Volcanoes are a good way for the earth to blow off a little steam. More correctly, volcanoes are vents in the earth's crust through which lava, rock fragments, hot vapor and gases are ejected. And while they are all natural events in the life of earth, there are different types of volcanoes. The types of volcanoes are differentiated based on their size, composition and explosive style.
daffirentiate structure and function
Neither. A volcano is a geologic structure.
Yes, volcanic eruptions affect the volcano. The lava being pushed out and reforming affects the volcano's internal and external structure.
shield volcano
Yes, it is possible to differentiate between aromatic and antiaromatic compounds based on their chemical properties and structural characteristics. Aromatic compounds have a stable, cyclic structure with delocalized pi electrons, while antiaromatic compounds have an unstable, cyclic structure with conjugated pi electrons that do not follow the rules of aromaticity. This difference in electron delocalization leads to distinct chemical behaviors and properties between the two types of compounds.
A crater is not a separate material or part of a volcano. It is a depression or hollow at the summit of a volcano that forms when the volcano erupts and releases magma, gases, and other materials. The crater is a result of the collapse or expulsion of material during the eruption.
stolen
Yes, the structure of composition of either a volcanic or igneous rock can be altered significantly upon their ejection from a volcano.
Bedrock in a volcano refers to the solid, unweathered rock that lies beneath the volcanic materials such as ash, lava, and pyroclastic flow deposits. It forms the foundation on which the volcano is built and can help determine the stability and structure of the volcano.
It's not easy to differentiate the pigment of p aeruginosa on pseudomonas agar P from the pigment of E. coli on MacConkey agar without referring to the colors, but it can be done based on the structure of the p aeruginosa.
A low, wide-based volcano is called a shield volcano. These types of volcanoes have gentle slopes and are formed by the gradual flow of low-viscosity lava. Examples include Mauna Loa in Hawaii and Iceland's shield volcanoes.
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