scholarly journals The Results of a Chemical, Microscopical and Bacteriological Examination of Samples of London Milks

1907 ◽  
Vol 7 (1) ◽  
pp. 22-31 ◽  
Author(s):  
R. Tanner Hewlett ◽  
George S. Barton
Keyword(s):  
Bacteriological Examination ◽  
Milk Supply ◽  
The South ◽  
The West ◽  
The North ◽  
South West ◽  
Pure Milk

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.

Prehistoric Roads and Tracks in Somerset, England: 2. Neolithic

1970 ◽  
Vol 36 ◽  
pp. 125-151 ◽  
Author(s):  
John M. Coles ◽  
F. Alan Hibbert ◽  
Colin F. Clements
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
The Third ◽  
The North ◽  
South West ◽  
Extensive Region ◽  
Peat Deposits ◽  
Third Millennium ◽  
South West England

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).

The West Court at Perachora

1967 ◽  
Vol 62 ◽  
pp. 353-371
Author(s):  
J. J. Coulton
Keyword(s):  
Short Distance ◽  
Sixth Century ◽  
East Side ◽  
The South ◽  
The West ◽  
Rock Face ◽  
North East ◽  
The North ◽  
South West ◽  
East And West

About 10 metres south-west of the sixth-century temple of Hera Akraia at Perachora, and nearly due west of the little harbour lies the small courtyard previously known as the ‘Agora’. Since its purpose is not known, it will here be non-committally referred to as the West Court. It was first excavated in 1932, and more fully, under the supervision of J. K. Brock, in 1933, but it was not entirely cleared until 1939, and it was at that time that the Roman house which stood in the middle of the court was demolished. The West Court is discussed briefly (under the name of ‘Agora’) in Perachora 1 and in the preliminary reports of the Perachora excavations. Short supplementary excavations were carried out in 1964 and 1966 to examine certain points of the structure.In shape the West Court is an irregular pentagon, about 24 metres from north to south and the same from east to west (Fig. 1; Plate 91 a, b). It is enclosed on the west, north, and on part, at least, of the east side by a wall of orthostates on an ashlar foundation. For a short distance on either side of the south corner, the court is bounded by a vertically dressed rock face which is extended to the north-east and west by walls of polygonal masonry. At the south-west corner the west orthostate wall butts against the polygonal wall, which continues for about 0·80 m. beyond it and then returns north for about 8 metres behind it.

Moča, a Tone Language of the Kafa Group in South-Western Ethiopia

Africa ◽  
1958 ◽  
Vol 28 (2) ◽  
pp. 135-147
Author(s):  
Wolf Leslau
Keyword(s):  
The South ◽  
The West ◽  
Tone Language ◽  
The North ◽  
South West ◽  
Opening Paragraph ◽  
Western Ethiopia

Opening ParagraphMoča is a dialect of the Kafa cluster, in the south-west of Ethiopia. It is spoken in the province of Ilubabor, to the west of Kafa, extending north across the river Baro. The language is called Šäkka by the Moča themselves; the term Moča is used by the Galla and by the Europeans.The dialects of the Kafa cluster are: Kafa spoken in the province of Kafa, between the rivers Omo and Goǧeb to the north and the Gimira tribes to the south; Boša (or Garo) spoken to the north of the river Goǧeb, and west of Omo; and Moča.

Evans's Greek finds: the early Greek town of Knossos, and its encroachment on the borders of the Minoan palace

2000 ◽  
Vol 95 ◽  
pp. 259-299 ◽  
Author(s):  
J. N. Coldstream
Keyword(s):  
Iron Age ◽  
Systematic Study ◽  
Early Iron Age ◽  
The South ◽  
The West ◽  
The North ◽  
South West ◽  
Greek Pottery

