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Blueschist on Île de Groix, France Photomicrograph of a thin section of blueschist facies metamorphosed basalt, from Sivrihisar, Turkey. Blueschist (/ ˈ b l uː ʃ ɪ s t /), also called glaucophane schist, is a metavolcanic rock [1] that forms by the metamorphism of basalt and rocks with similar composition at high pressures and low temperatures (200–500 °C (392–932 °F ...
Hint: The first one can be found in the top half of the board. Here are the first two letters for each word: LA. DA. DU. PO. FR. MO. SM. AL (SPANGRAM) NYT Strands Spangram Answer Today.
Eaves of a house in Northern Australia.The white underside would be referred to as a soffit. In this example the soffit is fixed to the slope of the rafters.The dark grey fascia boards form the outer edge and have a groove to receive the soffit lining sheets which cover the rafter tails.
The blueschist metamorphic facies gets its name from abundant blue minerals glaucophane and lawsonite.Glaucophane generally forms in blueschist metamorphic rocks of gabbroic or basaltic composition that are rich in sodium and have experienced low temperature-high pressure metamorphism such as would occur along a subduction zone.
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The pressures exceed those of greenschist, blueschist, amphibolite or granulite facies. Eclogites containing lawsonite (a hydrous calcium-aluminium silicate) are rarely exposed at Earth's surface, although they are predicted from experiments and thermal models to form during normal subduction of oceanic crust at depths between about 45–300 km ...