Predictive Mineralogy
There are no predicted missing minerals from this locality based on our current calculations.
Predicting paragenetic modes of deposit
Green indicates almost certain match based on minerals unique to a certain deposit type. Yellow indicates a possibly poor match, but should not be entirely discounted. Scores > 100 indicate strong confidence.
| Paragenetic Mode | Score |
|---|
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]
Unique: Smithsonite | 100 |
| 53 : Other minerals with taphonomic origins | 7 |
| 47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 7 |
| 54 : Coal and other mine fire minerals (see also #51 and #56) | 2 |
| 50 : Coal and/or oil shale minerals | 2 |
| 47b : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites] | 2 |
| 45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates] | 2 |
| 45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 1 |
| 47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 1 |
| 57 : Other minerals formed by human processes | 1 |
| 49 : Oxic cellular biomineralization (see also #44) | 0 |