Display title | Earth:Neoglaciation |
Default sort key | Neoglaciation |
Page length (in bytes) | 5,300 |
Namespace ID | 3028 |
Namespace | Earth |
Page ID | 400053 |
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 |
Page image |  |
HandWiki item ID | None |
Edit | Allow all users (infinite) |
Move | Allow all users (infinite) |
Page creator | imported>LinuxGuru |
Date of page creation | 11:01, 10 October 2021 |
Latest editor | imported>LinuxGuru |
Date of latest edit | 11:01, 10 October 2021 |
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 neoglaciation ("renewed glaciation") describes the documented cooling trend in the Earth's climate during the Holocene, following the retreat of the Wisconsin glaciation, the most recent glacial period. Neoglaciation has followed the hypsithermal or Holocene Climatic Optimum, the warmest point in... |