Winchester

2020 ◽  
Author(s):  
Simon Roffey
Keyword(s):  
Iron Age ◽  
Central Place ◽  
British History ◽  
Anglo Saxon ◽  
The South ◽  
Norman Conquest ◽  
The North ◽  
South Central ◽  
Charles Ii ◽  
Power Center

Winchester lays claim to being one of the most important cities in British history. The city has a central place in British myth and legend and was once ancient capital and residence of the Anglo-Saxon and early Norman kings. Winchester is also one of the most extensively excavated medieval towns in England and was the training ground for modern British archeology. Situated in south-central England, Winchester was close to key communication routes via the south coast and the important medieval port at Southampton. Founded in the Roman period as Venta Belgarum, close to the site of the Iron Age market settlement, Winchester quickly grew into a prosperous Roman civitas. After the decline of Roman power in Britain, Winchester remained as an important power center in the south and by the mid-7th century was the pre-eminent town in the newly established Anglo-Saxon kingdom of Wessex. With the consolidation of Wessex’s power in the 9th and 10th centuries and the eventual re-establishment of control over the former Viking-influenced areas of the midlands and the north, Winchester became the seat of English royal power. With the Norman Conquest in 1066, the early Norman kings sought to keep Winchester as the royal seat. However, with the rising pre-eminence of London in the mid-12th century, Winchester’s power declined as royal and secular power shifted to London. Nevertheless, Winchester was still to remain of some importance throughout the medieval period and its bishop one of the most powerful, influential, and richest lords in medieval England; a status still attested to by the city’s medieval cathedral. As a city of many religious foundations, Winchester’s fortunes waned after the Reformation to be briefly reborn in the later 17th century with the planned construction of Charles II palace on the site of the former medieval castle. Charles’ plans to reinvent Winchester as a revitalized English royal city were aborted with his untimely death in 1688, with the palace, designed by Christopher Wren, barely finished.

Manuscripts containing English decoration 871–1066, catalogued and illustrated: a review

1978 ◽  
Vol 7 ◽  
pp. 239-266 ◽  
Author(s):  
Linda L. Brownrigg
Keyword(s):  
High Standard ◽  
Tenth Century ◽  
Eighth Century ◽  
Anglo Saxon ◽  
The South ◽  
Norman Conquest ◽  
Southern England ◽  
The North ◽  
Careful Preparation ◽  
Service Books

In the period from Alfred's reign to the Norman Conquest scribes and artists in southern England once more achieved a high standard in bookmaking, comparable to the brilliant tradition which had been established in both the north and the south in the eighth century. Some codices survive which are rough in execution, written on poorly prepared membrane by unskilled hands, but the majority – by no means chiefly service books produced for ecclesiastical and royal patrons – demonstrate that by the end of the tenth century a large number of scribes understood the techniques of careful preparation of membranes and inks, had mastered the letter-forms of two scripts, Caroline minuscule and Anglo-Saxon square minuscule, and were disciplined to follow consistently a hierarchy of scripts for the openings of texts and major divisions, chapter titles, incipits and explicits. What remains must be only a fragment of the production of Benedictine monks and nuns, secular clerks and lay scribes. But however incomplete and unbalanced the evidence, the over-all level of accomplishment cannot be doubted.

Climatology and Trends of Climate Extremes of Temperature and Precipitation in Belo Monte Hydropower Plant – Eastern Amazon, Brazil

2021 ◽  
Author(s):  
Wanderson Luiz-Silva ◽  
Pedro Regoto ◽  
Camila Ferreira de Vasconcellos ◽  
Felipe Bevilaqua Foldes Guimarães ◽  
Katia Cristina Garcia
Keyword(s):  
Climate Change ◽  
Climate Extremes ◽  
Annual Rainfall ◽  
The South ◽  
North Central ◽  
Adaptation Capacity ◽  
The North ◽  
South Central ◽  
Daily Data ◽  
Belo Monte

