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Translations:Benutzer:Arian/Klett-Mini-Test/1385/en
Aus BiodynWiki
narrow, thread-like formations that themselves branch only slightly (Figure 27). These gestures of the radiating and the rounding point to features that are characteristic of the wealth of forms in which mineral lime (CaCO3) appears — for instance the radiating character of aragonite, or the spherical and rounded forms of crystalline limes, löss nodules, stalactites, and the like.
