Large Botryoidal Clinochlore (Seraphinite) Specimen
Approx. Dimensions: 6x3.5x2.5 inches
Approx. Weight: 712 grams
Locality: Korshunovskiy Mine, Irkutskaya Oblast, Russia
From the Korshunovskiy Mine, this specimen of clinochlore (seraphinite) is a wonderful example of how this material forms. Featuring several large botryoidal formations that have been fractured, you can see the radiating pattern of clinochlore crystals from their centers. Acrylic stand is not included.
Clinochlore is a green-colored mineral belonging to the chlorite group, a subset of phyllosilicates. It forms in metamorphic environments, particularly in regions with low-grade metamorphism, such as shale and slate deposits. Historically, clinochlore has been recognized and used in various applications, including as a decorative stone and for its perceived healing properties. Chemically, clinochlore is a hydrated magnesium iron aluminum silicate, with a complex composition that may include other elements such as chromium and manganese. It exhibits a foliated or scaly texture and a hardness ranging from 2 to 2.5 on the Mohs scale. Clinochlore's green coloration is attributed to its iron content, and it often occurs as aggregates or masses rather than individual crystals. The mineral's association with serpentine and talc makes it a valuable indicator of certain geological environments and processes.
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