<p>This research aims to support studies related to the adaptation capacity of the Amazon region to climate change. The Belo Monte Hydroelectric Power Plant (HPP) is in the Xingu River basin, in eastern Amazonia. Deforestation coupled with changes in water bodies that occurred in the drainage area of Belo Monte HPP over the past few decades can significantly influence the hydroclimatic features and, consequently, ecosystems and energy generation in the region. In this context, we analyze the climatology and trends of climate extremes in this area. The climate information comes from daily data in grid points of 0.25° x 0.25° for the period 1980-2013, available in http://careyking.com/data-downloads/. A set of 17 climate extremes indices based on daily data of maximum temperature (TX), minimum temperature (TN), and precipitation (PRCP) was calculated through the RClimDex software, recommended by the Expert Team on Climate Change Detection and Indices (ETCCDI). The Mann-Kendall and the Sen’s Curvature tests are used to assess the statistical significance and the magnitude of the trends, respectively. The drainage area of the Belo Monte HPP is dominated by two climatic types: an equatorial climate in the north-central portion of the basin, with high temperatures and little variation throughout the year (22°C to 32°C), in addition to more frequent precipitation; and a tropical climate in the south-central sector, which experiences slightly more pronounced temperature variations throughout the year (20°C to 33°C) and presents a more defined wet and dry periods. The south-central portion of the basin exhibits the highest temperature extremes, with the highest TX and the lowest TN of the year occurring in this area, both due to the predominant days of clear skies in the austral winter, as to the advance of intense masses of polar air at this period. The diurnal temperature range is lower in the north-central sector when compared to that in the south-central region since the first has greater cloud cover and a higher frequency of precipitation. The largest annual rainfall volumes are concentrated at the north and west sides (more than 1,800 mm) and the precipitation extremes are heterogeneous across the basin. The maximum number of consecutive dry days increases from the north (10 to 20 days) to the south (90 to 100 days). The annual frequency of warm days and nights is increasing significantly in a large part of the basin with a magnitude ranging predominantly from +7 to +19 days/decade. The annual rainfall shows a predominant elevation sign of up to +200 mm/decade only in the northern part of the basin, while the remainder shows a reduction of up to -100 mm/decade. The duration of drought periods increases in the south-central sector of the basin, reaching up to +13 days/decade in some areas. The results of this study will be used in the future as an important input, together with exposure, sensibility, and local adaptation capacity, to design adaptation strategies that are more consistent with local reality and to the needs of local communities.</p>

The Britons in Southern Scotland

Antiquity ◽  
1955 ◽  
Vol 29 (114) ◽  
pp. 77-88 ◽  
Author(s):  
Kenneth Jackson
Keyword(s):  
Iron Age ◽  
Roman Period ◽  
Anglo Saxon ◽  
Medieval Period ◽  
The West ◽  
Early Medieval Period ◽  
The North ◽  
Dark Ages ◽  
The People ◽  
Northern Portion

The archaeological background of the people of what is now Scotland south of the Forth and Clyde in the Roman period was a La Téne one, and specifically chiefly Iron Age B. This links them intimately with the Britons of southern Britain in the conglomeration of Celtic tribes who called themselves Brittones and spoke what we call the Brittonic or Ancient British form of Celtic, from which are descended the three modern languages of Welsh, Cornish and Breton. To the north of the Forth was a different people, the Picts. They too were Celts or partly Celts; probably not Brittones however, but a different branch of the Celtic race, though more closely related to the Brittones than to the Goidels of Ireland and (in later times) of the west of Scotland. Not being Brittonic, the Picts may be ignored here. Our southern Scottish Brittones are nothing but the northern portion of a common Brittonic population, from the southern portion of which come the people of Wales and Cornwall. Some historians speak of the northern Brittones as Welsh, following good Anglo-Saxon precedent, but this is apt to lead to confusion. The best term for them, in the Dark Ages and early Medieval period, as long as they survived, is ‘Cumbrians’, and for their language, ‘Cumbric’. They called themselves in Latin Cumbri and Cumbrenses, which is a Latinization of the native word Cymry, meaning ‘fellow-countrymen’, which both they and the Welsh used of themselves in common, and is still the Welsh name for the Welsh to the present day. The centre of their power was Strathclyde, the Clyde valley, with their capital at Dumbarton.

