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Difference between revisions of "Siliceous ooze"

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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]].
 
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[[File:Nitzschia-kerguelensis_hg.jpg|thumb|300px|center|A diatom, seen under a powerful microscope.]]
  
 
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Latest revision as of 00:46, 21 December 2022

Siliceous ooze
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Properties
Contains

Wikipedia article

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.

A diatom, seen under a powerful microscope.
Topsoil
Ocean floor
Sand
Clay