Linked from

The 13 pages that link to Cinder cone, each with the reason it gives.

• StratovolcanoCompared with: It is typically simpler and smaller than a stratovolcano, with less extensive lava-and-debris layering.

• Shield volcanoCompared with: It forms chiefly from erupted fragments rather than extensive fluid lava flows.

• VolcanoBroader topic: It is a simple volcanic landform built from material thrown out during eruptions.

• Trans-Mexican Volcanic BeltNarrower topic: Cinder cones are widespread across the belt’s volcanic fields.

• Mauna KeaBroader topic: Late-stage eruptions produced cinder cones across Mauna Kea’s summit region.

• ParícutinNarrower topic: Parícutin is a classic example of this volcanic form.

• ScoriaNarrower topic: Many cinder cones are built largely from scoria thrown out around a vent.

• Volcanic coneBroader topic: It is the classic cone built from accumulated loose tephra.

• Chaîne des PuysBroader topic: Many Puys are built from scoria and other fragments erupted around a single vent.

• Craters of the Moon National Monument and PreserveRelated: These cones rise above the lava fields and mark explosive episodes in the area’s volcanism.

• HaleakalāRelated: Numerous cones rise from the floor of Haleakalā’s summit depression.

• KoryakskyCompared with: Its simple, fragment-built form differs from Koryaksky’s large composite structure.

• Mount Edziza volcanic complexNarrower topic: Numerous small cones contrast with the complex’s much larger shield volcano.