If you are fascinated by the hidden structures of our planet, you have likely come across
PAULINGITE-K. 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
PAULINGITE-K. 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,
PAULINGITE-K is defined by the chemical formula
(K,Na,Ca,Ba,□)10[(Si,Al)42O84]·34H2O.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.
PAULINGITE-K crystallizes in the
Isometric 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
Cubic hexoctahedral.
- Point Group: 4/m 3 2/m
- Space Group: Im3m
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
PAULINGITE-K, the dimensions of this microscopic building block are:
a=35.09Å, Z=16
The internal arrangement of these atoms is described as:
Tektosilicates: tetrahedra are linked into 3-D framework with zeolitic H2O; with complex structure of 7 diff types of cage, incl α-cages (truncated cuboctahedra) & γ-cages (4-membered analog of 3-membered gmelinite cage) connected by double 8-membered rings; & л-cages (modified form of levyne cages) connected to α-cages by single 6-membered rings.2 Structure of paulingite was determined by Gordon et al (1966), confirming space grp Im3m, proposed by Kamb & Oke (1960); unit cell (a = 35.1 Å) is largest of all known zeolites, & framework filling this cell is complex array of cages & double 8-rings (PAU); framework consists of 4 regular polyhedra or cages & 3 irregular polyhedra, acct for interstices; alpha-cage (also named lta in PAU) is loc at cell center & at cell corners; connected to each of 6 single 8-ring faces of lta are d8R (double 8-ring) & pau polyhedra (PAU); sequence of these cages is ita-d8R-pau-d8R-pau-d8R-ita along 1 edge of unit cell; each unit cell contains 672 tetrahedral sites, & Si,Al distribution thru out these site appears to be random (Bieniok et al (1996, Lengauer et al (1997)).3 See “Additional Structures” tab for entry(s).4 Zeolites are alumino-silicate frameworks with usually loosely bonded alkali or alkali-earth cations, or both; molecules of H2O occupy extra-framework positions; paulingite has framework which contains several kinds of large polyhedral cages; Ca is most abundant extra-framework cation.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
PAULINGITE-K in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
- Common Habit: As dodecahedra, modified by the cube and trapezohedron; faintly striated (for orginal mineral)
- Twinning:
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If PAULINGITE-K 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 vesicles in basalt flowsKnowing 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.
PAULINGITE-K is often related to other species, either through similar chemistry or structure.
Relationship Data:
Zeolite family, paulingite subgroupUnderstanding 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 PAULINGITE-K?The standard chemical formula for PAULINGITE-K is
(K,Na,Ca,Ba,□)10[(Si,Al)42O84]·34H2O. This defines its elemental composition.
2. Which crystal system does PAULINGITE-K belong to?PAULINGITE-K crystallizes in the
Isometric system. Its internal symmetry is further classified under the Cubic hexoctahedral class.
3. How is PAULINGITE-K typically found in nature?The “habit” or typical appearance of PAULINGITE-K is described as
As dodecahedra, modified by the cube and trapezohedron; faintly striated (for orginal mineral). This refers to the shape the crystals take when they grow without obstruction.
4. In what geological environments does PAULINGITE-K form?PAULINGITE-K is typically found in environments described as:
In vesicles in basalt flows. This gives clues to the geological history of the area where it is discovered.
5. Are there other minerals related to PAULINGITE-K?Yes, it is often associated with or related to other minerals such as:
Zeolite family, paulingite subgroup.
External Resources for Further Study
For those looking to dive deeper into the specific mineralogical data of
PAULINGITE-K, we recommend checking high-authority databases:
Final Thoughts
PAULINGITE-K 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
(K,Na,Ca,Ba,□)10[(Si,Al)42O84]·34H2O and a structure defined by the
Isometric 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.
