FUCK YEAH MINERALOGY
A blog dedicated to minerals of all sorts.

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Hemimorphite is the most common mineral in the rhombic-pyramidal class, which has two perpendicular mirror planes and one 2-fold rotation axis (1A2, 2m). (Source: Tulane University)
  1. Hemimorphite is the most common mineral in the rhombic-pyramidal class, which has two perpendicular mirror planes and one 2-fold rotation axis (1A2, 2m). (Source: Tulane University)

  1. 18 notesTimestamp: Sunday 2013/01/13 12:01:38Source: rockhoundblog.commineralogymineralscrystalcrystalshemimorphitecrystal classcrystal classesrhombic-pyramidalmirror planesrotational symmetrygeology
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