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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 PhD scholarships
Madrid / 07.04.2021
As part of its technical cooperation and training programme, the International Olive Council (IOC) has awarded four PhD scholarships to students from its member countries for a period of four years dedicated to scientific...
A delegation from Libya visits the University of Córdoba
Cordoba / 05.04.2021
Following the bilateral meeting held at the IOC headquarters between the Executive Secretariat and a delegation from the Government of Libya dedicated to the development of the country’s olive sector, it was decided to...
IOC Newsletter 161
Madrid / 31.03.2021
Here is the latest edition of the IOC newsletter. It is our duty, but above all our pleasure, to give our dear readers the latest news from the olive oil sectors in our member countries and around the world. In addition to...
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