HALURGITE Mineral Details

Complete mineralogical data for HALURGITE. Chemical Formula: Mg4[B8O13(OH)2]2(H2O)4·3H2O. Crystal System: Monoclinic. Learn about its geologic occurrence, habit, and identification.

HALURGITE

Mg4[B8O13(OH)2]2(H2O)4·3H2O

Crystal System

Monoclinic

Crystal Class

Prismatic

Space Group

P2/c

Point Group

2/m

Structure & Data

Crystal Structure

Borate structures are based on constitution of FBB with triangles (Tr) & tetrahedra (Tt); tetraborates; phyllo-tetraborates; structure unknown.1 8 B polyhedra form FBB [B8O16(OH)2], which is 6-membered borate ring (built by 2 pairs of B tetrahedra & 2 B triangles) with 2 add’l triangular BO2(OH) grp; each [B8O16(OH)2] ring is linked to 6 adjacent analog rings to form [B8O13(OH)2]∞ layer; these layers are connected via MgO6 & Mg (OH)2(H2O)4 octahedra into microporous heteropolyhedral pseudo-framework.2 Xl structure can also be described in terms of approach developed for heterophyllosilicates containg 3-layer HOH modules, where HOH refers to octahedral layer O sandwiched btw 2 heteropolyhedral layers H; in halurgite HOH module consists of 2 heteropolyhedral (BO3 triangles + BO4 tetrahedra) borate H layers [B8O13(OH)2]∞ & central interrupted O layer composed of MgO6 octahedra whereas more voluminous Mg(OH)2(H2O)4 octahedral complex add’l H2O molecules are loc btw HOH modules.3 There are 4 related synthetic H-free borates M2Cd3 B16O28 & M2Ca3B16O28 (M = Rb or Cs) can be considered microporous heterophylloborates.4

Cell Data

a=13.201Å, b=7.5622Å, c=13.185Å, ß=91.834o, Z=2

Geology & Identification

Geologic Occurrence

Secondary mineral formed by alteration of chromite, pentlandite, millerite in serpentinites-ultramafic rocksHALURGITEHALURGITE

Habit

Coatings of fibrous to spherulitic microcrystals and gelike amorphous material

Twinning

Relationships

RELATIONSHIP TO OTHER MINERALS

If you are fascinated by the hidden structures of our planet, you have likely come across HALURGITE. 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 HALURGITE. 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, HALURGITE is defined by the chemical formula Mg4[B8O13(OH)2]2(H2O)4·3H2O.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. HALURGITE 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 Prismatic.
  • Point Group: 2/m
  • Space Group: P2/c
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.
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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 HALURGITE, the dimensions of this microscopic building block are:
a=13.201Å, b=7.5622Å, c=13.185Å, ß=91.834o, Z=2
The internal arrangement of these atoms is described as:Borate structures are based on constitution of FBB with triangles (Tr) & tetrahedra (Tt); tetraborates; phyllo-tetraborates; structure unknown.1 8 B polyhedra form FBB [B8O16(OH)2], which is 6-membered borate ring (built by 2 pairs of B tetrahedra & 2 B triangles) with 2 add’l triangular BO2(OH) grp; each [B8O16(OH)2] ring is linked to 6 adjacent analog rings to form [B8O13(OH)2]∞ layer; these layers are connected via MgO6 & Mg (OH)2(H2O)4 octahedra into microporous heteropolyhedral pseudo-framework.2 Xl structure can also be described in terms of approach developed for heterophyllosilicates containg 3-layer HOH modules, where HOH refers to octahedral layer O sandwiched btw 2 heteropolyhedral layers H; in halurgite HOH module consists of 2 heteropolyhedral (BO3 triangles + BO4 tetrahedra) borate H layers [B8O13(OH)2]∞ & central interrupted O layer composed of MgO6 octahedra whereas more voluminous Mg(OH)2(H2O)4 octahedral complex add’l H2O molecules are loc btw HOH modules.3 There are 4 related synthetic H-free borates M2Cd3 B16O28 & M2Ca3B16O28 (M = Rb or Cs) can be considered microporous heterophylloborates.4This 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 HALURGITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
  • Common Habit: Coatings of fibrous to spherulitic microcrystals and gelike amorphous material
  • Twinning: 
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Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If HALURGITE 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: Secondary mineral formed by alteration of chromite, pentlandite, millerite in serpentinites-ultramafic 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. HALURGITE is often related to other species, either through similar chemistry or structure.Relationship Data:Understanding 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 HALURGITE?The standard chemical formula for HALURGITE is Mg4[B8O13(OH)2]2(H2O)4·3H2O. This defines its elemental composition.2. Which crystal system does HALURGITE belong to?HALURGITE crystallizes in the Monoclinic system. Its internal symmetry is further classified under the Prismatic class.
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3. How is HALURGITE typically found in nature?The “habit” or typical appearance of HALURGITE is described as Coatings of fibrous to spherulitic microcrystals and gelike amorphous material. This refers to the shape the crystals take when they grow without obstruction.4. In what geological environments does HALURGITE form?HALURGITE is typically found in environments described as: Secondary mineral formed by alteration of chromite, pentlandite, millerite in serpentinites-ultramafic rocks. This gives clues to the geological history of the area where it is discovered.5. Are there other minerals related to HALURGITE?Yes, it is often associated with or related to other minerals such as: .

External Resources for Further Study

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

Final Thoughts

HALURGITE 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 Mg4[B8O13(OH)2]2(H2O)4·3H2O 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.
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