The Misfortunes of William, Fourth Lord Petre (1638–1655)

1971 ◽  
Vol 11 (2) ◽  
pp. 87-116 ◽  
Author(s):  
Christopher Clay
Keyword(s):  
Sixteenth Century ◽  
17Th Century ◽  
The Other ◽  
Total Income ◽  
The West ◽  
The Third ◽  
South West ◽  
Secretary Of State ◽  
The Family ◽  
Large Estate

The Lords Petre were always one of the most prominent of English Catholic families, and they were also one of the richest. Their landed estates had been built up in the middle of the sixteenth century by Sir William Petre, Secretary of State to three Tudor sovereigns. Sir William's son, John, was created a Baron in 1611, but in the early 17th century the family properties ceased to grow in size, partly because Catholicism excluded them from the profits of office, and partly because provision for younger sons offset such new acquisitions as were made. But even so the estates inherited by the third Lord Petre in 1637 were large enough to place him clearly in the ranks of the great landed magnates. In Essex he had a well-consolidated belt of land lying to the west and south-west of Chelmsford, and centred on the two family residences of Ingatestone Hall and Thorndon Hall. Altogether in Essex Petre had about 11,000 acres of freehold land and the lordship of seventeen manors, and these produced some £5,500 per annum or considerably more than half his total income from land. In addition he had a large estate on the opposite side of the country, in Devon. This lay in two distinct areas, one centred on Axminster and extending down the Axe valley and its tributaries, and the other in the southerly projection of the county on the southern edge of Dartmoor, where the principal possession was the vast moorland manor of South Brent. Besides the main estates in Essex and Devon, there were some isolated properties: the manor of Osmington down on the Dorset coast; Toddenham and Sutton in Gloucestershire; Kennett and Kentford on the Cambridgeshire-Suffolk border.

scholarly journals Stratigraphy of the wall paintings in the main church of the Praskvica Monastery

Zograf ◽  
2014 ◽  
pp. 153-163
Author(s):  
Dragan Vojvodic
Keyword(s):  
Seventeenth Century ◽  
Sixteenth Century ◽  
Wall Painting ◽  
The Other ◽  
Stylistic Analysis ◽  
Wall Paintings ◽  
The West ◽  
The Third ◽  
Technical Features ◽  
The Church

In the katholikon of the monastery of Praskvica there are remains of two layers of post-Byzantine wall-painting: the earlier, from the third quarter of the sixteenth century, and later, from the first half of the seventeenth century, which is the conclusion based on stylistic analysis and technical features. The portions of frescoes belonging to one or the other layer can be clearly distinguished from one another and the content of the surviving representations read more thoroughly than before. It seems that the remains of wall-painting on what originally was the west facade of the church also belong to the earlier layer. It is possible that the church was not frescoed in the lifetime of its ktetor, Balsa III Balsic.

An English Library at Trinidad, 1633

1955 ◽  
Vol 12 (1) ◽  
pp. 25-41
Author(s):  
Eleanor B. Adams
Keyword(s):  
Sixteenth Century ◽  
West Indian ◽  
The West ◽  
The Third ◽  
Caribbean Area ◽  
The Caribbean ◽  
El Dorado ◽  
Short Time

The island of Trinidad was discovered by Columbus on the third voyage in 1498. One of the largest and most fertile of the West Indian islands, for many years it remained on the fringe of European activity in the Caribbean area and on the coasts of Venezuela and Guiana. A Spanish settlement was founded there in 1532, but apparently it disintegrated within a short time. Toward the end of the sixteenth century Berrio and Raleigh fought for possession of the island, but chiefly as a convenient base for their rival search for El Dorado, or Manoa, the Golden Man and the mythical city of gold. Throughout the sixteenth and early seventeenth centuries explorers, corsairs, and contraband traders, Spanish, French, English, and Dutch, passed near its shores, and many of them may well have paused there to refresh themselves and to make necessary repairs to their vessels. But the records are scanty and we know little of such events or of the settlements that existed from time to time.

scholarly journals Maciej Ziemierski, Testamenty krakowskiej rodziny Królików z XVII w.

