TOBERMORITE Mineral Details

Complete mineralogical data for TOBERMORITE. Chemical Formula: Ca4[Si6O17](H2O)2·Ca·3H2O. Crystal System: Monoclinic. Learn about its geologic occurrence, habit, and identification.

TOBERMORITE

Ca4[Si6O17](H2O)2·Ca·3H2O

Crystal System

Monoclinic

Crystal Class

Domatic

Space Group

Bm

Point Group

m

Structure & Data

Crystal Structure

Inosilicates: tetrahedra form chains of infinite length with 3-periodic single & multiple chains; has 3-periodic single chains // [010], as in wollastonite.2 Layers formed by linking of xonolite strips, which during condensation at 2 levels overlap somewhat, radical taking formula [Si12O31]; btw layers lie Ca & H2O; number of latter changes stepwise, which causes appreciable increase in c parameter.3 Layers || to (001), formed by [7] coordniated Ca polyhedra; tetrahedral double chains, built up thru condensation of “Dreiereinfachketten” of wollastonite type & running along b, link together adjacent Ca layers in clinotobermorite & tobermorite 11 Å, whereas single tetrahedral chains connect adjacent Ca layers in tobermorite 9 Å; relatively wide channels of clinotobermorite & tobermorite 11 Å host “zeolitic” Ca cations & H2O molecules.4 Common structural feature of polytype 11 Å are infinite layers of Ca polyhedra, || (001), with tetrahedral chains of wollastonite-type running along b & attached on both sides of these layers; composite layers stacked along c & connected thru formation of double tetrahedral chains, with ‘ideal’ composition [Si6O15(OH)2] & [Si6O16(OH)]; most distinctive feature is content of structural cavities.5

Cell Data

a=6.735Å, b=7.385Å, c=22.487Å, ß=123.25o, Z=2

Geology & Identification

Geologic Occurrence

Hydrothermal alteration of Ca-carbonate rocks due to metamorphism-metasomatism; in basaltic rocksTOBERMORITETOBERMORITE

Habit

As minute laths of fibers; fibrous bundles, rosettes, sheaves, radiating, plumose; granular, massive

Twinning

Relationships

RELATIONSHIP TO OTHER MINERALS

Tobermorite group; dimorphous with clinotobermorite; compare plombièrite; related to tacharanite

If you are fascinated by the hidden structures of our planet, you have likely come across TOBERMORITE. This mineral is a compelling subject for study, offering a unique glimpse into the complex chemistry that shapes the Earth’s crust.Whether you are a student identifying a hand sample, a researcher looking for crystallographic data, or a collector curious about a new find, this guide breaks down everything you need to know about TOBERMORITE. From its precise chemical formula to the geological environments where it thrives, let’s explore what makes this mineral distinct.

The Chemistry Behind the Crystal

Every mineral tells a story through its chemistry. At its core, TOBERMORITE is defined by the chemical formula Ca4[Si6O17](H2O)2·Ca·3H2O.This isn’t just a string of letters and numbers; it represents the precise recipe of elements that nature used to build this specimen. This specific chemical composition is what gives the mineral its stability and dictates how it reacts with acids, heat, or other minerals. It is the fundamental “DNA” that geologists use to classify it within the larger mineral kingdom.

Crystallography: Geometry in Nature

One of the most beautiful aspects of mineralogy is the hidden geometry within every stone. TOBERMORITE crystallizes in the Monoclinic system.Think of this as the mineral’s architectural blueprint. It dictates the symmetry and the angles at which the crystal faces grow. Digging deeper into its symmetry, it falls under the Domatic.
  • Point Group: m
  • Space Group: Bm
Why does this matter? These crystallographic details are like a fingerprint. They influence optical properties—how light travels through the crystal—and physical traits like how it breaks or cleaves when struck.
READ ALSO  LINDSLEYITE Mineral Details

