The boron resources of Chile are all located in the northern part of the co
untry mainly in the evaporitic basins known as 'salares' (salt flats) and a
re genetically related to Upper Tertiary - Quaternary volcanic activity. Th
e most important deposits are located in the Andean basins of the Altiplano
at Surire, Ascotan, Aguas Calientes Norte, Quisquiro, Aguas Calientes Sur,
Maricunga and Pedernales. In addition other Altiplano basins may have boro
n resources, but have yet to be evaluated. The borates are present primaril
y in horizons known as 'barras' and usually form lenses wh ich interdigitat
e with evaporitic and elastic detrital sediments. In other instances boron
minerals form nodules referred to as 'papas' which are up to decimeters in
diameter. Economic accumulations of boron are always located within the fir
st few meters of the saline deposits. The only Chilean economic boron-beari
ng mineral is ulexite, a Ca-Na berate; other minerals appear in minor amoun
ts. Boren is also present in the lithium-rich brines of the Salar de Atacam
a from which boron can be recovered as by-product of lithium extraction (0,
84 g/l as polyborates). A third, and far less important type of deposit, Is
present in the Pampa del Tamarugal within berate-rich horizons associated
with paleosols. Finally, other boron accumulations, currently not exploitab
le, are associated with geothermal brines and the nitrate industry, both as
by-products.