WAVELLITE Mineral Details

Complete mineralogical data for WAVELLITE. Chemical Formula: Al3(PO4)2(OH)3(H2O)3·2H2O. Crystal System: Orthorhombic. Learn about its geologic occurrence, habit, and identification.

Table of Contents

WAVELLITE

Al3(PO4)2(OH)3(H2O)3·2H2O

Crystal System

Orthorhombic

Crystal Class

Dipyramidal

Space Group

Pcmn

Point Group

2/m 2/m 2/m

Structure & Data

Crystal Structure

Phosphates, arsenates, vanadates: anions [PO4]3-, [AsO4]3-, [VO4]3- are usually insular; cations may be small with [4] coordination, medium-sized with [6] coordination or large with [8] or higher coordination; medium-sized cations with octahedral [6] coordination may be insular, corner-, edge- or face-sharing & form major structural units with add’l anions with H2O with medium-sized cations, (OH, etc.):RO4 = 1:1 < 2:1; chains of edge-sharing Al[6] octahedra linked by PO4 tetrahedra, forming framework that lodges H2O molecules.1 Heterogeneous frameworks consisting of chains of AlO4F2 octahedra linked to PO4 tetrhedra via common vertices.2 2 Al atoms in structure are octahedrally coordinated: 1 is bonded to 2 O, 2 (OH), & 2 H2O; & other to 3 O, (OH), & 1 H2O; P is in tetrahedral coordination with O; Al octahedra,linked thru (OH) corners, form chains || to c axis, & P tetrahedra are attached to this chain by sharing O atoms of subsequent octahedra; extra H2O molecule occupied large cavity btw chains &, as indicated by high temp factor, it has statistical distribution within this cavity.3 P atoms display tetrahedral coordination, while Al cations display octahedral coordination; framework is repetition of cationic arrays made up of AlO6 polyhedra, bridged by PO4 grp & further joined by O—H…O H—bonds.4

Cell Data

a=9.62Å, b=17.36Å, c=6.99Å, Z=4

Geology & Identification

Geologic Occurrence

Secondary minerlal in low-grade metamorphic rocks and phosphate deposits; rare in hydrothermal veinsWAVELLITEWAVELLITE

Habit

Short to long prismatic macro crystals, elongated, striated; commonly in flat to spherical radial aggregates, massive

Twinning

Relationships

RELATIONSHIP TO OTHER MINERALS

Compare allenpringite

If you are fascinated by the hidden structures of our planet, you have likely come across WAVELLITE. 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 WAVELLITE. 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, WAVELLITE is defined by the chemical formula Al3(PO4)2(OH)3(H2O)3·2H2O.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. WAVELLITE crystallizes in the Orthorhombic 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 Dipyramidal.
  • Point Group: 2/m 2/m 2/m
  • Space Group: Pcmn
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.

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 WAVELLITE, the dimensions of this microscopic building block are:
a=9.62Å, b=17.36Å, c=6.99Å, Z=4
The internal arrangement of these atoms is described as:
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Phosphates, arsenates, vanadates: anions [PO4]3-, [AsO4]3-, [VO4]3- are usually insular; cations may be small with [4] coordination, medium-sized with [6] coordination or large with [8] or higher coordination; medium-sized cations with octahedral [6] coordination may be insular, corner-, edge- or face-sharing & form major structural units with add’l anions with H2O with medium-sized cations, (OH, etc.):RO4 = 1:1 < 2:1; chains of edge-sharing Al[6] octahedra linked by PO4 tetrahedra, forming framework that lodges H2O molecules.1 Heterogeneous frameworks consisting of chains of AlO4F2 octahedra linked to PO4 tetrhedra via common vertices.2 2 Al atoms in structure are octahedrally coordinated: 1 is bonded to 2 O, 2 (OH), & 2 H2O; & other to 3 O, (OH), & 1 H2O; P is in tetrahedral coordination with O; Al octahedra,linked thru (OH) corners, form chains || to c axis, & P tetrahedra are attached to this chain by sharing O atoms of subsequent octahedra; extra H2O molecule occupied large cavity btw chains &, as indicated by high temp factor, it has statistical distribution within this cavity.3 P atoms display tetrahedral coordination, while Al cations display octahedral coordination; framework is repetition of cationic arrays made up of AlO6 polyhedra, bridged by PO4 grp & further joined by O—H...O H—bonds.4This internal structure is the invisible framework that supports everything we see on the outside, from the mineral’s density to its hardness.
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Physical Appearance (Habit)

When you find WAVELLITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
  • Common Habit: Short to long prismatic macro crystals, elongated, striated; commonly in flat to spherical radial aggregates, massive
  • Twinning: 
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If WAVELLITE 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 minerlal in low-grade metamorphic rocks and phosphate deposits; rare in hydrothermal veinsKnowing 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. WAVELLITE is often related to other species, either through similar chemistry or structure.Relationship Data: Compare allenpringiteUnderstanding 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 WAVELLITE?The standard chemical formula for WAVELLITE is Al3(PO4)2(OH)3(H2O)3·2H2O. This defines its elemental composition.
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2. Which crystal system does WAVELLITE belong to?WAVELLITE crystallizes in the Orthorhombic system. Its internal symmetry is further classified under the Dipyramidal class.3. How is WAVELLITE typically found in nature?The “habit” or typical appearance of WAVELLITE is described as Short to long prismatic macro crystals, elongated, striated; commonly in flat to spherical radial aggregates, massive. This refers to the shape the crystals take when they grow without obstruction.4. In what geological environments does WAVELLITE form?WAVELLITE is typically found in environments described as: Secondary minerlal in low-grade metamorphic rocks and phosphate deposits; rare in hydrothermal veins. This gives clues to the geological history of the area where it is discovered.5. Are there other minerals related to WAVELLITE?Yes, it is often associated with or related to other minerals such as: Compare allenpringite.

External Resources for Further Study

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

Final Thoughts

WAVELLITE 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 Al3(PO4)2(OH)3(H2O)3·2H2O and a structure defined by the Orthorhombic 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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