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As Poles like to say: the situation is critical but not serious. The project is far too important to be denied by the ballot box.")Juncker is becoming a bit of a poster-boy for what's wrong with the European project as currently envisaged, having also made a guest appearance in the latest "If at the end of the ratification process, we do not manage to solve the problems, the countries that would have said No, would have to ask themselves the question again," "President" Juncker told the Belgian newspaper Le Soir. You have the right to vote, but only if you give the answer your rulers want you to give.But don't worry, if you don't, we'll treat you like a particularly backward nursery school and keep asking the question until you get the answer right.

the European Union constitution on Sunday, pitching the EU into crisis and dealing a potentially fatal blow to a charter designed to make the enlarged bloc run smoothly...

Chirac swiftly conceded defeat in a televised address to the nation as the "No" camp celebrated a crushing victory with about 55 percent of votes to 45 percent.

The problem is that it has never been "the people" who had plunged Europe into conflict but their rulers, so transferring more power to increasingly less accountable politicians doesn't seem like the best solution to the problem, even if those politicians like to think of themselves as our virtuous betters.

The Mt Somers Volcanics are part of a suite of mid-Cretaceous (89 ± 2 Ma) intermediate to silicic volcanics, erupted onto an eroded surface of Torlesse sediments.

Inclusions of this most important group are generally situated on planar elements.

High-density (Type 2) and low-density (Type 3) inclusions occur isolated in coarse unshocked quartz grains (without planar elements), in post-shock recrystallized quartz grains and in mafic minerals apparently unaffected by the shock event.The fact that fluid inclusions are situated on planar elements indicates that the CO gas must have been available immediately after the shock event.Measurements of the homogenization temperatures of the fluid inclusions in samples from the Vredefort basement allow subdivision of the CO.Type-2 inclusions with densities of about 0.9 g/cm are believed to belong to an early generation which was formed during the granulite-facies metamorphism predating the static high-temperature Vredefort metamorphism.Low-density inclusions of Type 3 homogenizing to the gaseous state could be explained as a very late generation of inclusions formed under near-surface conditions.The chemical variation displayed by the rhyolites is best explained by fractional crystallization of the observed high-pressure phenocryst assemblage.

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