I.—On some Buildings of the Romano-British Period discovered at Clanville, near Andover, and on a deposit of Pewter Vessels of the same period found at Appleshaw, Hants. With Appendixes

Archaeologia ◽  
1898 ◽  
Vol 56 (1) ◽  
pp. 1-20 ◽  
Author(s):  
G. H. Engleheart ◽  
Charles H. Read ◽  
William Gowland
Keyword(s):  
The Other ◽  
North West ◽  
Left Hand ◽  
The North ◽  
Western Border ◽  
The One ◽  
Point Of Intersection ◽  
The Village ◽  
The Town ◽  
North Western

In the immediate neighbourhood of my house in the village of Appleshaw, on the north-western border of Hampshire, the sites are unusually close together of those dwellings of the Romano-British period which are, with a certain vagueness, termed Roman villas. Appleshaw is distant five miles north-west from Andover; one mile north of Andover two Roman roads intersect, the one running from Old Sarum north-easterly to Silchester, the other from Winchester north-westerly to Cirencester. At Finkley, close to the point of intersection, pottery and other Roman material has from time to time been unearthed, and the locality is one of those which have, by a somewhat unconvincing reference to the Antonine itinerary and to etymology, been identified with the unascertained site of Vindomis. Imagine these two roads at their crossing to stand like an upright capital X over the town of Andover, with that town in the lowest angle; my own nearer neighbourhood will lie in the western or left-hand angle. Three-quarters of a mile east of my house is the lately-examined site upon which I have to report particularly this evening. One mile north and a little west (all the distances mentioned are measured in radius from my house) is a villa on the Redenham estate, excavated some fifty years back by Sir John Pollen, the landowner. It appears that no plans were made and no record kept.

III.—Some new Rock-building Organisms from the Lower Carboniferous Beds of Westmorland

1914 ◽  
Vol 1 (6) ◽  
pp. 265-271 ◽  
Author(s):  
E. J. Garwood
Keyword(s):  
Presidential Address ◽  
The Other ◽  
Lower Carboniferous ◽  
North West ◽  
Western Province ◽  
The North ◽  
Calcareous Alga ◽  
The Village ◽  
Important Form ◽  
North Western

In my account of the Lower Carboniferous rocks of the North-West of England, published in 1912, I figured an organism, probably the thallus of a calcareous alga, which plays an important part as a rock-builder at the base of the Seminula gregaria sub-zone in Westmorland and Lancashire. More recently, at the meeting of the British Association in Birmingham, I pointed out the need of some distinctive name for this important form, and suggested for it the generic name of ‘Ortonella’, from the village of Orton, near Tebay, in the neighbourhood of which this fossil is specially abundant. Two other structures were mentioned at the same time which occur constantly in microscopic sections of the Lower Carboniferous rocks of the North-West of England and elsewhere. The first of these was alluded to under the general descriptive term ‘festoon structure’, and the other was referred to Gurich's somewhat obscure genus Spongiottroma. In view of the zonal value of these organisms in the North-Western Province and the probability that they will be found to be widely distributed in the Lower Carboniferous rocks elsewhere, I propose here to give a somewhat fuller description of these forms than could be attempted in the limits of a presidential address.

Ugliness and Beauty: the Politics of Landscape in Walter Greenwood's Love on the Dole

2013 ◽  
Vol 29 (1) ◽  
pp. 35-47
Author(s):  
Claire Warden
Keyword(s):  
Twentieth Century ◽  
Working Class ◽  
The Other ◽  
Surrounding Area ◽  
North West ◽  
Avant Garde ◽  
The North ◽  
The One ◽  
The University ◽  
Open Fields

