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Arenal Volcano in Costa Rica is situated along the Central American Volcanic Arc, formed by subduction of the Cocos Plate beneath the Caribbean Plate, and is widely recognized as a classic open-vent system that sustained continuous activity from 1968 to 2010. During this period, persistent Strombolian eruptions, lava effusion, and steady summit degassing reflected efficient gas escape from a shallow magmatic conduit, limiting overpressure and large explosive events. Summit fumaroles served as the primary pathway for volatile release, emitting high-temperature magmatic gases dominated by H₂O, CO₂, and SO₂, with minor H₂S, HCl, and HF. Following the cessation of eruptive activity in 2010, Arenal entered a quiescent state characterized by weak, steam-rich summit fumaroles with minimal SO₂ output, suggesting a transition from magmatic to hydrothermal degassing and the absence of significant shallow magma recharge. In 2022 we designed a digital model of the Arenal Volcano summit to support the hazard mitigation and public safety initiatives of Costa Rica.