v50 Steam/Premium information for editors
- v50 information can now be added to pages in the main namespace. v0.47 information can still be found in the DF2014 namespace. See here for more details on the new versioning policy.
- Use this page to report any issues related to the migration.
This notice may be cached—the current version can be found here.
Calcareous ooze
Jump to navigation
Jump to search
| This article was migrated from DF2014:Calcareous ooze and may be inaccurate for the current version of DF (v50.14). See this page for more information. |
| ||||||||||||||||||||||||||||||||||||
| Properties | ||||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| ||||||||||||||||||||||||||||||||||||
| Contains | ||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
v50.14 · v0.47.05 This article is about the current version of DF.Note that some content may still need to be updated. |
Calcareous ooze is one of the several types of soil that can be found on the floors of deep oceans. Not surprisingly, such layers occasionally contain an aquifer.
Calcareous ooze is a type of pelagic sediment. It is formed by particles of calcium carbonate, as opposed to siliceous ooze, which is formed by the silica in diatoms and other microorganisms.
Undersea soil densities from "Geotechnical Properties of Deep Continental Margin Soils"
http://www.informaworld.com/index/907178093.pdf
Undersea soils are fairly dense, being compacted.
[INORGANIC:CALCAREOUS_OOZE]
[USE_MATERIAL_TEMPLATE:SOIL_TEMPLATE]
[STATE_NAME_ADJ:ALL_SOLID:calcareous ooze][DISPLAY_COLOR:4:7:0][TILE:177]
[SOIL_OCEAN][AQUIFER]
[SOLID_DENSITY:2690]
[STATE_COLOR:ALL_SOLID:TAUPE_PURPLE] |
| Topsoil | |
|---|---|
| Ocean floor | |
| Sand | |
| Clay | |