If you are fascinated by the hidden structures of our planet, you have likely come across
REDLEDGEITE. 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
REDLEDGEITE. 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,
REDLEDGEITE is defined by the chemical formula
Ba(Ti6Cr3+2)O16.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.
REDLEDGEITE crystallizes in the
Tetragonal 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
Tetragonal dipyramidal.
- Point Group: 4/m
- Space Group: I4/m
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
REDLEDGEITE, the dimensions of this microscopic building block are:
a=10.15Å, c=2.95Å, Z=1
The internal arrangement of these atoms is described as:
Cation coordinations varying from [2] to [10] & polyhedra linked in var ways with large cations; tunnel structures; edge-sharing M(O, OH)6 octahedra form double chains // [001]; chains share corners to form framework with large zeolitic tunnels // [001] occupied by large cations & sometimes H2O & Cl; monoclinic structures represent minor deformations of tetragonal structures.2 Isostructural with hollandite; ¼ of Ti is repl by Cr & Fe3+, which gives □ (R8O16)∞ chain (-) charge, which is neutralized by Mg & K within channels; powder pattern contains intermediate lay lines, which imply doubling of cell parameters & alteration of s.g.3 Pairs of edge sharing octahedra forms columns || to [001] which in turn share corners to form □ tunnels which run thru structure; Ba occupy [8]-coordinated sites within tunnels.4 Has Ti8O6 framework of octahedra with [0,0,z] & [½,½,z] tunnels; Ba occurs in tunnels, allowing substition of Cr3+, Fe3+, & V3+ for Ti4+; majority of Ba atoms are loc at Ba1 site at 0,0,0 & ½,½,½; short c-dimension prohibits occupancy of adjacent sites along [0,0,z] & [½,½,z], yielding formula Ba11[M3+2Ti4+6] O16; Ba occupancy greater than Ba1 per unit cell is attained by partial occupancy of Ba2 sites at special sequence of occupied sets of sites allows 2/3 of sets to be occupied, yielding hypothetical max occupancy of Ba1.33[M3+2.67Ti4+5.33]O15; structural constraints on max occupancy have major implications for waste-loading in synthetic phase.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
REDLEDGEITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
- Common Habit: Short prismatic macro crystals with flat pyramidal terminations; radial fibrous, massive
- Twinning: Common on {101} or {101}
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If REDLEDGEITE 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:
Primary mineral in contact metamorphic Mn-ores; secondary weathering product of ealier Mn-bearing mineralsKnowing 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.
REDLEDGEITE is often related to other species, either through similar chemistry or structure.
Relationship Data:
Hollandite supergroup, priderite group; isostructural with mannarditeUnderstanding 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 REDLEDGEITE?The standard chemical formula for REDLEDGEITE is
Ba(Ti6Cr3+2)O16. This defines its elemental composition.
2. Which crystal system does REDLEDGEITE belong to?REDLEDGEITE crystallizes in the
Tetragonal system. Its internal symmetry is further classified under the Tetragonal dipyramidal class.
3. How is REDLEDGEITE typically found in nature?The “habit” or typical appearance of REDLEDGEITE is described as
Short prismatic macro crystals with flat pyramidal terminations; radial fibrous, massive. This refers to the shape the crystals take when they grow without obstruction.
4. In what geological environments does REDLEDGEITE form?REDLEDGEITE is typically found in environments described as:
Primary mineral in contact metamorphic Mn-ores; secondary weathering product of ealier Mn-bearing minerals. This gives clues to the geological history of the area where it is discovered.
5. Are there other minerals related to REDLEDGEITE?Yes, it is often associated with or related to other minerals such as:
Hollandite supergroup, priderite group; isostructural with mannardite.
External Resources for Further Study
For those looking to dive deeper into the specific mineralogical data of
REDLEDGEITE, we recommend checking high-authority databases:
Final Thoughts
REDLEDGEITE 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
Ba(Ti6Cr3+2)O16 and a structure defined by the
Tetragonal 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.