Bronze Age Barrows on Charmy Down and Lansdown, Somerset

1950 ◽  
Vol 30 (1-2) ◽  
pp. 34-46 ◽  
Author(s):  
Audrey Williams
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
The South ◽  
Stream Flows ◽  
North East ◽  
The North

Charmy Down is a plateau three miles north-east of Bath (fig. 1, 1), east of the Bath-Tetbury road. About a square mile in extent it has a general height of well over 600 ft. To the north the scarp falls swiftly, on the east more gently, to the wooded valley of St. Catherine's Brook, a tributary of the Bristol Avon and the modern Somerset–Gloucester boundary. At the foot of the steep western scarp a second stream flows south to the Avon. On the south Chilcombe Bottom separates Charmy Down from Solsbury Hill, distinguished by its Iron Age earthwork. The underlying rock is oolite, a southward continuation of the Cotswold formation.

Surface faulting along the Superstition Hills fault zone and nearby faults associated with the earthquakes of 24 November 1987

1989 ◽  
Vol 79 (2) ◽  
pp. 252-281
Author(s):  
R. V. Sharp ◽  
K. E. Budding ◽  
J. Boatwright ◽  
M. J. Ader ◽  
M. G. Bonilla ◽  
...  
Keyword(s):  
Fault Zone ◽  
Lateral Displacement ◽  
Vertical Displacement ◽  
Repeated Measurements ◽  
The South ◽  
Surface Rupture ◽  
Imperial Valley ◽  
The North ◽  
South Central ◽  
The Right

Abstract The M 6.2 Elmore Desert Ranch earthquake of 24 November 1987 was associated spatially and probably temporally with left-lateral surface rupture on many northeast-trending faults in and near the Superstition Hills in western Imperial Valley. Three curving discontinuous principal zones of rupture among these breaks extended northeastward from near the Superstition Hills fault zone as far as 9 km; the maximum observed surface slip, 12.5 cm, was on the northern of the three, the Elmore Ranch fault, at a point near the epicenter. Twelve hours after the Elmore Ranch earthquake, the M 6.6 Superstition Hills earthquake occurred near the northwest end of the right-lateral Superstition Hills fault zone. Surface rupture associated with the second event occurred along three strands of the zone, here named North and South strands of the Superstition Hills fault and the Wienert fault, for 27 km southeastward from the epicenter. In contrast to the left-lateral faulting, which remained unchanged throughout the period of investigation, the right-lateral movement on the Superstition hills fault zone continued to increase with time, a behavior that was similar to other recent historical surface ruptures on northwest-trending faults in the Imperial Valley region. We measured displacements over 339 days at as many as 296 sites along the Superstition Hills fault zone, and repeated measurements at 49 sites provided sufficient data to fit with a simple power law. Data for each of the 49 sites were used to compute longitudinal displacement profiles for 1 day and to estimate the final displacement that measured slips will approach asymptotically several years after the earthquakes. The maximum right-lateral slip at 1 day was about 50 cm near the south-central part of the North strand of Superstition Hills fault, and the predicted maximum final displacement is probably about 112 cm at Imler Road near the center of the South strand of the Superstition Hills fault. The overall distributions of right-lateral displacement at 1 day and the estimated final slip are nearly symmetrical about the midpoint of the surface rupture. The average estimated final right-lateral slip for the Superstition Hills fault zone is about 54 cm. The average left-lateral slip for the conjugate faults trending northeastward is about 23 cm. The southernmost ruptured member of the Superstition Hills fault zone, newly named the Wienert fault, extends the known length of the zone by about 4 km. The southern half of this fault, south of New River, expressed only vertical displacement on a sinuous trace. The maximum vertical slip by the end of the observation period there was about 25 cm, but its growth had not ceased. Photolineaments southeast of the end of new surface rupture suggest continuation of the Superstition Hills fault zone in farmland toward Mexico.

scholarly journals Performance of Landscape Roses Grown with Minimal Input in the North-central, Central, and South-central United States

2017 ◽  
Vol 27 (5) ◽  
pp. 718-730 ◽  
Author(s):  
David C. Zlesak ◽  
Randy Nelson ◽  
Derald Harp ◽  
Barbara Villarreal ◽  
Nick Howell ◽  
...  
Keyword(s):  
United States ◽  
National Level ◽  
The United States ◽  
The South ◽  
Flower Number ◽  
North Central ◽  
The North ◽  
South Central ◽  
Central United States ◽  
Plant Hardiness

