[3] Dark brown or black colors typically indicate that the soil has a high organic matter content.[8] Soil in anaerobic, saturated environments may appear gray or blue in color due to the redox reduction and/or depletion of iron.This often exposes the light gray colors of bare silicate minerals, and soils with a low chroma from iron reduction or depletion are said to be gleyed.[9][10] Celadonite in hydrothermally-altered basalt within the Mojave Desert has been observed to weather into a green colored smectite-rich clay soil.[13][14] White colors are common in soils with salt, carbonate, or calcite accumulations, which often occur in arid environments.
Dark soil color imparted by organic matter in Illinois, US
Highly oxidized red soil in Tirunelveli District, India
Glauconitic, green soil from Maryland, US
Jarosite accumulation in acidic soil in Cambridgeshire, UK
Multiple soil colors in a marsh soil in South Australia