The types of volcanoes resulting from non-explosive eruptions, like those in Hawaii, are primarily shield volcanoes. These volcanoes are characterized by their broad, gently sloping profiles formed by the accumulation of low-viscosity basalt lava that can flow over long distances. The eruptions are typically effusive, allowing lava to flow steadily rather than explosively. This results in the creation of large, expansive landforms that are less steep compared to other volcanic types, such as stratovolcanoes.
A combination of explosive and nonexplosive eruptions will create a complex volcanic landscape characterized by varied landforms and deposits. Explosive eruptions can produce ash clouds, tephra, and pyroclastic flows, while nonexplosive eruptions typically result in the formation of lava flows and shield volcanoes. This interplay can lead to diverse geological features, such as stratovolcanoes that exhibit layered deposits from both eruption types. The resulting environment can also influence local ecosystems and geological hazards.
A combination of explosive and nonexplosive eruptions will create a diverse volcanic landscape characterized by various features. Explosive eruptions can form steep-sided stratovolcanoes with layers of ash and lava, while nonexplosive eruptions typically lead to the formation of broad shield volcanoes with gentle slopes. This interplay can result in complex volcanic structures, such as calderas, lava plateaus, and pyroclastic deposits, showcasing a range of volcanic activity and geology. Such environments often exhibit varied ecosystems and geological hazards.
Oceans do not collide but oceanic crustal plates can collide, and when they do collide, island arcs are formed along the subduction zone.
This would result in a non-explosive, "runny" eruption, similar to what you get in Hawaii, where the volcano simply pours out lava. Explosive reactions occur when rocks contain large amounts of water and silica, which flash into steam, resulting in a rapid expansion, and thus a dangerously explosive reaction.
Although large tsunami waves from Japan's earthquake hit Hawaii with some force, there are no reported fatalities as a result. There was one reported death in California, from an observer being swept out to sea by the tsunami wave.
The result is a cinder cone.
The result is a cinder cone.
Earthquakes, Volcanos, etc.. :) hope it helped
Volcanos and Earthquakes are not weather, neither are Tidal waves as they result from earthquakes or volcanos, however Winds (tornados) and Percipitation (Storms and sheet ice for example) are
Land ownership
Yes as a result of overtaking Japan who tried to take it away from hawaii
Volcanos form usually from thin spots in the Earth's crust where magma pipes may extend up to the surface. Magma flow may build up from these pipes resulting in the formation of volcanos. Also, plate tectonics may result in regions of upheval and the formation of mountains and volcanos.
A combination of explosive and nonexplosive eruptions will create a complex volcanic landscape characterized by varied landforms and deposits. Explosive eruptions can produce ash clouds, tephra, and pyroclastic flows, while nonexplosive eruptions typically result in the formation of lava flows and shield volcanoes. This interplay can lead to diverse geological features, such as stratovolcanoes that exhibit layered deposits from both eruption types. The resulting environment can also influence local ecosystems and geological hazards.
This type of convergence may result in the occurrence of deep earthquakes or the formation of volcanoes.
A combination of explosive and nonexplosive eruptions will create a diverse volcanic landscape characterized by various features. Explosive eruptions can form steep-sided stratovolcanoes with layers of ash and lava, while nonexplosive eruptions typically lead to the formation of broad shield volcanoes with gentle slopes. This interplay can result in complex volcanic structures, such as calderas, lava plateaus, and pyroclastic deposits, showcasing a range of volcanic activity and geology. Such environments often exhibit varied ecosystems and geological hazards.
This would result in a non-explosive, "runny" eruption, similar to what you get in Hawaii, where the volcano simply pours out lava. Explosive reactions occur when rocks contain large amounts of water and silica, which flash into steam, resulting in a rapid expansion, and thus a dangerously explosive reaction.
Land ownership was taken over mainly by the businesses.