TERRIUM — A mineralogy cabinet


Okenita

Okenita is a mineral with formula Ca₅Si₉O₂₃·9H₂O, in the Filosilicatos group. This specimen comes from Malad Quarry, Mumbai Suburban District, Konkan, Maharashtra, India.

Okenita from Malad Quarry, Mumbai Suburban District, Konkan, Maharashtra, India — Terrium

Description

Single, minute spherical aggregate of white acicular crystals with cottony appearance and silky lustre, on matrix.

History of this specimen

This is an specimen from the classic Malad Quarry in Mumbai, now closed. A locality famed for cavities in the Deccan basalts, where okenite formed with zeolites and prehnite.

About Okenita

It resembles a ball of cotton wool, but it is made of thousands of very fragile microscopic needles. It is a secondary mineral occurring in cavities of volcanic rocks, especially in the Deccan basalts of India. Okenite forms at low temperature under specific conditions of moisture and internal chemistry. Its delicate appearance contrasts with the harsh environment in which it forms, and specimens are much prized by collectors.

About the locality

For decades the basalt cavities at Malad yielded fine okenite specimens. The quarry is now closed, and available pieces come from old material, so they are increasingly valued.

Technical data

Catalogue No.
0420
Internal reference
T0027
Composition
Ca₅Si₉O₂₃·9H₂O
Name
Okenita
Group
Filosilicatos
Category
Asteris Explosio
Mine
Malad Quarry
District / Municipality
Mumbai Suburban District
Province
Konkan
Region
Maharashtra
Country
India
Size (cm)
1 x 1 x 1
Weight
4.5 g
Etymology
Okenite is named in honour of the German naturalist Lorenz Oken (1779–1851) for his contribution to nineteenth-century science. It was first described in 1828.
Quality
Buena
Value trend
Estable

Related specimens

← Back to Terrium catalogue