The multi-spatial landscape of the North-West of England (Manchester–Salford and the surrounding area) provides the setting for Walter Greenwood's 1934 play Love on the Dole. Both the urban industrialized cityscape and the rural countryside that surrounds it are vital framing devices for the narrative – these spaces not simply acting as backdrops but taking on character roles. In this article Claire Warden reads the play's presentation of the North through the concept of landscape theatre, on the one hand, and Raymond Williams's city–country dialogism on the other, claiming that Love on the Dole is imbued with the revolutionary possibility that defines the very landscape in which it is set. From claustrophobic working-class kitchen to the open fields of Derbyshire, Love on the Dole has a sense of spatial ambition in which Greenwood regards all landscapes as tainted by the industrial world while maintaining their capacity to function independently. Ugliness and beauty, capitalist hegemony and socialistic hopefulness reside simultaneously in this important under-researched example of twentieth-century British theatre, thereby reflecting the ambivalent, shifting landscape of the North and producing a play that cannot be easily defined artistically or politically. Claire Warden is a Lecturer in Drama at the University of Lincoln. Her work focuses on peripheral British performances in the early to mid-twentieth century. She is the author of British Avant-Garde Theatre (Palgrave MacMillan, 2012) and is currently writing Modernist and Avant-Garde Performance: an Introduction for Edinburgh University Press, to be published in 2014.

scholarly journals Балцкія элементы ў граматыцы традыцыйных мясцовых гаворак паўночна‑заходняй Беларусі

2015 ◽  
Vol 36 ◽  
pp. 51-59
Author(s):  
Вера [Vera] Астрэйка [Astrėĭka]
Keyword(s):  
The Other ◽  
North West ◽  
Language Support ◽  
The North ◽  
The Status ◽  
Formal Level ◽  
The Baltic ◽  
Language Assimilation ◽  
The Given ◽  
North Western

The Baltic elements in the grammar of traditional local dialects of north-western BelarusThe article analyzes a number of grammatical features typical for the North-West dialect zone of the Belarusian language. These peculiarities are interpreted as a possible result of Slavic-Baltic contacts in the region. Some phenomena can be explained as a Baltic (mainly (great)Lithuanian) substratum in North-West Belarusian dialects.The factor of areal neighborhood has to be taken into consideration too. Such phenomenon as language support has effect just in connection with the last one. A lot of the appropriate lingual facts are in restricted and inconsistent use. However, it is possible to be said about more or less significant (now or/and before) tendencies of regional lingual development. These tendencies has not got the status of a structural (= constitutional) lingual regularity. As a rule the wide and compact areas are characterized of some lingual facts (= lexemes), which illustrate the given transformations in the system of Belarusian dialects. Baltic influence upon the North-West Belarusian dialects grammar is detected on as the formal level so the structural one. And it is not noticeable at all times. The definite changes in the sphere of morphology and syntax can provoke different modifications in the other parts of a language system (word building, semantics). The results of this process are the evidences of ethnic and language assimilation of native Balts by Slavs in the region. That comes in support of forming the singular North-West Belarusian regiolect (= the regionally marked variety of a dialect language). Балтийские грамматические элементы в говорах северо-западной БеларусиВ статье анализируется ряд грамматических черт, характерных для говоров северо-западной диалектной зоны беларусского языка. Эти особенности квалифицируются автором как весьма вероятное следствие славяно-балтского языкового взаимодействия в соответствующем регионе. Отдельные явления есть основания рассматривать в качестве возможного проявления балтского (главным образом (пра-) литовского) субстрата в северо-западных беларусских говорах. Фактор ареальной смежности здесь также должен быть принят во внимание. В связи с последним следует упомянуть и действие феномена языковой поддержки. Многие соответствующие языковые факты имеют существенные ограничения в употреблении, в говорах выступают не всегда последовательно и регулярно. В некоторых случаях, однако, можно говорить о действии более или менее выраженных (в настоящем и/или прошлом) тенденций регионального языкового развития, которые пока не приобрели статус структурно значимой (= конститутивной) языковой закономерности. Широкие и компактные ареалы образуют, как правило, лишь отдельные языковые факты (= лексемы), иллюстрирующие данные трансформации в системе традиционных беларусских говоров. Балтское влияние на грамматический строй беларусских говоров северо-западной диалектной зоны выявляется как в плане формального выражения, так и на внутриструктурном уровне. Оно не всегда может быть заметно на первый взгляд. Определенные сдвиги в сфере морфологии и синтаксиса могут повлечь за собой изменения в других областях языковой системы (словообразовании, семантике). Результаты этого процесса являются ярким свидетельством того, что на отмеченной территории действительно имела место этноязыковая ассимиляция неславянского (= балтского) населения и происхо- дило формирование своеобразного северо-западного беларусского региолекта (= регионально обусловленной разновидности диалектной речи).

