| Display title | Physics:Undulation of the geoid |
| Default sort key | Undulation of the geoid |
| Page length (in bytes) | 2,923 |
| Namespace ID | 3020 |
| Namespace | Physics |
| Page ID | 642590 |
| 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>Steve Marsio |
| Date of page creation | 22:55, 26 June 2023 |
| Latest editor | imported>Steve Marsio |
| Date of latest edit | 22:55, 26 June 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. | Undulation of the geoid is the height of the geoid relative to a given ellipsoid of reference. In maps and common use the height over the mean sea level (such as orthometric height) is used to indicate the height of elevations while the ellipsoidal height results from the GPS system.
The process of... |
