It seems possible that the characteristic hydrated minerals of the postulated assemblage would be amphiboles and that the metamorphic grade in the top 20 km of the oceanic mantle might correspond roughly to various subfacies within the amphibolite facies. A convenient name for these hypothetical rock types would be ‘ampholite’ or amphibole-olivine rock.]

Pre-conciliar changes to the horarium or any entrenched practices were often small in scope...

official duties

Cruising in overdrive at legal highway speed keeps rpm right at 1800, depending on rear-axle ratio.