Excavations at Fishbourne, 1963. Third Interim Report

1964 ◽  
Vol 44 (1) ◽  
pp. 1-8
Keyword(s):  
Interim Report ◽  
The West ◽  
Civic Society ◽  
North West ◽  
The Third ◽  
North East ◽  
The North ◽  
The Future ◽  
Set Up

Early in 1963 much of the land occupied by the Roman building at Fishbourne was purchased by Mr. I. D. Margary, M.A., F.S.A., and was given to the Sussex Archaeological Trust. The Fishbourne Committee of the trust was set up to administer the future of the site. The third season's excavation, carried out at the desire of this committee, was again organized by the Chichester Civic Society.1 About fifty volunteers a day were employed from 24th July to 3rd September. Excavation concentrated upon three main areas; the orchard south of the east wing excavated in 1962, the west end of the north wing, and the west wing. In addition, trial trenches were dug at the north-east and north-west extremities of the building and in the area to the north of the north wing. The work of supervision was carried out by Miss F. Pierce, M.A., Mr. B. Morley, Mr. A. B. Norton, B.A., and Mr. J. P. Wild, B.A. Photography was organized by Mr. D. B. Baker and Mrs. F. A. Cunliffe took charge of the pottery and finds.

House I 10,8

2007 ◽  
Author(s):  
Penelope M. Allison
Keyword(s):  
Ground Level ◽  
The West ◽  
Comparable Group ◽  
North West ◽  
North East ◽  
The North ◽  
South Wall ◽  
Domestic Use ◽  
Small Shell ◽  
Lead Weights

The surviving plaster on the walls of this entranceway consisted of a high pink socle, delineated in red, with a white zone above. Ling observed that this overlay an earlier First-Style decoration on the east wall and that it had been patched in antiquity. Breaches are found in both the east and west walls. Outside the entrance, to either side, is a masonry bench (east bench: l.: 2.1 m, d.: 380 mm; west bench: l.: 2.4 m, d.: 460 mm), both much damaged. Finds within the entranceway consisted of bronze and iron studs, undoubtedly from the house door. Remains of plastered decoration survive on the south wall. Elia recorded a yellow dado, surmounted by a red band, with white plaster above. There is a breach in the north-west corner through to Unit no. 9, above a blocked doorway. At the centre of this front hall is a tufa impluvium (2.4 m × 2.1 m). In the north-west corner, 1 m above the pavement, were found: a small bronze ring; a bronze stud, similar to those in the entranceway and probably also from the front door; a fragment of a stone mortar or hand-mill; some glass beads; a small shell; and two bronze quadrantes, one of Nero dated ad 64. The fragmentary or loseable nature of these items suggests that they were disturbed from the ground level. Other small loseable items were found in the north-east corner: a small glass bottle, probably a toilet item; and possibly five more coins. One metre from the west side of the impluvium were found: another part of a hand-mill; two large stone weights; at least fifty-three lead weights, probably from a loom; and two other spherical stones, possibly also weights. The large number of lead weights is comparable with the quantity found under the stairway in room i of the Casa del Principe di Napoli. Another comparable group of forty loom weights was found together in a pit at Zugmantel. As Jongman noted, this amount would be equivalent to that required for one or perhaps two warp-weighted looms. It is therefore commensurate with the existence of such a loom, or looms, in this area, or of replacement loom weights, for domestic use.

