Volcanic eruptions influence the Earth system across timescales ranging from days to millions of years. This paper examines how repeated and large-magnitude volcanism affects the atmosphere, hydrosphere, biosphere, and lithosphere, with emphasis on the distinction between short-term disturbances and cumulative geological impacts. Explosive eruptions can inject sulfur dioxide into the atmosphere, producing sulfate aerosols and temporary surface cooling, whereas prolonged volcanic activity can release carbon dioxide and contribute to longer-term warming. Volcanic gases and ash can also alter soil and water chemistry, promote acidification, modify nutrient supply, and contribute indirectly to marine deoxygenation. At the same time, repeated lava emplacement and intrusive activity reshape landscapes and crustal structure. The environmental significance of large volcanic episodes is further illustrated through the Siberian Traps, Central Atlantic Magmatic Province, and Deccan Traps, which are compared in terms of scale, gas emissions, climatic responses, and biodiversity change. Overall, volcanism produces interconnected environmental effects whose magnitude and persistence depend strongly on eruption duration, frequency, composition, and geological context.
Research Article
Open Access