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).
IOC Newsletter 165: latest issue
Madrid / 30.07.2021
Welcome, here are the latest news from the Executive Secretariat of the International Olive Council, including stats on world market trends for olive oil and table olives, with information on prices per product on the main...
World catalogue of the main olive tree varieties
Madrid / 29.07.2021
The Executive Secretariat held a virtual meeting to discuss the World catalogue of the main genetically authenticated olive tree varieties. Some of the world’s most important experts on the cataloguing of varieties...