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 / 25.03.2025
This week on the Olive Health Information System website The newsletter of the University of Navarra and the IOC dedicated to health Olive oil, a key component of the Mediterranean diet, is well known for its long-term...
IOC at the Abrantes Olive Oil Symposium
Abrantes, Portugal / 24.03.2025
The International Olive Council (IOC) took part in the the Abrantes Olive Oil Symposium, held in the framework of the Iberian Olive Oil Meeting at the Abrantes Vocational School for Rural Development on 22 March 2025. The...