Forest Dialect

English Today ◽  
2020 ◽  
Vol 36 (3) ◽  
pp. 70-76
Author(s):  
Michelle Straw
Keyword(s):  
Identity Construction ◽  
Nation State ◽  
The South ◽  
The West ◽  
South West ◽  
Special Place ◽  
West Midlands ◽  
National Borders

The Forest of Dean (henceforth Forest) is one of the lesser known English Royal Forests. The area is considered locally to be a special place with a distinctive dialect. The Forest lies at the intersection of three regions: South East Wales, West Country, also known as the South West, and the West Midlands. The Forest is situated between two rivers: the River Severn to the East separates it from the rest of Gloucestershire; the River Wye to the West separates it from Wales. National borders and physical boundaries seem to play an important role in identity construction. ‘Identities matter most’ (Llamas & Watt, 2010: 17) to those communities ‘at the physical margins of the nation state’ (Llamas, 2010: 225). Such communities may engage in practices that differentiate their dialect and situate it at the centre of their own region.

The Base and Top of the Coral-rock in Barbados

1937 ◽  
Vol 74 (8) ◽  
pp. 337-359 ◽  
Author(s):  
C. T. Trechmann
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
East Part ◽  
Varying Thickness ◽  
South West ◽  
New Information ◽  
Main Portion ◽  
Coral Rock

1. The coral-rock commences nearly everywhere with a basal bed of varying thickness containing a fauna of pre-Pleistocene aspect among which the genus Haliotis (absent from these coasts at the present day), Pleurotomaria, Meiocardia, etc., are noticeable. This faunule may have lived at a depth of 700–1,000 feet.2. The supposition that the southerly anticlines are a later uplift than the main portion of Barbados is supported by the absence of ravines, and the presence of post-coral-rock beds which occur as coastal veneers at low altitudes, and in greater thickness in the south-east corner near Whitehaven.3. The south-east part of the island from Consett Point to Ragged Point has probably extended further seawards in comparatively recent times ; the series of converging faults and dislocations in the cliff sections suggest that the thrusts from the west or south-west may have been resisted by this part of the island.4. The relative claims of fault-scarping or marine erosion in production of the rising terraces is discussed ; and new information regarding the thickness of the coral-rock at sea-level from a boring is detailed.5. The finding of a faunule with Pliocene or possibly Miocene affinities at the base of the coral-rock puts the Oceanic series further back, into the Miocene.

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.

scholarly journals Learning from the transfer of a fellowship programme to support primary care workforce needs in the UK: a qualitative study

BMJ Open ◽  
2019 ◽  
Vol 9 (1) ◽  
pp. e023384 ◽  
Author(s):  
Carol Bryce ◽  
Rachel Russell ◽  
Jeremy Dale
Keyword(s):  
Health Service ◽  
Qualitative Study ◽  
Workforce Development ◽  
Urgent Care ◽  
The South ◽  
The West ◽  
Clinical Placements ◽  
Funding Model ◽  
West Midlands ◽  
The Impact

ObjectivesService redesign, including workforce development, is being championed by UK health service policy. It is allowing new opportunities to enhance the roles of staff and encourage multiprofessional portfolio working. New models of working are emerging, but there has been little research into how innovative programmes are transferred to and taken up by different areas. This study investigates the transferability of a 1-year post-Certification of Completion of Training fellowship in urgent and acute care from a pilot in the West Midlands region of England to London and the South East.DesignA qualitative study using semistructured interviews supplemented by observational data of fellows’ clinical and academic activities. Data were analysed using a thematic framework approach.Setting and participantsTwo cohorts of fellows (15 in total) along with key stakeholders, mentors, tutors and host organisations in London and the South East (LaSE). Fellows had placements in primary and secondary care settings (general practice, emergency department, ambulatory care, urgent care and rapid response teams), together with academic training.ResultsSeventy-six interviews were completed with 50 participants, with observations in eight clinical placements and two academic sessions. The overall structure of the West Midlands programme was retained and the core learning outcomes adopted in LaSE. Three fundamental adaptations were evident: broadening the programme to include multiprofessional fellows, changes to the funding model and the impact that had on clinical placements. These were felt to be key to its adoption and longer-term sustainability.ConclusionThe evaluation demonstrates a model of training that is adaptable and transferable between National Health Service regions, taking account of changing national and regional circumstances, and has the potential to be rolled out widely.

