Depositional models 2025

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Depositional landforms consist of (but are not limited to) drumlins, erratics, moraines, eskers, and kames. Depositional landforms can be used to reconstruct former ice mass extent and movement.
The many depositional environments which can be grouped into three major categories - marine, transitional, and continental.
Sketch representing the four main types of depositional features observed on mixed systems: down-slope elongated mounded drifts (A), channel-drifts (B), channel-levees / levees (C), and submarine fans / lobes (D).
Depositional landforms include beaches (sandy and pebble), sand dunes, spits, and bars.
In coastal environments, sediments are deposited along or near a coastline by low-energy waves that can no longer support their sediment load. Material carried by the sea is washed up by the water and begins to build up along the coastline, creating beaches and other coastal features such as spits and shoals.
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5.5: Depositional Environments LocationSedimentCommon Rock Types Alluvial mud to boulders, poorly sorted clastic rocks Lacustrine (lake) fine-grained laminations shale Paludal (swamp) plant material coal Aeolian (dunes) very well-sorted sand and silt sandstone12 more rows Nov 6, 2023
Spits. form where the coastline changes direction and longshore drift continues to move material along the beach. Longshore drift will deposit material in the sea after the coastline has changed direction. Over time the level of the sand deposited will build-up until it is above sea level.

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