Internal Structure and Unit Cell

If we could zoom in to the atomic level, we would see the “Unit Cell”—the smallest repeating box of atoms that builds up the entire crystal. For TOBERMORITE, the dimensions of this microscopic building block are:
a=6.735Å, b=7.385Å, c=22.487Å, ß=123.25o, Z=2
The internal arrangement of these atoms is described as:Inosilicates: tetrahedra form chains of infinite length with 3-periodic single & multiple chains; has 3-periodic single chains // [010], as in wollastonite.2 Layers formed by linking of xonolite strips, which during condensation at 2 levels overlap somewhat, radical taking formula [Si12O31]; btw layers lie Ca & H2O; number of latter changes stepwise, which causes appreciable increase in c parameter.3 Layers || to (001), formed by [7] coordniated Ca polyhedra; tetrahedral double chains, built up thru condensation of “Dreiereinfachketten” of wollastonite type & running along b, link together adjacent Ca layers in clinotobermorite & tobermorite 11 Å, whereas single tetrahedral chains connect adjacent Ca layers in tobermorite 9 Å; relatively wide channels of clinotobermorite & tobermorite 11 Å host “zeolitic” Ca cations & H2O molecules.4 Common structural feature of polytype 11 Å are infinite layers of Ca polyhedra, || (001), with tetrahedral chains of wollastonite-type running along b & attached on both sides of these layers; composite layers stacked along c & connected thru formation of double tetrahedral chains, with ‘ideal’ composition [Si6O15(OH)2] & [Si6O16(OH)]; most distinctive feature is content of structural cavities.5This internal structure is the invisible framework that supports everything we see on the outside, from the mineral’s density to its hardness.

Physical Appearance (Habit)

When you find TOBERMORITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
  • Common Habit: As minute laths of fibers; fibrous bundles, rosettes, sheaves, radiating, plumose; granular, massive
  • Twinning: 
READ ALSO  HAMBERGITE Mineral Details
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If TOBERMORITE exhibits twinning, it can be a dead giveaway for identification, distinguishing it from look-alike minerals.

Where is it Found? (Geologic Occurrence)

Minerals are the products of their environment. They don’t just appear anywhere; they need specific conditions—pressure, temperature, and chemical ingredients—to form.Geologic Occurrence: Hydrothermal alteration of Ca-carbonate rocks due to metamorphism-metasomatism; in basaltic rocksKnowing this context helps geologists reconstruct the history of a rock formation. It tells us whether the rock was born from cooling magma, settled in an ancient ocean, or was transformed by the intense heat and pressure of metamorphism. For more broad geological context, resources like the U.S. Geological Survey (USGS) provide excellent maps and data.

Related Minerals

No mineral exists in a vacuum. TOBERMORITE is often related to other species, either through similar chemistry or structure.Relationship Data: Tobermorite group; dimorphous with clinotobermorite; compare plombièrite; related to tacharaniteUnderstanding these relationships is key. It helps us see the “family tree” of the mineral world, showing how different elements can substitute for one another to create an entirely new species with similar properties.

Frequently Asked Questions (FAQs)

1. What is the chemical formula of TOBERMORITE?The standard chemical formula for TOBERMORITE is Ca4[Si6O17](H2O)2·Ca·3H2O. This defines its elemental composition.2. Which crystal system does TOBERMORITE belong to?TOBERMORITE crystallizes in the Monoclinic system. Its internal symmetry is further classified under the Domatic class.
READ ALSO  GWIHABAITE Mineral Details
3. How is TOBERMORITE typically found in nature?The “habit” or typical appearance of TOBERMORITE is described as As minute laths of fibers; fibrous bundles, rosettes, sheaves, radiating, plumose; granular, massive. This refers to the shape the crystals take when they grow without obstruction.4. In what geological environments does TOBERMORITE form?TOBERMORITE is typically found in environments described as: Hydrothermal alteration of Ca-carbonate rocks due to metamorphism-metasomatism; in basaltic rocks. This gives clues to the geological history of the area where it is discovered.5. Are there other minerals related to TOBERMORITE?Yes, it is often associated with or related to other minerals such as: Tobermorite group; dimorphous with clinotobermorite; compare plombièrite; related to tacharanite.

External Resources for Further Study

For those looking to dive deeper into the specific mineralogical data of TOBERMORITE, we recommend checking high-authority databases:

Final Thoughts

TOBERMORITE is more than just a name on a list; it is a testament to the orderly and beautiful laws of nature. With a chemical backbone of Ca4[Si6O17](H2O)2·Ca·3H2O and a structure defined by the Monoclinic system, it holds a specific and important place in the study of mineralogy.We hope this overview has helped clarify the essential data points for this specimen. Whether for academic study or personal interest, understanding these properties brings us one step closer to understanding the Earth itself.
Scroll to Top