the plume is the smoke coming out
a 'nom de plume' is apseudonym for writers. There is no registration.
My favorite author uses a nom de plume.
Charles Dodgson is best known today by his nom de plume, Lewis Carroll.
uhm i think its shield volcano but im not sure ...... but i kno its between A, HOT SPOT B, CINDER - CONE VOLCANO C, COMPOSITE D, SHIELD VOLCANO or the storage of magma under the volcano
I like to do word associations. Aplomb means self-confidence or assurance even under pressure. Aplomb sounds like a plume, and a plume is a large feather, often worn in hats. You'd have to be pretty self-confident to wear a hat with a big old feather in it in a high pressure situation. Hope that helps.
A volcano formed by a rising plume of magma that is not located at a plate boundary.
A volcano.
A hotspot volcano.
Magma chamber? Or the lithosphere or a mantle plume, depending on where the volcano is.
A place where hot mantle material rises in a semi-permanent plume, and affects the overlying crust.
Mantle plumes appear to remain nearly stationary. However, the lithospheric plate above a mantle plume continues to drift slowly. So, the volcano on the surface is eventually carried away from the mantle plume. The activity of the volcano stops because it has moved away from the hot spot that supplied it with magma. A new volcano forms, however, at the point on the plate's surface that is now over the mantle plume. Some mantle plumes are long and linear. As magma generated by these plumes rises through cracks in Earth's crust, a line of hotspot volcanoes forms. Unlike volcanoes that form individually as a plate moves over a mantle plume, hot-spot volcanoes that form in lines over a long plume do not have any particular age relationship to each another.Mantle plumes appear to remain nearly stationary. However, the lithospheric plate above a mantle plume continues to drift slowly. So, the volcano on the surface is eventually carried away from the mantle plume. The activity of the volcano stops because it has moved away from the hot spot that supplied it with magma. A new volcano forms, however, at the point on the plate's surface that is now over the mantle plume. Some mantle plumes are long and linear. As magma generated by these plumes rises through cracks in Earth's crust, a line of hotspot volcanoes forms. Unlike volcanoes that form individually as a plate moves over a mantle plume, hot-spot volcanoes that form in lines over a long plume do not have any particular age relationship to each another.
A hot spot deep in the Earth's mantle creates a rising plume of magma that is even hotter than the regular magma of which the mantle is composed. When this plume of magma hits the crust, it breaks through and causes a volcano. The reason why we eventually wind up with a whole chain of volcanoes, rather than just one, is continental drift. The Earth's crust is moving, while the plume of magma is always directed at the same spot, so as the tectonic plate slowly drifts by, the plume will impact different parts of that plate.
of Plume
A volcanic mountain made up of volcanic ash, cinders, and bombs is called a Cinder Cone Volcano.
A volcano. See the excellent book "Krakatoa" by Simon Winchester.
When a volcano is erupting, it is generally not safe to be near or approach the volcano. It is advised to avoid the area and not attempt to see the eruption up close. Additionally, flying or operating aircraft near an erupting volcano can pose significant risks due to the ash plume and potential disruption to air traffic.
Fall-out tuff is a volcanic deposit formed from ash and lapilli that fall out of the eruption plume of a volcano. This is opposed to tuff formed by pyroclastic flows.