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2. 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.

3. Serpentine subgroup - Wikipedia

   en.wikipedia.org/wiki/Serpentine_subgroup

   The name comes from the greenish color and smooth or scaly appearance from the Latin serpentinus, meaning "snake-like". Serpentine subgroup is a set of common rock-forming hydrous magnesium iron phyllosilicate ((Mg,Fe) 3 Si 2 O 5 4) minerals, resulting from the metamorphism of the minerals that are contained in mafic to ultramafic rocks. [6]

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5. Granite - Wikipedia

   en.wikipedia.org/wiki/Granite

   Granite (/ ˈ ɡ r æ n ɪ t / GRAN-it) is a coarse-grained intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase.It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground.

6. Barnenez - Wikipedia

   en.wikipedia.org/wiki/Barnenez

   They are built of large slabs of slate and granite. Originally, all the chambers were entirely enclosed by the mound. The fact that several of them are partially exposed now is the result of modern quarrying. Each of the 11 chambers is reached from the southeast via a long narrow passage (7–12 m long). They are arranged parallel to each other.

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