They are solar flares.
Basaltic
An eruption with thin, runny magma containing very little silica is called an effusive eruption. This type of eruption usually results in lava flows that can travel long distances from the volcano.
There were 4 large eruptions of Mount Aso, from 300,000 BC to 90,000 BC. They were all very powerful, explosive eruptions. The last was the most powerful, probably as powerful as the Santorini eruption of c. 1620 BC, or some 4 times more powerful than that of Krakatoa in 1883.
Not necessarily. The most powerful eruptions generally come from stratovolcanoes. These can be very tall, but do not have to be. The second most powerful eruption of the Twentieth Century was the 1991 eruption of Mount Pinatubo. This volcano is not nearly as tall as other stratovolcanoes. The most powerful eruptions come from supervolcanoes that often fail to build into any sort of mountain.
A large volcanic eruption can send gases and clouds of particulates very high in the atmosphere, where they can be carried great distances by the wind, even in some cases for 1000 miles.
inside the earth is gases and it gets very hot. this melts the rock and builds up pressure. Eventually it causes a volcanic eruption
The eruption of a very large volcano
Silica(te) rich magma is usually an explosive eruption. The explosiveness of an eruption depends on - a) Gases trapped within the magma at eruption b) The Silica content c) The fragility of the crater walls and/or the volcanic plug.
During the eruption very hot gases are released, lava, hot rock fragments which in contact with dry vegetation causes fires.
Gases present in the air in very small amounts are called trace gases. These include gases such as argon, carbon dioxide, methane, and ozone, which, despite their low concentrations, can have significant environmental and climatic effects. Trace gases play crucial roles in various atmospheric processes, including the greenhouse effect and air quality.
They are called fragments, fragments.
they are very very hot!