Synonyms Stones can have many aliases. This is due to language differences, supplier choice, coloquial trends or slang, or sometimes errors and ambiguity between rocks. Read more here. |
Balmoral Red, Finnish Red |
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Category Commercial classification sometimes differs to the scientific, geological designation. In particular, some limestones are deemed marble especially if they take a high polish. Read more here. |
Granite |
Petrographic assignment | Plutonite |
Age | 900 Million years (Pre-Cambrian) |
Colouring minerals: | Red feldspar, brown-grey quartz, black biotite |
Average hardness MOHS is the standard scale of hardness for minerals 1-10, with 10 being the MOHS of diamond. We also use the broad terms Hard and Soft for simplicity. Read more here. |
6 (Hard) |
Origin | Finland |
The images of each stone aim to give a faithful representation of the structure and colouring. The close-ups are generally taken from a sample around 100mm in height to get the detailing of the grain and crystals. The slab images are usually between 2000x1000mm and 3000x1900mm approximately, to give a more overall picture of the pattern.
This is for guidance only, when seeking a specific pattern and colour matching, please obtain a sample or arrange for the slab to be viewed in person. When placing the order, you may require a photo of the actual slab before production, the colour and character can vary significantly even throughout the same block within natural materials. Also monitor calibration, camera settings and lighting can all effect how the materials are perceived.
Two Balmoral types are quarried in the area of Taivassolo-Vehmaa, which only differ in the grain size, Balmoral coarse and Balmoral fine.
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Popular and typical usage
Petrology:A separated, evenly distributed medium to coarse-grained crystal structure. Up to 2cm intense red orthoclase feldspars determine the shade. Consisting of about 15% quartz, the 3-5mm grey-brown crystals make little visual impact. By contrast, the black biotite mica (10-15%) accentuates the homogeneous granular structure.
Petrogenesis:Several granite melts of different composition entered the lower earth crust in the southern Scandinavian area during primeval times of the earth and crystallised over millions of years to medium to coarse hard rocks. Their main components are feldspar, quartz and mica.
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