There is no easy answer to this question, as scientists classify volcanoes in several different ways, including size, shape, explosivity, lava type, and tectonic occurrence. Furthermore, these different classifications often correlate. A volcano that has very effusive eruptions, for example, is unlikely to form a stratovolcano.
eruptive vent, the location of the eruptive vent, and the character of the eruptive vent, also volume, mass, and height
There are three syllables in the word "volcano."
the lava, the mantle, the outside. so there you are you have the three basic parts to a volcano.
There are many types of information used by modern taxonomists to classify organisms. Two types of information used for this purpose include whether the organism has a present backbone or not; and the body covering of the organism such as fur, feathers, skin, hair, etc..
The Three Stages of a Volcano are:Active StageDormant StageExtinct Stage
By looking at the water to find the classify
According to scientists a living being should have following three character 1 capable of multiplication. 2 capable of growth 3 capable of moving
i dnt know u tell me?
list three things that the scientists learned about earth in the 1800's?
Modern scientists study morphology (physical characteristics), genetics (DNA and hereditary factors), and behavior when classifying organisms. These factors help determine the evolutionary relationships and taxonomic classification of different species.
When classifying organisms, scientists look for three main things: shared physical characteristics, genetic similarities, and evolutionary relationships. They observe and compare features such as anatomy, behavior, and molecular traits to determine how closely related different species are and how they should be classified into groups or categories.
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eruptive vent, the location of the eruptive vent, and the character of the eruptive vent, also volume, mass, and height
Scientists classify rocks based on their mineral composition, texture, and how they were formed. These classifications help geologists understand the history and properties of rocks. There are three main categories for classifying rocks: igneous, sedimentary, and metamorphic.
Volcanoes can be classified based on their eruption style (explosive or effusive), shape (stratovolcano, shield volcano, cinder cone, etc.), and location (submarine, intra-plate, or convergent boundary volcanoes).
Scientists classify rocks into three main categories - sedimentary, igneous, and metamorphic - based on how they are formed. Sedimentary rocks are formed from the accumulation and solidification of sediments, igneous rocks are formed from the cooling and solidification of magma or lava, and metamorphic rocks are formed from the alteration of existing rocks through heat and pressure.
Color and texture is one way to classify igneous rocks. Another way to do this is modal classification and normative classification.