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  2. Amphibolite - Wikipedia

    en.wikipedia.org/wiki/Amphibolite

    Amphibolite from Cape Cod, Massachusetts Garnet bearing amphibolite from Val di Fleres, Italy. Amphibolite (/ æ m ˈ f ɪ b ə l aɪ t /) is a metamorphic rock that contains amphibole, especially hornblende and actinolite, as well as plagioclase feldspar, but with little or no quartz.

  3. Metamorphic facies - Wikipedia

    en.wikipedia.org/wiki/Metamorphic_facies

    The amphibolite facies is a facies of medium pressure and average to high temperature. It is named after amphiboles that form under such circumstances. It has the following mineral assemblages: In metabasites: hornblende + plagioclase ± epidote, garnet, cummingtonite, diopside, biotite; In metapelites:

  4. Metamorphism - Wikipedia

    en.wikipedia.org/wiki/Metamorphism

    The facies are named after the metamorphic rock formed under those facies conditions from basalt. [79] The particular mineral assemblage is somewhat dependent on the composition of that protolith, so that (for example) the amphibolite facies of a marble will not be identical with the amphibolite facies of a pellite.

  5. Gore Mountain Garnet - Wikipedia

    en.wikipedia.org/wiki/Gore_Mountain_Garnet

    Gore Mountain Garnet, found in the Adirondack Mountains in New York, contains the world's largest garnets. [1] [2] The rock that holds these garnets, garnet amphibolite, is sometimes referred to as 'black ore' or 'dark ore.' [1] [3] This rock formation formed during metamorphism during the Ottawan phase of the Grenvillian orogeny, and extremely high temperatures combined with introduction of ...

  6. Shield (geology) - Wikipedia

    en.wikipedia.org/wiki/Shield_(Geology)

    Shields can be very complex: they consist of vast areas of granitic or granodioritic gneisses, usually of tonalitic composition, and they also contain belts of sedimentary rocks, often surrounded by low-grade volcano-sedimentary sequences, or greenstone belts. These rocks are frequently metamorphosed greenschist, amphibolite, and granulite facies.

  7. Gneiss - Wikipedia

    en.wikipedia.org/wiki/Gneiss

    The greenstone belts are surrounded by high-grade gneiss terrains showing highly deformed low-pressure, high-temperature (over 500 °C (932 °F)) metamorphism to the amphibolite or granulite facies. These form most of the exposed rock in Archean cratons .

  8. 'I thought I was done for': Watch video of humpback whale ...

    www.aol.com/thought-done-watch-video-humpback...

    Watch video of whale 'swallowing' kayaker. Simancas was unharmed in the incident, which was caught on video by his father in another kayak. "I turned on the camera and heard a wave crash behind me ...

  9. Petrogenetic grid - Wikipedia

    en.wikipedia.org/wiki/Petrogenetic_grid

    Figure 1. Petrogenetic grid for metapelites (several authors). [1] [2] Metamorphic facies included are: BS = Blueschist facies, EC = Eclogite facies, PP = Prehnite-Pumpellyite facies, GS = Granulite facies, EA = Epidote-Amphibolite facies, AM = Amphibolite facies, GRA = Granulite facies, UHT = Ultra-High Temperature facies, HAE = Hornfels-Albite-Epidote facies, Hbl = Hornblende-Hornfels facies ...