scholarly journals Sir Vincent Brian Wigglesworth, C. B. E., 17 April 1899 - 12 February 1994

1996 ◽  
Vol 42 ◽  
pp. 541-553 ◽  
Keyword(s):  
Eighteenth Century ◽  
General Practitioner ◽  
Early Death ◽  
The South ◽  
North West ◽  
South West ◽  
Scale Models ◽  
The University ◽  
University Of Manchester ◽  
Artistic Talent

On 17 April 1899, in Kirkham, Lancashire, Vincent Brian Wigglesworth was born into a talented and idiosyncratic Victorian family with roots going back to the hamlet of Wigglesworth in the south-west comer of Yorkshire. He was the son of Sydney Wigglesworth, M.R.C.S., L.R.C.P., Captain R.A.M.C., and Margaret Emmeline (née Pierce). Sydney Wigglesworth was a general practitioner but also an amateur mechanic and inventor who had studied engineering at Owens College (later the University of Manchester) before changing to medicine. He made scale models of locomotives and was a passionate pioneer motorist. Margaret Pierce came from a well-to-do family of London solicitors originating from Devon yeoman stock with business and nautical interests (Pierce Sound in North West Canada is named after an eighteenth-century ancestor). As an amateur painter trained at South Kensington she developed a great eye for colour. It was the kind of family that produced many famous Englishmen, artists as well as scientists. V.B.W.’s scientific illustrations show that he inherited his mothers artistic talent. His elder brother’s career as a landscape painter was cut short by his early death in 1936.

Velumtätigkeit bei der Erzeugung stimmhafter und stimmloser Nasalkonsonanten im Isländischen

1981 ◽  
Vol 4 (1) ◽  
pp. 19-28 ◽  
Author(s):  
Magnús Pétursson
Keyword(s):  
Temporal Patterns ◽  
Stop Consonants ◽  
The South ◽  
Research Instrument ◽  
North West ◽  
South West ◽  
Different Types ◽  
Nasal Consonant

In modern Icelandic, spoken in the South, West, and North-West of Iceland, there is a phonemic opposition between voiced and voiceless nasals before stop consonants. For the present investigation the research instrument was the velograph. The purpose of the research was to investigate patterns of velar movement associated with each type of nasal consonants. The results show different types of velar movement organized according to two separate temporal patterns. For the voiceless nasals the movement of the velum is more rapid and begins earlier than for the voiced nasals. There are also significant differences in the nasalization of the preceding vowel according to whether the following nasal consonant is voiced or voiceless.

Archaeological Discoveries in Sicily and Magna Graecia

1939 ◽  
Vol 59 (2) ◽  
pp. 213-228
Author(s):  
Umberto Zanotti-Bianco
Keyword(s):  
Eighteenth Century ◽  
Ground Level ◽  
The South ◽  
Total Length ◽  
Magna Graecia ◽  
South West ◽  
Southern Side ◽  
The Temple ◽  
Southern Flank

In my previous report (JHS, 1938, p. 247) I spoke of the work being carried on at Syracuse to bring to light the remains of the temple of Apollo. The east, north, and west sides had been freed by then, whilst the southern side was still hidden under seventeenth- and eighteenth-century houses, so that it had never been possible to dig trial trenches through their foundations to ascertain if any part of the temple was preserved there. The demolition of the houses and the excavation under the modern ground level beginning from the south-west angle have fully satisfied our hopes. Five columns of the southern flank of the peristasis have appeared, preserved to a height of over 2 metres, with the stylobate beneath them (Fig. 1): only the angle column had been destroyed during the building of the walls of the Spanish barracks. The cella is equally well preserved, and a third of its total length has already been liberated, although the work is in temporary suspense owing to unsettled disputes with the owners of the houses. The southern flank of the archaic Syracusan temple appears to be in much better condition than the others.

Part VI. The Cyclopean Terrace Building and the Deposit of Pottery beneath It

1954 ◽  
Vol 49 ◽  
pp. 267-291
Author(s):  
Elizabeth B. Wace
Keyword(s):  
Contour Line ◽  
The South ◽  
Main Road ◽  
North West ◽  
North East ◽  
The North ◽  
South West

The Cyclopean Terrace Building lies to the north-west of the Lion Gate on the northern end of the Panagia Ridge and faces almost due west across the valley of the Kephissos and modern main road from Corinth to Argos. It lies just below the 200 m. contour line, and one terrace below the houses excavated in 1950–51 by Dr. Papadimitriou and Mr. Petsas to the east at the same end of the ridge. The area contains a complex of buildings, both successive and contemporary, and in view of the discovery of structures both to the south-west and, by the Greek Archaeological Service, to the north-east it is likely that this whole slope was covered by a portion of the outer town of Mycenae. This report will deal only with the structure to which the name Cyclopean Terrace Building was originally given, the so-called ‘North Megaron’, supported by the heavy main terrace wall.The excavation of this structure was begun in 1923. The main terrace wall was cleared and two L.H. IIIC burials discovered in the top of the fill in the south room. In 1950 it was decided to attempt to clear this building entirely in an endeavour to find out its date and purpose. The clearing was not, however, substantially completed until the close of the 1953 excavation season, and this report presents the available evidence for the date as determined by the pottery found beneath the building; the purpose is still a matter for study, though various tentative conclusions can be put forward.

