Pontica

1900 ◽  
Vol 20 ◽  
pp. 151-158 ◽  
Author(s):  
J. G. C. Anderson

About forty-five miles in an air-line west-south-west of Samsun (Amisos) lies the town of Vezir Keupru, situated at the eastern edge of a rolling plain bounded towards the west by the Halys, on the south by the long ridge of Tavshan Dagh, and on the north by the mountain-rim of the plateau through which the Halys forces its way to the sea. This undulating tract is the extreme westerly part of the ancient Phazemonitis, over which passed the one great ‘through route’ from Constantinople across Paphlagonia to the Euphrates, following throughout its course a line curiously parallel to the coast. Though this road is not described in any ancient document, its importance for the Roman period is amply proved by a remarkably complete series of milestones, erected or re-erected by successive emperors between Nerva and Constantine, which we discovered last summer between the Halys and Neocaesareia. In modern times it cannot claim any such importance.

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.


2007 ◽  
Vol 37 (2) ◽  
pp. 219-225 ◽  
Author(s):  
Jo Verhoeven

Hamont is a small town located on the north-eastern edge of the Belgian province of Limburg, on the national border with the Netherlands. It is situated about 30 km south of Eindhoven and 15 km west of Weert in the Netherlands. The town has about 13,500 inhabitants. According to Belemans, Kruijsen & Van Keymeulen (1998), the dialect of Hamont belongs to the West Limburg dialects (subclassification: Dommellands). Limburg dialects occupy a unique position among the Belgian and Dutch dialects in that their prosodic system has a lexical tone distinction, which is traditionally referred to as SLEEPTOON ‘dragging tone’ and STOOTTOON ‘push tone’. In line with recent conventions, stoottoon is referred to as Accent 1 and transcribed as superscript 1; sleeptoon is referred to as Accent 2 and is transcribed as superscript 2 (cf. Schmidt 1986).


Archaeologia ◽  
1910 ◽  
Vol 62 (1) ◽  
pp. 333-352 ◽  
Author(s):  
G. Wyman Abbott ◽  
Reginald A. Smith

The series of relics exhibited to the Society come from an early settlement at Peterborough, dating from a time when flint was in general use, perhaps before the introduction of metal, at least among the poorer inhabitants of the country. The site is a promontory rising out of the Fens and lying on the north-east side of the town. The river Nene joined the Fens about half a mile to the south-west of the site, which is only a few feet above sea-level, and was almost surrounded in times of flood. So far as can be determined at present, the extent of the settlement is several acres, but the ground has not yet been moved except on the west side, where unfortunately no observations were taken. There were no surface indications of human habitation, and no burrows noticed on the promontory or in its neighbourhood. The subsoil is gravel, fine and coarse, varying in depth from 8 to 10 feet. The top 18 inches of gravel, underlying the soil, is reddish brown, mixed with a reddish loam, which sometimes occupies natural pockets 3 to 8 feet deep, cutting down through the gravel and at times reaching the cornbrash below.


1946 ◽  
Vol 66 ◽  
pp. 99-107 ◽  
Author(s):  
A. W. Lawrence

The argument of this paper is that the fort on the Euryalus at Syracuse was modernised by Archimedes, who is recorded to have been the chief military engineer or scientific adviser to his native city before and during the siege by the Romans.The fort lay outside the populated area of Syracuse though within the walls. The town had originally been confined to an island between the two harbours, but soon extended on to the mainland of Sicily; the ground to the west was swampy, hence the suburbs necessarily spread up the Epipolae hill to the north. This hill forms a tilted plateau, 3½ miles long, which slopes towards the island, but is surrounded elsewhere by a cliff, except at the inland extremity where it joins on to higher country. Since the cliff afforded a strong line of defence, the town walls were eventually carried all round the edge of the plateau, making them 17 miles in circuit. This great extension was the work of the tyrant Dionysius I, in the year 402 and later; the need for it had been demonstrated twelve years earlier, when the Athenians captured the plateau and almost starved the town into surrender. The strongest part of the fortifications was necessarily at the inland extremity of the plateau, the one place where nature provided no obstacles. Here the highest ground runs off to the west in a ridge that rises into two gentle mounds, one of which was called Euryalus, meaning the ‘wide nail’ (or wart). The town-walls included only one of these summits, and upon it stands the fort in question, overlooking one of the main gateways of the city.


