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Difference between revisions of "Calcareous ooze"
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Calcareous ooze is a type of [[soil|pelagic sediment]]. It is formed by particles of [[flux|calcium carbonate]], as opposed to [[siliceous ooze]], which is formed by the silica in diatoms and other microorganisms. | Calcareous ooze is a type of [[soil|pelagic sediment]]. It is formed by particles of [[flux|calcium carbonate]], as opposed to [[siliceous ooze]], which is formed by the silica in diatoms and other microorganisms. | ||
| − | [[File: | + | [[File:Calcareous_Soil_Profile,_Seven_Sisters_Country_Park_-_geograph.org.uk_-_1280181.jpg|thumb|300px|center|Said soil, once the water is gone.]] |
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{{DF2014 soil}} | {{DF2014 soil}} | ||
Latest revision as of 00:22, 21 December 2022
| 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. |
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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. |
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 | |