Hydrological changes and landform evolution since the Bølling-Allerød interstadial in the Eastern Great Rann of Kachchh, India
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The post-glacial (Bølling-Allerød) sedimentary archive preserved in the Eastern Great Rann of Kachchh (EGRK) is used to reconstruct the pattern of Indian Summer Monsoon (ISM) variability, landform evolution, and the impact on the Indus Valley Civilization (IVC). Employing the sedimentology, geochemistry, and chronology supported by statistical analysis, four major phases of strengthened and weakened monsoon conditions are inferred. The pattern of geochemical variability during Phase-I (13.6 ka and 12.7 ka) indicates a relatively wetter condition (improved ISM); following this, during phase-II (11.9 ka and 11.1 ka), the ISM strength weakened. However, the ISM began to restrengthen during the phase-III (11 ka and >5 ka), with fluctuations. The phase-IV
Chronology · Ephemeral key · Indus · Landform · Lithology · Monsoon · Palaeochannel · Sedimentary rock · Stadial · STREAMS · Geology and Paleoclimatology Research · Hydrology and Sediment Transport Processes · Landslides and related hazards
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