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. broken pleces of larger crystals. Open Crystallographic Forms Closed Crystallographic Forms Dihedron (2 intersecting planes
The typical shape of a mineral or of aggregates of the same mineral is called the min shown in Fig. 3.6 2. Fibrous, like asbe
or crystal habits shown in Fig. 3.6 do you recognize in the ice 3. Which of the crystal forms shown in Fig. 3.5 crystals?
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Ice crystals are hexa gonal in external habit and during the growth of comes to the needleces site as denopitic pefferen, He

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