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Capa superior de la corteza terrestre, formado lentamente a partir de la descomposición del material rocoso subyacente (roca madre) por acción de las condiciones atmosféricas (clima) y de la vegetación, o mediante el depósito de materiales transportados por los ríos, los mares (suelos aluviales) o el viento (“loess” o suelos de cenizas volcánicas).
Last Posts
THIRD WORKSHOP ON THE HARMONISATION OF IOC-RECOGNISED PANELS
Madrid, Spain / 29.09.2022
The Standardisation and Research Unit held the third workshop to harmonise tasting panels with IOC-recognition from 14 to 16 September 2022. As per its programme of activities for 2022, the Standardisation and Research Unit...
4th Yale International Symposium on Olive Oil and Health
Roma, Italia / 28.09.2022
The fourth edition of the Yale International Symposium on Olive Oil and Health was held in Rome (Italy) from 15-18 September 2022. The event was hosted by the Yale School of Public Health, the University of Rome Tor Vergata,...
IOC expert meeting on the organoleptic assessment of virgin olive oils
On 20 and 21 September 2022, the Standardisation and Research Unit held a videoconference for 40 experts on the organoleptic assessment of virgin olive oils, the majority of whom were panel leaders from around the world....
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