The armies of the Ṣaffārids

1968 ◽  
Vol 31 (3) ◽  
pp. 534-554 ◽  
Author(s):  
C. E. Bosworth
Keyword(s):  
Ninth Century ◽  
The South ◽  
The West ◽  
Islamic World ◽  
North West ◽  
The Third ◽  
The Core ◽  
The North ◽  
Frontier Region ◽  
Short Time

It is not too much to describe the Ṣaffārids of S‚stān as an archetypal military dynasty. In the later years of the third/ninth century, their empire covered the greater part of the non-Arab eastern Islamic world. In the west, Ya'qūb. al-Laith's army was only halted at Dair al-'Āqūl, 50 miles from Baghdad; in the north, Ya'qūb and his brother 'Arm campaigned in the Caspian coastlands against the local 'Alids, and 'Amr made serious attempts to extend his power into Khwārazm and Transoxania; in the east, the two brothers pushed forward the frontiers of the Dār al-Islām into the pagan borderlands of what are now eastern Afghanistan and the North-West Frontier region of West Pakistan; and in the south, Ṣaffārid authority was acknowledged even across the persion Gulf in ‘Umān. This impressive achievement was the work of two soldiers of genius, Ya'qūub and 'Amr, and lasted for little more than a quarter of a century. It began to crumble when in 287/900 the Sāmānid Amīr Ismā'īl b. Aḥmad defeated arid captured ‘Amr b. al-Laith, and 11 years later, the core of the empire, Sīstān itself, was in Sāmānid hands. Yet such was the effect in Sīstān of the Ṣaffārid brothers’ achievement, and the stimulus to local pride and feeling which resulted from it, that the Ṣaffārids returned to power there in a very short time. For several more centuries they endured and survived successive waves of invaders of Sīstān—the Ghaznavids, the Seljūqs, the Mongols—and persisted down to the establishment of the Ṣafavid state in Persia.

scholarly journals CHECKLIST AND DISTRIBUTION OF MARINE AND FRESHWATER LEECHES (ANNELIDA, CLITELLATA, HIRUDINEA) IN TUNISIA WITH IDENTIFICATION KEY

2015 ◽  
Vol 2 (1) ◽  
pp. 3-19 ◽  
Author(s):  
Raja Ben Ahmed ◽  
Yasmina Romdhane ◽  
Saïda Tekaya
Keyword(s):  
Identification Key ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
West Region ◽  
The World ◽  
The Future

In this study 13 leech species from Tunisia are listed. They belong to 2 orders, 2 suborders, 4 families and 11 genera. The paper includes also data about hosts and habitats, distribution in the world and in Tunisia. Faunistic informations on leeches were found in literature and in the results of recent surveys conducted by the authors in the North East and the South of the country. The objectives of this study were to summarize historical and recent taxonomic data, and to propose an identification key for species signalized. This checklist is to be completed, taking into account the hydrobiological network of the country especially the North West region, which may reveal more species in the future

The Ancient Road Systems of the Central and Northern Ager Faliscus. (Notes on Southern Etruria, 2)

1957 ◽  
Vol 25 ◽  
pp. 67-203 ◽  
Author(s):  
M. W. Frederiksen ◽  
J. B. Ward Perkins
Keyword(s):  
Northern Limit ◽  
The West ◽  
North West ◽  
The Road ◽  
North East ◽  
The North ◽  
Arterial Road ◽  
Road Systems ◽  
The Right ◽  
North Western

The modern Via Cassia, now as in antiquity the great arterial road up through the heart of south-eastern Etruria, after crossing the Fosso dell'Olgiata less than a kilometre to the west of the north-western gate of Veii, climbs steadily for about 7 km. to cross the Monti Sabatini, the line of extinct volcanic craters that runs eastwards from Lake Bracciano, forming a natural northern boundary to the Roman Campagna. After cutting through the southern crest of the crater of Baccano, with its magnificent views southwards and eastwards over Rome towards Tivoli, Palestrina and the Alban Hills, the road drops into the crater, skirts round the east side of the former lake, and climbs again to the far rim, before dropping once more into the head of the Treia basin, on its way to Monterosi and Sutri.From this vantage-point a whole new landscape is spread out before one (pl. XLVII). To the west and north-west, the tangle of volcanic hills that forms the northern limit of the Monti Sabatini, rising at its highest point to the conical peak of Monte Rocca Romana (612 m.); beyond and to the right of those, past Monterosi and filling the whole of the north-western horizon, some 10–15 km. distant, the spreading bulk of Monte Cimino (1053 m.), with its characteristically volcanic, twin-peaked profile; to the north and north-east, the gently rolling woods and fields of the Faliscan plain, deceptively smooth, stretching away to the distant Tiber.

