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The 55 pages that link to Stratovolcano, each with the reason it gives.

• Shield volcanoCompared with: Its steeper slopes and more varied deposits contrast with shield construction.

• AndesiteRelated: Andesite commonly erupts from stratovolcanoes at subduction zones.

• Mount St. HelensNarrower topic: Mount St. Helens’s layered cone is characteristic of this volcano type.

• Mount FujiNarrower topic: Fuji’s symmetrical cone was built by repeated eruptions that formed a classic stratovolcano.

• Flood basaltCompared with: Flood basalts spread from fissures across regions rather than building a single steep cone.

• Cinder coneCompared with: Its size and alternating layers distinguish it from a cone built mostly from loose fragments.

• VolcanoBroader topic: Its layered structure reflects repeated effusive and explosive activity.

• Mount EtnaNarrower topic: Etna’s layered cone is the defining structure of this volcano type.

• Mount RainierNarrower topic: Rainier’s layered volcanic structure defines its form and eruption style.

• Trans-Mexican Volcanic BeltNarrower topic: Several prominent belt volcanoes, including Popocatépetl, are stratovolcanoes.

• Mount KilimanjaroNarrower topic: Kilimanjaro’s cones belong to this broad type of volcanic landform.

• Mount TamboraNarrower topic: Tambora’s layered cone identifies it as this kind of volcano.

• Fissure eruptionCompared with: Its familiar summit-vent eruptions differ from the linear vent pattern of fissure eruptions.

• Mount ElbrusNarrower topic: Elbrus’s volcanic structure gives its summit massif a broad, twin-peaked form.

• Mount PeléeNarrower topic: Pelée's steep layered structure is characteristic of this volcano type.

• Mount DamavandNarrower topic: Damavand’s layered cone gives it the characteristic form of this volcano type.

• Volcanic coneBroader topic: Its broad, layered edifice contrasts with cones made chiefly of loose fragments.

• Izu IslandsRelated: Several Izu Islands contain steep volcanic edifices built through repeated eruptions.

• Klyuchevskaya SopkaNarrower topic: Klyuchevskaya Sopka’s layered cone is the defining structure of this volcano type.

• Mount AraratNarrower topic: Ararat’s broad volcanic massif is commonly described as a stratovolcano.

• Pico IslandNarrower topic: Mount Pico’s profile and layered construction fit this volcanic form.

• 1883 eruption of KrakatoaNarrower topic: Krakatoa was a volcanic island formed by this common, often explosive volcano type.

• Mount HoodNarrower topic: Mount Hood’s layered cone and explosive history fit this volcano type.

• Mount KenyaNarrower topic: Mount Kenya’s original volcanic edifice formed through repeated eruptions of this kind.

• Mount MerapiNarrower topic: Merapi’s layered structure explains its steep slopes and varied eruptive deposits.

• NevisNarrower topic: Nevis Peak is the island’s volcanic summit.

• PopocatépetlNarrower topic: Popocatépetl’s layered cone and explosive activity fit this common volcano form.

• Mount ShastaNarrower topic: Shasta’s overlapping cones and layered deposits give it this broad volcanic form.

• São Jorge IslandRelated: São Jorge’s volcanic relief reflects repeated eruptions along its central ridge.

• São Miguel IslandNarrower topic: São Miguel’s major volcanic massifs are stratovolcanoes shaped by repeated eruptions.

• SupervolcanoCompared with: Stratovolcanoes can erupt explosively, but their eruptions are generally far smaller than supereruptions.

• AvachinskyNarrower topic: Avachinsky’s steep cone is the defining form of this volcano type.

• KoryakskyNarrower topic: Koryaksky’s layered cone is the defining form of this volcano type.

• LlullaillacoNarrower topic: Llullaillaco’s cone is classified as a stratovolcano.

• Mount BromoCompared with: Bromo is a small cone within a caldera, unlike a typical large stratovolcano.

• Nevado SajamaNarrower topic: Sajama’s cone belongs to this volcano type, shaped by accumulated eruptions.

• Ojos del SaladoNarrower topic: This volcanic form describes Ojos del Salado’s broad geological type.

• OmetepeRelated: Both Concepción and Maderas are stratovolcanoes, giving Ometepe its twin-peaked profile.

• Pico de OrizabaNarrower topic: Pico de Orizaba’s layered volcanic cone is characteristic of this volcano type.

• TeideNarrower topic: Teide’s layered cone gives it this characteristic volcanic form.

• Whakaari / White IslandRelated: Whakaari’s volcanic edifice is a submerged stratovolcano with its summit above sea level.

• Complex volcanoCompared with: A stratovolcano can be one component of a complex, rather than the whole multi-center structure.

• Daisetsuzan Volcanic GroupRelated: Several peaks in the group are understood through this common volcano form.

• GalerasNarrower topic: Galeras’s layered cone and steep slopes place it in this volcano class.

• Glacier PeakNarrower topic: Glacier Peak’s steep cone and alternating eruptive deposits fit this broad volcano type.

• HeklaNarrower topic: Hekla’s layered cone gives it the profile of this volcano type.

• Irazú VolcanoNarrower topic: Irazú’s layered cone and explosive activity fit this volcanic form.

• MayonNarrower topic: Mayon’s layered deposits and steep profile are characteristic of this volcano type.

• MistiNarrower topic: Misti’s cone and layered deposits place it in this volcanic form.

• Mount AsamaNarrower topic: Asama’s cone consists of layered deposits produced by repeated eruptions.