽  
The Subject

The north-west corner of Spain was long neglected by Roman archaeologists, who have tended to concentrate on the more spectacular remains to be found in the south and east. However, recently more attention has been directed there by workers of several nationalities, who have now produced a quite extensive literature on the gold mines, as well as on wider aspects, chiefly in connection with the activities of the legion VII Gemina. Yet there has been little attempt in all this to examine why a substantial military force was maintained in the region for so long. This paper aims to review that problem to about the end of the second century A.D. The evidence available is almost entirely epigraphic, chiefly consisting of epitaphs and religious dedications. Building inscriptions are scarce. For convenience all the epigraphic material from the north-west of Spain that is relevant to the disposition of the army is collected in the appendix, and in the main text reference will be made to the numbers given there. In addition a few historical passages are of importance, but the archaeological site evidence is very slight. The nature of the evidence is such that most attention must be devoted to the units attested in the region and their deployment, with little to be said about their actual bases. Previous work on the subject has been dominated by the late Antonio García y Bellido in several masterly papers. However it has tended to concentrate more on the history of the units themselves than on questions of topography and the reasons behind their presence.

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