Excavations at Verulamium, 1961. Seventh and Final Interim Report

1962 ◽  
Vol 42 (2) ◽  
pp. 148-159 ◽  
Author(s):  
S. S. Frere
Keyword(s):  
Small Scale ◽  
Natural Soil ◽  
Masonry Building ◽  
Interim Report ◽  
The West ◽  
North East ◽  
The North

Two small-scale excavations were carried out at Verulamium during 1961. In January it became necessary to explore the site about to be occupied by the museum extension, and several trenches were cut on the north-east and south-east sides of the existing museum building. It was not possible in the time and with the resources available to excavate down to natural soil, but only to examine those layers due for removal by the builders. Considerable depths of deposit are known to exist here, possibly filling an early ditch. The site lies in the west corner of Insula XVIII: the earliest structure reached was a timber-framed building, burnt down possibly c. A.D. 155. This was succeeded by an Antonine masonry building with channel hypocausts. Possibly c. A.D. 300 this building was enlarged by encroachment on the street frontages. It clearly extends some way outside the area excavated both towards east and south. The character of the structure is domestic.

The Place of the North-Eastern Transvaal Sotho in the South Bantu Complex

Africa ◽  
1938 ◽  
Vol 11 (3) ◽  
pp. 265-293 ◽  
Author(s):  
Eileen Jensen Krige
Keyword(s):  
Total Population ◽  
The West ◽  
North West ◽  
Effective Barrier ◽  
North East ◽  
The North ◽  
North Eastern ◽  
Game Reserve ◽  
Olifants River ◽  
Opening Paragraph

Opening ParagraphThe Sotho of the North-Eastern Transvaal Lowveld occupy an area with fairly well-marked geographical boundaries. To the east, the Game Reserve, low-lying, unhealthy, very sparsely populated even in the old days, remains an effective barrier to contact with and further migrations from the Shangana-Tonga of Portuguese East Africa. South are the Olifants River and the towering Drakensberg range curving north-west then northwards to merge into the well-marked escarpment on the west dividing Lowveld from Highveld. On the north the Klein Letaba river roughly demarcates our area from the Venda and the Shangana-Tonga of the Knobnose Location. The Sotho-speaking Venda of Tswale and Moila, who fall well within this area, resemble in culture their Sotho-ized neighbours more than their own Venda kin to the north; but the Shangana- Tonga, who occupy most of the lower-lying eastern and north-eastern portion of the area and comprise at least one-third of its total population, are unassimilated strangers of different stock coming from the north-east and east. They have been entering since about 1840, usually in small bands, at first seeking the protection of and subjecting themselves to the Sotho owners of the land. On the arrival of the white man, some of their headmen were granted independent locations which have served as nuclei for the building up of more united tribal groups. (See accompanying map.)

Rainsborough, Northants, England: Excavations 1961–5

1968 ◽  
Vol 33 ◽  
pp. 207-306 ◽  
Author(s):  
Michael Avery ◽  
J. E. G. Sutton ◽  
J. W. Banks ◽  
M. S. Tite ◽  
J. G. Evans ◽  
...  
Keyword(s):  
Tree Roots ◽  
The West ◽  
Outer Slope ◽  
North West ◽  
Gentle Slope ◽  
The Core ◽  
North East ◽  
The North ◽  
South West ◽  
Visible Part

