Geology of Sri Lanka: A Journey Through Ancient Landscapes and Unique Geological Features.

Sri Lanka’s geological landscape, predominantly composed of Precambrian strata, offers a critical window into the evolution of ancient continental fragments and the dynamics of supercontinent cycles. The island is divided into five major geological units: the Highland Complex, Vijayan Complex, Wanni Complex, Kadugannawa Complex, and Miocene sedimentary formations. Over 90% of Sri Lanka’s surface is covered by Precambrian rocks, with the Highland Complex distinguished by granulite-facies rocks such as gneisses, quartzites, marbles, and charnockites, while the Vijayan Complex is characterized by amphibolite-facies gneisses and granites. These high-grade metamorphic terrains, dating back to the Archean and Proterozoic eons, provide key insights into the assembly and breakup of the Gondwana supercontinent, particularly during the Pan-African orogeny and Gondwana’s fragmentation approximately 200 million years ago. Sri Lanka’s geological stability, attributed to its central position within the Indian plate, contrasts with its dynamic tectonic history, including the northeastward movement of the Indian plate and the Himalayan uplift around 55 million years ago. The island also hosts significant mineral resources, such as globally important graphite deposits and gem-bearing sedimentary formations, alongside fossil records spanning the Jurassic, Miocene, and Pleistocene epochs. By integrating advancements in geochronology, petrology, structural geology, and paleontology, this study synthesizes field observations, geochemical analyses, and geophysical data to construct a comprehensive model of Sri Lanka’s tectonic evolution. The findings enhance our understanding of Precambrian crustal processes, supercontinent cycles, and the formation of ancient continental nuclei, positioning Sri Lanka as a natural laboratory for studying Earth’s deep-time geological history. This research underscores the island’s significance in unraveling the complex interplay of tectonic, metamorphic, and magmatic processes that have shaped the planet over billions of years.