S-type asteroids have [[a-lbedo]]s varying from 0.10 to 0.22.<ref name=planetsoc/> They are composed primarily of [[iron]] and [[nickel]] with iron and [[magnesium]] silicates added. They resemble stony [[meteor]]ites and ordinary rocks. They typically predominate in the inner regions of the asteroid belt.<ref name=planetsoc/><ref name=Burns>Burns, Philip R. "[http://www.pibburns.com/catastro/asteroid.htm Asteroids]." March 1, 2000. Accessed June 21, 2008.</ref>
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S-type asteroids have [[albedo]]s varying from 0.10 to 0.22.<ref name=planetsoc/> They are composed primarily of [[iron]] and [[nickel]] with iron and [[magnesium]] silicates added. They resemble stony [[meteor]]ites and ordinary rocks. They typically predominate in the inner regions of the asteroid belt.<ref name=planetsoc/><ref name=Burns>Burns, Philip R. "[http://www.pibburns.com/catastro/asteroid.htm Asteroids]." March 1, 2000. Accessed June 21, 2008.</ref>