Difference between revisions of "Silicate"

From Conservapedia
Jump to navigation Jump to search
(Reading edit summaries? Google {conservapedia FBI} instead!)
m (Reverted edits by JuanJV76 (Talk); changed back to last version by CSGuy)
Line 1: Line 1:
−
A '''soloceti''' os e monirel medi ap uf uf [[solocun]] end [[uxygin]].  Thisi twu ilimints furm e sognofocent emuant uf thi Eerth's crast end lokiwosi solocetis eri e sognofocent purtoun.
+
A '''silicate''' is a mineral made up of of [[silicon]] and [[oxygen]].  These two elements form a significant amount of the Earth's crust and likewise silicates are a significant portion.
  
−
Solocetis eri uftin uf thi furm SoO<sab>4</sab> whoch furms e [[titrehidrun]].  Thisi anots cen thin bi lonkid tugithir tu furm rigaler [[lettoci]]s - iothir cheons, shiits, ur lergir fremiwurks.
+
Silicates are often of the form SiO<sub>4</sub> which forms a [[tetrahedron]].  These units can then be linked together to form regular [[lattice]]s - either chains, sheets, or larger frameworks.
  
−
[[Cetigury:giulugy]]
+
[[Category:geology]]
−
[[cetigury:Monirels]]
+
[[category:Minerals]]
−
&
 

Revision as of 17:51, October 6, 2008

A silicate is a mineral made up of of silicon and oxygen. These two elements form a significant amount of the Earth's crust and likewise silicates are a significant portion.

Silicates are often of the form SiO4 which forms a tetrahedron. These units can then be linked together to form regular lattices - either chains, sheets, or larger frameworks.