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As discussed above, the type of sphere does not affect the intermediate stage of sedimentation behavior, however the final sphere depth depends significantly on the material.
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The clear record of the final stages of sedimentation and ancient pedogenesis within profiles of soils in bipartite sediments may help to derive paleoclimatic interpretations from the last interglacial - glacial cycle till present.
The final stages of sedimentation within the Wainway Channel record its progressive infilling and final inning at c. ad 1600.
Over these stages, dependencies of sedimentation processes to the rate of sea-level rise are obvious.
The upper part of the Ecca Group reflects a filled stage of shallow marine sedimentation followed by the overfilled style of fluvial sedimentation of the overlying Beaufort and Stormberg groups (Catuneanu et al. 2005).
Staged process of sedimentation resulted in polygenetic soil profiles.
Changes in facies associations and palaeosol types enable to distinguish three stages in evolution of sedimentation and landscapes.
The settled water had an elevated level of Al3+ and it can be attributed to the aluminium sulphate added at this stage of treatment for flocculation and sedimentation.
Schematic models of (a) past lake setting after glacial erosion (i.e., the initiation of sedimentation processes during the marine phase) and (b) present lake setting (lacustrine stage).
The earlier phases of sedimentation are tectonic-controlled, however later stages appear to be linked to global eustatic changes.
The subsequent warming combined with a decrease of precipitation at the second half of the first millennium BC caused the stabilization of sedimentation and the beginning of the current stage of soil formation in the region.
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