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Couche supérieure de la croûte terrestre formée lentement par la décomposition du matériau rocheux sous-jacent (roche-mère), par l’action des conditions atmosphériques (climat) et la végétation ou des dépôts de matières transportés par les fleuves, les mers (terrains d’alluvions) ou le vent (« lœss » ou sols constitués de cendres volcaniques).
Last Posts
THE WHITE PAPER
Madrid / 20.09.2021
Of all the cultural models of healthy, sustainable plant-forward dietary patterns and food systems, the heavily researched traditional Mediterranean Diet stands out for the inspiration it offers to American, Northern...
OLIVAE 128. WELCOME URUGUAY
Montevideo / 17.09.2021
The 128th issue of Olivae, the official magazine of the IOC, will be entirely dedicated to olive growing in Uruguay. The Council of Members approved the decision to spotlight the country at its 112th session and the College...
IOC EVENT AT EXPOLIVA 2021
Jaen / 16.09.2021
The Executive Secretariat will soon stage an important event for the world olive sector in Jaen (Spain) on 22 September 2021. The event will take place as part of Expoliva 2021, a trade fair on all things olive that will be...
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