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The 33 pages that link to Shield volcano, each with the reason it gives.

• StratovolcanoCompared with: Its fluid lava builds wide slopes rather than the steep layered cone typical of stratovolcanoes.

• Volcanic islandBroader topic: Repeated fluid eruptions can construct the broad, sloping form of many oceanic volcanic islands.

• Hawaiian IslandsBroader topic: Shield volcanoes built the major high islands through successive eruptions.

• KīlaueaNarrower topic: Kīlauea’s gently sloping profile is characteristic of this volcano type.

• Cinder coneCompared with: Its lava-built, gentle profile contrasts with the steep slopes of loose cinder deposits.

• VolcanoBroader topic: Its gentle slopes result from fluid lava spreading far from the vent.

• Prince Edward IslandsNarrower topic: Marion Island’s volcanic landforms were built by eruptions of this general type.

• Fissure ventRelated: Repeated fissure-fed flows can contribute to the growth of shield volcanoes.

• Mauna KeaNarrower topic: Mauna Kea’s wide profile and lava-built slopes are characteristic of shield volcanoes.

• Fissure eruptionRelated: Its shape often reflects repeated effusive eruptions, including activity along rift-zone fissures.

• Olympus MonsNarrower topic: Olympus Mons is the Solar System’s largest known example of this volcanic form.

• Tibesti MountainsRelated: Shield volcanoes account for major volcanic structures in the Tibesti massif.

• Volcanic coneCompared with: Its low, expansive profile contrasts with the steeper slopes of many volcanic cones.

• HallasanNarrower topic: Hallasan’s broad profile reflects the low-viscosity lava that built a shield volcano.

• Hawaii hotspotBroader topic: Hawaiian islands are built chiefly from shield volcanoes fed by hotspot eruptions.

• Lava fieldRelated: Its low-viscosity eruptions commonly create extensive lava fields.

• Lord Howe IslandNarrower topic: Lord Howe Island’s volcanic foundations formed through this kind of effusive activity.

• Mascarene IslandsRelated: Shield-building eruptions formed the main volcanic massifs of Réunion and Mauritius.

• Mount KenyaCompared with: Mount Kenya’s steep stratovolcanic origins differ from this broad volcanic form.

• Mount BlackburnNarrower topic: Blackburn’s broad volcanic form belongs to this volcano type.

• SupervolcanoCompared with: Its typical low-explosivity eruptions contrast with the rare, enormous explosive events associated with supervolcanoes.

• Amsterdam IslandBroader topic: The island’s volcanic massif has the broad profile associated with shield volcanism.

• Emi KoussiNarrower topic: Emi Koussi’s broad profile reflects the shield-volcano form.

• HaleakalāNarrower topic: Haleakalā’s immense, gently sloping form is characteristic of this volcano type.

• KoryakskyCompared with: Its low profile contrasts with Koryaksky’s steep, layered stratovolcano cone.

• Peter I IslandNarrower topic: Peter I Island is a volcanic island whose broad form reflects volcanic construction.

• Complex volcanoCompared with: Its commonly broad, unified profile contrasts with an irregular complex edifice.

• KauaʻiNarrower topic: Kauaʻi began as a shield volcano rising from the Pacific seafloor.

• LānaʻiBroader topic: Lānaʻi formed from shield-volcano activity before erosion reshaped its slopes.

• MenengaiNarrower topic: The volcano that produced Menengai’s caldera was a shield volcano.

• Mount Edziza volcanic complexNarrower topic: Mount Edziza’s central volcano has the low, expansive form of a shield volcano.

• Mount SidleyNarrower topic: Mount Sidley’s low, expansive profile is characteristic of this volcanic form.

• Rocher de SelNarrower topic: Réunion’s volcanic landforms provide the geological setting for its coastal rocks.