Share
Capa superior de la corteza terrestre, formado lentamente a partir de la descomposición del material rocoso subyacente (roca madre) por acción de las condiciones atmosféricas (clima) y de la vegetación, o mediante el depósito de materiales transportados por los ríos, los mares (suelos aluviales) o el viento (“loess” o suelos de cenizas volcánicas).
Last Posts
IOC hosts 2nd Olive Oil World Congress presentation
MADRID, SPAIN / 04.02.2026
The International Olive Council (IOC) hosted a presentation of the second edition of the Olive Oil World Congress (OOWC) at its headquarters in Madrid on 4 February 2026, as part of efforts to strengthen the event’s...
Olive oil diplomacy: Embassies sample excellence at the IOC
MADRID, SPAIN / 03.02.2026
The International Olive Council (IOC) welcomed today a group of agricultural counsellors from several European embassies in Madrid for a dedicated virgin olive oil tasting session at its headquarters. The event was held at...
IOC Joins VI AOVE Forum Internacional
ALICANTE, SPAIN / 29.01.2026
Highlighting mediterranean cooperation in the olive sector The International Olive Council (IOC) is taking part in the VI AOVE Fórum Internacional – Fira de Tots Sants de Cocentaina, a key event promoting...
