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This approach yields information on lateral variability of facies as well as vertical sequences, which contributes to deciphering the facies geometry and stratigraphic pattern.
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These layers are called horizons, and the full vertical sequence of horizons constitutes the soil profile (see the figure).
This being so, the term cyclothem may now be extended to any sequence of sedimentary rocks that is repeated in vertical sequence.
One or more horizons make up what is known as the soil profile, the vertical sequence of distinct layers that is unique to each soil type.
Farther east, around Wapo Creek, the Era River, and Uramu Island, sacred boards had faces, but, instead of bodies, the field shows a vertical sequence of floating abstract designs, which can be read as extremely stylized anatomic elements.
Nevertheless, in spite of this variability, soils have a unique structural characteristic that distinguishes them from mere earth materials and serves as a basis for their classification: a vertical sequence of layers produced by the combined actions of percolating waters and living organisms.
The vertical sequence contains coarsening-upward inverted layered cycles with rare positive cycles.
The molecular basis of SV was inferred using three genus-wide vertical sequence datasets.
The main vertical sequence is composed of positive cycles with a small number of inverted layers and some composite cycles.
The vertical sequence is dominated by a positive rhythm, but a compound rhythm can also be seen.
There is a very general vertical sequence with more weathered material near the top and less weathered material near the bottom; however, the pattern is quite irregular.
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