| Display title | Earth:Slab pull |
| Default sort key | Slab pull |
| Page length (in bytes) | 7,084 |
| Namespace ID | 3028 |
| Namespace | Earth |
| Page ID | 414298 |
| 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>Ohm |
| Date of page creation | 12:45, 5 February 2024 |
| Latest editor | imported>Ohm |
| Date of latest edit | 12:45, 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. | Slab pull is a geophysical mechanism whereby the cooling and subsequent densifying of a subducting tectonic plate produces a downward force along the rest of the plate. In 1975 Forsyth and Uyeda used the inverse theory method to show that, of the many forces likely to be driving plate motion, slab pull... |
