Vorlanite, (CaU6+)O4, from Jabel Harmun, Palestinian Autonomy, Israel

Vorlanite (CaU6+)O4 Fm3̄m, a = 5.3647(9) Å, V = 154.40(4) Å3, Z = 2 was found in larnite pyrometamorphic rocks of the Hatrurim formation at the Jabel Harmun locality, Judean Desert, Palestinian Autonomy. Vorlanite crystals from these larnite rocks are dark-gray with greenish hue in transmitted light. This color in transmitted light is in contrast to dark-red vorlanite Fm3̄m, a = 5.3813(2) Å, V = 155.834(10)Å3, Z = 2 from the type locality Upper Chegem caldera, Northern Caucasus. Heating above 750 °C of dark-gray vorlanite from the Jabel Harmun, as well as dark-red vorlanite from Caucasus, led to formation of yellow trigonal uranate CaUO4. The unusual color of vorlanite from Jabel Harmun is assumed to be related to small impurities of tetravalent uranium.

Stratigraphic Continuity in 400 Mhz Short-Pulse Radar Profiles of Firn in West Antarctica

We track dated firn horizons within 400 MHz short-pulse radar profiles to find the continuous extent over which they can be used as historical benchmarks to study past accumulation rates in West Antarctica. The 30-40 cm pulse resolution compares with the accumulation rates of most areas. We tracked a particular set that varied from 30 to 90 m in depth over a distance of 600 km. The main limitations to continuity are fading at depth, pinching associated with accumulation rate differences within hills and valleys, and artificial fading caused by stacking along dips. The latter two may be overcome through multi-kilometer distances by matching the relative amplitude and spacing of several close horizons, along with their pulse forms and phases. Modeling of reflections from thin layers suggests that the - 37 to - 50 dB range of reflectivity and the pulse waveforms we observed are caused by the numerous thin ice layers observed in core stratigraphy. Constructive interference between reflections from these close, high-density layers can explain the maintenance of reflective strength throughout the depth of the firn despite the effects of compaction. The continuity suggests that these layers formed throughout West Antarctica and possibly into East Antarctica as well.

The Politics of Local Autonomy: Measuring Cantonal (De)Centralisation in Switzerland

In Switzerland, there are 26 systems of cantonal decentralisation because regulating municipal autonomy is an exclusively cantonal competency. Existing measures of local autonomy/cantonal decentralisation are confined to measuring the real or perceived distribution of functions. Alternatively, they weigh expenditures (Dafflon 1992) or tax revenues (Dlabac and Schaub forthcoming) of municipalities against those of the canton. Complementing these indices, this paper additionally measures the politics dimension of cantonal decentralisation. Seven aspects are measured: intra-cantonal regionalism, cumuldesmandats (double tenure of cantonal MP and mayoral office), territorial quotas for legislative and executive elections, direct local representation and lobbying, party decentralisation, the number and size of constituencies, and direct democracy (communal referendum and initiative). This results in a ranking of all 26 cantons as regards the politics of local autonomy within their political systems. The measure will help scholars to test assumptions held for decentralisation in general, be it as a dependent (explaining decentralisation) or as an independent variable (decentralisation—so what?), within but also beyond the Swiss context.