A volcano in the ocean under water.
Well after the eruption 1883 eruption Krakatoa was an Oceanic volcano, (around 1889) until it grew and regained it's height. It is now a land volcano.
Mount Si is a remnant of an oceanic plate volcano.
A shield volcano.
volcanoes are caused by subduction. it could be an oceanic plate sub-ducting under a continental plate which would result in a coastal volcano or it could be an oceanic plate sub-ducting under another oceanic plate, which would result in a volcanic island.
Mid-oceanic ridges, at the divergance of 2 SiMa plates. Hawii is an example of a shield volcano.
When a trench or volcano comes.
Well after the eruption 1883 eruption Krakatoa was an Oceanic volcano, (around 1889) until it grew and regained it's height. It is now a land volcano.
When an oceanic plate and a continental plate collide, it forms a volcano. The oceanic plate subducts underneath the continental plate. As the oceanic plate slides underneath, a magma chamber is formed. This magma chamber is what feeds the volcano.
Mount Si is a remnant of an oceanic plate volcano.
A shield volcano.
Intraplate volcanism.
Volcanoes cannot be formed at a continental rift, due to the fact that a volcano cannot form between two continental plates: it normally forms when one continental plate and an oceanic plate collide. Normally, a volcano forms when one continental and one oceanic plate collides. The denser oceanic plate
A trench and a strata volcano.
volcanoes are caused by subduction. it could be an oceanic plate sub-ducting under a continental plate which would result in a coastal volcano or it could be an oceanic plate sub-ducting under another oceanic plate, which would result in a volcanic island.
Mid-oceanic ridges, at the divergance of 2 SiMa plates. Hawii is an example of a shield volcano.
Mid-oceanic ridges, at the divergance of 2 SiMa plates. Hawii is an example of a shield volcano.
oceanic crest and volcano.