Rainsborough is 1 mile South of Charlton village, in the parish of Newbottle, S. Northants, 20 miles North of Oxford, (SP 526348). The camp lies atc. 480′ OD, and the area enclosed isc. 6·25 acres.It lies on the edge of a plateau: the approaches to it are flat on the north-east, east, south and south-west, but a gentle slope to the north, north-west and west gives it a wide view across the Cherwell valley, towards Madmarston and Tadmarton (see map, fig. 1 and also pl. XXV). The defences are bivallate: the inner bank stands to 10 feet above the interior, and there is a drop of about 15 feet from the crest into the inner ditch; the second bank is very much lowered by ploughing, but still reaches a height of about 4 feet on the south side, where a hedge line has protected it; the outer ditch is nowhere visible on the surface, except on the west, when it carries a higher growth of weeds. The defences are covered with turf: the inner bank has also trees, bushes and the stumps of large beeches felledc. 1950. The bank is riddled with tree roots, and the sandy character of the core has attracted rabbits: recent attempts to dig and smoke out the warrens have slightly damaged the profile of the bank. A small dry stone wall is visible part way up the outer slope of the inner bank in several places.

The Petrology of the Hecla Hook Formation in Central Spitsbergen

1933 ◽  
Vol 70 (10) ◽  
pp. 437-454 ◽  
Author(s):  
P. E. Fairbairn
Keyword(s):  
The South ◽  
The West ◽  
North West ◽  
Eastern Margin ◽  
North East ◽  
The North ◽  
Glacier System ◽  
Return Journey ◽  
Bad Weather ◽  
Rock Specimens

The rock specimens described in this paper were collected by N. W. Pirie on the Cambridge Spitsbergen Expedition of 1930,1 and by the writer on the second and larger expedition of 1932. They represent an area forming the “neck” of Central Spitsbergen between Klaas Billen Bay to the south and Wijde Bay to the north, together with an area to the east and north-east of the Mittag-Leffler Glacier, extending northwards to the upper portion of the Lomme Bay Glacier, thus including the Stubendorff Mountains to the east of Wijde Bay and the western flanks of the Chydenius Range. The 1930 expedition started from the mouth of Ebba Valley in Petunia Bay and reached Wijde Bay by way of the Ebba and Mittag-Leffler Glaciers; after reconnoitring part of the Stubendorff Glacier they returned over the Mittag-Leffler and Ragnar Glaciers, passing to the north-west of Mount Hult. Most of the ground was again covered by the 1932 expedition, but in addition a sledge party reached the highland ice of Garwood Land at the head of the Ebba Glacier, turned north along the eastern margin of the Mittag-Leffler Glacier system and passing to the west of the Newton-Chernishev massif succeeded in carrying out topographical and geological observations on the Lomme Bay Glacier, though these were much curtailed by bad weather. On the return journey the party made their way down the “Vallee de Martin Conway”, crossed the divide between the Mittag-Leffler and Ebba Glaciers, and reached Petunia Bay by the same route that they had followed on the way up.

Post-memory and the third generation’s inheritance of the Indian partition (1947): A comparative study of the linguistic register across spatial axes

2021 ◽  
pp. 175069802110333
Author(s):  
Avishek Ray
Keyword(s):  
Comparative Study ◽  
West Bengal ◽  
Western India ◽  
Growing Up ◽  
The West ◽  
North East India ◽  
The Third ◽  
North East ◽  
The North ◽  
The Difference

The experience of the Partition (1947)—the contexts of migration and the experience of refugeehood—in East-India is assumed to be different from that in the West. But, even after some 70 years after the Partition, there has been no substantial study on the difference in the ontology of refugeehood across the two sites. More to it, narratives from the North-east (Meghalaya, Assam, Tripura), which again differ significantly from their western Indian or West Bengali counterparts, are under-represented in the existing database of oral narratives and ethnographies on the Partition. Departing from here, this paper engages in a critical comparative study—across three spatial axes: western India, West Bengal, and North-east India—of the third generation’s experience of “growing up refugee” in India. It offers a nuanced, but empirically-grounded, insight on how memories and narratives of the Partition are grounded in the linguistic registers of those who “grew up refugee” (not the refugees per se). Based on interviews, this paper analyzes the patterns, circulations, transactions, tropes, and motifs in the linguistic registers using methodologies of Digital Humanities, and how they compare across spatial axes.

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