Agrotermos

Preferred term

Leptosols

Leptosols comprise very thin soils over continuous rock and soils that are extremely rich in coarse fragments. Leptosols are particularly common in mountainous regions. Leptosols include Lithosols of the Soil Map of the World (FAO–UNESCO, 1971–1981), Lithic subgroups of the Entisol Order (United States of America), Leptic Rudosols or Tenosols (Australia), and Petrozems and Litozems (Russia). In many national systems and in the Soil Map of the World, Leptosols on calcareous rocks belong to Rendzinas and those on other rocks to Rankers. Continuous rock at the surface is considered nonsoil in many soil classification systems.

World Reference Base soil types

French

Created

2021-09-30T08:50:42Z

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

da0af025

Leptosols

Portuguese

Created

2021-09-30T08:50:42Z

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

da0af025

Leptosols

Portuguese (Brazil)

Created

2021-09-30T08:50:42Z

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

da0af025

Leptosols

Spanish

Created

2024-07-03T16:11:42Z

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

da0af025

Leptosol

URI

http://aims.fao.org/aos/agrovoc/c_da0af025

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Created 1/20/20, 11:55 AM, last modified 9/30/24, 11:30 AM