Linked from

The 43 pages that link to Caldera basin, each with the reason it gives.

• StratovolcanoCompared with: Calderas are collapse features, not the steep cone defined by stratovolcano structure.

• Volcanic islandRelated: Collapse after major eruptions can reshape an island’s summit and create a caldera.

• Impact craterCompared with: Calderas can be circular, but their collapse structures distinguish them from impact excavations.

• Volcanic craterCompared with: Calderas are generally much larger and more collapse-dominated than ordinary craters.

• Impact crateringCompared with: Calderas are collapse structures, unlike craters excavated by incoming bodies.

• Sierra Madre OccidentalRelated: Caldera-forming eruptions contributed to the region’s extensive ignimbrite deposits.

• VolcanoCompared with: A caldera is a volcanic landform, but not necessarily an active vent or cone.

• Impact eventCompared with: Its collapse origin distinguishes it from a depression excavated by a collision.

• MaarCompared with: Calderas result mainly from collapse, unlike the explosive excavation characteristic of maars.

• Volcanic crater lakeNarrower topic: Many of the world's largest volcanic lakes occupy calderas.

• Mount PinatuboBroader topic: The summit collapsed into a caldera as magma was withdrawn in 1991.

• Yellowstone CalderaNarrower topic: Yellowstone is a caldera produced by collapse after enormous eruptions.

• Fissure ventCompared with: Calderas are collapse structures, whereas fissure vents are eruptive openings.

• Mount KilimanjaroRelated: Kibo contains a caldera formed during its volcanic history.

• Mount TamboraBroader topic: The 1815 eruption emptied part of Tambora’s magma system and left its broad summit caldera.

• SantoriniNarrower topic: Santorini is a conspicuous island example of this landform.

• Olympus MonsNarrower topic: Olympus Mons’s nested summit depressions are calderas, not impact craters.

• Taupō Volcanic ZoneBroader topic: Several major volcanic centers in the zone are calderas created by large magma withdrawals.

• Tibesti MountainsBroader topic: Calderas such as the one at Emi Koussi record major volcanic episodes in the range.

• Lake TobaNarrower topic: Lake Toba is a water-filled example of this volcanic landform.

• Mount AsoNarrower topic: This landform accounts for the vast basin surrounding Aso’s central cones.

• 1883 eruption of KrakatoaRelated: Collapse of Krakatoa’s volcanic structure helped displace seawater and produce tsunamis.

• Mount PaektuNarrower topic: Paektu’s summit basin is a prominent example of this landform.

• Santorini calderaNarrower topic: Santorini’s basin is one example of this collapse structure.

• Craters of the Moon National Monument and PreserveRelated: The monument includes volcanic depressions that help explain the field’s eruptive history.

• São Miguel IslandRelated: Several of the island’s celebrated lakes occupy calderas.

• SupervolcanoBroader topic: Collapse of the roof above an emptied magma system can create the vast basin left by a supereruption.

• Terceira IslandBroader topic: Terceira’s interior includes caldera landscapes formed by volcanic collapse.

• Crater Lake National ParkNarrower topic: Crater Lake fills the caldera left by Mount Mazama.

• Emi KoussiRelated: A large caldera marks Emi Koussi’s summit.

• HaleakalāCompared with: Haleakalā’s summit depression is often called a crater, but erosion—not summit collapse—formed it.

• KoryakskyCompared with: Koryaksky is a prominent cone rather than a volcano defined by a collapse basin.

• Lake TaupōNarrower topic: This landform explains the lake’s broad, steep-sided volcanic basin.

• Minoan eruptionRelated: The eruption emptied and destabilized the volcano, contributing to Thera’s caldera.

• Raoul IslandNarrower topic: Raoul Island’s defining landform is one example of this collapse structure.

• Complex volcanoRelated: Caldera collapse can disrupt an edifice and create space for later vents.

• Daisetsuzan Volcanic GroupRelated: Caldera formation helps explain the group’s broad craters and complex volcanic landscape.

• GalerasRelated: Galeras occupies a caldera created by earlier volcanic collapse.

• Île Saint-PaulBroader topic: The island’s central flooded depression is a volcanic caldera.

• Jebel MarraNarrower topic: Deriba is the defining example of this landform within Jebel Marra.

• Lake MashūNarrower topic: Mashū Caldera is one example of this volcanic landform.

• MenengaiNarrower topic: Menengai’s broad depression is the defining landform produced by its volcanic collapse.

• Mount SidleyRelated: A prominent caldera marks Mount Sidley’s summit.