An Elevated Seabed
Neduntheevu, or Delft Island, is a flat, oval landmass of about 50 square kilometers in the Palk Strait. Geologically, it is an uplifted section of the seabed, composed primarily of coralline material, limestone, and other marine deposits from the Eocene, Miocene, and Pliocene eras. The island has a low relief, mostly under 5 meters above sea level, and lacks any rivers or lakes. Its freshwater comes from rainfall collected in natural depressions. The soil is thin, sandy, and coarse, overlying the coral bedrock. These soils, identified as Solodized Solonetz and Grumusols, are highly salinized.
The climate is semi-arid, with an average annual rainfall around 500 mm. A long dry season lasts from February to September, followed by a wet season from October to January. This environment, combined with the porous coral-based geology, creates hypersaline conditions in the island's salt marshes and tidal flats. These extreme conditions limit the types of vegetation that can survive, making the island a natural laboratory for studying plant adaptations to salinity. The island's flora is classified as belonging to the AI floristic zone, typical of Sri Lanka's coastal and marine belts.