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Difference between revisions of "DF2014:Calcareous ooze"
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LethosorBot (talk | contribs) (LethosorBot moved page DF2014:Calcareous ooze to Calcareous ooze: Migrating v50 page (440/4618) (content)) Tag: New redirect |
LethosorBot (talk | contribs) (Migrating v50 page (440/4618) (content)) Tag: Removed redirect |
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| − | + | {{Quality|Superior|19:20, 16 August 2017 (UTC)}} | |
| + | {{soillookup/0|wiki=Pelagic sediment}} | ||
| + | {{av}} | ||
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| + | '''Calcareous 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]]. | ||
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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. | ||
| + | [[File:Calcareous_Soil_Profile,_Seven_Sisters_Country_Park_-_geograph.org.uk_-_1280181.jpg|thumb|300px|center|Said soil, once the water is gone.]] | ||
| + | {{gamedata}} | ||
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| + | {{DF2014 soil}} | ||
Latest revision as of 03:12, 20 December 2022
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| This article is about an older version of DF. |
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] |
| Topsoil | |
|---|---|
| Ocean floor | |
| Sand | |
| Clay | |