The statement thatthe angles between congruent crystal faces on samples of a single mineralare always identical. A consequence of, and therefore evidence for theexistence of crystalline structure in minerals.
Trouvé sur https://www.encyclopedie.fr/local/298
Aucun résultat n’a été trouvé dans l’encyclopédie.
The statement thatthe angles between congruent crystal faces on samples of a single mineralare always identical. A consequence of, and therefore evidence for theexistence of crystalline structure in minerals.