Local Government in a Devolved Scotland
Since the arrival of devolution on the political agenda in the 1970s, there has been an expectation that its introduction would inevitably lead to a reconsideration of the structure and functions of local government (Gunn 1977; Page 1979). Indeed, both the SNP and the Liberals committed themselves in electoral manifestos to transferring functions from local government to a Scottish Parliament, dismantling the big regions, and shaping local authorities around the former district councils. Even after the recent reorganisation, that anticipation of further structural change remains.
The changing roles of local government in education
This article explores the ongoing debate about the changing roles of local government in education in Britain. It focuses on research evidence from Scotland, especially issues associated with devolving management to schools and reorganising local government. These findings are compared with the debate and evidence about the changing role of local government in education in England and Wales during the past decade. It is suggested that while there has been substantial reform of education and local government throughout Britain, the policies have differed in nature and outcomes north and south of the border.
Mesozoic rifting and basin inversion along the northern African Tethyan margin: an overview
Abstract The northern African Tethyan margin registered three major rifting episodes from the latest Palaeozoic-earliest Mesozoic to the earliest Cenozoic. Break-up of Gondwana was initiated in the late Carboniferous. Along the northern African-Arabian plate margin rifting propagated westward from the northeastern Arabian margin to Morocco during the Permian and Triassic, and was accompanied by Mid-Late Triassic-earliest Liassic extensive alkaline flow basalts. Rifting continued during the Liassic, e.g. in the Moghrebian Atlas troughs. A second stage of rifting occurred in the Late Jurassic and continued into, or was rejuvenated during, the Early Cretaceous. Along the east Mediterranean margin, some large E-W trending rifts formed, often with associated volcanism, e.g. southern Sirt and Abu Gharadig. Most researchers believe the oceanization of the eastern Mediterranean basin occurred at this time. Flexural subsidence affected the Moghrebian Atlas, including the Riffian-Tellian domain, where a thick flysch series was deposited. Two short-lived, but widespread and tectonically important, compressional or wrench-dominated events occurred during the Santonian and the latest Maastrichtian. From Morocco to Oman, most sedimentary basins were folded and inverted at these times. The Santonian event resulted from onset of the collision between the African-Arabian and Eurasian plates. New stress-fields favoured NE-SW extension along the African plate margin, generating or rejuvenating some rifts, e.g. in the Euphrates trough and in the Libya-Tunisia region (northwestern Sirt, Pelagian Sea). Rifting and magmatism continued in these regions into the Paleocene. During the Mesozoic, therefore, the northern margin of the African-Arabian plate registered both rifting resulting in the oceanization of the Tethys and rifting resulting from the initiation of the closure of the Tethys. The intraplate domain exhibited echoes of the tectonic events affecting the margin.