1983 ◽  
Vol 15 (1) ◽  
pp. 47-57 ◽  
Author(s):  
R. Calderon

The natural region of the Jara, with an area of 2500 km2 occupies much of the south west of the province of Toledo, and extends into the provinces of Caceres and Ciudad Real. It is situated between the Tajo and Guadiana rivers, south of the town of Talavera de la Reina, the centre of the economic life in this region. Its highlands are covered with xerophytic vegetation, of which the most common plant is the jara (Cistus ladaniferus), from which this zone takes it name, (Fig. 1). It has been occupied from the neolithic period onwards by peoples of different origins, e.g. Romans, Muslims, Jews, Mozarabs (Jimenez de Gregorio, 1959) but the present population derives from settlement from the north of the Tajo river beginning in the 14th century following the upheavals of the Moslem–Christian wars.


1907 ◽  
Vol 7 (1) ◽  
pp. 22-31 ◽  
Author(s):  
R. Tanner Hewlett ◽  
George S. Barton

In view of the importance of a pure milk supply, we considered that it might be of interest to examine chemically, microscopically, and bacteriologically, a number of specimens of milk coming into the Metropolis for which purpose we decided to select samples from the various counties, the milk of which is consigned to London. We found that milk so consigned comes from about twenty-six counties extending from Derby in the North, to Hampshire and Devonshire in the South and South-West, and from Hereford in the West, to Norfolk in the East.


Antiquity ◽  
1955 ◽  
Vol 29 (114) ◽  
pp. 77-88 ◽  
Author(s):  
Kenneth Jackson

The archaeological background of the people of what is now Scotland south of the Forth and Clyde in the Roman period was a La Téne one, and specifically chiefly Iron Age B. This links them intimately with the Britons of southern Britain in the conglomeration of Celtic tribes who called themselves Brittones and spoke what we call the Brittonic or Ancient British form of Celtic, from which are descended the three modern languages of Welsh, Cornish and Breton. To the north of the Forth was a different people, the Picts. They too were Celts or partly Celts; probably not Brittones however, but a different branch of the Celtic race, though more closely related to the Brittones than to the Goidels of Ireland and (in later times) of the west of Scotland. Not being Brittonic, the Picts may be ignored here. Our southern Scottish Brittones are nothing but the northern portion of a common Brittonic population, from the southern portion of which come the people of Wales and Cornwall. Some historians speak of the northern Brittones as Welsh, following good Anglo-Saxon precedent, but this is apt to lead to confusion. The best term for them, in the Dark Ages and early Medieval period, as long as they survived, is ‘Cumbrians’, and for their language, ‘Cumbric’. They called themselves in Latin Cumbri and Cumbrenses, which is a Latinization of the native word Cymry, meaning ‘fellow-countrymen’, which both they and the Welsh used of themselves in common, and is still the Welsh name for the Welsh to the present day. The centre of their power was Strathclyde, the Clyde valley, with their capital at Dumbarton.


2019 ◽  
pp. 1-8
Author(s):  
Thomas Waters

This chapter shows that the history of black magic in modern times is a cosmopolitan drama. Human movement rapidly accelerated from the nineteenth century. People, goods, technologies, and ideas began crossing the earth at a dizzying rate. Travellers took their magical beliefs abroad and encountered new mysticisms when they got there. Empires regulated their colonial subjects in all sorts of ways, including how they dealt with witches. Witchcraft became more international, though at the same time it remained fundamentally rooted in local circumstances. This means that, to understand modern witchcraft, one must combine a global orientation with a local focus. And an excellent place for that local focus is a large island, lying on the eastern edge of the North Atlantic Ocean: Britain.