scholarly journals Regional Differences in Postnatal Care Service Utilisation and Child Morbidity in Nigeria: Evidence from 2018 Nigeria Demographic and Health Survey (NDHS)

2020 ◽  
Author(s):  
Endurance Uzobo ◽  
Aboluwaji D. Ayinmoro
Keyword(s):  
Socioeconomic Factors ◽  
Health Survey ◽  
Postnatal Care ◽  
Demographic And Health Survey ◽  
The South ◽  
North Central ◽  
North West ◽  
North East ◽  
South West ◽  
Child Morbidity

Abstract Introduction: Modern Postnatal Care Services (PNC) in Nigeria is vital tool for providing quality health for mothers and newborns. Nonetheless, many regions in Nigeria are still struggling to achieve optimum utilisation of modern PNC services due to variation in associated socioeconomic factors of mothers based on their regions. This study aims at assessing regional socioeconomic factors associated with PNC services utilisation and its relationship with child morbidity in Nigeria. Methods Data for this study was extracted from the Nigeria Demographic and Health Survey (NDHS) 2018 birth recoded file dataset, with a sample size of 30713 women (aged 15–49). Data were analysed using descriptive statistics, Chi-Square Test and logistic regression. The main predictor variable was the region, while others included the type of PNC service utilised and various demographic variables of the respondents – age, education, type of residence, religion, ethnicity among others. Results The average age of the respondents was 29.5 ± 6.8. The use of modern PNC services ranged from South-West (20.3%), South-South (10.9%), South-East (23.0%), North-Central (22.0%), North-East (13.0%) to North-West (10.9%). The prevalence of child morbidity ranged from South-West (8.5%), South-South (9.8%), South-East (11.4%), North-Central (15.3%), North-East (26.3%) to North-West (28.7%). Child morbidity is significantly higher in the South-South (OR = 1.46), South-East (OR = 1.50), North-Central (OR = 1.13), North-East (OR = 2.31) and North-West (OR = 1.35) compared to the South-West. Conclusion Majority of women in Nigeria are not using modern PNC services. Regional variations in the use of PNC services and socio-demographic characteristics of mothers influence child morbidity in Nigeria. There is need for regional-specific context sensitisation for mothers in the use of modern PNC services.

VI.—The Salt Deposits of Dax and the Pyrenees

1904 ◽  
Vol 1 (6) ◽  
pp. 265-272
Author(s):  
P. W. Stuart-Menteath
Keyword(s):  
Rock Salt ◽  
Mineral Water ◽  
Igneous Rocks ◽  
Thermal Springs ◽  
Salt Formation ◽  
The South ◽  
North West ◽  
The North ◽  
South West ◽  
Salt Deposits

On the rail to Biarritz the roots of the Pyrenees first appear at Dax, and are accompanied by those ophites and thermal springs which are special features of the entire chain. Vast deposits of salt, to whose first development I contributed, have added an important industry to the resources of this ancient capital of Aquœ Tarbelliœ, where the exact harness depicted on Roman medals is still characteristic of every cart. Beneath the existing ditch of the Roman fortifications rock-salt was accidentally discovered by a boring for mineral water, and the salt is now worked at three miles to the south-east, and is indicated by springs for a distance of seven miles. The deposit is known to be about 100 feet in thickness, but is of unknown depth beneath the existing borings.Along the entire outskirts of both sides of the Pyrenees similar salt deposits abound, and they are often similarly accompanied by igneous rocks.The salt formation of Dax is distinctly limited by the valley of the Adour, which here ceases to wander among the sands of the plain, and is suddenly and sharply diverted along a tectonic depression, running towards the Pyrenees in a south-west direction. Precisely parallel to this course, in the Cretaceous and Tertiary rocks of the Pyrenees, there runs, at a dozen miles to the north-west, the most remarkable example known of a tectonic valley sunk beneath the ocean. The Gouf de Capbreton, sinking with steep sides to over 3,000 feet beneath the even bottom of the Atlantic skirt, and affording evidence of igneous rocks in its surroundings and in the irregularities of its floor, is a perfect analogue of the neighbouring tectonic portion of the Adour.

