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  2. Connemara marble - Wikipedia

    en.wikipedia.org/wiki/Connemara_marble

    The distinct green colour of the middle slab is a result of an abundance of serpentine minerals Connemara marble ornament, Museum Building, Trinity College Dublin. Connemara marble or "Irish green" is a rare variety of green marble from Connemara, Ireland. It is used as a decoration and building material.

  3. Serpentine subgroup - Wikipedia

    en.wikipedia.org/wiki/Serpentine_subgroup

    Colors range from white to grey, yellow to green, and brown to black, and are often splotchy or veined. Many are intergrown with other minerals, such as calcite and dolomite . The basic structural unit of serpentine is a polar layer 0.72 nm thick.

  4. Unakite - Wikipedia

    en.wikipedia.org/wiki/Unakite

    Granite: Unakite is a metamorphic rock that is altered granite composed of pink orthoclase feldspar, green epidote, and generally colorless quartz. Discovery

  5. Decomposed granite - Wikipedia

    en.wikipedia.org/wiki/Decomposed_granite

    Decomposed granite is a kind of granite rock that is weathered to the point that the parent material readily fractures into smaller pieces of weaker rock. Further weathering yields material that easily crumbles into mixtures of gravel -sized particles known as grus that further may break down to produce a mixture of clay and silica sand or silt ...

  6. Rapakivi granite - Wikipedia

    en.wikipedia.org/wiki/Rapakivi_granite

    Eroded rapakivi granite in Finland. Rapakivi is a fairly uncommon type of granite, but has been described from localities in North and South America (Illescas Batholith, Uruguay, [5] Rondônia, Brazil [6]) parts of the Baltic Shield, southern Greenland, southern Africa, India and China.

  7. Forbach Granite - Wikipedia

    en.wikipedia.org/wiki/Forbach_Granite

    Forbach Granite (German: Forbachgranit), also called Raumünzach Granite (Raumünzach-Granit), is a type of granite rock that occurs in the Northern Black Forest. It is part of the Northern Black Forest's granitic massif, to which Bühlertal granite and Wildbad granite also belong.