@prefix agrovoc: <http://aims.fao.org/aos/agrovoc/> .
@prefix rdf: <http://www.w3.org/1999/02/22-rdf-syntax-ns#> .
@prefix ns0: <http://art.uniroma2.it/ontologies/vocbench#> .
@prefix dc: <http://purl.org/dc/terms/> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .

agrovoc:xDef_30982cbe
  rdf:value "Regosols are very weakly developed mineral soils in unconsolidated materials that do not have a mollic or umbric horizon, are not very thin or very rich in coarse fragments (Leptosols), not sandy (Arenosols), and not with fluvic materials (Fluvisols). Regosols are extensive in eroding lands and accumulation zones, particularly in arid and semiarid areas and in mountainous terrain. Many Regosols correlate with soil taxa that are marked by incipient soil formation such as Entisols (United States of America), Rudosols (Australia), Regosole (Germany), Sols peu évolués régosoliques d’érosion or even Sols minéraux bruts d’apport éolien ou volcanique (France), Pelozems (Russia) and Neossolos (Brazil)."@en ;
  ns0:hasSource "IUSS Working Group WRB. 2015. World Reference Base for Soil Resources 2014, update 2015 International soil classification system for naming soils and creating legends for soil maps. World Soil Resources Reports No. 106. FAO, Rome." ;
  dc:created "2020-01-20T14:46:31.652+01:00"^^xsd:dateTime ;
  dc:modified "2025-01-31T12:46:29"^^xsd:dateTime .

agrovoc:c_6492 skos:definition agrovoc:xDef_30982cbe .