Kilauea is one of the world's most studied volcanoes, but its deep plumbing still holds mysteries. In this episode, we dive into a "bottoms-up" view of Hawaii’s magmatic system with Gaetano Ferrante, exploring how pressure changes in the deep mantle conduit propagate to the surface.While volcanologists often focus on shallow, top-down triggers like summit collapses or CO2 degassing, Gaetano’s recent research suggests that the deep mantle pathway—stretching nearly 100 km down—plays a much more active role in regulating magma supply than previously thought. We break down the mechanics of mantle plumes, the transition from magmastatic to lithostatic pressure, and why the "elastic" response of volcanic pipes might explain Kilauea’s stable behavior following the massive 2018 eruption.Inside the EpisodeThe Bottom-Up Model: Why the deep magmatic system can drive surface activity independently of shallow reservoir changes.Mantle Plume Dynamics: How hot mantle rock rises and undergoes decompression melting to fuel the Hawaiian hotspot.The CO2 Proxy: Understanding why carbon dioxide is our best "telescope" for looking 35 km beneath the island.Conduit Elasticity: How deep magma pathways deform to accommodate surges in supply rate, like the stable surge observed between 2003 and 2007.Geoid Humor: A classic geodynamics joke to wrap up the season’s deep dives.Show Timeline(00:00) Hawaii: Volcanoes, Frogs, and Microclimates(02:25) Top-Down vs Bottom-Up Eruption Dynamics(04:20) Introducing PhD Candidate Gaetano Ferrante(06:40) From Italy’s Vesuvius to Hawaii’s Hotspots(09:40) Is Kilauea a Normal Volcano?(13:30) Plumbing the 100km Deep Magma Pathway(15:10) Mapping the Summit Magma Reservoirs(19:00) Lessons from Top-Down Rift Processes(23:00) CO2 and Deep Volatile Solubilities(26:30) Magmastatic vs Lithostatic Pressure(33:45) The 2003-2007 Surge and Conduit Elasticity(40:45) Steady States and 2018 Eruption Feedback(45:50) Viscoelastic Futures and Heat Transfer(52:40) Perpendicular to the Geoid: A Science JokeLinksPapers: Bottoms up: Coupling versus decoupling within Kı̄lauea’s magma supply systemWeb: WhimsicalWavelengths.comSupport: PateronSocials: Bluesky | Instagram | FacebookWhimsical Wavelengths: Deep-dive conversations where a working scientist unpacks how we know what we know, one paper, one idea, or whimsical detour at a time. Hosted by Dr. Jeffrey Zurek (P.Geo).

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