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  • Not in my backyard ! Sports stadia location and the property market
  • How green is my valley? Desktop geographic information systems as a community-based participatory mapping tool
  • Uplift deduced from remanent magnetism Sudbury area since 1250 My
  • The analysis and interpretation of pre-Brunhes (>.73 -.79 my) glacial landforms in the Nithi River Basin, on the eastern flank of Mount Kenya, provide evidence for the dynamics of early Quaternary ice. - (L'A.).
  • Conscious of the University of Kiel's motto of Pax optima a rerum, my aim in this fairly non technical addron is to overview the world's situation with regard to population, resources and food : where we are, how we got there and where we might
  • and alluvial deposits at Perrier Plateau and surroundings is presented correlatively with new K/Ar measurements. Precisions are given concerning faunas from Roca Neyra and Pardines (< 2.4 My), and from Champeix ( 0.8 My). These new data allow to point out
  • the fauna from Perrier-Etonaires at 2.6-2.5 My. This questions the lower limit of villafranchian stage.
  • are used to estimate mean erosion rates for the 3 periods (16 to 13 My, 13 o 8 My, and following 8 My). The landscape of the Huasco Valley is in a transient state, as indicated by well-preserved pediment surfaces in interfluves, valleys deeply incised
  • of the Quaternary is set at the top of the Olduvai event at 1.7 my. Four FADs, twelve LADs, two acme datums, and one ratio reversal datum occur above the base of the Quaternary at an average rate of about 1 per 100,000 yr. Five FADs and twelve LADs are recognized
  • in the 0.8 my interval between the top of the Olduvai event and the Gauss/Matuyama boundary at 2.5 my at an average incidence of about 1 per 50,000 yr.
  • obvious comparison is with the more general gamma distribution: although fitting is technically more awkward, methods publicised here allow estimation of parameters by maximum likelihood and computations for probably plots. The exponential my be a good
  • and by applying a new method, which calculates the amount of retreat from the width of beheaded valleys of known age. Rates of retreat range from 0.5 to 6.7 km/my. The results show that the rates of retreat are controlled by the thickness and resistance
  • ‘I wanted my child to go to a more mixed school’ : schooling and ethnic mix in East London
  • I don't like my children to grow up in this bad area : parental anxieties about living in informal settlements
  • The Postmodern Life of My Aunt - A chronotope of postocialist China
  • Movement is a constant feature in my life : contextualising migration processes of highly skilled Indians
  • 'It is my home. I will die here : tourism development and the politics of place in Lijiang, China
  • My garden is a great help” : gender and urban gardening in Buea, Cameroon
  • My Space/Mi Espacio: Evangelical Christianity and Identity Politics in Mexico
  • For my children : different functions of the agricultural landscape and attitudes of farmers on different areas of Greece towards small scale landscape change
  • ‘How dare you say that about my friend’: negotiating disability and identity within Australian high schools