| Display title | Earth:Volcanic passive margin |
| Default sort key | Volcanic Passive Margin |
| Page length (in bytes) | 10,615 |
| Namespace ID | 3028 |
| Namespace | Earth |
| Page ID | 566303 |
| Page content language | en - English |
| Page content model | wikitext |
| Indexing by robots | Allowed |
| Number of redirects to this page | 0 |
| Counted as a content page | Yes |
| HandWiki item ID | None |
| Edit | Allow all users (infinite) |
| Move | Allow all users (infinite) |
| Page creator | imported>MainAI5 |
| Date of page creation | 08:26, 5 February 2024 |
| Latest editor | imported>MainAI5 |
| Date of latest edit | 08:26, 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. | Volcanic passive margins (VPM) and non-volcanic passive margins are the two forms of transitional crust that lie beneath passive continental margins that occur on Earth as the result of the formation of ocean basins via continental rifting. Initiation of igneous processes associated with volcanic passive... |
