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Statements

Subject Item
dbr:Parna_(geology)
rdfs:label
Parna (geology)
rdfs:comment
Parna is a windblown sediment, in many ways similar to loess. It is found in the Riverina Plains, in south-east Australia. It was named by Bruce Butler, a pedologist working for CSIRO in 1956.. Parna is an aeolian deposit, like loess, but the particles are small clay mineral agglomerates. The material sources are dried up lakes and river floodplains. It has been described as calcareous red clay material, of aeolian origin, that blankets large parts of the Murrumbidgee and Murray River valleys.
dct:subject
dbc:Clay_minerals_group
dbo:wikiPageID
53480377
dbo:wikiPageRevisionID
810016504
dbo:wikiPageWikiLink
dbr:Loess dbc:Clay_minerals_group dbr:CSIRO
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n5:2qRwA wikidata:Q30594566
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dbt:Reflist dbt:Silicate-mineral-stub
dbo:abstract
Parna is a windblown sediment, in many ways similar to loess. It is found in the Riverina Plains, in south-east Australia. It was named by Bruce Butler, a pedologist working for CSIRO in 1956.. Parna is an aeolian deposit, like loess, but the particles are small clay mineral agglomerates. The material sources are dried up lakes and river floodplains. It has been described as calcareous red clay material, of aeolian origin, that blankets large parts of the Murrumbidgee and Murray River valleys.
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wikipedia-en:Parna_(geology)?oldid=810016504&ns=0
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1164
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wikipedia-en:Parna_(geology)