Along the coast of East and South India, a slow and minor sea level fa
ll as an immediate response to the Last Glacial Maximum (LGM) followed
by strong aridity and fast retreat of the sea to the outer shelf are
indicated by coastal ironstones, traces of channels in nearshore shall
ow seismic reflectors, and submerged, structureless, multimineral plac
er sands. Nearshore peat beds and inland beach ridges reflect perturba
tions during Early to Mid-Holocene sea level rise. The Little Ice Age
witnessed shifts in littoral sediment budget, possibly as a result of
reduced transport of sediments from the Himalaya to the Bay of Bengal.