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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
Advanced course on olive growing and climate change
Madrid / 21.07.2021
The International Olive Council (IOC) and the Mediterranean Agronomic Institute of Zaragoza (IAMZ) have planned to organise an advanced course on Olive Growing and Climate Change from 27 September to 1 October 2021. Given...
LATEST NEWS FROM OHIS
Madrid / 19.07.2021
The OHIS is the result by an agreement between the International Olive Council, the world’s only international intergovernmental organisation in the field of olive oil and table olives and the School of Medicine of...
STANDARDISATION AND RESEARCH: NEXT MEETINGS
Madrid / 16.07.2021
15 – 17 September: The second edition of the workshop on panel harmonisation, in which 100 panels approved by the IOC will taste samples of olive oil. The objective of the workshop is to harmonise panels, minimise...
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