Vulcan was the Roman god of fire and metalworking, adapted from Hephaestus in Greek mythology. The volcanic island of Vulcano was believed by both the Greeks and Romans to be this god's workshop. It is from this island that we get the word volcano.
Volcanic eruption can be classified mainly based on the name of the volcano. They are Surtseyan eruption, Plinian eruption, Vulcanian eruption, Strombolian eruption and Hawaiian eruption.
Typically, Plinian eruptions are more destructive than Vulcanian eruptions. Plinian eruptions produce massive volcanic columns and pyroclastic flows, which can travel long distances and cause widespread devastation. In contrast, Vulcanian eruptions are characterized by short, explosive bursts of ash and gas, which are generally less powerful and have a more limited impact.
The most destructive to least destructive kinds of eruptions are as follows:PlinianPeleanStrombolianHawaiianMost to leastPlinian, Pelean, Vulcanian, Fissure
scientists classify volcanoes in four general groups, Hawaiian, Strombolian, vulcanian, and peleean
1630 BC eruption of Santorini is recognized as one of the most explosive volcanic eruptions in historic times, the event is only a single eruption in a continuum of eruptive activity associated with subduction. The geologic record over the past one million years indicates that less explosive Strombolian and Vulcanian eruptions have occurred at Santorini about once every 5000 years, and that Plinian-typeevents have occurred about once every 20,000 years. Since the late Bronze Age eruption, the two Kameni islands, Nea and Palea Kameni, have formed in the center of the caldera by numerous eruptive events over the past 2000 years. Santorini thus appears to be particularly active compared to its geologic past. There have been several eruptions in the 19th and 20th centuries, with the most recent occurring in 1950
it has a stombolian eruption
Volcanic eruption can be classified mainly based on the name of the volcano. They are Surtseyan eruption, Plinian eruption, Vulcanian eruption, Strombolian eruption and Hawaiian eruption.
Volcanic eruption can be classified mainly based on the name of the volcano. They are Surtseyan eruption, Plinian eruption, Vulcanian eruption, Strombolian eruption and Hawaiian eruption.
Vulcanian is not a kind of volcano. It is a kind of volcanic eruption. The term Vulcanian comes from Vulcano, a volcanic island off the cost of Italy prone to this kind of eruption. This island also gives us the word volcano. This island in turn gets its name from Vulcan, the Roman god of fire and metalworking who was believed to have is forge within the island of Vulcano.
Typically, Plinian eruptions are more destructive than Vulcanian eruptions. Plinian eruptions produce massive volcanic columns and pyroclastic flows, which can travel long distances and cause widespread devastation. In contrast, Vulcanian eruptions are characterized by short, explosive bursts of ash and gas, which are generally less powerful and have a more limited impact.
The most destructive to least destructive kinds of eruptions are as follows:PlinianPeleanStrombolianHawaiianMost to leastPlinian, Pelean, Vulcanian, Fissure
When eruption types are arranged from most destructive to least, it is in descending order.
When eruption types are arranged from most destructive to least, it is in descending order.
scientists classify volcanoes in four general groups, Hawaiian, Strombolian, vulcanian, and peleean
the eruption that did it was a eruption
1630 BC eruption of Santorini is recognized as one of the most explosive volcanic eruptions in historic times, the event is only a single eruption in a continuum of eruptive activity associated with subduction. The geologic record over the past one million years indicates that less explosive Strombolian and Vulcanian eruptions have occurred at Santorini about once every 5000 years, and that Plinian-typeevents have occurred about once every 20,000 years. Since the late Bronze Age eruption, the two Kameni islands, Nea and Palea Kameni, have formed in the center of the caldera by numerous eruptive events over the past 2000 years. Santorini thus appears to be particularly active compared to its geologic past. There have been several eruptions in the 19th and 20th centuries, with the most recent occurring in 1950
no it was a loud eruption