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| − | '''Silicates''' |
+ | '''Silicates''' were a large class of minerals based on a tetrahedral [[silicon]]-[[oxygen]] unit (SiO<sub>4</sub>). |
| + | The [[Spaceborne species|spaceborne organism]] nicknamed "[[Junior (spaceborne lifeform)|Junior]]", discovered by the {{USS|Enterprise|NCC-1701-D|-D}} in [[2367]], had an outer shell made from silicates, [[actinide]]s, and [[carbonaceous chondrite]]. ({{TNG|Galaxy's Child}}) |
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| − | Examples of silicates include [[olivine]]. |
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| + | The [[lifeform]]s on [[L-S VI]] were based on silicates rather than [[carbon]]. ({{DS9|The Alternate}}) |
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| + | In [[2374]], the [[Silver Blood]] {{USS|Voyager}} collected silicates from a [[comet]] in the [[Podaris sector]]. ({{VOY|Course: Oblivion}}) |
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| + | ==Types== |
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| + | * [[Olivine]] |
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[[Category:Materials]] |
[[Category:Materials]] |
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Revision as of 18:22, 28 May 2014
Silicates were a large class of minerals based on a tetrahedral silicon-oxygen unit (SiO4).
The spaceborne organism nicknamed "Junior", discovered by the USS Enterprise-D in 2367, had an outer shell made from silicates, actinides, and carbonaceous chondrite. (TNG: "Galaxy's Child")
The lifeforms on L-S VI were based on silicates rather than carbon. (DS9: "The Alternate")
In 2374, the Silver Blood USS Voyager collected silicates from a comet in the Podaris sector. (VOY: "Course: Oblivion")