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Entisols
most limited soil development
horizons are absENT
ochric epipedon

Inceptisols
minimal soil development (INCEPTion of soil development)
ochric epipedon
cambic Bw horizon
variable productivity
mountainous & arid regions

Histosols
wetland soils
high organic content
water saturation; lack oxygen; slows down decomposers
gleying (Bg)
geographically widespread
agriculture

Alfisols
well developed
moderately weathered & leached
argillic/kandic or natric
brown ochric or umbric epipedon
forests

Ultisols
highly leached with clay accumulation
umbric epipedon & argillic
low base saturation
reddish color
warm/humid climate

Vertisols
shrinking & swelling of clays
deep/wide cracks
dry/wet seasons
grasslands

Aridosols
salt accumulation
arid regions (low precipitation)
poorly developed
ochric epipedon

Mollisols
highly fertile
>50% cation saturation (nutrients)
deep, dark A horizon (mollic)
grasslands

Andisols
volcanic ash deposit
young soil
melanic epipedon
andic soil properties (glass, Al, Fe)
can be highly productive
Western MT

Gelisols
permafrost
minimal soil development
mollic, histic, umbric
high organic matter content
low rates of chemical weathering
limited productivity
crytoturbation (freeze & thaw cycles churn & mix horizons)

Spodosols
Sandy, acidic
humus accumulation
albic E horizon
highly leached (light color)
Al & Fe oxides (spodic horizon)
cold, wet climates

Oxisols
Most highly weathered
low nutrient content
oxic (Bo)
yellowish-red
humid, tropical climates
limited productivity