Among over 1800 boxes of Sir Arthur Evans's finds now stored in the Stratigraphical Museum at Knossos, at least 150 contain Greek pottery from Subminoan to Classical. A systematic study of this material, in relation to its recorded find spots, throws new light on the eastern part of the early Greek town, bordering the site of the Minoan Palace. Above the Palace itself, fresh evidence is produced, and fresh interpretation offered, for the Greek sanctuary described by Evans. In its immediate surroundings, there are signs of busy domestic and industrial life in the early Greek town above the South-West Houses, the West Court, the Theatral Area, and the Pillared Hall outside the North Entrance to the Palace. Greek occupation is also noted above the House of Frescoes, the Little Palace and the Royal Villa. A wider aim of this article is to trace the limits of the early Greek town of Knossos, both of its original Early Iron Age nucleus surviving from Late Minoan times, and of its spacious extension towards the north in the late eighth and seventh centuries BC.

scholarly journals An ultrabasic pipe in the eastern Sukkertoppen region, southern West Greenland

1980 ◽  
Vol 100 ◽  
pp. 69-73
Author(s):  
R.P Hall
Keyword(s):  
Granulite Facies ◽  
The South ◽  
The West ◽  
West Side ◽  
West Greenland ◽  
North East ◽  
The North ◽  
South West ◽  
Unusual Occurrence ◽  
Anorthosite Complex

An unusual occurrence of ultrabasic material was located in the eastern Sukkertoppen region during the reconnaissance mapping programme of 1977, the findings of which were described by Allaart et al. (1978). It occurs on a small exposure on the west side of a north-pointing peninsula in the middle of the large nunatak Majorqap alangua (65°53'N, 50°40'W), to the north-east of the Majorqaq valley (Hall, 1978, fig. 21). The area is composed predominantly of a suite of granulite facies granitic gneisses which contain numerous enclaves of pyroxene-bearing amphibolites, and locally anorthositic and gabbroic rocks similar to those seen in the Fiskenæsset anorthosite complex (Myers, 1975). The gneisses in the centre af the nunatak are highly irregular in orient at ion, occupying the complex interseclion af closures af at least two major fold phases. A belt af amphibolitcs forms the cliff at the south-west tip af Majorqap alangua. Related rocks occur in arnphibolite facies in the acea around the lakc Qardlit taserssuat immediately to the soulh (Hall, 1978).

I 10, 10-11: Casa Degli Amanti

1997 ◽  
Author(s):  
Roger Ling ◽  
Paul Arthur ◽  
Georgia Clarke ◽  
Estelle Lazer ◽  
Lesley A. Ling ◽  
...  
Keyword(s):  
The Other ◽  
Central Axis ◽  
The South ◽  
The West ◽  
The North ◽  
Small Window ◽  
South West ◽  
Dining Room ◽  
North Wall ◽  
North And South

The casa degli amanti (house of the lovers), at the south-west corner of the insula, falls into two fairly distinct halves: the atrium complex, oriented on the street to the west, and the peristyle with its surrounding rooms, oriented on the street to the south and on the property boundary to the east. In the atrium complex, the atrium is misplaced to the south of the central axis, allowing space for two large rooms to the north, one of which was possibly a shop or workshop (5.50 m. × 4.70 m.), with a separate entry from the street (I 10, 10), while the other (5.80 m. × 4.50 m.), decorated with mythological wallpaintings and provided with a wide opening on to the peristyle, must have been a dining-room or oecus (room 8). Each of these had a segmental vault rising from a height of about 3.50 m. at the spring to slightly over 4 m. at the crown. In the first the vault is missing, but the holes for some of its timbers are visible in the east wall and a groove along the north wall marks the seating for the planking attached to them; at a higher level, in the north and south walls, are the remains of beam-holes for the joists of the upper floor or attic (see below). The arrangements in room 8 are now obscured by the modern vault constructed to provide a surface for the reassembled fragments of the ceiling-paintings; but the shape of the vault is confirmed by the surviving plaster of the lunettes, while a beam-hole for the lowest of the vault-timbers is visible above the corner of the western lunette in an early photograph (Superintendency neg. C 1944). The shop I 10, 10 had a small window high in the street wall to the south of Its entrance; whether there were any additional windows above the entrance, it is impossible to say, since this part of the wall is a modern reconstruction. Room 8 was lit by a splayed window cut in the angle of the vault and the eastern lunette, opening into the upper storey of the peristyle.