Deep Sinking for Coal in the Wyre Forest Coal-Field

The Geologist ◽  
1861 ◽  
Vol 4 (11) ◽  
pp. 468-469
Author(s):  
George E. Roberts
Keyword(s):  
Coal Seam ◽  
Coal Mining ◽  
The Other ◽  
Coal Field ◽  
Coal Seams ◽  
North West ◽  
The North ◽  
Western Border ◽  
Shaft Sinking ◽  
Considerable Range

Some other memoranda which I find among my papers relating to this work (for a section of which, with particulars of shaft-sinking, see “Geologist” of last month) may not be unacceptable to your coal-mining readers.The spot where the shaft was sunk was 476 feet above the level of the Severn Valley Railway at Eymoor, and about 510 feet above the ordinary height of the River Severn, from which it was distant about two miles. The coal seam met with and worked at the depth of 176 yards, has in other parts of the coal-field a thickness of four feet. The colliers regard it as a Flying Reed (red?) coal. Two of the thin coal-seams afterwards sunk through were entirely made up of the remains of Sigillariæ; the coal, in consequence, was “long grained” and slaty. These Sigillarian coals have a considerable range through the Wyre Forest field, and in common with most of the other seams, crop out along the western border. At the Baginswood pits, in the north-west corner of the coal·field, the upper coal, two feet four inches in thickness, worked by hand-draw, being only ten yards from surface, is a most interesting seam, made up entirely of compressed Sigillariæ.

The Underground Structure of Eastern England

1927 ◽  
Vol 64 (1) ◽  
pp. 10-26 ◽  
Author(s):  
R. H. Rastall
Keyword(s):  
Underground Structure ◽  
The Other ◽  
General Shape ◽  
North West ◽  
North East ◽  
The North ◽  
General Line ◽  
Geological Features ◽  
The One ◽  
Southern Flank

The foregoing sketch brings out marked resemblances in the geological features of eastern and southern England on the one hand, and the neighbouring parts of the continent on the other. In both areas we find an old plateau of pre-Devonian rocks, against which Devonian and Carboniferous rocks are violently thrust from the south by Armorican and Variscan folds, giving rise to highly complex coal-basins in Belgium, France and Somerset, a type of structure possibly to be encountered in the future in Kent. In Belgium this plateau sinks to the north-east under the Campine coalfield, while in England its north-west margin is complicated by the incidence of posthumous folds of Charnian strike.In eastern England, east of the Charnwood line, there is evidence for the existence of Professor Kendall's Willoughby axis, with north-west strike; between this and the Charnwood line there are indications of similar parallel buried trend-lines in the folding and faulting of the visible Yorks-Derby-Notts coalfield, and also, as suggested by Professor Fearnsides, in the general shape of this basin.Further to the north, however, the general line of the Cleveland and Market Weighton axes is not Charnian, being about west 5° north. The Market Weighton axis, which is of Charnian type, with many repeated movements, does not form the boundary of the coalfield; this is in fact constituted by the southern flank of the broad Cleveland uplift, which is of Wealden type; an anticline superposed on an earlier sinking area.

scholarly journals Art. XIV.—The Migrations and Early History of the White Huns; principally from Chinese Sources

