The Lex Irnitana: a New Copy of the Flavian Municipal Law

1986 ◽  
Vol 76 ◽  
pp. 147-243 ◽  
Author(s):  
Julián González
Keyword(s):  
Place Names ◽  
North East ◽  
South West ◽  
Municipal Law ◽  
Metal Detectors ◽  
The Town

In the spring of 1981, on a hill called Molino del Postero, in undulating territory 5 km south-west of El Saucejo and 3 km north-east of Algámitas, in the province of Seville, a group of men looking for ancient coins and armed with metal-detectors discovered six bronze tablets and some small fragments of other tablets, containing part of the municipal law of a hitherto unknown town, the Municipium Flavium Irnitanum. Although the name of the town was probably Irni, since ancient place-names in Spain ending with -i are very common, such as Astigi, Ucubi, Tucci, Iptuci etc, a name such as Irnium remains possible.

scholarly journals XI.—Notes on the Geology of the Eildon Hills, in Roxburghshire

1853 ◽  
Vol 20 (2) ◽  
pp. 211-217
Author(s):  
James D. Forbes
Keyword(s):  
Small Group ◽  
The Other ◽  
Careful Examination ◽  
Eastern Slope ◽  
The West ◽  
North East ◽  
The North ◽  
South West ◽  
North Bank ◽  
The Town

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.

Amorium 1987: A Preliminary Survey

1988 ◽  
Vol 38 ◽  
pp. 175-184 ◽  
Author(s):  
R. M. Harrison
Keyword(s):  
First Century ◽  
Preliminary Survey ◽  
North East ◽  
The North ◽  
South West ◽  
Ancient Site ◽  
The Town

Amorium is in eastern Phrygia, 170 km. south-west of Ankara, 70 km. north-east of Afyon, 12 km. east of the town of Emirdaǧ, and near the source of the Sakarya (Sangarius) (Fig. 1). It lies on the north-facing lower slopes of the mountains of Emirdaǧ (the Turkish town, previously called Aziziye, has the same name), and the ancient site of Amorium lies within the relatively recent village of Hisarköy. The mountain of Emirdaǧ gives rise to various streams which flow into a tributary of the Sakarya, and at Amorium the view to the north extends over some 50 km., showing, in the middle distance, the tree-lined course of the river, and the mountains of Sivrihisar beyond. The ancient town (which includes a large prehistoric hüyük) was mentioned by Strabo, and indeed the name of Amorium appeared earlier on coins, in the second or first century B.C. The site was rediscovered by W. J. Hamilton in 1836.

scholarly journals Old English Hula ‘Sheds’ and Hull, Yorkshire

2019 ◽  
Vol 24 (1) ◽  
pp. 149
Author(s):  
Andrew Breeze
Keyword(s):  
Old English ◽  
Place Names ◽  
South West ◽  
Rational Explanation ◽  
The Town

Hull or Kingston-upon-Hull is a port upon the River Hull. With a population of over 300,000, it is the fourth biggest city in Yorkshire (after Leeds, Sheffield, and Bradford) and the fifteenth biggest in Britain. Yet its name, like those of other English cities (London, Manchester, Leeds, York, Doncaster), has lacked rational explanation until lately. In 2018 the writer proposed that Hull is not (as long asserted) called after the River Hull, supposedly with an obscure pre-English name. The river is instead called after the town, because Hull derives not from some opaque Celtic hydronym but from Old English hula ‘sheds, huts’. Hull is thus a greater namesake of (Much) Hoole ‘shed(s)’ south-west of Preston, Lancashire.1 As for the River Hull, its old name may have been Leven ‘smooth one’, still that of a village near its source. The original account being a summary one, what follows presents the case in detail.Keywords: Hull; place-names; Old English; Celtic

A new species of velvet gecko (Diplodactylidae: Oedura) from north-east Queensland, Australia

Zootaxa ◽  
2008 ◽  
Vol 1788 (1) ◽  
pp. 21 ◽  
Author(s):  
CONRAD J. HOSKIN ◽  
MEGAN HIGGIE
Keyword(s):  
New Species ◽  
Multivariate Analyses ◽  
Colour Pattern ◽  
Species Boundaries ◽  
North East ◽  
South West ◽  
Reptile Species ◽  
The Town ◽  
A New Species ◽  
Grey Body

We describe a new species of velvet gecko (Diplodactylidae: Oedura) from north-east Queensland, Australia. Oedura jowalbinna sp. nov. is a robust, medium-sized (SVL 60–69 mm) gecko that is readily distinguished from its congeners by its distinctive dorsal colour pattern. The dorsum is grey with faint freckling and a pale, dark-edged band across the neck and another across the base of the tail. The combination of a yellow tail and a grey body is also distinctive. Oedura jowalbinna sp. nov. also differs significantly from the most similar congener, O. coggeri, in a multivariate analysis of morphology and scalation, primarily due to its smaller body size, higher interorbital, supralabial and infralabial scale counts, and lower subdigital lamellae scale count. These traits are generally non-overlapping between O. jowalbinna sp. nov. and O. coggeri, however, more individuals of O. jowalbinna sp. nov. need to be assessed to accurately determine variation within the new species. All O. jowalbinna sp. nov. were found at night on overhangs in dissected sandstone escarpment south-west of the town of Laura. Surveys are required to determine the distribution of O. jowalbinna sp. nov. across the sandstone escarpments of the Laura region. This species is the third reptile species (along with the skinks Ctenotus quinkan and C. nullum) described that has a highly localised range centred on the sandstone escarpments of the Laura region. Additionally, included herein is a comparison of O. coggeri and O. monilis. Typical dorsal colour pattern differs between these two species but the large amount of variation (particularly in O. coggeri) merges these differences. Oedura coggeri and O. monilis could not be distinguished in multivariate analyses of morphology and scalation. Genetic data and further analyses of colour pattern, morphology and scalation are required to resolve species boundaries within and between these two species.

