SHULAMITITE Mineral Details

Complete mineralogical data for SHULAMITITE. Chemical Formula: Ca3TiFe3+AlO8. Crystal System: Orthorhombic. Learn about its geologic occurrence, habit, and identification.

SHULAMITITE

Ca3TiFe3+AlO8

Crystal System

Orthorhombic

Crystal Class

Dipyramidal

Space Group

Pmma

Point Group

2/m 2/m 2/m

Structure & Data

Crystal Structure

No partitioning among octahedral sites for Ti & Fe3+; these cations are randomly distributed among all octahedra indicating example of “valency-imposed double site occupancy”.

Cell Data

a=5.420Å, b=11.064Å, c=5.538Å, Z=2

Geology & Identification

Geologic Occurrence

In a high-temperature larnite mayenite rockSHULAMITITESHULAMITITE

Habit

As subhedral submicro grains or prismatic platelets

Twinning

Relationships

RELATIONSHIP TO OTHER MINERALS

Perovskite related, intermediate between perovskite and brownmillerite

If you are fascinated by the hidden structures of our planet, you have likely come across SHULAMITITE. 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 SHULAMITITE. 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, SHULAMITITE is defined by the chemical formula Ca3TiFe3+AlO8.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. SHULAMITITE 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: Pmma
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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 SHULAMITITE, the dimensions of this microscopic building block are:
a=5.420Å, b=11.064Å, c=5.538Å, Z=2
The internal arrangement of these atoms is described as:No partitioning among octahedral sites for Ti & Fe3+; these cations are randomly distributed among all octahedra indicating example of “valency-imposed double site occupancy”.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 SHULAMITITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
  • Common Habit: As subhedral submicro grains or prismatic platelets
  • Twinning: 
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If SHULAMITITE exhibits twinning, it can be a dead giveaway for identification, distinguishing it from look-alike minerals.
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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: In a high-temperature larnite mayenite rockKnowing 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. SHULAMITITE is often related to other species, either through similar chemistry or structure.Relationship Data: Perovskite related, intermediate between perovskite and brownmilleriteUnderstanding 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 SHULAMITITE?The standard chemical formula for SHULAMITITE is Ca3TiFe3+AlO8. This defines its elemental composition.2. Which crystal system does SHULAMITITE belong to?SHULAMITITE crystallizes in the Orthorhombic system. Its internal symmetry is further classified under the Dipyramidal class.3. How is SHULAMITITE typically found in nature?The “habit” or typical appearance of SHULAMITITE is described as As subhedral submicro grains or prismatic platelets. This refers to the shape the crystals take when they grow without obstruction.
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4. In what geological environments does SHULAMITITE form?SHULAMITITE is typically found in environments described as: In a high-temperature larnite mayenite rock. This gives clues to the geological history of the area where it is discovered.5. Are there other minerals related to SHULAMITITE?Yes, it is often associated with or related to other minerals such as: Perovskite related, intermediate between perovskite and brownmillerite.

External Resources for Further Study

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

Final Thoughts

SHULAMITITE 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 Ca3TiFe3+AlO8 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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