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The 33 pages that link to Lava flow, each with the reason it gives.

• Volcanic hazardRelated: Lava flows often move slowly but can destroy buildings and infrastructure in their path.

• Volcanic eruptionBroader topic: Lava commonly destroys structures and vegetation along its path while reshaping terrain.

• VolcanismBroader topic: Its reach and speed determine how an effusive eruption affects nearby terrain.

• Pyroclastic flowCompared with: Lava is molten rock; pyroclastic flows are mixtures of hot gas and fragmented material.

• Shield volcanoBroader topic: Successive long-running flows accumulate to form the volcano’s wide, shallow shape.

• Deccan TrapsBroader topic: Repeated lava flows built the Deccan Traps’ characteristic layered structure.

• Volcanic hazard mapBroader topic: Its likely paths and reach can define zones of severe local exposure.

• Flood basaltBroader topic: Repeated, overlapping lava flows make up the thick sequences.

• Lava tubeNarrower topic: A lava tube develops within a flow whose outer surface cools before its interior.

• LavaBroader topic: Flow speed, shape, and reach depend on lava properties and terrain.

• KomatiiteRelated: Komatiite’s cooling history is recorded in layers within ancient lava flows.

• Volcanic ventRelated: Lava emerging from a vent can form flows that reshape nearby terrain.

• Columnar jointingRelated: Cooling lava flows commonly develop columnar joints as their interiors solidify.

• Mount EtnaRelated: Etna’s effusive eruptions send lava down its slopes, sometimes toward settlements.

• Fissure ventRelated: Fissure vents commonly feed flows that spread far from the eruptive line.

• Lava lakeCompared with: A flow spreads away from its vent; a lake remains pooled at or near the vent.

• Mauna KeaRelated: Successive lava flows built Mauna Kea’s broad volcanic flanks.

• ParícutinRelated: Parícutin’s lava flows extended the volcano’s impact beyond its cone.

• Fissure eruptionRelated: Lava issuing along a crack spreads outward and can form extensive flow fields.

• Olympus MonsRelated: Successive lava flows built Olympus Mons’s broad shield and extensive flanks.

• Thermoremanent magnetizationRelated: Cooling lava commonly acquires a strong record of the ambient field.

• Volcanic coneRelated: Flows from a cone's vent may build its flanks or extend beyond its base.

• A‘āNarrower topic: A‘ā is one surface-texture type of lava flow.

• HallasanRelated: Successive lava flows built the shield-shaped body of Hallasan.

• Lava fieldBroader topic: Lava flows are the deposits whose accumulation creates a lava field.

• Chaîne des PuysRelated: Flows from Puys spread across the surrounding landscape and shaped local valleys.

• Fuji Five LakesNarrower topic: Solidified flows from Mount Fuji formed barriers and basins in the lake region.

• Emi KoussiRelated: Repeated lava flows built Emi Koussi’s broad volcanic edifice.

• HaleakalāBroader topic: Successive lava flows built Haleakalā’s broad flanks.

• Mount NyiragongoNarrower topic: Its flank eruptions produce lava flows that can reach inhabited areas.

• Volcanic plugCompared with: A flow spreads at the surface, unlike magma solidifying inside a conduit.

• Mount SidleyRelated: Repeated lava flows built Mount Sidley’s broad shield shape.

• Nicolas DesmarestBroader topic: Desmarest used the arrangement of ancient flows to reconstruct Auvergne’s volcanic history.