a cinder con volcano is an explosive volcano
Cinder cone volcanoes are generally considered to be non-explosive compared to stratovolcanoes. They typically erupt with fire fountains and release lava flows rather than explosive eruptions with ash and pyroclastic flows. However, some cinder cone eruptions can exhibit some degree of explosivity depending on the gas content of the magma.
Strato and Cinder-cone volcanos but cinder cones can have non explosive too but not strato
No. A shield volcano is a large volcano with broad, shallow slopes formed from layers of lava flows formed by non-explosive eruptions. A cinder cone volcano is a small, steep-sloped volcano composed of pieces of rock formed by lava that was ejected explosively into the air.
Mount Pelee is a stratovolcano, which is a composite volcano. It is known for its explosive eruptions due to the composition of its magma. Shield volcanoes, on the other hand, are characterized by their broad, gently sloping profile and quiet, non-explosive eruptions.
Cinder cones are small and steep-sloped, composed of volcanic cinders, and have mildly explosive eruptions. Shield volcanoes are large and shallow-sloped with very runny lava and generally non-explosive eruptions.
Yes. The ash and cinder layers are from explosive eruptions while the lava flows are from non-explosive eruptions.
A cinder cone volcano typically has quiet eruptions, characterized by the ejection of small fragments of lava and ash. Composite volcanoes can have both quiet and explosive eruptions, due to the buildup of pressure from the highly viscous magma. Shield volcanoes generally have non-explosive eruptions, with flowing lava that travels long distances.
Paricutin is an explosive volcano. It is classified as a scoria cone volcano, which is a type of volcanic cone that is formed by explosive eruptions. Paricutin's eruptions were characterized by the ejection of molten rock fragments, ash, and gases, leading to the formation of a cone-shaped structure. The explosive nature of Paricutin's eruptions is attributed to the high gas content and viscosity of the magma beneath the volcano.
It is explosive (it is a stratovolcano). In a worst-case scenario, more than 400,000 people would have to be evacuated from the proximity of the volcano: up to 30 km / 19 mi from the cone.
It's a shield volcano. Curtesy of a quick google search [from geography.learnontheinternet.co.uk] Shield Volcanoes Eruptions are typically non-explosive. Shield volcanoes produce fast flowing fluid [lava] that can flow for many miles. Eruptions tend to be frequent but relatively gentle.
There are mainly four types of volcano classifications based on their shape and eruption style: stratovolcanoes (composite volcanoes), shield volcanoes, cinder cone volcanoes, and lava dome volcanoes. Stratovolcanoes have steep sides and explosive eruptions, shield volcanoes have gentle slopes and non-explosive eruptions, cinder cone volcanoes are small and composed of tephra, and lava dome volcanoes are formed by thick lava flows.
When it explodes!