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).

Athens Honours Proxenos (IG i2. 146)

1974 ◽  
Vol 69 ◽  
pp. 295-298
Author(s):  
Michael B. Walbank
Keyword(s):  
West Coast ◽  
Fifth Century ◽  
Small Island ◽  
The South ◽  
The West ◽  
South West

This document is one of a number of Attic proxeny-decrees that A. G. Woodhead considered to be evidence for Athenian concern with the south-west Aegean towards the end of the fifth century B.C. He identified the honorand Proxenos as a native of Chalke, a small island off the west coast of Rhodes. I share the view of J. and L. Robert that Woodhead has not proved his case either for the date or for the ethnic.The inscription is non-stoichedon, its engraving inexpert and careless, with several mistakes untidily erased and corrected. There is a mixture of Attic and Ionic letter-forms in the first three lines (gamma, eta, and lambda are Ionic, while xi is written chi sigma); otherwise the lettering is Attic, indicating a date before 403 B.C.

Population and Habitat Selection of the Noisy Scrub-bird, Atrichornis clamosus, 1962-83

1985 ◽  
Vol 12 (3) ◽  
pp. 479 ◽  
Author(s):  
GT Smith
Keyword(s):  
Habitat Selection ◽  
Incomplete Data ◽  
The South ◽  
The West ◽  
Population Index ◽  
South West ◽  
Number Of Males ◽  
Selection Of

The noisy scrub-bird Atrichornis clamosus at Two Peoples Bay was censused, the number of singing males being used as the population index. Incomplete data from 1962 to 1968 suggest that the number of males varied from 40 to 50 during this period. The first rigorous census found 45 males in 1970 and this number increased to 138 in 1983. The most likely reason for this increase is the absence of fire from the area since 1970. Since 1975 the population has expanded out of its headland stronghold to the south-west of Two Peoples Bay to form a subpopulation around Lake Gardner that is well separated from the headland population by roads, firebreaks and a strip of control burnt blocks. The growth of this subpopulation has added a further safeguard to the population. Observations on the vegetation formations (heath, thicket, low forest A and low forest B) used by male noisy scrub-birds on the headland indicate that most of the best habitat (low forest B) is occupied and that an increasing number of males are occupying suboptimal habitat (heath and thicket). There is sufficiently good habitat to the west of Lake Gardner to allow at least 30 additional males to live in the area.

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.

scholarly journals The Works of Pergamon and their Influence

1886 ◽  
Vol 7 ◽  
pp. 251-274
Author(s):  
L. R. Farnell
Keyword(s):  
Good Reason ◽  
Right Wing ◽  
Left Wing ◽  
The South ◽  
Hellenic Journal ◽  
The West ◽  
West Side ◽  
South West ◽  
The Right ◽  
Made In

The questions concerning the art of Pergamon, its characteristics and later influence, depend partly for their solution on the reconstruction and explanation of the fragments in Berlin. Much progress has been made in the work during the last year. The discovery which decided what was the breadth of the staircase, and what were the figures which adorned the left wing and the left staircase wall, has been already mentioned in the Hellenic Journal. It is now officially stated that the staircase was on the west side of the altar, although Bohn, in his survey of the site, at first conceived that this was impossible. Assuming that this point is now settled, we may note what is certain, or probable, or what is merely conjectural, in the placing of the groups. We know that the wing on the left of the staircase, and the left staircase-wall, were occupied by the deities of the sea and their antagonists: by Triton, Amphitrite, Nereus, and others which we cannot name. Among them, also, we may perhaps discern the figure of Hephaestos, and in their vicinity we must suppose Poseidon. On the right wing of the staircase, and around the south-west corner, we have good reason for placing Dionysos, with Cybele and her attendant goddesses, although the order of the slabs on which these latter are found is not the same as was formerly supposed.

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