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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
IOC receives a delegation from ‘Mujer Alma de Olivo’
Madrid, Spain / 16.06.2026
On 16 June 2026, the headquarters of the International Olive Council (IOC) welcomed a delegation from the recently established Women Soul of the Olive Tree Association (Mujer Alma de Olivo), led by its...
IOC workshops underline the strategic importance of data and geographical indications for the future of the olive sector
The International Olive Council (IOC) concluded yesterday two specialised workshops dedicated to strengthening knowledge-sharing and international cooperation in two key areas for the olive sector: data collection and crop...
This week on OHIS
Madrid, Spain / 12.06.2026
This week on the Olive Health Information System The newsletter of the University of Navarra and the IOC dedicated to health Article 1 Recent research in the field of olive-related products continues to progress along two...