XIV.—The Discovery of Prehistoric Pits at Peterborough and the Development of Neolithic Pottery

Archaeologia ◽  
1910 ◽  
Vol 62 (1) ◽  
pp. 333-352 ◽  
Author(s):  
G. Wyman Abbott ◽  
Reginald A. Smith
Keyword(s):  
Sea Level ◽  
East Side ◽  
The West ◽  
West Side ◽  
North East ◽  
The North ◽  
South West ◽  
Early Settlement ◽  
Human Habitation ◽  
The Town

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.

The Earliest English Place Names in North East Scotland

1999 ◽  
Vol 18 (First Serie (2) ◽  
pp. 67-82 ◽  
Author(s):  
W.F.H. Nicolaisen
Keyword(s):  
Place Names ◽  
North East

Using Census Returns and the Own-Children Method to Measure Marital Fertility in Rawtenstall, 1851-1901

2017 ◽  
pp. 54-73 ◽  
Author(s):  
H.M. (Mac) Boot
Keyword(s):  
19Th Century ◽  
Marital Fertility ◽  
Cotton Textile ◽  
England And Wales ◽  
North East ◽  
Proximate Determinants ◽  
Birth Records ◽  
The 19Th Century ◽  
The Town ◽  
Fertility Estimation

The incompleteness of Victorian census returns of marriage and birth records for England and Wales, and the high costs of using civil and church records, have greatly restricted research into the timing and character of the decline in marital fertility in the second half of the 19th century. This article argues that, in spite of these limitations, the census returns provide enough data to allow the well-known the 'Own-children method of fertility estimation', when used within Bongaarts' framework for analysing the proximate determinants of fertility, to derive estimates of total and age-specific marital fertility for women 15 to 49 years of age. It uses data from the census returns for the town of Rawtenstall, a small cotton textile manufacturing town in north-east Lancashire, to generate these estimates and to test their credibility against other well respected measures of marital fertility for England and Wales.

A Study in the History of Clare, Suffolk; with Special Reference to its Development as a Borough (Alexander Prize Essay, 1928)

1928 ◽  
Vol 11 ◽  
pp. 83-115
Author(s):  
Gladys A. Thornton
Keyword(s):  
Special Reference ◽  
Middle Ages ◽  
Subsequent Development ◽  
Considerable Importance ◽  
Medieval Period ◽  
South West ◽  
Full Development ◽  
History Of ◽  
The Town ◽  
Prize Essay

Clare is situated in the south-west corner of Suffolk, in the valley of the Stour River. At the present day it is only a village, for its market is no longer held; yet its history shows that in earlier times it was of considerable importance, especially during the medieval period, when it was a favourite residence of the Clare lords. The town then had a busy market and a flourishing cloth-making industry; and at one time it seemed possible that Clare might attain full development as a borough, possessing as it did some burghal characteristics. In the following pages it is proposed to study in detail the history of Clare as a seignorial borough during the Middle Ages, and its subsequent development.

The Metamorphosed Limestones and Associated Contaminated Igneous Rocks of the Carlingford District, Co. Louth

1932 ◽  
Vol 69 (5) ◽  
pp. 209-233 ◽  
Author(s):  
G. D. Osborne
Keyword(s):  
Igneous Rocks ◽  
The South ◽  
Ordnance Survey ◽  
Igneous Complex ◽  
North East ◽  
The North ◽  
South West ◽  
Carboniferous Limestone ◽  
Contamination Effects

THE Carlingford-Barnave district falls within the boundaries of Sheet 71 of the Ordnance Survey of Ireland, and forms part of a broad promontory lying between Carlingford Lough on the north-east and Dundalk Bay on the south-west. The greater part of this promontory is made up of an igneous complex of Tertiary age which has invaded the Silurian slates and quartzites and the Carboniferous Limestone Series. This complex has not yet been investigated in detail, but for the purposes of the present paper certain references to it are necessary, and these are made below. The prevalence of hybrid-relations and contamination-effects between the basic and acid igneous rocks of the region is a very marked feature, and because of this it has been difficult at times to decide which types have been responsible for the various stages of the metamorphism.

Inbreeding, Migration and Age at Marriage in Rural Toledo, Spain

1983 ◽  
Vol 15 (1) ◽  
pp. 47-57 ◽  
Author(s):  
R. Calderon
Keyword(s):  
Economic Life ◽  
Neolithic Period ◽  
Ciudad Real ◽  
Age At Marriage ◽  
The North ◽  
Natural Region ◽  
South West ◽  
Different Origins ◽  
The Town ◽  
Common Plant

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.

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