Museum Collection This specimen is part of the museum collection catalog. Not for Sale.
Thomsonite
Drain, Douglas Co., Oregon, USA
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![Thomsonite](/Files/Minerals/Thomsonite_475_lg.jpg)
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Classification |
Mineral |
Tags |
Perky Box
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Origin Location |
Drain, Douglas Co., Oregon, USA |
Description |
An exemplary thumbnail of the calcium zeolite Thomsonite with associated Analcime, from a western US location. |
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 |
Thumbnail |
Weight |
Not weighed precisely yet, please inquire. |
Dimensions |
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Quantity |
1 Specimen |
Mineral List |
IMA minerals have not been identified, but may be present.
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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
Quartz![Quartz](/Files/Minerals/Quartz_548_sm.jpg) Ulexite![Ulexite](/Files/Minerals/Ulexite_460_sm.jpg) Quartz![Quartz](/Files/Minerals/Quartz_366_sm.jpg) Zinkenite![Zinkenite](/Files/Minerals/Zinkenite_647_sm.jpg) Phenakite![Phenakite](/Files/Minerals/Phenakite_761_0_sm.jpg) Pyrolusite![Pyrolusite](/Files/Minerals/Pyrolusite_569_sm.jpg) |
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
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Tools |
Edit Specimen Search Wikipedia: Thomsonite (Wiki) Search Mindat: Thomsonite Search Web Mineral DB: Thomsonite Search for Handbook of Mineralogy: Thomsonite
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