Salisbury House in London, 1599-1694.: The Strand Palace of Sir Robert Cecil

2009 ◽  
Vol 52 ◽  
pp. 31-78 ◽  
Author(s):  
Manolo Guerci
Keyword(s):  
Residential Area ◽  
Elizabeth I ◽  
Single Family ◽  
The West ◽  
West Side ◽  
James I ◽  
Two Generations ◽  
Architectural Patronage ◽  
Country Houses

Salisbury House is but one example from a significant corpus of architectural patronage carried out by a single family. In two generations, the Cecils created three great ‘prodigy houses’ among a range of notable country houses including Cranborne Manor in Dorset, Pymmes in Hertfordshire, Wothorpe Lodge near Burghley House in Northamptonshire, and Snape Castle in Yorkshire. It was William Cecil, 1st Baron Burghley (1520/21-98), who from the early 1560s initiated this prolific campaign of building with Burghley House in Northamptonshire, Theobalds in Hertfordshire, and Burghley House in London. Both Thomas Cecil (1542-1623) and Robert Cecil (1563-1612) inherited their father’s passion for architecture. Even when Burghley House in the Strand was nearing completion, Thomas continued work on his remarkable Italianate villa in Wimbledon (begun 1588, demolished c. 1720), one of the most innovative houses of the period, with a three-sided plan, built on a steeply sloping hillside that prompted the composition of elaborate terraces. Like the family’s other properties, Wimbledon House was able to offer hospitality to Elizabeth I, while Hatfield House, built by Robert Cecil between 1607 and 1612, was specifically designed to entertain James I and his Queen, Anne of Denmark. In London, Robert Cecil’s architectural patronage started in about 1596 with the improvement and remodelling of Beaufort House in Chelsea, apparently in order to extend his influence into that area, although the scheme was quickly abandoned. Three years later, Robert began Salisbury House in the Strand, while in 1609 he built the first commercial centre in the West End, known as the ‘New Exchange’. From 1612, he also developed a strip of land along the west side of St Martin’s Lane as a new residential area, but did not live to see it completed.

Introduction

2018 ◽  
Author(s):  
Rosamund Oates
Keyword(s):  
Civil Wars ◽  
Pivotal Role ◽  
Elizabeth I ◽  
Henry Viii ◽  
James I ◽  
Protestant Church ◽  
Charles I ◽  
Turbulent Times ◽  
Stuart England ◽  
The Church

Tobie Matthew (c.1544–1628) lived through the most turbulent times of the English Church. Born during the reign of Henry VIII, he saw Edward VI introduce Protestantism, and then watched as Mary I violently reversed her brother’s changes. When Elizabeth I came to the throne in 1558, Matthew rejected his family’s Catholicism to join the fledgling Protestant regime. Over the next sixty years, he helped build a Protestant Church in England under Elizabeth I, James I, and Charles I. Rising through the ranks of the Church, he was Archbishop of York in the charged decades leading up to the British Civil Wars. Here was a man who played a pivotal role in the religious politics of Tudor and Stuart England, and nurtured a powerful strain of Puritanism at the heart of the established Church....

scholarly journals La datation du choeur de l’église de Vaucelles reproduit en plan par Villard de Honnecourt

2018 ◽  
Vol 81 (3) ◽  
pp. 411-417
Author(s):  
Laurence Terrier Aliferis
Keyword(s):  
Nineteenth Century ◽  
Historical Sources ◽  
The West ◽  
West Side ◽  
Villard De Honnecourt ◽  
The Church

Abstract The ruined Cistercian church of Vaucelles is known only by a few preserved fragments and a plan of the choir reproduced by Villard of Honnecourt. Historical sources provide three key dates: 1190 (start of construction), 1215 (entry into the new church), 1235 (date of the dedication). From the nineteenth century until now, it was considered that the foundations were laid in 1190 and that the construction started on the west side of the church. In 1216, the nave would have been completed, and the choir would have been built between 1216 and 1235. Consultation of the historical sources and examination of the historiographic record changes this established chronology of the site. In fact, the construction proceeded from east to west. The choir reproduced in 1216 or shortly before by Villard de Honnecourt presents the building as it then appeared, with the eastern part of the building totally completed.

St Audrie's Bay, Somerset, England: a candidate Global Stratotype Section and Point for the base of the Jurassic System

1994 ◽  
Vol 131 (2) ◽  
pp. 191-200 ◽  
Author(s):  
G. Warrington ◽  
J. C. W. Cope ◽  
H. C. Ivimey-Cook
Keyword(s):  
Type Locality ◽  
International Commission ◽  
The West ◽  
West Side ◽  
Type Area ◽  
Jurassic System ◽  
Stratotype Section

AbstractIn 1967 the Somerset coastline near Watchet was proposed as the type area of the basal (Planorbis) chronozone of the Hettangian Stage and thus of the Jurassic System. Neither at that time nor subsequently, however, has a type locality and section been nominated from those available in the area. There is urgent need to select a Global Stratotype Section and Point (GSSP) for the base of the Hettangian, and of the Jurassic System. The cliff forming the headland at the west side of St Audrie's Bay, three kilometres east of Watchet, Somerset, is here proposed as the type locality and section, with the base of the Hettangian Stage, at the base of the Planorbis Chronozone, being placed at the horizon currently recognized as that at which ammonites of the genus Psiloceras appear. In this section the base of the Planorbis Chronozone corresponds with the base of the Psiloceras planorbis Biozone. The proposal of this section is conditioned by the availability of comprehensive litho- and biostratigraphic information, and the ability of the section to fulfil International Commission on Stratigraphy (ICS) requirements for a candidate GSSP.

