TOP LAYER OF THE EARTH WHICH HAS SLOWLY FORMED THROUGH DECOMPOSITION OF THE UNDERLYING ROCK MATERIAL (PARENT ROCK) UNDER THE ACTION OF ATMOSPHERIC CONDITIONS (CLIMATE) AND VEGETATION OR THROUGH THE DEPOSIT OF MATERIALS TRANSPORTED BY RIVERS, SEAS (ALLUVIAL SOILS) OR THE WIND (“LOESS OR VOLCANIC ASH SOILS).
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
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