No Longer Available This specimen was sold to a private collection. This page is for provenance reference only.
Smithsonite
M'fouti, Congo [Republic]
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Classification |
Mineral |
Tags |
No special tags. |
Origin Location |
M'fouti, Congo [Republic] |
Description |
A fine miniature plate of the high quality smithsonite that has been produced at the M'fouti quarries since this new find surfaced in 2021. This material is found in an area of the Republic of Congo west of Brazzaville. |
Luster |
Vitreous |
Luster (Groundmass) |
Not noted, see photo. |
Optical Phenomena |
Not noted, see photo. |
Mineral Group / Note |
Not noted, check reference links below. |
Handling |
No special handling is required. |
Modifications |
No modifications. |
Size Group |
Miniature |
Weight |
Not weighed precisely yet, please inquire. |
Dimensions |
Not measured precisely yet, please inquire. |
Quantity |
1 Specimen |
Mineral List |
Smithsonite: Zn(CO3) zinc carbonate *
* Formula chemical names are auto-generated - may be incorrect on complex formulas.
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Specimen Analysis |
Color Table
Colors found in this specimen image are shown below. Higher number indicates greater concentration of that color.
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Similarly Colored Minerals:
Minerals with similar color profiles are shown below.
How it Works
Hemimorphite Smithsonite Pectolite var. Larimar (Polished) Smithsonite Baryte Beryl var. Aquamarine |
Elements in this Specimen:
Elements that are part of the official chemical structure of the minerals occurring in this specimen are indicated below.
How it Works
Element List:
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Minerals with Similar Chemistry:
Minerals that are similar in terms of their chemical makeup are shown below.
How it Works
This Mineral Formula Similar Mineral Formula
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Mineral Group:
Search the catalog for minerals that share the same group as this specimen:
How it Works
Structural Group(s):
Fleischers Group(s): calcite
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Tools |
Edit Specimen Search Wikipedia: Smithsonite (Wiki) Search Mindat: Smithsonite Search Web Mineral DB: Smithsonite Search for Handbook of Mineralogy: Smithsonite
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