A 500-Million-Year Geological Story
The dramatic seascape of Hạ Long Bay consists of roughly 1,600 limestone islands and islets spread across 1,553 square kilometers. This landscape is the result of a geological history stretching back 500 million years. The process began with the formation of a more than 1,000-meter-thick layer of limestone during the Carboniferous and Permian periods (340 to 250 million years ago) in a shallow, warm sea.
Over millions of years, tectonic forces lifted this massive limestone block. A long period of erosion, lasting about 20 million years under a tropical climate, carved the stone into a classic terrestrial karst landscape of conical hills (fengcong) and isolated towers (fenglin). The current bay was formed much more recently. During the last glacial period, sea levels were lower, and this was a mountainous region. As the glaciers melted, the sea level rose, culminating in the Holocene transgression which began around 11,000 years ago. This event submerged the valleys, leaving only the tops of the karst mountains visible as the thousands of islands we see today, a drowned karst landscape.
A Mosaic of Isolated Ecosystems
The bay's complex geology creates a high degree of biodiversity. It has two main ecosystems: a tropical evergreen rainforest and a marine and coastal system. The isolation of the islands and their unique topographies—featuring caves, arches, and lagoons, have produced numerous distinct habitats. This has led to the evolution of endemic species found nowhere else. Scientists have identified at least 17 endemic plant species and 60 endemic animal species in the area.
Endemic plants include the Ha Long fan-palm (Livistona halongensis) and the Ha Long cycad (Cycas tropophylla). The bay's caves and grottos host their own specialized fauna, such as the Ha Long cave loach (Draconectes narinosus). The bay's ecosystems are diverse. The larger islands support tropical forests with mammals like macaques and squirrels. Sheltered areas contain mangrove forests, which are nurseries for marine life. In the clearer waters, coral reefs thrive, with 232 species of coral providing a habitat for hundreds of species of fish, mollusks, and crabs. The base of each limestone pillar, with its wave-cut notches and tide pools, forms a distinct intertidal ecosystem, further fragmenting habitats and driving biological diversification.