2020 ◽  
Vol 26 ◽  
pp. 11-41
Author(s):  
Maciej Ziemierski
Keyword(s):  
18Th Century ◽  
Family Members ◽  
17Th Century ◽  
16Th Century ◽  
Fourth Generation ◽  
Third Generation ◽  
The Third ◽  
The Family ◽  
The Town ◽  
Distinguished Member

17th century testaments of the Królik family from Krakow The article is dedicated to the Królik family from Krakow, who lived in the town from the late 16th century until the first years of the 18th century. The family members initially worked as tailors, later reinforcing the group of Krakow merchants in the third generation (Maciej Królik). Wojciech Królik – from the fourth generation – was a miner in Olkusz. The text omits the most distinguished member of the family, Wojciech’s oldest brother, the Krakow councillor Mikołaj Królik, whose figure has been covered in a separate work. The work shows the complicated religious relations in the family of non-Catholics, initially highly engaged in the life of the Krakow Congregation, but whose members gradually converted from Evangelism to Catholicism. As a result, Wojciech Królik and his siblings became Catholics. This work is complemented by four testaments of family members, with the first, Jakub Królik’s, being written in 1626 and the last one, Wojciech Królik’s, written in 1691.

scholarly journals Ronald George Hatton,1886-1965

1966 ◽  
Vol 12 ◽  
pp. 250-258 ◽  
Keyword(s):  
Later Life ◽  
The Other ◽  
The South ◽  
Successful Career ◽  
South West ◽  
The Family ◽  
The Law ◽  
Outdoor Pursuits ◽  
To Receive

Ronald George Hatton was a distinguished pomologist, an able administrator and a man who won the affection and esteem of his friends and colleagues alike. Ronald was born on 6 July 1886, in Yorkshire, a county for which he always retained a great affection. He was the youngest child of Ernest Hatton who was a barrister of the Inner Temple. Ronald’s mother was Amy Pearson, a woman of forceful character who came from a similar environment, since she was the daughter of William Pearson, also a barrister, who had taken silk. With such legal forebears on both sides of the family it would scarcely have been surprising if their son had followed the law, but perhaps this hereditary influence manifested itself, in later life, in a marked ability for administration and the handling of finance. But, though Ronald’s ancestry was mainly non-scientific, there was one very distinguished scientist on the mother’s side, namely his uncle, Professor Karl Pearson, F.R.S., the famous statistician and author of The grammar of science . The other members of the family were two sisters. The elder of these, Margerie, followed a successful career as a nurse. She became Matron of the Cottage Hospital at Lyme Regis and, later, for a period of thirteen years till the time of her death, was Matron of the hospital at Teignmouth. The younger sister, Dorothy, studied modern languages at Exeter and was indeed the first woman to receive the Batchelor of Arts Degree from the, then newly established, College of the South-West. She next turned her attention to chemistry, though at this time and subsequently, after her marriage, outdoor pursuits always claimed her great interest.

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).

scholarly journals Contesting “Conversion” and “Reversion” among Young Adult Asian American Buddhists

Religions ◽  
2019 ◽  
Vol 10 (4) ◽  
pp. 261
Author(s):  
Chenxing Han
Keyword(s):  
Young Adults ◽  
Young Adult ◽  
Predominantly White ◽  
Asian American ◽  
Lived Experiences ◽  
The Other ◽  
The West ◽  
Other Hand ◽  
The Family ◽  
The One

This paper engages the perspectives of thirty young adult Asian American Buddhists (YAAABs) raised in non-Buddhist households. Grounded in semi-structured, one-on-one in-person and email interviews, my research reveals the family tensions and challenges of belonging faced by a group straddling multiple religious and cultural worlds. These young adults articulate their alienation from both predominantly white and predominantly Asian Buddhist communities in America. On the one hand, they express ambivalence over adopting the label of “convert” because of its Christian connotations as well as its associations with whiteness in the American Buddhist context. On the other hand, they lack the familiarity with Asian Buddhist cultures experienced by second- or multi-generation YAAABs who grew up in Buddhist families. In their nuanced responses to arguments that (1) American convert Buddhism is a non-Asian phenomenon, and (2) Asians in the West can only “revert” to Buddhism, these young adults assert the plurality and hybridity of their lived experiences as representative of all American Buddhists, rather than incidental characteristics of a fringe group within a white-dominated category.