scholarly journals Art. XXVII.—Notes on Malayalam Literature

1900 ◽  
Vol 32 (4) ◽  
pp. 763-768
Author(s):  
T. K. Krishṇa Menon
Keyword(s):  
Indian Ocean ◽  
Arabian Sea ◽  
The South ◽  
The West ◽  
The Third ◽  
The North ◽  
South West ◽  
The Indian Ocean

Malayalam is the language of the south-west of the Madras Presidency. It is the third most important language of the Presidency, the first and the second being Tamil and Telugu respectively. It is spoken in Malabar, Cochin, and Travancore. Out of a total of 5,932,207 inhabitants of these parts, 5,409,350 persons are those who speak Malayalam. These countries, taken as a whole, are bounded on the north, by South Canara, on the east by the far-famed Malaya range of mountains, on the south by the Indian Ocean, and on the west by the Arabian Sea.

An Iron Age Hill-Fort at Grimthorpe, Yorkshire, England

1969 ◽  
Vol 34 ◽  
pp. 148-190 ◽  
Author(s):  
I. M. Stead ◽  
M. Jarman ◽  
Angela Fagg ◽  
E. S. Higgs ◽  
C. B. Denston
Keyword(s):  
Iron Age ◽  
The South ◽  
The West ◽  
Circular Area ◽  
North West ◽  
The North ◽  
South West ◽  
White Horse ◽  
The Hill ◽  
Grave Goods

The Iron Age hill-fort at Grimthorpe (Grid reference SE.816535) in the parish of Millington, East Riding of Yorkshire, is on the western edge of the Yorkshire Wolds, with a commanding position over the Vale of York. There is an uninterrupted view to the White Horse on the Hambleton Hills, 25 miles to the north-west; beyond York, 13 miles to the west, to the Pennines; and to the south 25 miles to the chimneys of Keadby and Scunthorpe. To the west and south the land slopes away to the Vale of York, and to the north and east there is a sharper fall to Given Dale and Whitekeld Dale. The hill-fort defences follow the 520 feet contour, and enclose an approximately circular area of eight acres (fig. 1).A traditional reference may be preserved in the field-name—Bruffs—perhaps a variation of ‘Brough’, which ‘refers in all cases to ancient camps, usually Roman ones’. But all surface indications have now been obliterated by ploughing, and even a century ago there was little more to be seen. John Phillips in 1853 noticed ‘unmistakable traces of ancient but unascertainable occupation’, and in 1871 an excavation by J. R. Mortimer located ‘the filled up inner ditch of a supposed camp’. But Mortimer was not concerned with the settlement; his interest had been aroused by the discovery, in 1868, of a burial with rich grave-goods, including metalwork with La Tène ornament, in a chalk-pit within the south-west sector of the hill-fort.

Mbadamassi of Lagos: A Soldier for King and Kaiser, and a Deportee to German South West Africa

2009 ◽  
Vol 2 (1) ◽  
pp. 103-124
Author(s):  
Jan-Bart Gewald
Keyword(s):  
West Africa ◽  
South African ◽  
Military Service ◽  
West African ◽  
The South ◽  
The West ◽  
The North ◽  
German Army ◽  
South West ◽  
South West Africa

