inceptisols

The dominant soil type is poorly evolved inceptisols formed due to the continual leaching of minerals from the soils by the high influx of water.

Talamancan montane forests 2010

Soils are primarily ultisols and inceptisols, generally older, infertile soils.

Borneo lowland rain forests 2008

The soils are either highly weathered lateritic clays (oxisols or ultisols) or very young inceptisols.

Marianas tropical dry forests 2008

Soils are predominantly inceptisols, but entisols are also common in the slopes and areas exposed to erosion.

Venezuelan Andes montane forests 2008

Soil types have not been well defined; however, most soils are entisols with alfisols and inceptisols in upland areas.

Arizona Mountains forests 2008

Montane soils are primarily inceptisols and ultisols.

Borneo montane rain forests 2007