The piedmont area
has granitic, rocky, clay soils that are very poor in organic material,
while the flatland soils are clay with a gravel subsoil; both areas
are generally alkaline.
Water for irrigation comes from the Andes Mountains through an
interconnected system of reservoirs with a total storage capacity
of approximately 1 billion square meters.
The water is brought to the lowland farms through a complex network
of canals and pipelines built exclusively for transporting irrigation
water.
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