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 / 08.05.2025
This week on the Olive Health Information System website The newsletter of the University of Navarra and the IOC dedicated to health Diet is recognized as a modifiable risk factor in the prevention and treatment of...
Highlighting the Role of Regenerative Agriculture in the Olive Sector
On 28 April 2025, Deputy Executive Director of the International Olive Council (IOC), Abderraouf Laajimi, took part in the “El secreto está en el suelo” (“The secret is in the soil”) conference on regenerative...