🌋 Volcano Cross-Section (2D): Magma Chamber Pressure, Conduit Flow, Plume Height and Lava Flow Lab
2D volcano cross-section: a recharged magma chamber builds overpressure, a Poiseuille conduit sets the flux, Henry-law gas fraction decides fragmentation, plume height follows fits to real eruptions and a lava flow stops by cooling, with live graphs and in-page numerical checks.
⚙ Under the hood
2D volcano cross-section: a recharged magma chamber builds overpressure, a Poiseuille conduit sets the flux, Henry-law gas fraction decides fragmentation, plume height follows fits to real eruptions and a lava flow stops by cooling, with live graphs and in-page numerical checks.
volcanomagma chamberplume heightlava flowviscosity
2D · HTML5 Canvas 2D · 60 FPS target · runs fully client-side, no install