| Display title | Physics:Sulfate crust |
| Default sort key | Sulfate crust |
| Page length (in bytes) | 1,472 |
| Namespace ID | 3020 |
| Namespace | Physics |
| Page ID | 477762 |
| Page content language | en - English |
| Page content model | wikitext |
| Indexing by robots | Allowed |
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| Counted as a content page | Yes |
| HandWiki item ID | None |
| Edit | Allow all users (infinite) |
| Move | Allow all users (infinite) |
| Page creator | imported>Rtextdoc |
| Date of page creation | 04:46, 5 February 2024 |
| Latest editor | imported>Rtextdoc |
| Date of latest edit | 04:46, 5 February 2024 |
| Total number of edits | 1 |
| Recent number of edits (within past 90 days) | 0 |
| Recent number of distinct authors | 0 |
Description | Content |
Article description: (description)
This attribute controls the content of the description and og:description elements. | Sulfate crust is a zone observed in the axial (central) parts of burning coal dumps and related sites. It is a zone built mainly by anhydrous sulfate minerals, such as godovikovite and millosevichite. The outer zone can easily be hydrated giving rise to minerals like tschermigite and alunogen. The zone... |
