Linked from

The 32 pages that link to Lava dome, each with the reason it gives.

• StratovolcanoCompared with: A dome is a localized lava buildup, unlike the broad, layered edifice of a stratovolcano.

• LaharRelated: Dome collapse can produce debris that becomes a lahar when mixed with water.

• Lava flowCompared with: Unlike spreading flows, dome-building lava resists movement and accumulates near its source.

• Shield volcanoCompared with: Its thick lava piles near the vent instead of spreading into shield-like slopes.

• AndesiteBroader topic: Silica-rich andesitic lava can be viscous enough to build domes.

• Mount St. HelensBroader topic: Dome growth inside the crater has marked episodes of Mount St. Helens’s post-1980 activity.

• LavaBroader topic: Very viscous lava can build a dome instead of spreading into a long flow.

• Pyroclastic density currentRelated: Dome collapse can release hot blocks and ash as a block-and-ash flow.

• Cinder coneCompared with: A lava dome is built by piled-up lava, not by fragments falling around the vent.

• Phreatic eruptionCompared with: Dome growth involves erupted magma, whereas phreatic explosions can occur without new magma reaching the surface.

• Explosive eruptionRelated: Dome growth can obstruct vents, building pressure and triggering explosive activity.

• Fissure ventCompared with: Dome growth concentrates viscous lava near an outlet rather than spreading it along a crack.

• Lava lakeCompared with: Unlike a lake, a dome is mostly solidified lava piled above its vent.

• ParícutinRelated: Parícutin’s later activity included dome growth within its volcanic complex.

• Mount PeléeRelated: Viscous lava built a dome at Pelée before repeated collapses generated destructive flows.

• Puy de DômeBroader topic: Its summit formed from viscous trachytic lava that piled up rather than flowing far.

• Volcanic coneCompared with: It forms a mound rather than the familiar cone built by outward-falling deposits.

• Lava fieldCompared with: A dome is a localized lava landform, unlike the broad area covered by a lava field.

• Mount MerapiRelated: Dome growth and collapse are central to Merapi’s frequent explosive activity.

• 1902 eruption of Mount PeléeRelated: Dome growth at Mount Pelée preceded the deadly flow.

• Chaîne des PuysBroader topic: Several Puys formed as thick lava piled up near its source.

• Mount ShastaRelated: Lava domes have formed within Shasta’s summit craters during its eruptive history.

• AvachinskyRelated: Dome growth and collapse have accompanied explosive activity at Avachinsky.

• David A. JohnstonRelated: A growing lava dome was among the visible changes monitored during the 1980 crisis.

• McDonald IslandsRelated: Lava domes have formed during eruptions on McDonald Island.

• Volcanic plugCompared with: A dome builds up at the vent; a plug solidifies within the conduit.

• Complex volcanoBroader topic: Dome growth can add local relief and new eruptive centers to a complex structure.

• Jebel MarraRelated: Lava domes occur among the massif’s volcanic features.

• MayonBroader topic: Dome growth at Mayon’s summit can destabilize and produce hazardous pyroclastic flows.

• Mount AsamaBroader topic: Asama’s summit area includes lava-dome formations associated with its eruptive history.

• Mount UnzenNarrower topic: Unzen’s 1990s eruption built a lava dome that repeatedly collapsed into pyroclastic flows.

• Volcán de AguaRelated: Dome growth is one process that can shape stratovolcanoes, though it is not the defining feature of Volcán de Agua.