2014 ◽  
Vol 11 ◽  
pp. 72-81
Author(s):  
Peter Wood

In April, 1845, the Rev. Richard Taylor passed through the area of the North Island now marked by the town of Levin. At this time, he described Lake Horowhenua as being of singular appearance for the small storehouses built over the water on poles. As was his predilection, Taylor made a drawing of the lake huts, a version of which was belatedly included in the second edition of his most important literary contribution, Te Ika-a-Māui (1870). This image would have remained as little more than a questionable curiosity was it not for Messrs Black Bros who, in the course of exploring the lake bed for Māori artefacts in 1932, legitimised Taylor's observation with their discovery of the submerged architectural remains of an aquatic hut. Nonetheless, almost a century after Taylor's original diary entry, GL Adkin, writing for The Journal of the Polynesian Society, lamented the neglect shown toward these remarkable structures, and which he cited as just one example of the "tantalising gaps" in the recorded history of Māori custom and culture. Sadly, it is well beyond the scope of this research to properly redress the historical neglect shown toward lake pātaka. What I do wish to do is to link these structures to an event on the shores of the Lake of Zurich, Switzerland, when Dr Ferdinand Keller noticed some half-submerged piles in 1854. Upon these remains Keller made a great, if erroneous, case for primitive "pile-work habitations" in the Swiss lakes. The impact of this argument cannot be understated. It became the privileged model for architectural origins in the German and French parts of Switzerland, and by the 1890s it was a part of standard teaching texts in Swiss schools, where it was firmly inculcated into the curriculum at the time that Charles Edouard Jeanneret was a child. This in turn has led Vogt to suggest that, in Keller's "dwellings on the water," Le Corbusier found a Primitive Hut typology that underpinned all his architectural thinking, and which is made most explicit in his principled use of piloti. What makes this all the more involved is that Keller, in searching for examples to visualise the construction of the Swiss lake dwellings, turned to the Pacific (which he categorised as at a developmental stage of architectural evolution akin to early Europe). In this paper I identify the exact etching by Louis Auguste de Sainson that Keller took for direct influence. The problem, however, is that de Sainson depicted a conventional whare built on land, and Keller transposed it to the water. So we have on the one side of this paper an authentic lake whare that is all but forgotten, and a famed European lake-hut that is all but Māori, and between the two is the figure of Le Corbusier who may or may not have unknowingly based one on his major innovations on influences found in the pātaka of Lake Horowhenua.


1970 ◽  
Vol 36 ◽  
pp. 125-151 ◽  
Author(s):  
John M. Coles ◽  
F. Alan Hibbert ◽  
Colin F. Clements

The Somerset Levels are the largest area of low-lying ground in south-west England, covering an extensive region between the highlands of Exmoor, the Brendon Hills and the Quantock Hills to the west, and the Cotswold and Mendip Hills to the east (Pl. XXIII, inset). The Quantock Hills and the Mendip Hills directly border the Levels themselves, and reach heights of over 250 metres above sea level. The valley between extends to 27 metres below sea level, but is filled to approximately the height of the present sea by a blue-grey clay. The Levels are bisected by the limestone hills of the Poldens, and both parts have other smaller areas of limestone and sand projecting above the peat deposits that cap the blue-grey clay filling. In this paper we are concerned with the northern part of the Levels, an area at present drained by the River Brue.The flat, peat-covered floor of the Brue Valley is some six kilometres wide and is flanked on the north by the Wedmore Ridge, and on the south by the Polden Hills (Pl. XXIII). In the centre of the valley, surrounded by the peat, is a group of islands of higher ground, Meare, Westhay, and Burtle. These islands, which would always have provided relatively dry ground in the Levels, are linked together by Neolithic trackways of the third millennium B.C. Several of these trackways formed the basis of a paper in these Proceedings in 1968 (Coles and Hibbert, 1968), which continued the work of Godwin and others (Godwin, 1960; Dewar and Godwin, 1963).


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