1878 ◽  
Vol 10 (2) ◽  
pp. 285-304 ◽  
Author(s):  
Thos. W. Kingsmill
Keyword(s):  
Early History ◽  
The Other ◽  
North West ◽  
The North ◽  
History Of ◽  
Physical Geology ◽  
The One

One of the most interesting migrations on record is that of the Yuehti from their old seats in the north-west of China to the site of the Greek kingdom of Bactria. Its interest is increased rather than diminished by the fact that we can trace its origin by the aid of authentic records, as well as from the knowledge that it was but one in a series, the original exciting cause of which still remains veiled in an obscurity apparently only to be pierced, on the one hand, by the geologist who shall work out the changes in the physical geology of Asia, within the human period, or, on the other, by the comparative mythologist, who, placing side by side the myths and traditions of its ancient inhabitants, sees, though dimly, some sort of order rising out of what, at first sight, is a veritable chaos.

scholarly journals Kos Astypalaia

1898 ◽  
Vol 4 ◽  
pp. 95-100
Author(s):  
Duncan Mackenzie
Keyword(s):  
The Other ◽  
Mountain Region ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
South West ◽  
The Village

From the modern town of Kos, on the site of the ancient capital at the north-east extremity of the island, to the village of Kephalos at the southwest end is a ride of eight hours.The village stands on a chalky plateau which beyond the isthmus marks the beginning of the mountain district of south-west Kos. This in turn is a repetition on a smaller scale of the mountain region, at the other end of the island, which forms the lofty termination to the long central tableland. The highest points of the mountain district are towards the south-east where the fall to the sea is very rapid. The highest neighbouring peak, Mount Ziní, is about an hour distant from the village in a south-easterly direction, while all that lies to the north-west of the main range is high pastoral country with many torrent beds.

From Red Ruthenia to Rawa Mazowiecka: the Works of the Anonymous “Master of Pełczyska” as a Contribution to the Geography of Rococo Sculpture in Mazovia

Ikonotheka ◽  
2018 ◽  
Vol 27 ◽  
pp. 211-240
Author(s):  
Michał Wardzyński
Keyword(s):  
18Th Century ◽  
Virgin Mary ◽  
Fourth Quarter ◽  
The Other ◽  
North West ◽  
External Influences ◽  
The North ◽  
Other Hand ◽  
The One ◽  
Current Stage

Current research on Rococo sculpture in Mazovia and northern Lesser Poland has not taken into consideration Lvov Rococo sculpture. A total of thirteen works by a yet unidentified woodcarving workshop, probably of Lvov provenance, was located at the intersection of these two artistic regions, in the vicinity of Końskie, Opoczno, Przysucha and Rawa Mazowiecka. Its activity, commenced after 1780 in Pełczyska near Wiślica, lasted until ca. 1800, when the reredoses and lesser works of sculpture in Studzianna-Poświętne, Skrzyńsko, Nowy Kazanów, Końskie, Gowarczów, Drzewica, Rawa and Regnów were created. In formal terms, the anonymous “Master of Pełczyska”, as an epigone of the Lvov school of Rococo sculpture, shows a far-reaching dependency on the style of sculptures similar to that in the side altar of the Virgin Mary of Dzików in Tarnogród, in the Zamoyski family fee tail. This reredos was indirectly attributed to master Franciszek Olędzki from Lvov (active since 1771, d. 1792). The oeuvre of the “Master of Pełczyska” constitutes the second-largest assembly of Lvov Rococo sculptures outside the historical Ruthenian lands of the Crown of Poland. At the current stage of research, the discussed works, located at the intersection of the former Sandomierz and Rawa voivodeships, indicate the maximal influential range of these remarkably mobile artists towards the north-west of the Crown of Poland. Their migrations were directly connected, on the one hand, with the artistic crisis that followed the First Partition of the Commonwealth in 1772 and the annexation of Lvov by Austria, and, on the other hand, with the liquidation of monasteries after 1780 and the termination of existing ecclesiastic commissions. The short-lived activity of this workshop in the vicinity of Rawa is an important contribution to the research on the mosaic of external influences on provincial late Rococo sculpture in the fourth quarter of the 18th century in Mazovia.