I. Giants' Hills 2 Long Barrow, Skendleby, Lincolnshire

Archaeologia ◽  
1991 ◽  
Vol 109 ◽  
pp. 1-45 ◽  
Author(s):  
J. G. Evans ◽  
D. D. A. Simpson
Keyword(s):  
Geographical Location ◽  
Historic Buildings ◽  
The South ◽  
Rescue Operation ◽  
Maximum Slope ◽  
Burial Practices ◽  
North West ◽  
Geographical Scale ◽  
The University ◽  
Southern Extremity

The Neolithic long barrow whose excavation is described in this report is one of a pair known as Giants' Hills, situated in the parish of Skendleby, Lincolnshire (NGR: TF(53)429709; Lat. 53° 12′ 40″ N., Long. 0° 8′ 30″ E.). The general geographical location is an outlier of the chalk at the southern extremity of the Lincolnshire Wolds (fig. 1). The site lay at between 56 and 58m O.D. along the gentle south-facing slope of a small river valley (fig. 2). The maximum slope is 7 degrees. Orientation was approximately south-east/north-west with what can be considered the more important end of the barrow (the front) towards the south-east. The dimensions of the preserved mound were 65 × 13m (maximum) (originally 77 × 19m), and of the entire site from the original outer edges of the ditch, 89 × 29m (maximum).The other barrow of the pair, Giants' Hills 1, was excavated by C. W. Phillips (1936). To the south-east beyond a low chalk ridge and in a topographical position similar to that of the Giants' Hills barrows lies another pair of long barrows, the Deadmen's Graves (fig. 2). On a broader geographical scale, both pairs belong to a group of about fifteen long barrows situated on the Lincolnshire Wolds (fig. 1).Excavation took place under the direction of the authors at the instigation of the Department of the Environment (now the Historic Buildings and Monuments Commission for England) because of damage sustained by ploughing. As well as being a rescue operation, the work can be seen as an integral part of research into prehistoric chalkland environments and Neolithic burial practices. Thus, financial support was provided not only by the DoE, but also by University College Cardiff and the University of Leicester. There were three field seasons. In the first two, from 4–28 September 1975 and 27 March to 10 April 1976, the western end of the site (west of line AL, fig. 4) was excavated totally. The main excavation took place between 14 August and 25 September 1976.

scholarly journals Pleistocene Geology of the South-West Yukon Territory, Canada

1965 ◽  
Vol 5 (40) ◽  
pp. 385-397 ◽  
Author(s):  
Daniel B. Krinsley
Keyword(s):  
Yukon Territory ◽  
River Valley ◽  
The South ◽  
North West ◽  
White River ◽  
North East ◽  
South West ◽  
M 12

Abstract A morainal sequence in south-west Yukon Territory, Canada, records at least four major, successively less extensive glaciations from ice fields in the St. Elias Mountains south of the glaciated area. The Nisling Moraine flanks the Klondike Plateau in a belt t km. wide to an altitude of 1,040 m., 12 km. north-east of Snag. The northernmost lobe of this moraine terminates at the junction of the Donjek and White Rivers, 120 km, from the nearest source of ice, Klutlan Glacier. 11 km. north-east of Snag, the prominent front of the Donjek Moraine lies 180 m. below the front of the Nisling Moraine. The northernmost lobe of the Donjek Moraine terminates 106 km. north of Klutlan Glacier and occupies the lower courses of canyons cut into the Nisling Moraine. The front of the Snag Moraine crosses the White River valley 210 m. below the front of the Donjek Moraine and 96 km. north of Klutlan Glacier. The Tchawsahmon Moraine, 38 km. north-west of Klutlan Glacier. consists of a series of concentric ridges, the oldest of which impounded Tchawsahmon Lake. Provisional correlations suggest that the Nisling Moraine is pre-Illinoian; the Donjek, Illinoian; the Snag, pre-classical Wisconsin; and the Tchawsahmon, classical Wisconsin.

scholarly journals Pleistocene Geology of the South-West Yukon Territory, Canada

1965 ◽  
Vol 5 (40) ◽  
pp. 385-397 ◽  
Author(s):  
Daniel B. Krinsley
Keyword(s):  
Yukon Territory ◽  
River Valley ◽  
The South ◽  
North West ◽  
White River ◽  
North East ◽  
South West ◽  
M 12

AbstractA morainal sequence in south-west Yukon Territory, Canada, records at least four major, successively less extensive glaciations from ice fields in the St. Elias Mountains south of the glaciated area.The Nisling Moraine flanks the Klondike Plateau in a belt t km. wide to an altitude of 1,040 m., 12 km. north-east of Snag. The northernmost lobe of this moraine terminates at the junction of the Donjek and White Rivers, 120 km, from the nearest source of ice, Klutlan Glacier. 11 km. north-east of Snag, the prominent front of the Donjek Moraine lies 180 m. below the front of the Nisling Moraine. The northernmost lobe of the Donjek Moraine terminates 106 km. north of Klutlan Glacier and occupies the lower courses of canyons cut into the Nisling Moraine. The front of the Snag Moraine crosses the White River valley 210 m. below the front of the Donjek Moraine and 96 km. north of Klutlan Glacier. The Tchawsahmon Moraine, 38 km. north-west of Klutlan Glacier. consists of a series of concentric ridges, the oldest of which impounded Tchawsahmon Lake.Provisional correlations suggest that the Nisling Moraine is pre-Illinoian; the Donjek, Illinoian; the Snag, pre-classical Wisconsin; and the Tchawsahmon, classical Wisconsin.

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