loess$45299$ - definizione. Che cos'è loess$45299$
Diclib.com
Dizionario ChatGPT
Inserisci una parola o una frase in qualsiasi lingua 👆
Lingua:

Traduzione e analisi delle parole tramite l'intelligenza artificiale ChatGPT

In questa pagina puoi ottenere un'analisi dettagliata di una parola o frase, prodotta utilizzando la migliore tecnologia di intelligenza artificiale fino ad oggi:

  • come viene usata la parola
  • frequenza di utilizzo
  • è usato più spesso nel discorso orale o scritto
  • opzioni di traduzione delle parole
  • esempi di utilizzo (varie frasi con traduzione)
  • etimologia

Cosa (chi) è loess$45299$ - definizione

WINDBLOWN SEDIMENT
Loess soil; Loessic; Glacial loess; Loesses; Loess Plain; Loess Plains; Löss
  • An [[outcrop]] of loess in [[Patagonia]]
  • display-authors=etal}}</ref>
  • Loess in [[Vicksburg, Mississippi]], United States
  • Loess near [[Hunyuan]], [[Datong]], [[Shanxi]], China
  • [[Medicinal clay]] produced by [[Luvos]] The clay is composed of loess with a fineness grade of 1.
  • Loess from the [[Rhine]] lowlands near [[Mannheim]] with calcareous concretions

Loess         
·noun A quaternary deposit, usually consisting of a fine yellowish earth, on the banks of the Rhine and other large rivers.
Loess         
Loess (, ; from ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits.
loess         
['l???s, l?:s]
¦ noun Geology a loosely compacted yellowish-grey deposit of wind-blown sediment.
Derivatives
loessial adjective
loessic adjective
Origin
C19: from Ger. Loss, from Swiss Ger. losch 'loose'.

Wikipedia

Loess

Loess (US: , UK: ; from German: Löss [lœs]) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits.

Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. Usually it is homogeneous and highly porous; it is traversed by vertical capillaries which permit the sediment to fracture and form vertical bluffs.