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Camblorite

@camblorite

I'm studying Geology at university and doing a undergraduate research in igneous petrology.
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Rock Fact #1: The most common mineral in the earths crust isn’t quartz, but feldspar! When you look at a granite it’s the pink and white stuff.

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Erythrites

Erythrite (Co3(AsO4)2.8H2O) is a mineral of the Vivianite group and it occurs as a product of the oxidation of Co-Ni-As minerals. The pink color is due to the presence of cobalt.

  1. Erythrite from Mont Cobalt, Queensland, Australia.
  2. Erythrite with Skutterudite from Longotoma, Aconcagua, Chile.
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m1male2

The Chauvet cave, France, the art of prehistory.

In 1994, three friends discovered in the south of France a cave with magnificent cave paintings, more than 30,000 years old.

Under the ground of the Ardèche region, an invaluable treasure is hidden for its antiquity, its conservation and the pictorial quality of the representations; one of the oldest and most splendid examples of Arieñaciense parietal art, dating approx. between 40,000 and 30,000 B.C.

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Diopsides

Diopsides from Canastra 1, Minas Gerais, Brazil.

Diopside (CaMgSi2O6) is a mineral of the pyroxene group and it's commonly found in metamorphic rocks. It forms a complete solid solution series with hedenbergite (CaFeSi2O6).

Sources:
Klein, C., Hurlbut, C. S., & Dana, J. D. (1999). Manual of mineralogy: (after James D. Dana) (21st ed. rev., pp. 481-482). Wiley.
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Lamproite with crustal xenolith (the lighter zone), from Murfreesboro, Arkansas, USA.

Lamproite is a potassic to ultramafic, dark-colored igneous rock group.

Xenoliths are rock fragments carried by igneous rocks. They are older and from a different source than the igneous rocks that contain them.

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