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The cycle is restarted with another phase of erosion and sediment bypass followed by deposition which makes up the second channel-fill.
This phase of erosion and deposition was followed by a long phase of stability and pedogenetic alteration of the old colluvium.
All s-form sites provide a snapshot of the last phase of erosion after evolution of the local landscape through multiple generations of s-form formation.
The recent phase of erosion (<1000 years), which is still continuing, is probably a result of the introduction and/or intensification of agriculture, livestock husbandry and iron smelting practices in the Irangi Hills.
These sediments accumulated in a low-gradient stream system (represented by domain 1) during an early phase of slip in the SJFZ, prior to the modern phase of erosion and degradation (domain 2).
It is possible that this earlier phase of erosion relates to the initial phases of monsoon intensification whose timing is not well defined but appears to strengthen around 23 Ma based on data from the South China Sea (Clift et al. 2008).
Similar(53)
Phases of erosion, redeposition, sedimentation, and soil formation demonstrate stages of activity and stability under varying climatic conditions.
In consequence, the early stages in the development of glacial landscapes have been overprinted or erased by later phases of erosion.
These phases of erosion and sedimentation resulted in a relative large and elongated Tortonian marine valley filled with complex sedimentary structures.
We analysed the surrounding soils and used corresponding pedosignatures in the mire sediments to characterise notable phases of erosion and deposition.
The applied variables predicted carbon release well (i.e. 95% of the carbon loss was predicted) and notably both the non-equilibrium and equilibrium phases of erosion was predicted.
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