noun a deposit of sand, clay, silt, etc., resulting from the action of flowing water
In geology, diluvium refers to sedimentary deposits left by a flood or deluge.
Archaeologists may use the term diluvium to refer to layers of sediment that have been disturbed by flooding or other natural events.
In hydrology, diluvium can refer to the effects of a large flood event on the landscape and water systems.
Diluvium may be relevant in climate science discussions about past extreme weather events and their impact on the Earth's surface.
Diluvium may be used in paleontology to describe the layer of sediment that contains fossils from a specific time period.
In geology, diluvium refers to the superficial deposits of gravel, sand, silt, and clay that have been transported and deposited by a flood or glacial action.
Archaeologists may use the term diluvium to refer to layers of sediment or debris left behind by ancient floods or catastrophic events.
Civil engineers may encounter the term diluvium when assessing the stability of soil and rock formations in areas prone to flooding or other natural disasters.
Hydrologists may study diluvium deposits to understand past flood events and predict future flooding patterns.
Environmental scientists may analyze diluvium layers to assess the impact of past floods on ecosystems and land use.