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In geology, depositional environment or sedimentary environment describes the combination of physical, chemical and biological processes associated with the deposition of a particular type of sediment and, therefore, the rock types that will be formed after lithification, if the sediment is preserved in the rock record. In most cases the environments associated with particular rock types or associations of rock types can be matched to existing analogues. However, the further back in geological time sediments were deposited, the more likely that direct modern analogues are not available (e.g. banded iron formations).
Types of depositional environments
Diagram to show the different depositional environments in which tsunami deposits are formed - partly after Shanmugam 2006 
Depositional environmental model of the Araripe Basin formations, NE Brazil
- Alluvial - type of Fluvial deposite. Caused by moving water in a fan shape (Alluvial Fan) and containing mostly impermeable and nonporous sediments well sorted.
- Aeolian – Processes due to wind activity. Often in deserts and coastal regions and well sorted, large scale cross-beds
- Fluvial - processes due to moving water, mainly streams. Common sediments are gravel, sand, and silt.
- Lacustrine - processes due to moving water, mainly lakes. Common sediments are sand, silt, and clay.
- Deltaic – Silt deposition landform at the mouth of a river (possible cross beds, ripple marks) Common sediments are sand, silt, and clay.
- Tide – Rise and fall of the sea level under astronomical gravitational influences - processes due to tidal currents, creates tidal flats (fine-grained, ripple marks, cross-beds). Common sediments are silt and clay
- Lagoonal – A shallow body of water separated from a larger body of water by barrier islands or reefs. Little transportation, creates lagoon bottom environment. Common sediments are carbonates (in tropical climates).
- Beach – Area of loose particles at the edge of the sea or other body of water. Caused by waves and longshore currents. Creates beaches, spits, and sandbars with the common sediments of gravel and sand.
- Lake – large body of relatively still water
- Shallow water marine environment - processes due to waves and tidal currents, creates shelves and slopes, lagoons. Common sediments are carbonates (in tropical climates) or sand, silt, and clay (elsewhere)
- Upper shoreface – The portion of the seafloor that is shallow enough to be agitated by everyday wave action
- Lower shoreface – The portion of the seafloor, and the sedimentary depositional environment, that lies below the everyday wave base
- Deep water marine environment – Flat area on the deep ocean floor (abyssal plains) caused by ocean currents. Common sediments are clay, carbonate mud, silica mud.
- Reef – A shoal of rock, sand, coral or similar material, lying beneath the surface of water caused by waves and tidal currents. Also creates adjacent basins. Common sediments are carbonates.
- Evaporite – A water-soluble mineral sediment formed by evaporation from an aqueous solution
- Till - angular to rounded grains, poorly sorted, unstratified (massive)
- Outwash - ripple marks, cross-beds, similar to stream channel
- Tsunami – Sedimentary unit deposited by a tsunami
Recognition of depositional environments in ancient sediments
Depositional environments in ancient sediments are recognised using a combination of sedimentary facies, facies associations, sedimentary structures and fossils, particularly trace fossil assemblages, as they indicate the environment in which they lived.
- Harold G. Reading. 1996. Sedimentary Environments: Processes, Facies and Stratigraphy. Blackwell Publishing Limited.