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Siliceous ooze
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| 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. |
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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 | |