Churches and the Governing of Schools in Northern Ireland: A Redistribution of Power?

This paper presents findings of research into the role of church nominees on school governing bodies. The data is drawn mainly from a wider study of school ethos and school governance undertaken in Northern Ireland in the period 1994 to 1997. The paper raises the question of the future roles and responsibilities of church nominees after legislative changes to the composition and responsibilities of school governing bodies. It also considers recent social and attitudinal change and explains how the combination of these factors have created a situation whereby the power of the churches in the individual school governing body is no longer guaranteed

Understanding leadership in local churches

A sociological examination of the concept of leadership and its application to understanding social interactions and power relations in local churches, based upon ethnographic investigation into London Methodist churches.

Review of Protestant Churches and the Formation of Political Consciousness in Southern Mozambique (1930–1974).

Book review of Protestant Churches and the Formation of Political Consciousness in Southern Mozambique (1930–1974). By TERESA CRUZ E SILVA. Introduction by DAVID HEDGES. Basel: P. Schlettwein Publishing, 2001. Pp. xvii+210. CHF 48; €32 (ISBN 3-908193-09-5).

Labour and the free churches 1918-1939: radicalism, righteousness and religion

It is a commonplace that the labour movement was somehow nurtured within the witness for liberty of the Free Churches. Exploring this at a range of levels - including organisation, rhetoric, policies, electoral politics and people - this book demonstrates the extent to which this remained a reality into the inter-war years. The distinctive religious setting in which it emerged indeed helps to explain the differences between Labour and more Marxist counterparts on the Continent. It is shown here that this setting continued to influence Labour approaches towards welfare, nationalisation and industrial relations between the wars. In the process Labour also adopted some of the righteousness of tone of the Free Churches. This setting was, however, changing. Dropping their traditional suspicion of the State, Nonconformists instead increasingly invested it with religious values, turning it through its growing welfare functions into the provider of practical Christianity. This nationalisation of religion continues to shape British attitudes to the welfare state as well as imposing narrowly utilitarian and material tests of relevance upon the churches and other social institutions. The elevation of the State was not, however, intended as an end in itself. What mattered were the social and individual outcomes. Socialism, for those Free Churchmen and women who helped to shape Labour in the early twentieth century, was about improving society as much as systems.

Morality and politics: the free churches and the Labour Party between the wars

The inter-war period saw the decline of the Liberal party, the traditional political ally of the free churches, and the rise of the Labour party. This article traces the responses of the free churches to these developments. The relationship of the free churches with the Labour party in this period is examined at three different levels; that of the free church leadership, that of the chapels and the ordinary people in the pews and that of the nonconformists who became active in the Labour party. Whilst attitudes towards the Labour party changed within free church institutions during the inter-war years they did not become important supporters of the party, or greatly influence it. The number and proportion of individual nonconformists who were active and influential in the party in this period was however considerable. In the process not only did Labour M.P.s become the main carriers of the nonconformist conscience on issues such as drink and gambling. They also made a distinctive and important contribution to the development and ideals of the Labour party.

Petrography and geochemistry of the McArthur Township area, Ontario /

The McArthur Township area in the Archean Abitibi Belt of northeast Ontario contains northwesterly trending volcanic rocks which are located on a limb of a large syncline. The axial trace of the syncline passes through the adjacent Douglas Township. The Archean volcanic rocks and associated sedimentary rocks are intruded and deformed by two large plutons and a few smaller hypabyssal intrusions. A petrographic and geochemical study of the Precambrian rocks exposed 1n the study area was undertaken in order to investigate the metamorphic grade and geochemical characteristics of the rocks. All the samples were studied with the microscope and analysis of 20 major and trace elements were determined on a selection of the less altered specimens by x-ray fluorescence. Three different periods of igneous activity have occurred in the study area. The first two periods were dominated by volcanic extrusive rocks accompanied by gabbroic sills. The third cycle is the diapiric intrusion of the granitic plutons and subsequent metamorphism of the older rocks to the low to medium grade. Two periods of sedimentation are also recognized in the study area which occurred after the first and second cycle of volcanism. Chemically, the lavas are subdivided into three main associations: (1) The komatiitic association is characterized by high MgO, high Ni, low Ti02 and a low FeO*/(FeO* + MgO) ratio. They occupy the base of each volcanic cycle and some of the flows exhibit spinifex textures. (2) The tholeiitic association displays distinct iron and titanium enrichment trends in the intermediate membersor -i r (3) The calc-alkaline association contains low FeO* and TI02 and high Ni contents relative to modern calc-alkaline types. They are formed at the end of each cycle of volcanism and overlie the tholeiitic flows. All three associations of the first volcanic cycle are exposed in the study area, while the second cycle is represented by a komatiltic sequence. The volcanic rocks were possibly formed by multiple partial melting of the Archean mantle to produce parental magmas under various P - T conditions.