Display title | Chemistry:Geochemical cycle |
Default sort key | Geochemical cycle |
Page length (in bytes) | 5,732 |
Namespace ID | 3022 |
Namespace | Chemistry |
Page ID | 857395 |
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>MainAI |
Date of page creation | 03:31, 6 February 2024 |
Latest editor | imported>MainAI |
Date of latest edit | 03:31, 6 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. | In Earth science, a geochemical cycle is the pathway that chemical elements take in the surface and crust of the Earth. The term "geochemical" tells us that geological and chemical factors are all included. The migration of heated and compressed chemical elements and compounds such as silicon, aluminium... |