EDAPHOLOGY

Soil Types

The origin of the soils in the municipality dates back to the Tertiary period. The soil units identified in the study area correspond to Chromic Cambisol Bc, Eutric Regosol Re, Eutric Fluvisol Je, Haplic Feozem Hh, Luvisolic Feozem Hl, Chromic Luvisol Lc, and Ferric Luvisol Lf. Due to their extent, the predominant units are Haplic Feozem, Chromic Luvisol, and Eutric Regosol.

Feozem:Dark-colored soil (rich in organic matter) Litosol:Soil with a depth of less than 10 cm Regosol:Soil with an ocheric or gleic horizon at more than 50 cm, coarse texture, without clay accumulations, without evidence of cambic or oxic horizons, never albic Luvisol:Other soils with argillic B horizon.

SIMBOLOGY

Guadalajara-Tepic Highway

Railway Line

Delimitation of Cultural

Landscape

Feozem Soil

Litosol Soil

Luvisol Soil Regosol Soil

Santiago River

SOURCE: Self elaborated with INEGI information 0