Revised Criteria and Procedures for the Establishment of New Primary Schools - Report of the Commission on School Accommodation

Part One explores the background factors relating to new school establishment, outlines the views received as a result of consultation with the public and the New Schools Advisory Committee (NSAC) and reviews international practice in relation to establishment of new schools. The population of the country experienced an unprecedented increase in the past ten years. Despite the current economic downturn, the effect of this recent population increase is that growth in demand for school places is set to increase over the short to medium term. The overriding objective is to ensure that a school place is available to every child. Part Two explores issues around planning for new schools in the future. It discusses patron selection, the mechanism for identifying the need for a new school and proposals for cost effectiveness, including campus arrangements. A school is of central importance to a local community and therefore the establishment of a new school must be carried out with reference to the overall plan of the local authority for any given area. Guidelines published under Section 28 of the Planning Act entitled “The Provision of Schools and the Planning System” (July 2008) establish a 7 framework for co-operation between the Department and planning authorities to ensure the timely and cost-effective provision of school facilities.

Emulador del Microcontrolador : Texas Instruments MSP430

Implementació d'un emulador del microcontrolador MSP430 de Texas Instruments. S'implementa l'emulació no només de la CPU, sinó també d'una part dels mòduls i els perifèrics integrats en el microcontrolador.

Biotic effects of the Chicxulub impact, K-T catastrophe and sea level change in Texas

Biotic effects of the Chicxulub impact, the K-T event and sea level change upon planktic foraminifera were evaluated in a new core and outcrops along the Brazos River, Texas, about 1000 km from the Chicxulub impact crater on Yucatan, Mexico. Sediment deposition occurred in a middle neritic environment that shallowed to inner neritic depths near the end of the Maastrichtian. The sea level fall scoured submarine channels, which were infilled by a sandstone complex with reworked Chicxulub impact spherules and clasts with spherules near the base. The original Chicxulub impact ejecta layer was discovered 45-60 cm below the sandstone complex, and predates the K-T mass extinction by about 300,000 years. Results show that the Chicxulub impact caused no species extinctions or any other significant biotic effects. The subsequent sea level fall to inner neritic depth resulted in the disappearance of all larger (>150 mu m) deeper dwelling species creating a pseudo-mass extinction and a survivor assemblage of small surface dwellers and low oxygen tolerant taxa. The K-T boundary and mass extinction was identified 40-80 cm above the sandstone complex where all but some heterohelicids, hedbergellids and the disaster opportunistic guembelitfids went extinct, coincident with the evolution of first Danian species and the global delta(13)C shift. These data reveal that sea level changes profoundly influenced marine assemblages in near shore environments, that the Chicxulub impact and K-T mass extinction are two separate and unrelated events, and that the biotic effects of this impact have been vastly overestimated. (C) 2008 Elsevier B.V. All rights reserved.

Iowa Transportation Map, 2004

State of Iowa transportation road map produced by the Department of Transportation.

From deep seated slope deformation to rock avalanche: Destabilization and transportation models of the Sierre landslide (Switzerland)

Sackung is a widespread post-glacial morphological feature affecting Alpine mountains and creating characteristic geomorphological expression that can be detected from topography. Over long time evolution, internal deformation can lead to the formation of rapidly moving phenomena such as a rock-slide or rock avalanche. In this study, a detailed description of the Sierre rock-avalanche (SW Switzerland) is presented. This convex-shaped postglacial instability is one of the larger rock-avalanche in the Alps, involving more than 1.5 billion m3 with a run-out distance of about 14 km and extremely low Fahrböschung angle. This study presents comprehensive analyses of the structural and geological characteristics leading to the development of the Sierre rock-avalanche. In particular, by combining field observations, digital elevation model analyses and numerical modelling, the strong influence of both ductile and brittle tectonic structures on the failure mechanism and on the failure surface geometry is highlighted. The detection of pre-failure deformation indicates that the development of the rock avalanche corresponds to the last evolutionary stage of a pre-existing deep seated gravitational slope instability. These analyses accompanied by the dating and the characterization of rock avalanche deposits, allow the proposal of a destabilization model that clarifies the different phases leading to the development of the Sierre rock avalanche.