A composite volcano is a combination of a cinder cone and a shield cone. The top of a composite volcano is steep like a cinder cone. The bottom of a composite volcano is flatter, like a shield volcano.
Parasitic cone volcanos and cinder cone volcanos are not the same when classifying. Cinder cone volcanos are the most popular type of volcano, named for its cone shaped formation. Cinder cone volcano are also considered the smallest type of volcanos and can stand alone or grow on the flanks of other volcanos. The parasitic cone volcanos are similar to the cinder cones, however, the volcano is found on the flanks of other volcanos, hence, the name. It is created by flank eruptions of larger volcanos.
kind of
Cinder cone volcanoes are generally small in size and often occur in groups or clusters. They are composed of pyroclastic material, such as cinders and volcanic ash, which build up around the vent in a cone shape. These types of volcanoes tend to form rapidly and typically have short-lived eruptions.
No, shield volcanoes are a specific type of volcano characterized by their broad, gentle slopes and low viscosity lava flows. "Volcano" is a general term that refers to any landform where volcanic activity occurs, encompassing a variety of volcano types such as shield, composite, and cinder cone volcanoes.
The three types of vocano are shield, cinder cone, and composite. All three vocano types can be found in the same regions, and all can be live. Although the eruption types are all different, they each can spill out lava and dangerous gasses.
Parasitic cone volcanos and cinder cone volcanos are not the same when classifying. Cinder cone volcanos are the most popular type of volcano, named for its cone shaped formation. Cinder cone volcano are also considered the smallest type of volcanos and can stand alone or grow on the flanks of other volcanos. The parasitic cone volcanos are similar to the cinder cones, however, the volcano is found on the flanks of other volcanos, hence, the name. It is created by flank eruptions of larger volcanos.
same ? here
Both erupt basaltic lava, which has a low silica content and a high temperature.
kind of
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.
Cinder cone volcanoes are generally small in size and often occur in groups or clusters. They are composed of pyroclastic material, such as cinders and volcanic ash, which build up around the vent in a cone shape. These types of volcanoes tend to form rapidly and typically have short-lived eruptions.
yes except a cone has more space in the crater
No, shield volcanoes are a specific type of volcano characterized by their broad, gentle slopes and low viscosity lava flows. "Volcano" is a general term that refers to any landform where volcanic activity occurs, encompassing a variety of volcano types such as shield, composite, and cinder cone volcanoes.
The three types of vocano are shield, cinder cone, and composite. All three vocano types can be found in the same regions, and all can be live. Although the eruption types are all different, they each can spill out lava and dangerous gasses.
No, not all volcanoes are formed the same way. They can be classified into different types based on their formation processes, such as shield volcanoes, stratovolcanoes, and cinder cone volcanoes. Shield volcanoes form from low-viscosity lava that flows easily over large areas, while stratovolcanoes are built from alternating layers of lava and ash. The specific geological conditions, including tectonic plate interactions, also influence how a volcano develops.
Same basic shape, except a cone has three dimensions, a triangle has two.
Volcanoes and related features are usually found along tectonic plate boundaries, such as the Ring of Fire around the Pacific Ocean and the East African Rift. They can also be present in hotspots like Hawaii, where magma rises from deep within the Earth's mantle.