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.
Difference between revisions of "Siliceous ooze"
Jump to navigation
Jump to search
m (SMH. Why use 2 separate words when a synonym'll do better.) |
LethosorBot (talk | contribs) (Tagging v50 page (3893/4888)) |
||
| (3 intermediate revisions by 3 users not shown) | |||
| Line 1: | Line 1: | ||
| − | {{Quality| | + | {{migrated article}} |
| + | {{Quality|Unrated}} | ||
{{soillookup/0|wiki=Siliceous ooze}} | {{soillookup/0|wiki=Siliceous ooze}} | ||
{{av}} | {{av}} | ||
| − | '''Siliceous ooze''' is one of the several types of [[soil]] that can be found on the floors of deep [[ocean]]s. | + | '''Siliceous ooze''' is one of the several types of [[soil]] that can be found on the floors of deep [[ocean]]s. Not surprisingly, such layers occasionally contain an [[aquifer]]. |
Siliceous ooze is a type of pelagic sediment. It is formed by the silica in diatoms and other microorganisms, as opposed to [[calcareous ooze]], which is formed by particles of [[flux|calcium carbonate]]. | Siliceous ooze is a type of pelagic sediment. It is formed by the silica in diatoms and other microorganisms, as opposed to [[calcareous ooze]], which is formed by particles of [[flux|calcium carbonate]]. | ||
| − | + | [[File:Nitzschia-kerguelensis_hg.jpg|thumb|300px|center|A diatom, seen under a powerful microscope.]] | |
{{gamedata}} | {{gamedata}} | ||
{{DF2014 soil}} | {{DF2014 soil}} | ||
Latest revision as of 00:46, 21 December 2022
| This article was migrated from DF2014:Siliceous 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. |
Siliceous 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.
Siliceous ooze is a type of pelagic sediment. It is formed by the silica in diatoms and other microorganisms, as opposed to calcareous ooze, which is formed by particles of calcium carbonate.
[INORGANIC:SILICEOUS_OOZE]
[USE_MATERIAL_TEMPLATE:SOIL_TEMPLATE]
[STATE_NAME_ADJ:ALL_SOLID:siliceous ooze][DISPLAY_COLOR:4:7:0][TILE:177]
[SOIL_OCEAN][AQUIFER]
[SOLID_DENSITY:2460]
[STATE_COLOR:ALL_SOLID:MIDNIGHT_BLUE] |
| Topsoil | |
|---|---|
| Ocean floor | |
| Sand | |
| Clay | |