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A secondary cone in a volcano refers to a smaller cone that forms on the flank of the main volcano. This secondary cone is created by the eruption of lava and other volcanic materials from a separate vent. It is a distinct feature from the central vent of the main volcano.
The cone indicates uncertainty in the path of the hurricane. The center line of the cone indicates the expected path of the storm, but it might go a given amount to the left or right of that path.
A sheild cone is volcano that is sorta flat and gently sloping up.
The permanent magnets in a stereo speaker are used to create a magnetic field that interacts with the electrical current flowing through the voice coil attached to the speaker cone. This interaction causes the voice coil to move back and forth, pushing and pulling the cone to produce sound waves. The permanent magnet near the cone provides a stationary magnetic field, while the magnet on the cone moves with it to drive the sound production.
A cone shaped mountain that is built from layers of lava is called a volcano.However, that description does not quite fit any of the three accepted descriptions of the world's volcanoes.A dome shaped mountain built from layers of lavais called a 'shield volcano'.A cone shaped mountain built from layers of cinders (tephra) is called a 'cinder cone' or a 'cinder cone volcano'.A cone shaped mountain built from alternating layers of lava and cinders is called a 'composite volcano'.
A parasitic cone (or satellite cone) is the cone-shaped accumulation of volcanic material created by eruptions from fractures other than the central vent of a volcano.
parasitic cone
A parasitic cone is a smaller cone-shaped volcanic structure that forms on the flanks of a larger volcano. These cones are formed from eruptions of lava, ash, and other volcanic materials that are typically less explosive than those from the main vent of the 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.
Parasitic Cone
The parasitic cone is the name of the smaller vent-structure on the side of some volcanoes. This structure is not part of the central vent of a volcano.
The correct spelling is "parasitic."
No, sponges are not parasitic.
parasitic
yes, they are parasitic
Sponges are not parasitic. Where as polyps.
Antihelminthics are the drugs that kill parasitic worms.