Human Rights under State Socialism

1984 ◽  
Vol 32 (3) ◽  
pp. 349-368 ◽  
Author(s):  
David Lane
Keyword(s):  
Human Rights ◽  
Interest Groups ◽  
Theory And Practice ◽  
The Other ◽  
The West ◽  
Russian Culture ◽  
Collective Rights ◽  
Normative Approach ◽  
The Third ◽  
The One

The paper is in four parts. The first outlines the debate that has occurred in the West about whether human rights, and about what human rights, are desirable and possible in socialist states. In the second it is contended that the normative approach to rights in socialist states has been influenced but not determined by the theory and practice of the USSR. Human rights under Marxism–Leninism are ambiguously defined: there is an unresolved tension between individual (and group) rights, on the one hand, and class and collective rights on the other. Socialist states, it is claimed, have different units, types of claims and priorities of rights. In the third section, it is argued that the Soviet model of rights has a particular correspondence with Russian culture. Its impact on other socialist countries (Poland is considered, as an illustration) depends on the internal social structure (the strength of interest groups) and the degree of legitimacy of the state. Finally, some prognostications are offered concerning the dynamics and likely developments of rights claims under socialism.

West African Languages Congress

1963 ◽  
Vol 6 (03) ◽  
pp. 30-31
Author(s):  
Joseph Greenberg
Keyword(s):  
Sierra Leone ◽  
The United States ◽  
West African ◽  
Financial Assistance ◽  
The Other ◽  
Substantial Portion ◽  
The West ◽  
African Languages ◽  
The Third ◽  
First Time

The Third West African Languages Congress took place in Freetown, Sierra Leone, from March 26 to April 1, 1963. This was the third of the annual meetings of those interested in West African languages sponsored by the West African Languages Survey, previous meetings having been held in Accra (1961) and Dakar (1962). The West African Languages Survey is a Ford Foundation project. Additional financial assistance from UNESCO and other sources contributed materially to the scope and success of the meeting. This meeting was larger than previous ones both in attendance and in number of papers presented and, it may be said, in regard to the scientific level of the papers presented. The official participants, seventy-two in number, came from virtually every country in West Africa, from Western European countries and from the United States. The linguistic theme of the meeting was the syntax of West African languages, and a substantial portion of the papers presented were on this topic. In addition, there was for the first time at these meetings a symposium on the teaching of English, French and African languages in Africa. The papers of this symposium will be published in the forthcoming series of monographs planned as a supplement to the new Journal of West African Languages. The other papers are to appear in the Journal of African Languages edited by Jack Berry of the School of Oriental and African Studies.

Wanted: A Comparative History of the Modern Mediterranean

2012 ◽  
Vol 46 (1) ◽  
pp. 47-53
Author(s):  
Edmund Burke
Keyword(s):  
Sixteenth Century ◽  
Third World ◽  
Dominant Role ◽  
The West ◽  
The Third ◽  
History Of ◽  
The Mediterranean ◽  
The Third World

There is something seriously flawed about models of social change that posit the dominant role of in-built civilizational motors. While “the rise of the West” makes great ideology, it is poor history. Like Jared Diamond, I believe that we need to situate the fate of nations in a long-term ecohistorical context. Unlike Diamond, I believe that the ways (and the sequences) in which things happened mattered deeply to what came next. The Mediterranean is a particularly useful case in this light. No longer a center of progress after the sixteenth century, the decline of the Mediterranean is usually ascribed to its inherent cultural deficiencies. While the specific cultural infirmity varies with the historian (amoral familism, patron/clientalism, and religion are some of the favorites) its civilizationalist presuppositions are clear. In this respect the search for “what went wrong” typifies national histories across the region and prefigures the fate of the Third World.

scholarly journals XI.—Notes on the Geology of the Eildon Hills, in Roxburghshire

1853 ◽  
Vol 20 (2) ◽  
pp. 211-217
Author(s):  
James D. Forbes
Keyword(s):  
Small Group ◽  
The Other ◽  
Careful Examination ◽  
Eastern Slope ◽  
The West ◽  
North East ◽  
The North ◽  
South West ◽  
North Bank ◽  
The Town

The following remarks, being the result of a careful examination of a small district of country characteristic of the relations of the trap formations, are perhaps worthy of being recorded; although the general features of the county of Roxburgh have been very clearly stated in a paper by Mr Milne, published in the 15th volume of the Edinburgh Transactions.The outburst of porphyritic trap forming the conspicuous small group of the Eildon Hills, may be stated to be surrounded by the characteristic greywacke of the south of Scotland. It forms an elongated patch on the map, extending from the west end of Bowden Muir in the direction of the town of Selkirk, and running from west-south-west to east-north-east (true) towards Bemerside Hill, on the north bank of the Tweed. The breadth is variable, probably less than is generally supposed; but it cannot be accurately ascertained, owing to the accumulated diluvium which covers the whole south-eastern slope of this elevated ridge. On this account, my observations on the contact of rocks have been almost entirely confined to the northern and western boundaries of the trap, although the other side was examined with equal care.

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