This stratigraphic sequence from bottom to top indicates a transgression or a fail in sea-level occurred in this location in the past.
Stratigraphic sequence is defined as a subdivision of geology that tries to split and link historical deposits into crustal bound units on various scales.
This also explain these stratigraphic units in terms of differences in sediment supply and variations in the rate of change in accommodation space.
While climbing in northern Arizona's Grand Canyon, a person come across an outcrop that reveals 3 distinct rock strata types.
A layer of shale is at the bottom, followed by a layer of limestone, which is then followed by a layer of sandstone.
Therefore, geologic sequence from bottom to top suggests a former sea-level transgression or failure in this site.
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