Abstract In 1915 troops of the South African Union Defence Force invaded German South West Africa, present day Namibia. In the north of the territory the South African forces captured an African soldier serving in the German army named Mbadamassi. Upon his capture Mbadamassi demanded to be released and claimed that he was a British national from Nigeria. In addition, he stated that he had served in the West African Frontier Force, and that he had been shanghaied into German military service in Cameroon. Furthermore, whilst serving in the German army in Cameroon, Mbadamassi claimed that he had participated in a mutiny, and that, as a consequence, he had been deported to GSWA. The article covers the remarkable military career of the African soldier, Mbadamassi, who between 1903 and 1917 served both the King of the British Empire as well as the Kaiser of the German Empire. In so doing, the article sheds light on the career of an individual African soldier serving in three colonial armies; the West African Frontier Force, the Schutztruppe in Cameroon, and the Schutztruppe in GSWA. The article argues that beyond the fact that colonial armies were institutions of repression, they also provided opportunity for those willing or condemned to serve within their ranks. Furthermore the article provides some indication as to the extent of communication that existed between colonial subjects in the separate colonies of Africa at the time. En 1915, les troupes de l'Union de l'Afrique du Sud ont envahi l'Afrique du Sud-Ouest allemande, l'actuelle Namibie. Dans le Nord du territoire, les forces sud-africaines ont capturé un soldat africain servant dans l'armée allemande nommé Mbadamassi. Celui-ci exigea d'être libéré et revendiqua être un Britannique du Nigeria. De plus, il déclara avoir servi dans la West African Frontier Force et avoir été enrôlé de force dans l'armée allemande au Cameroun. En outre, pendant qu'il servait dans l'armée allemande au Cameroun, Mbadamassi a prétendu avoir pris part à une mutinerie, ce qui avait conduit à sa déportation vers l'Afrique du Sud-Ouest allemande. Cet article couvre la remarquable carrière militaire du soldat africain Mbadamassi, qui, entre 1903 et 1917, a servi à la fois le roi de l'empire britannique et le Kaiser de l'empire allemand. Ainsi, l'article éclaire sur la carrière individuelle d'un soldat africain servant dans trois armées coloniales; la West African Frontier Force, le Schutztruppe au Cameroun et le Schutztruppe en Afrique du Sud-Ouest allemande. L'article soutient qu'au-delà du fait que les armées coloniales étaient des institutions de répression, elles ont aussi offert la possibilité à ceux qui le voulaient ou ceux qui y étaient condamnés de servir dans leurs rangs. En outre, l'article fournit une indication sur l'étendue de la communication qui a existé entre les sujets coloniaux dans les colonies d'Afrique séparées de l'époque.

Excavation of Four Barrows, and a Middle Bronze Age Cremation Cemetery, at Heatherstone Grange, Bransgore, Hampshire

2018 ◽  
Vol 73 (1) ◽  
pp. 11-89
Author(s):  
Richard Massey ◽  
Elaine L. Morris
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Early Bronze Age ◽  
The South ◽  
The West ◽  
Radiocarbon Dates ◽  
North West ◽  
The North ◽  
South West ◽  
Middle Bronze Age

Excavation at Heatherstone Grange, Bransgore, Hampshire, investigated features identified in a previous evaluation. Area A included ring ditches representing two barrows. Barrow 1.1 held 40 secondary pits, including 34 cremation-related deposits of Middle Bronze Age date, and Barrow 1.2 had five inserted pits, including three cremation graves, one of which dated to the earlier Bronze Age, and was found with an accessory cup. A number of pits, not all associated with cremation burials, contained well-preserved urns of the regional Deverel-Rimbury tradition and occasional sherds from similar vessels, which produced a closely-clustered range of eight radiocarbon dates centred around 1300 BC. Of ten pits in Area C, three were cremation graves, of which one was radiocarbon-dated to the Early Bronze Age and associated with a collared urn, while four contained only pyre debris. Barrow 1.3, in Area E, to the south, enclosed five pits, including one associated with a beaker vessel, and was surrounded by a timber circle. Area F, further to the south-west, included two pits of domestic character with charcoal-rich fills and the remains of pottery vessels, together with the probable remains of a ditched enclosure and two sets of paired postholes. Area H, located to the north-west of Area E, partly revealed a ring ditch (Barrow 1.4), which enclosed two pits with charcoal-rich fills, one with a single Late Bronze Age/Early Iron Age potsherd, and the other burnt and worked flint. A further undated pit was situated to the east of Barrow 1.4. The cremation cemetery inserted into Barrow 1.1 represents a substantial addition to the regional record of Middle Bronze Age cremation burials, and demonstrates important affinities with the contemporary cemeteries of the Stour Valley to the west, and sites on Cranborne Chase, to the north-west.

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