Because cinder cones are very big and it takes lot of presure for them to erupt and once pressure stops buildinng up the volcano becomes extinct
Because they are caused by the escape of gasses from the magma and mamas degas quickly.
Cinder cone volcanoes are recognized by their small, steep-sided cones with a symmetrical shape. They are typically formed by explosive eruptions that eject cinders, ash, and lava fragments into the air, which then accumulate and form a cone-shaped mountain. Cinder cones are usually short-lived and can be found in volcanic fields or as isolated volcanic features.
Cinder cones are generally formed when volcanoes eject a combination of ash, cinders, and lava fragments during explosive eruptions. These materials pile up around the vent, creating a steep-sided cone-shaped hill. The eruptions are typically short-lived and can occur suddenly.
Cinder cone volcanoes are built from loose, unconsolidated volcanic debris, making them more susceptible to erosion from wind, water, and gravity. The steep slopes of cinder cones facilitate rapid erosion, causing them to be relatively short-lived compared to other types of volcanoes.
Yes, although technically, strato-volcanoes *are* cinder cones (composite cones), built up of layers of ash. But the term "cinder cones" (ash cones) is usually applied to smaller cones that form within the vicinity of large volcanic calderas, such as Crater Lake in Oregon. They may be associated with either strato-volcanoes or shield volcanoes.
Because they are caused by the escape of gasses from the magma and mamas degas quickly.
Cinder cones generally have a very steep slope. This slope is also considered gentle compared to the cones' short height.
No. Cinder cones usually produce relatively explosive eruptions and are short-lived. Some only erupt for a few years before going extinct.
Cinder cone volcanoes are recognized by their small, steep-sided cones with a symmetrical shape. They are typically formed by explosive eruptions that eject cinders, ash, and lava fragments into the air, which then accumulate and form a cone-shaped mountain. Cinder cones are usually short-lived and can be found in volcanic fields or as isolated volcanic features.
Yes, cinder cones can produce lava flows. Typically, these flows are relatively short and are composed of basaltic lava. Cinder cones are formed from the accumulation of volcanic cinders and ash around a central vent.
their are 6 cinder cone volcanes
Cinder cones are generally formed when volcanoes eject a combination of ash, cinders, and lava fragments during explosive eruptions. These materials pile up around the vent, creating a steep-sided cone-shaped hill. The eruptions are typically short-lived and can occur suddenly.
Cinder Cones are composed of rock fragments and the eruption of cinders. The rock fragments pile up around a single crater forming a Cinder Cone.
explosive
yes
explosive
no