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Fine-grained sediments can stay in the air and be transported by wind as suspended load.
The finer‐grained clastic sedimentary rocks are referred to as shale, siltstone, and mudstone. Shale is a easy, thinly layered rock this is made up of fine‐grained silt and clay debris. Shale is taken into consideration a fissile rock as it splits very certainly along its layers.
High-quality-grained sediments associated with low-power conditions have proved to be useful archives of relative sea-stage statistics. Low-strength intertidal environments, such as saltmarshes and mangroves, are intently connected to the tidal body
Sediments gathering in those environments, and the plant and animal remains they contain, can therefore be used to reconstruct the former position of relative sea degree in time and space. a number of methodologies using a blended lithostratigraphic.
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