Swiss Shock: Minaret Rejection, European Values, and the Challenge of Tolerant neutrality

In 2009 Switzerland, for long an apparent beacon of European toleration and neutrality, voted to ban the erection of minarets. Internal religious matters are normally dealt with at the regional or local level – not at the level of the Swiss national parliament, although the state does seek to ensure good order and peaceful relations between different faith communities. Indeed, the freedom of these communities to believe and function publicly is enshrined in law. However, as a matter of national policy, now constitutionally embedded, one religious group, the Muslim group, is not permitted to build their distinctive religious edifice, the minaret. Switzerland may have joined the rest of Europe with respect to engaging the challenge of Islamic presence to European identity and values, but the rejection of a symbol of the presence of one faith – in this case, Islamic – by a society that is otherwise predominantly secular, pluralist, and of Christian heritage, poses significant concerns. How and why did this happen? What are the implications? This paper will discuss some of the issues involved, concluding the ban is by no means irreversible. Tolerant neutrality may yet again be a leitmotif of Swiss culture and not just of foreign policy.

Reactive mass transport modelling of a three-dimensional vertical fault zone with a finger-like convective flow regime

For a three-dimensional vertically-oriented fault zone, we consider the coupled effects of fluid flow, heat transfer and reactive mass transport, to investigate the patterns of fluid flow, temperature distribution, mineral alteration and chemically induced porosity changes. We show, analytically and numerically, that finger-like convection patterns can arise in a vertically-oriented fault zone. The onset and patterns of convective fluid flow are controlled by the Rayleigh number which is a function of the thermal properties of the fluid and the rock, the vertical temperature gradient, and the height and the permeability of the fault zone. Vigorous fluid flow causes low temperature gradients over a large region of the fault zone. In such a case, flow across lithological interfaces becomes the most important mechanism for the formation of sharp chemical reaction fronts. The degree of rock buffering, the extent and intensity of alteration, the alteration mineralogy and in some cases the formation of ore deposits are controlled by the magnitude of the flow velocity across these compositional interfaces in the rock. This indicates that alteration patterns along compositional boundaries in the rock may provide some insights into the convection pattern. The advective mass and heat exchanges between the fault zone and the wallrock depend on the permeability contrast between the fault zone and the wallrock. A high permeability contrast promotes focussed convective flow within the fault zone and diffusive exchange of heat and chemical reactants between the fault zone and the wallrock. However, a more gradual permeability change may lead to a regional-scale convective flow system where the flow pattern in the fault affects large-scale fluid flow, mass transport and chemical alteration in the wallrocks