cinder cones
A scoria cone volcano, also known as a cinder cone volcano, is the type of volcano that has small basaltic cones built during one short eruptive episode. These volcanoes are characterized by their steep sides and formed by the accumulation of volcanic debris, such as scoria and ash, ejected during explosive eruptions.
A relatively small summit depression on a volcano marking a former eruptive vent is called a volcanic crater. It is typically shaped like a bowl or a funnel and is formed during explosive volcanic activity when the magma is ejected from the volcano. Craters can vary in size and can often contain a lake, known as a crater lake, or be filled with volcanic debris.
their are many types of magma because when a volcano has soft magma that means it either exploded small or the magma was going really slow and fast magma and big exploding volcano's are hard magma.:)
Basaltic magma contains small amounts of silica and has a low viscosity, meaning it is relatively fluid and flows easily.
Shield volcanoes are characterized by their broad, gently sloping sides and primarily produce low-viscosity basaltic lava, allowing it to flow over long distances. Cinder cone volcanoes, on the other hand, are typically smaller and have steep sides, formed from the explosive eruption of volcanic ash, cinders, and small lava fragments ejected from a single vent. Deposit refers to the accumulation of volcanic materials, including ash and lava, that can occur around these volcanoes during eruptions. Together, these types of volcanoes represent different eruptive styles and geological formations associated with volcanic activity.
A scoria cone volcano, also known as a cinder cone volcano, is the type of volcano that has small basaltic cones built during one short eruptive episode. These volcanoes are characterized by their steep sides and formed by the accumulation of volcanic debris, such as scoria and ash, ejected during explosive eruptions.
A relatively small summit depression on a volcano marking a former eruptive vent is called a volcanic crater. It is typically shaped like a bowl or a funnel and is formed during explosive volcanic activity when the magma is ejected from the volcano. Craters can vary in size and can often contain a lake, known as a crater lake, or be filled with volcanic debris.
their are many types of magma because when a volcano has soft magma that means it either exploded small or the magma was going really slow and fast magma and big exploding volcano's are hard magma.:)
Basaltic magma contains small amounts of silica and has a low viscosity, meaning it is relatively fluid and flows easily.
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Basaltic lava is far less viscous, has less silica, erupts at a higher temperature and is denser than granitic lava (properly called rhyolitic lava when it is on the surface). Basaltic lava is composed primarily of pyroxenes and calcium rich plagioclase with small amounts of olivine. Rhyolitic lava primarily contains alkali feldspars and quartz.
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Shield volcanoes are characterized by their broad, gently sloping sides and primarily produce low-viscosity basaltic lava, allowing it to flow over long distances. Cinder cone volcanoes, on the other hand, are typically smaller and have steep sides, formed from the explosive eruption of volcanic ash, cinders, and small lava fragments ejected from a single vent. Deposit refers to the accumulation of volcanic materials, including ash and lava, that can occur around these volcanoes during eruptions. Together, these types of volcanoes represent different eruptive styles and geological formations associated with volcanic activity.
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Layers of ash and lava refer to the various levels of volcanic material deposited during an eruption. Ash is composed of small fragments of volcanic rock, while lava is molten rock that flows out of a volcano. Together, these layers provide a record of the volcano's eruptive history and can help scientists understand past volcanic activity.