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Most have erupted at some point. Some are dormant now, but could still erupt. Mt. Etna, Vesuvius, St. Helens, Shasta are just some that have erupted in the past.
The second eruption is called a reawakening or re-eruption.Most volcanoes erupt multiple times over the course of their lifespan; the period during which a volcano doesn't erupt is called its dormant period or dormancy.
volcanoes no problem lack :dd:d:d:d:d:d:d:::dd:d:d:d:d: :p
People living near a dormant volcano may be unaware of the danger. A dormant volcano may become active at any point of timeand the people living near the volcano may not realize it is about to erupt.
Effusive eruptions occur when hot, (1200oC) runny basalt magmas reach the surface. Dissolved gases escape easily as the magma erupts, forming lava that flows downhill quite easily. Effusive eruptions build up gently-sloping Shield Volcanoes like Hawaii. Explosive eruptions occur where cooler, more viscous magmas (such as andesite) reach the surface. Dissolved gases cannot escape as easily, so pressure may build up until gas explosions blast rock and lava fragments into the air! Lava flows are much more thick and sticky so do not flow downhill as easily. These eruptions build up more steeply-sloping Composite volcanoes like this one in Chile.
People living near a dormant volcano may be unaware of the danger. A dormant volcano may become active at any point of timeand the people living near the volcano may not realize it is about to erupt.
Most have erupted at some point. Some are dormant now, but could still erupt. Mt. Etna, Vesuvius, St. Helens, Shasta are just some that have erupted in the past.
no all the volcanoes do not erupt.there are three types of volcanoes extinct,average and active. no because there are dome mountains that do not erupt and they are full of lava and they will erupt in more or less than 300 years.
The second eruption is called a reawakening or re-eruption.Most volcanoes erupt multiple times over the course of their lifespan; the period during which a volcano doesn't erupt is called its dormant period or dormancy.
It will erupt for the same reason that all volcanoes erupt: magma is collecting in the magma chamber and pressure is increasing. This will eventually reach a breaking point and result in an eruption. The chances of that occuring in our lifetimes however, are very small.
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People living near a dormant volcano may be unaware of the danger. A dormant volcano may become active at any point of timeand the people living near the volcano may not realize it is about to erupt.
Not in the slightest. There is NO connection between an eclipse and a volcano. The point is, eclipses happen twice a year or so. Volcanoes go off every few years. Just by sheer coincidence, some volcanoes will erupt during an eclipse. But there is no causal connection between them.
Effusive eruptions occur when hot, (1200oC) runny basalt magmas reach the surface. Dissolved gases escape easily as the magma erupts, forming lava that flows downhill quite easily. Effusive eruptions build up gently-sloping Shield Volcanoes like Hawaii. Explosive eruptions occur where cooler, more viscous magmas (such as andesite) reach the surface. Dissolved gases cannot escape as easily, so pressure may build up until gas explosions blast rock and lava fragments into the air! Lava flows are much more thick and sticky so do not flow downhill as easily. These eruptions build up more steeply-sloping Composite volcanoes like this one in Chile.
Volcanoes are driven by forces deep inside the Earth, where it is always very hot. Conditions that deeps are not affected by temperatures at the surface. The rising molten rock is extremely hot and does not lose heat all that quickly, and so can erupt regardless of climate. Compared with something as hot as magma, the temperature difference between places such as Iceland and Hawaii is relatively small. Both are much cooler than the melting point of rock.
volcanoes is the natural fenomenom most difficult to predict. That duty belong to the people at the seismic intitutions and seismic observatories. They are called geologists. Volcanologists monitor information from sensors near volcanoes to provide short-term forecasts of possible eruptions or changes in the course of existing eruptions. These sensors detect physical changes such as earthquake activity, shape of the volcano, and the release of volcanic gases.
To this point the fuego volcano is active