If you are fascinated by the hidden structures of our planet, you have likely come across
AGRELLITE. 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
AGRELLITE. 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,
AGRELLITE is defined by the chemical formula
NaCa2[Si4O10]F.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.
AGRELLITE crystallizes in the
Triclinic 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
Pinacoidal.
- Point Group: 1
- Space Group: P1
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
AGRELLITE, the dimensions of this microscopic building block are:
a=7.76Å, b=18.95Å, c=6.99Å, α=89.9o, ß=116.6o, γ=94.3o, Z=4
The internal arrangement of these atoms is described as:
Inosilicates: tetrahedra form chains of infinite length with 4-periodic single chains, Si4O12; 2 Si4O11 chains, as in vlasovite, linked by shared O into [Si4O10]2 6-periodic double chain, which creates 4-, 6-, 8-membered rings; chains // [001] linked to form tubules // [100] that lie in (010) plane; this plane alternates with slabs consisting of chains of edge- & face-sharing Ca[6,7] polyhedra; Na ions lodged in silicate tubules.1 Consists of 2 diff NaO8 polyhedra which are distorted cubes, 2 each of CaO5F octahedra & CaO6F2 polyhedra, & 2 diff [Si8O20] double chains which are hollow tubes, formed by polymerization of 2 vlasovite-type [Si4O11] single chains, consisting of corner-sharing 4-membered rings; silicate tubes, whose diameter is defined by basket-shaped 6-membered ring, run || to c axis & are hexagonally close-packed in (001) plane; Na atoms occurring in cavities cross-link these tubes to form Na silicate layers || to (010) plane; these layers alternate with Ca polyhedral layers along b axis to form 3-D framework.2 Tubular silicate mineral which xl structure is typified by exteded [Si8O20]8- tubes & has 2-D channel system; contains some structural voids (not micro-porous) which is able to host single guest atoms, molecules or radicals which can affect their physical properties; canals house H2O or (OH)-.3This 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
AGRELLITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
- Common Habit: Elongated parallel crystals; platy aggregates
- Twinning:
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If AGRELLITE 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:
In pegmatite lenses, mafic gnesses in regionally metamorphosed agpaitic alkalic 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.
AGRELLITE 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 AGRELLITE?The standard chemical formula for AGRELLITE is
NaCa2[Si4O10]F. This defines its elemental composition.
2. Which crystal system does AGRELLITE belong to?AGRELLITE crystallizes in the
Triclinic system. Its internal symmetry is further classified under the Pinacoidal class.
3. How is AGRELLITE typically found in nature?The “habit” or typical appearance of AGRELLITE is described as
Elongated parallel crystals; platy aggregates. This refers to the shape the crystals take when they grow without obstruction.
4. In what geological environments does AGRELLITE form?AGRELLITE is typically found in environments described as:
In pegmatite lenses, mafic gnesses in regionally metamorphosed agpaitic alkalic rock. This gives clues to the geological history of the area where it is discovered.
5. Are there other minerals related to AGRELLITE?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
AGRELLITE, we recommend checking high-authority databases:
Final Thoughts
AGRELLITE 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
NaCa2[Si4O10]F and a structure defined by the
Triclinic 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.
