Pleistocene sediments found around Kandivali in northern Bombay by Todd in 1939 indicate that these islands were inhabited since the Stone Age.

Pleistocene sediments found near Kandivali in northern Mumbai by British archaeologist Todd in 1939 suggest that these islands were inhabited since the South Asian Stone Age.

Pleistocene non-marine sediments are found primarily in fluvial deposits, lakebeds, slope and loess deposits as well as in the large amounts of material moved about by glaciers.

Fossil leaves from Early Pleistocene sediments at Regatta Point in Western Tasmania show similarities to E. lucida and suggest a close relationship.

The surface Paso Robles and Careaga formations are Pleistocene sediments.

Pleistocene sediments found near Kandivali in northern Mumbai by British archaeologist Todd in 1939 indicate habitation since the Stone Age.

The oldest fossils of the species are known from Early Pleistocene sediments deposited off the coast of Luzon in the Philippines.

This is a Geological Conservation Review site because temporary exposures here have shown Pleistocene sediments, including interglacial fluvial sands and marine gravels and cold-stage fluvial gravels.

Pleistocene sediments found along the coastal areas around Kandivali in northern Mumbai suggest that the islands were inhabited since the Stone Age.

It is known only from fossil leaves and fruiting "cones" found in Late Pleistocene sediment at Melaleuca Inlet in western Tasmania.