| Display title | Earth:Late Glacial Interstadial |
| Default sort key | Late Glacial Interstadial |
| Page length (in bytes) | 19,358 |
| Namespace ID | 3028 |
| Namespace | Earth |
| Page ID | 278532 |
| 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>NBrush |
| Date of page creation | 19:36, 15 May 2023 |
| Latest editor | imported>NBrush |
| Date of latest edit | 19:36, 15 May 2023 |
| 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. | The Late Glacial Interstadial (LGI) c.14,670 to c.12,890 BP represents the first pronounced warming since the end of the Last Glacial Maximum (LGM). Human populations, which had previously forced into refuge areas, gradually begin to repopulate the Northern Hemisphere's Eurasian landmass and eventually... |
