Loess
Query URLs
https://term.museum-digital.de/md-de/tag/56406
- Note
- "A loess (US: /ˈlɛs, ˈlʌs, ˈloʊ.əs/, UK: /ˈloʊ.əs, ˈlɜːs/; 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 loesses or similar deposits.
A loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay with 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, they are homogeneous and highly porous and have vertical capillaries that permit the sediment to fracture and form vertical bluffs." - (en.wikipedia.org 01.09.2023)
-
Negatív/pozitív nagyítás
Lakóház a háttérben...
Object information
Image: Viski Károly Múzeum Kalocsa - RR-F -
Negatív/pozitív nagyítás
Présház a löszfal előtt.
Object information
Image: Viski Károly Múzeum Kalocsa - RR-F -
Negatív/pozitív nagyítás
Löszfal pincelyukkal.
Object information
Image: Viski Károly Múzeum Kalocsa - RR-F -
Negatív/pozitív nagyítás
Löszfal pincelyukakkal.
Object information
Image: Viski Károly Múzeum Kalocsa - RR-F
[]