https://wiki.pathfindersonline.org/index.php?action=history&feed=atom&title=Translations%3AAdventist_Youth_Honors_Answer_Book%2FNature%2FSoils%2F15%2FenTranslations:Adventist Youth Honors Answer Book/Nature/Soils/15/en - Revision history2026-05-03T18:42:40ZRevision history for this page on the wikiMediaWiki 1.35.5https://wiki.pathfindersonline.org/index.php?title=Translations:Adventist_Youth_Honors_Answer_Book/Nature/Soils/15/en&diff=312708&oldid=prevFuzzyBot: Importing a new version from external source2021-01-10T23:19:33Z<p>Importing a new version from external source</p>
<p><b>New page</b></p><div>The main processes of soil formation of oxisols are weathering, humification and pedoturbation due to animals. These processes produce the characteristic soil profile. They are defined as soils containing at all depths no more than 10 percent weatherable minerals, and low cation exchange capacity. Oxisols are always a red or yellowish color, due to the high concentration of iron(III) and aluminium oxides and hydroxides. In addition they also contain quartz and kaolin, plus small amounts of other clay minerals and organic matter.</div>FuzzyBot