EWINGITE Mineral Details

Complete mineralogical data for EWINGITE. Chemical Formula: Mg8Ca8(UO2)24(CO3)30O4(OH)12(H2O)138. Crystal System: Tetragonal. Learn about its geologic occurrence, habit, and identification.

EWINGITE

Mg8Ca8(UO2)24(CO3)30O4(OH)12(H2O)138

Crystal System

Tetragonal

Crystal Class

Ditetragonal dipyramidal

Space Group

I41/acd

Point Group

4/m 2/m 2/m

Structure & Data

Crystal Structure

Structure contains nanometer-scale anionic uranyl carbonate cages that contain 24 uranyl polyhedra, as well as Ca & Mg cations & H2O grp loc in interstitial regions inside & btw cages.1 Unit cell volume is much larger than those of most minerals, & is consequence of presence of 2.3 nm diameter cage consisting of uranyl & carbonate polyhedra; uranyl carbonate cage contains 3 FBB known from other uranyl compounds; in all of these, (UO2)2+ uranyl ions are ± linear & have U—O bond lengths of ~1.8 ŝ; FBB-1 consists of 3 uranyl ions, each of which is coordinated by 5 O atoms arranged about equatorial regions of pentagonal bi-∆; single O atom in equatorial planes of bi-∆ is bonded to all 3 uranyl ions, & bi-∆ each share 2 of their equatorial edges with 2 other bi-∆; in FBB-2 uranyl ion is coordinated by 3 bidentate carbonate grp, resulting in hexagonal bi-∆ with carbonate grp in equatorial region of uranyl ion; in FBB-3, uranyl ion is coordinated by 2 bidentate carbonate grp & 2 H2O grp in equatorial region of hexagonal bi-∆; 1 carbon site in cage is 50% occupied, & avg of cage requires 4 FBB-1 & 6 each of FBB-2 & FBB-3; in 8 of FBB-3; linkages btw FBBs within cage are thru carbonate grp; there are 6 Ca cations & 2 Mg cations inside uranyl carbonate cage, where they are coordinated by O atoms of cage, as H2O grp; uranyl carbonate cages are linked to other cages in xl structure by bonds to Ca & Mg cations, as well as H—bonds assoc with H2O grps in interstitial regions; interstitial components exhibit partial occupancy & disorder.2

Cell Data

a=35.401Å, c=48.157Å, Z=8

Geology & Identification

Geologic Occurrence

Postmining oxidation of primary uraniniteEWINGITEEWINGITE

Habit

As aggregates of equant micro crystals

Twinning

Relationships

RELATIONSHIP TO OTHER MINERALS

If you are fascinated by the hidden structures of our planet, you have likely come across EWINGITE. 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 EWINGITE. 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, EWINGITE is defined by the chemical formula Mg8Ca8(UO2)24(CO3)30O4(OH)12(H2O)138.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. EWINGITE 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 Ditetragonal dipyramidal.
  • Point Group: 4/m 2/m 2/m
  • Space Group: I41/acd
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 EWINGITE, the dimensions of this microscopic building block are:
a=35.401Å, c=48.157Å, Z=8
The internal arrangement of these atoms is described as:
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Structure contains nanometer-scale anionic uranyl carbonate cages that contain 24 uranyl polyhedra, as well as Ca & Mg cations & H2O grp loc in interstitial regions inside & btw cages.1 Unit cell volume is much larger than those of most minerals, & is consequence of presence of 2.3 nm diameter cage consisting of uranyl & carbonate polyhedra; uranyl carbonate cage contains 3 FBB known from other uranyl compounds; in all of these, (UO2)2+ uranyl ions are ± linear & have U—O bond lengths of ~1.8 ŝ; FBB-1 consists of 3 uranyl ions, each of which is coordinated by 5 O atoms arranged about equatorial regions of pentagonal bi-∆; single O atom in equatorial planes of bi-∆ is bonded to all 3 uranyl ions, & bi-∆ each share 2 of their equatorial edges with 2 other bi-∆; in FBB-2 uranyl ion is coordinated by 3 bidentate carbonate grp, resulting in hexagonal bi-∆ with carbonate grp in equatorial region of uranyl ion; in FBB-3, uranyl ion is coordinated by 2 bidentate carbonate grp & 2 H2O grp in equatorial region of hexagonal bi-∆; 1 carbon site in cage is 50% occupied, & avg of cage requires 4 FBB-1 & 6 each of FBB-2 & FBB-3; in 8 of FBB-3; linkages btw FBBs within cage are thru carbonate grp; there are 6 Ca cations & 2 Mg cations inside uranyl carbonate cage, where they are coordinated by O atoms of cage, as H2O grp; uranyl carbonate cages are linked to other cages in xl structure by bonds to Ca & Mg cations, as well as H—bonds assoc with H2O grps in interstitial regions; interstitial components exhibit partial occupancy & disorder.2This internal structure is the invisible framework that supports everything we see on the outside, from the mineral’s density to its hardness.
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Physical Appearance (Habit)

When you find EWINGITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
  • Common Habit: As aggregates of equant micro crystals
  • Twinning: 
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If EWINGITE 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: Postmining oxidation of primary uraniniteKnowing 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. EWINGITE 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.
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Frequently Asked Questions (FAQs)

1. What is the chemical formula of EWINGITE?The standard chemical formula for EWINGITE is Mg8Ca8(UO2)24(CO3)30O4(OH)12(H2O)138. This defines its elemental composition.2. Which crystal system does EWINGITE belong to?EWINGITE crystallizes in the Tetragonal system. Its internal symmetry is further classified under the Ditetragonal dipyramidal class.3. How is EWINGITE typically found in nature?The “habit” or typical appearance of EWINGITE is described as As aggregates of equant micro crystals. This refers to the shape the crystals take when they grow without obstruction.4. In what geological environments does EWINGITE form?EWINGITE is typically found in environments described as: Postmining oxidation of primary uraninite. This gives clues to the geological history of the area where it is discovered.5. Are there other minerals related to EWINGITE?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 EWINGITE, we recommend checking high-authority databases:

Final Thoughts

EWINGITE 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 Mg8Ca8(UO2)24(CO3)30O4(OH)12(H2O)138 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.
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