Secondary minerals are recrystallized products of the chemical breakdown and/or alteration of primary minerals.

Name: Secondary minerals are recrystallized products of the chemical breakdown and/or alteration of primary minerals.
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Secondary minerals are formed through the alteration or breakdown of primary minerals, resulting in the formation of new minerals with different chemical compositions and crystal structures. Examples of secondary minerals include chlorite, epidote, and calcite.

Secondary Minerals Are Recrystallized Products of the Chemical Breakdown And/or