Landscape roses (Rosa sp.) are popular flowering shrubs. Consumers are less willing or able to maintain landscape beds than in years past and require plants that are not only attractive, but well-adapted to regional climatic conditions, soil types, and disease and pest pressures. Marketing and distribution of rose cultivars occurs on a national level; therefore, it is difficult for U.S. consumers in the U.S. Department of Agriculture (USDA) Plant Hardiness Zones 3 to 5 to identify well-adapted, cold-hardy cultivars. Identifying suitable cultivars that have strong genetic resistance to pests and disease and that will tolerate temperature extremes without winter protection in the USDA Plant Hardiness Zones 3 to 5 is of tremendous value to consumers and retailers in northern states. Twenty landscape rose cultivars, primarily developed in north-central North America, were evaluated at five locations in the United States (three in the north-central United States, one in the central United States, and one in the south-central United States) using the low-input, multiyear Earth-Kind® methodology. Six roses had ≥75% plant survival at the end of the study and were in the top 50% of performers for overall mean horticultural rating at each of the three north-central U.S. sites: ‘Lena’, ‘Frontenac’, ‘Ole’, ‘Polar Joy’, ‘Sunrise Sunset’, and ‘Sven’. Five of these six roses met the same criteria at the central United States (exception ‘Lena’) and the south-central United States (exception ‘Polar Joy’) sites. Cultivar, rating time, and their interaction were highly significant, and block effects were not significant for horticultural rating for all single-site analyses of variance. Significant positive correlations were found between sites for flower number, flower diameter, and overall horticultural rating. Significant negative correlations were found between flower number and diameter within each site and also between black spot (Diplocarpon rosae) lesion size from a previous study and overall horticultural rating for three of the five sites. Cane survival ratings were not significantly correlated with overall horticultural rating, suggesting some cultivars can experience severe winter cane dieback, yet recover and perform well. Data from this study benefit multiple stakeholders, including nurseries, landscapers, and consumers, with evidence-based regional cultivar recommendations and breeders desiring to identify regionally adapted parents.

A new North American chorus frog species (Amphibia: Hylidae: Pseudacris) from the south-central United States

Zootaxa ◽  
2008 ◽  
Vol 1675 (1) ◽  
pp. 1 ◽  
Author(s):  
EMILY MORIARTY LEMMON ◽  
ALAN R. LEMMON ◽  
JOSEPH T. COLLINS ◽  
DAVID C. CANNATELLA
Keyword(s):  
United States ◽  
New Species ◽  
North American ◽  
Advertisement Call ◽  
The South ◽  
The North ◽  
South Central ◽  
Central United States ◽  
Chorus Frog ◽  
Genetic Characters

We describe a new species of chorus frog of the North American treefrog genus Pseudacris from the south-central United States. This new species is morphologically similar to the parapatric species P. feriarum and has thus previously been considered synonymous with this species. The new species is geographically distinct from P. feriarum and from its sister species, P. nigrita. We diagnose the new species based on advertisement call, morphological, and genetic characters.

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.

Archangel in the Margins: St. Michael in the Homilies of Cambridge, Corpus Christi College 41

Traditio ◽  
1998 ◽  
Vol 53 ◽  
pp. 63-91 ◽  
Author(s):  
Richard F. Johnson
Keyword(s):  
Ninth Century ◽  
Devotional Literature ◽  
Anglo Saxon ◽  
The South ◽  
Cambridge University ◽  
Corpus Christi ◽  
University Library ◽  
The North ◽  
Devotional Practices

In the preface to his edition of the ninth-century Book of Cerne (Cambridge, University Library, MS L1. 1.10), A. B. Kuypers notes “two great currents of influence, two distinct spirits, Irish and Roman” at work in the composition of the prayers in this private devotional book. Moreover, Kuypers asserts that “these influences are traceable through the whole range of the strictly devotional literature of the period.” Since it is generally acknowledged that the two great forces shaping the early Anglo-Saxon church were the Roman missionaries in the south and Irish monks in the north, it is reasonable to suspect that the Anglo-Saxon devotional practices to St. Michael the Archangel were also influenced by both traditions.

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