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).
This week on OHIS
Madrid, Spain / 14.07.2026
This week on the Olive Health Information System website The newsletter of the University of Navarra and the IOC dedicated to health Article 1 Recent scientific evidence reinforces the benefits of the Mediterranean diet and...
Lisbon brings together the global olive sector to analyse the challenges of an expanding market
The 123rd session of the IOC Council of Members examined trends in global consumption, priority areas for action in the coming months and the challenges posed by climate change On 29 and 30 June, the Portuguese capital...

