Explore the change:
Click on the map to view a specific ecoregion
Ecoregions represent and classify our planet's biodiversity. These biogeographic regions are relatively large units of land or water containing a distinct combination of natural communities that have a majority of species and environmental conditions in common.
Soil having an argic horizon, CECclay < 50%.
Soil having an argic horizon and albeluvic tonguin.
Soil having an argic horizon with CECclay >24 and BS < 50%.
Soil having an andic or vitric horizon.
Soil having a coarse texture up to >100 cm depth.
Soil having a calcic or petrocalcic horizon.
Soil having a cambic horizon.
Soil having a chernic or blackish mollic horizon.
Soil having a cryic horizon.
Soil having a duric or petroduric horizon.
Soil having a ferralic horizon.
Soil having a fluvic materials.
Soil having a gleyic properties.
Soil having a gypsic or petrogypsic horizon.
Soil having organic matter >40 cm depth.
Soil having a brownish mollic horizon and secondary CaCO3.
Shallow soils, <=25 cm deep
Soil having an argic horizon and CECclay <24.
Soil having an argic horizon and CECclay >24.
Soil having a nitic horizon.
Soil having a mollic horizon.
Soil having reducing condition and pedogenetic abrupt textural change.
Soil having plinthite or petroplinthite.
Soil having a spodic horizon.
Soil without a diagnostic horizon
Soil having a salic horizon.
Soil having a natric horizon.
Soil having reducing condition.
Soil having an umbric horizon.
Soil having a vertic horizon.
Soil data is based on predictions for basic soil properties, such as pH (in water), texture fractions, coarse fragments, bulk density, total nitrogen, organic carbon concentration and cation exchange capacity.
Source: International Soil Reference and Information Centre SoilGrids™ system.