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  • 1
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    Integration and Resettlement of Refugees and Forced Migrants (2021)
    MDPI - Multidisciplinary Digital Publishing Institute
    Details
    Publication Date: 2022-02-01
    Description: Since 2017, the United States and Europe—among many other refugee-hosting countries—have made significant changes in their refugee policies. New visa restrictions, travel bans, and other regulations were imposed by national governments. At the local level, towns and cities responded in different ways: some resisted national policy by declaring themselves “sanctuary cities”, while others supported exclusionary policies. These different responses influenced refugees’ ability to settle and become integrated. The Refugees in Towns (RIT) project at Tufts University explores local urban integration experiences, drawing on the knowledge and perspectives of refugees and citizens in towns around the world. Since 2017, more than 30 RIT case studies have deepened our local knowledge about the factors that enable or obstruct integration, and the ways in which migrants and hosts co-exist, adapt, and struggle with integration. In this Special Issue, seven articles explore urban integration in towns in Europe (Frankfurt-Rödelheim, Germany; Newcastle, UK; Ambertois, France; Italy’s cities; and Belgrade, Serbia) and in North America: Bhutanese refugee-hosting US cities, and Antigonish, Canada. The papers explore how refugees and citizens interact; the role of officials and politicians in enabling or obstructing integration; the social, economic, and cultural impact of migration; and the ways—inclusive or exclusive—locals have responded.
    Keywords: HM401-1281 ; H1-99 ; newcomer ; Italian ; education ; two-way integration ; refugees ; forced migration ; intercultural ; language ; youth ; Bhutanese ; autonomy ; inclusion ; diversity ; physical literacy ; asylum seekers ; local politics ; ecological systems ; participatory action research (PAR) ; austerity ; Frankfurt am Main ; temporary integration ; France ; fragile spaces ; resettlement policy ; recreation ; refugee accommodation ; employment ; social ecological ; neighborhood activism ; municipalities ; resettled refugees ; physical activity ; non-metropolitan areas ; difficulty ; refugee ; community relations ; North East of England ; dispersal policy ; integration ; asylum seeker ; Italy ; local refugee reception ; sport ; Germany
    Language: English
    Format: application/octet-stream
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  • 2
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    Scandinavia: A former Tibet? (2013)
    In:  Geochemistry Geophysics Geosystems (G3)
    Details
    Publication Date: 2020-02-12
    Description: The Himalaya and the Tibetan Plateau are uplifted by the ongoing northward underthrusting of the Indian continental lithosphere below Tibet resulting in lithospheric stacking. The layered structure of the Tibetan upper mantle is imaged by seismic methods, most detailed with the receiver function method. Tibet is considered as a place where the development of a future craton is currently under way. Here we study the upper mantle from Germany to northern Sweden with seismic S receiver functions and compare the structure below Scandinavia with that below Tibet. Below Proterozoic Scandinavia, we found two low-velocity zones on top of each other, separated by a high-velocity zone. The top of the upper low-velocity zone at about 100 km depth extends from Germany to Archaean northern Sweden. It agrees with the lithosphere-asthenosphere boundary (LAB) below Germany and Denmark. Below Sweden it is known as the 8°discontinuity, or as a mid-lithospheric discontinuity (MLD), similar to observations in North America. Seismic tomography places the LAB near 200 km in Scandinavia, which is close to the top of our deeper low-velocity zone. We also observed the bottom of the asthenosphere (the Lehmann discontinuity) deepening from 180 km in Germany to 260 km below Sweden. Remnants of old subduction in the upper about 100 km below Scandinavia and Finland are known from controlled source seismic experiments and local earthquake studies. Recent tomographic studies indicate delamination of the lithosphere below southern Scandinavia and northern Germany. We are suggesting that the large-scale layered structure in the Scandinavian upper mantle may be caused by processes similar to the ongoing lithospheric stacking in Tibet.
    Keywords: 550 - Earth sciences
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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