WAIMIRITE-(Y) Mineral Details

Complete mineralogical data for WAIMIRITE-(Y). Chemical Formula: YF3. Crystal System: Orthorhombic. Learn about its geologic occurrence, habit, and identification.

WAIMIRITE-(Y)

YF3

Crystal System

Orthorhombic

Crystal Class

Dipyramidal

Space Group

Pnma

Point Group

2/m 2/m 2/m

Structure & Data

Crystal Structure

Y atom forms[9]-coordinated YF9 tricapped trig prism; substitution of Y for Dy, as well as for other lanthanoids, causes no notable deviations in xllographic values.

Cell Data

a=6.386Å, b=6.877Å, c=4.401Å, Z=4

Geology & Identification

Geologic Occurrence

In hydrothermal veins cross-cutting albite-enriched facies of the A-type Madeira granite; hydrothermally altered quartz-rich micrograniteWAIMIRITE-(Y)WAIMIRITE-(Y)

Habit

As massive aggregates of platy submicro crystals

Twinning

Relationships

RELATIONSHIP TO OTHER MINERALS

Known sythetic analog

If you are fascinated by the hidden structures of our planet, you have likely come across WAIMIRITE-(Y). 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 WAIMIRITE-(Y). 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, WAIMIRITE-(Y) is defined by the chemical formula YF3.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. WAIMIRITE-(Y) 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: Pnma
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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 WAIMIRITE-(Y), the dimensions of this microscopic building block are:
a=6.386Å, b=6.877Å, c=4.401Å, Z=4
The internal arrangement of these atoms is described as:Y atom forms[9]-coordinated YF9 tricapped trig prism; substitution of Y for Dy, as well as for other lanthanoids, causes no notable deviations in xllographic values.This 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 WAIMIRITE-(Y) in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
  • Common Habit: As massive aggregates of platy submicro crystals
  • Twinning: 
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If WAIMIRITE-(Y) 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.
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Geologic Occurrence: In hydrothermal veins cross-cutting albite-enriched facies of the A-type Madeira granite; hydrothermally altered quartz-rich micrograniteKnowing 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. WAIMIRITE-(Y) is often related to other species, either through similar chemistry or structure.Relationship Data: Known sythetic analogUnderstanding 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 WAIMIRITE-(Y)?The standard chemical formula for WAIMIRITE-(Y) is YF3. This defines its elemental composition.2. Which crystal system does WAIMIRITE-(Y) belong to?WAIMIRITE-(Y) crystallizes in the Orthorhombic system. Its internal symmetry is further classified under the Dipyramidal class.3. How is WAIMIRITE-(Y) typically found in nature?The “habit” or typical appearance of WAIMIRITE-(Y) is described as As massive aggregates of platy submicro crystals. This refers to the shape the crystals take when they grow without obstruction.
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4. In what geological environments does WAIMIRITE-(Y) form?WAIMIRITE-(Y) is typically found in environments described as: In hydrothermal veins cross-cutting albite-enriched facies of the A-type Madeira granite; hydrothermally altered quartz-rich microgranite. This gives clues to the geological history of the area where it is discovered.5. Are there other minerals related to WAIMIRITE-(Y)?Yes, it is often associated with or related to other minerals such as: Known sythetic analog.

External Resources for Further Study

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

Final Thoughts

WAIMIRITE-(Y) 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 YF3 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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