Gāndhārī

1946 ◽  
Vol 11 (4) ◽  
pp. 764-797 ◽  
Author(s):  
H. W. Bailey
Keyword(s):  
Literary Text ◽  
Official Language ◽  
North West ◽  
The North ◽  
Chinese Texts ◽  
The One ◽  
North Western

The word Gāndhārī has been chosen to head this study as a term sufficiently wide in its scope to embrace the forms of the one Middle Indian dialect of the north-west of India, centred in the old Gāndhāra region, around modern Peshawar, and which we meet in most varied sources. Under this name I propose to include those inscriptions of Aśoka which are recorded at Shahbazgaṛhi and Mansehra in the Kharoṣṭhī script, the vehicle for the remains of much of this dialect: To be included also are the following sources: the Buddhist literary text, the Dharmapada found in Khotan, written likewise in Kharoṣṭhī, of which a new reading of the text available in facsimile is given in BSOAS 11. 488–512; the Kharoṣṭhī documents on wood, leather, and silk from Caḍ'ota (the Niya site) on the border of the ancient kingdom of Khotan, which represented the official language of the capital Krorayina, K 572, 512 lou-lan <ləu-lan (lou in a series with alternation of k and l) of the Shan-shan kingdom, and of one document, no. 661, dated in the reign of the Khotana maharaya rayatiraya hinajha dheva ṿijida-siṃha. With this more copious material must be grouped the scattered traces of the same Middle Indian dialect in Khotanese, Tibetan, Agnean, Kuchean, the earlier Chinese Buddhist transliterations, as, in particular, in the Dīrghāgama of the Dharmaguptaka ṡect and the remains in Sogdian, Uigur Turkish, and in Mongol (in living use), and also in Manchu texts. The modern Dardic languages Ṣiṇā, Khowar, Phalūᵛa and others represent the same type of Middle Indian. Much material in Chinese texts, for most of us hidden and inaccessible, remains to be gathered and sifted. The preliminary studies of P. Pelliot in Les noms propres dans les traductions chinoises du Milindapañha (JA 1914. 2. 379–419), of Fr. Weller in his paper Über den Aufbau des Pāṭikasuttanta (Asia Major 5. 1928), and of E. Waldschmidt in his Bruchstücke buddhistischer Sūtras aus dem zentralasiatischen Sanskritkanon I, 1932, have hardly realized the importance of this North-Western Prakrit.

Chastleton Camp, Oxfordshire, a hill-fort of the Early Iron Age

1931 ◽  
Vol 11 (4) ◽  
pp. 382-398 ◽  
Author(s):  
E. Thurlow Leeds
Keyword(s):  
Iron Age ◽  
Short Distance ◽  
The Other ◽  
Early Iron Age ◽  
Original Condition ◽  
North West ◽  
The Road ◽  
The North ◽  
East End ◽  
The One

Chastleton Camp, or Chastleton Barrow (pl. LIV, 1 and 2), as it is sometimes called, is situated at the south-east end of the parish, which projects like some huge spur from the north-west edge of the county and from the line of the road which on either side of the base of the spur for a short distance divides Oxfordshire from Gloucestershire on the one hand and from Warwickshire on the other. This road is an age-long trackway running diagonally across England by way of the Jurassic Belt from the Cotswolds to Northamptonshire, and is fringed by many remains of prehistoric man, in addition to the Rollright Stones and the dolmen known as the Whispering Knights. Along it must have moved the invaders of the early Iron Age to their conquest of the Midlands, establishing a line of strongholds of which Chastleton must in its original condition have been a formidable example.

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