Using reflection seismic method to estimate the fluid dynamics parameters related to wakes

2021 ◽  
Author(s):  
Wenhao Fan ◽  
Haibin Song ◽  
Kun Zhang ◽  
Yi Gong ◽  
Shun Yang ◽  
...  
Keyword(s):  
Potential Vorticity ◽  
Negative Potential ◽  
Distribution Area ◽  
The West ◽  
West Side ◽  
Reflection Seismic ◽  
Vorticity Distribution ◽  
Positive Vorticity ◽  
Coherent Vortices ◽  
Survey Line

<p>In this study, when using reflection seismic data to study the wakes of the Batan Islands, a method for estimating the fluid dynamics parameters such as the relative vorticity (relative Rossby number) and the relative potential vorticity is proposed. Although the relative Rossby number estimation method proposed in this study cannot guarantee absolute accuracy in the calculation value, this method is more accurate in describing the positive and negative vorticity distribution for the wakes, and the resolution of the positive and negative vorticity distribution described by this method is higher than the result of the reanalysis data. For the wakes developed in the Batan Islands, the reflection events in the wake development area have the larger inclination than the reflection events in the western Pacific water distribution area. It is also found that the negative vorticity wakes are mainly distributed on the west side of the island/ridge, and the positive vorticity wakes are mainly distributed on the east side of the island/ridge. This is consistent with the understanding of previous wakes simulations. The strong vorticity values in the study area are mainly distributed at depths above 300m, and the maximum impact depth of wakes can reach 600m. At the downstream position of the wake on the survey line 7, it can be seen that the bottom boundary layer has separated, and there is the negative vorticity wakes on the west side intruding into the positive vorticity wakes on the east side , which is presumed to be caused by the disturbance of the small anticyclone existing near the Batan Islands. For the survey line 7, the negative potential vorticity is mainly distributed on the west side of the island/ridge, and the influence range can reach the sea depth of 600m. In the negative potential vorticity region, there is strong energy dissipation and vertical shear. In this study, we don’t find the existence of submesoscale coherent vortices on the survey line 7, but find the reflection structure similar to filaments on the seismic section. Combined with the analysis of the balanced Richardson number angle of survey line 7, we speculate that the wake in the negative potential vorticity distribution area has the characteristics of symmetrical instability, and the symmetrical instability may destroy the process of filaments forming submesoscale coherent vortices.</p>

A Romano-British Interment, with Bucket and Sceptres, from Brough, East Yorkshire

1938 ◽  
Vol 18 (1) ◽  
pp. 68-74 ◽  
Author(s):  
Philip Corder ◽  
I. A. Richmond
Keyword(s):  
Present Note ◽  
Fourth Century ◽  
The Other ◽  
The West ◽  
West Side ◽  
The Road ◽  
The Subject ◽  
Chief Interest ◽  
Roman Age ◽  
The Way

The Roman Ermine Street, having crossed the Humber on the way to York from Lincoln, leaves Brough Haven on its west side, and the little town of Petuaria to the east. For the first half-mile northwards from the Haven its course is not certainly known: then, followed by the modern road, it runs northwards through South Cave towards Market Weighton. In the area thus traversed by the Roman road burials of the Roman age have already been noted in sufficient quantity to suggest an extensive cemetery. The interment which is the subject of the present note was found on 10th October 1936, when men laying pipes at right angles to the modern road, in the carriage-drive of Mr. J. G. Southam, having cut through some 4 ft. of blown sand, came upon a mass of mixed Roman pottery, dating from the late first to the fourth century A.D. Bones of pig, dog, sheep, and ox were also represented. Presently, at a depth of about 5 ft., something attracted closer attention. A layer of thin limestone slabs was found, covering two human skeletons, one lying a few feet from the west margin of the modern road, the other parallel with the road and some 8 ft. from its edge. The objects described below were found with the second skeleton, and the first to be discovered was submitted by Mr. Southam to Mr. T. Sheppard, F.S.A.Scot., Director of the Hull Museums, who visited the site with his staff. All that can be recorded of the circumstances of the discovery is contained in the observations then made, under difficult conditions. ‘Slabs of hard limestone’, it was reported, ‘taken from a local quarry of millepore oolite and forming the original Roman road, were distinctly visible beneath the present roadway—one of the few points where the precise site of the old road has been located. On the side of this… a burial-place has been constructed. What it was like originally it is difficult to say, beyond that a layer of thin … slabs of limestone occurred over the skeletons. This had probably been kept in place or supported by some structure of wood, as several large iron nails, some bent at right angles, were among the bones.’ If this were all that could be said about the burials, they would hardly merit a place in these pages. The chief interest of the record would be its apparent identification of the exact course of the Roman road at a point where this had hitherto been uncertain. Three objects associated with the second skeleton are, however, of exceptional interest.

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