A co-publication of the World Bank, International Finance Corporation and Oxford University Press

An analysis of the influences on urban planning in Europe. Detailed case studies are used to explore planning policies in a range of European cities, and discuss the social and environmental objectives that influence today's urban planner.

This book highlights aspects distinctive to France in economic, social, political and cultural spheres.

Play is one of humanity's straightforward yet deceitful ideas: though the notion is unanimously agreed upon to be universal, used for man and animal alike, nothing defines what all its manifestations share, from childish playtime to on stage drama, from sporting events to market speculation. Within the author's anthropological field of work (Mongolia and Siberia), playing holds a core position: national holidays are called "Games," echoing in that way the circus games in Ancient Rome and today's Olympics. These games convey ethical values and local identity. Roberte Hamayon bases her analysis of the playing spectrum on their scrutiny. Starting from fighting and dancing, encompassing learning, interaction, emotion and strategy, this study heads towards luck and belief as well as the ambiguity of the relation to fiction and reality. It closes by indicating two features of play: its margin and its metaphorical structure. Ultimately revealing its consistency and coherence, the author displays play as a modality of action of its own. "Playing is no 'doing' in the ordinary sense" once wrote Johan Huizinga. Isn't playing doing something else, elswhere and otherwise ?

How well are the French? What are the most important health-related issues for children of under 15 years of age, for young and older adults, for the elderly? What geographically and socially based inequalities affect health status? How can patients and users of the health care system -- members of the public -- be brought into the making of decisions that affect them in this literally vital field? Is our health care system well organised? And is it working in an efficient and democratic way? How are questions of resource allocation settled? This is the third in a series of official reports (the previous ones were published in 1994 and 1998) compiled by the High Committee on Public Health to analyse health status in the country, with an in-depth review of the strengths and weaknesses of the system as a whole. This report combines a critical analysis of the current health care system with a review of key current and projected health-related issues, focusing on public health targets identified from as broad and all-inclusive a perspective as possible.

Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under went, can usually best be determined by straightforward observation in the field.