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Strato superiore della crosta terrestre, formatosi lentamente dalla decomposizione del materiale roccioso soggiacente (roccia madre), per l’azione delle condizioni atmosferiche (clima) e della vegetazione o mediante depositi di materiali trasportati dai fiumi, dai mari (terreni alluviali) o dal vento (“loess” o terreni di ceneri vulcaniche).
Last Posts
Iraq’s flag raised at IOC headquarters to celebrate its membership
The International Olive Council (IOC) celebrated the Republic of Iraq’s membership today with a flag-raising ceremony at its headquarters in Madrid on 21 October, bringing together ambassadors and diplomatic...
IOC and UPB sign MoU
Portugal / Spain / 21.10.2026
The International Olive Council (IOC) and the Bragança Polytechnic University (UPB) in Portugal have signed a Memorandum of Understanding (MoU) to strengthen cooperation in the olive sector. The agreement was signed by Mr...
This week on OHIS
Madrid, Spain / 20.10.2026
This week on the Olive Health Information System website The newsletter of the University of Navarra and the IOC dedicated to health Article 1 Understanding the biological mechanisms through which the Mediterranean dietary...
