All lava is the same- molten(liquid) rock
Shield volcanoes are known to produce the most lava annually compared to other types of volcanoes. Shield volcanoes have gentle sloping sides and are fueled by low viscosity magma, allowing for the rapid flow of lava over a large area. This results in high-volume eruptions that can cover vast areas with lava.
Directly along active oceanic ridges, such as the mid-oceanic ridge in the Atlantic (which Iceland straddles) and on active volcanoes, such as Hawaii. When lava from volcanoes such as Hawaii and the mostly undersea volcanoes of mid-oceanic ridges cools, it solidifies into brand new rock.
A volcano can be associated with either continental or oceanic crust, depending on its location. Oceanic volcanoes typically form along mid-ocean ridges or subduction zones and are composed primarily of basaltic lava. In contrast, continental volcanoes, which can form at convergent plate boundaries or hot spots, are often made up of more diverse rock types, including andesitic or rhyolitic lavas. Therefore, the type of crust associated with a volcano varies based on its geological setting.
Runny lava, which is typically associated with low-viscosity basaltic magma, is primarily found on oceanic plates. This type of lava is characteristic of shield volcanoes and mid-ocean ridges, where tectonic activity allows magma to rise easily to the surface. In contrast, continental plates often host more viscous lava due to the higher silica content, resulting in more explosive volcanic eruptions.
Shield volcanoes are typically located at hot spots and divergent plate boundaries, such as in Hawaii or Iceland. These volcanoes have a low profile with gentle sloping sides due to the low-viscosity lava they erupt. Shield volcanoes are characterized by their broad, dome-like shape formed by repeated eruptions of fluid basaltic lava flows.
Shield volcanoes are known to produce the most lava annually compared to other types of volcanoes. Shield volcanoes have gentle sloping sides and are fueled by low viscosity magma, allowing for the rapid flow of lava over a large area. This results in high-volume eruptions that can cover vast areas with lava.
Directly along active oceanic ridges, such as the mid-oceanic ridge in the Atlantic (which Iceland straddles) and on active volcanoes, such as Hawaii. When lava from volcanoes such as Hawaii and the mostly undersea volcanoes of mid-oceanic ridges cools, it solidifies into brand new rock.
A volcano can be associated with either continental or oceanic crust, depending on its location. Oceanic volcanoes typically form along mid-ocean ridges or subduction zones and are composed primarily of basaltic lava. In contrast, continental volcanoes, which can form at convergent plate boundaries or hot spots, are often made up of more diverse rock types, including andesitic or rhyolitic lavas. Therefore, the type of crust associated with a volcano varies based on its geological setting.
Runny lava, which is typically associated with low-viscosity basaltic magma, is primarily found on oceanic plates. This type of lava is characteristic of shield volcanoes and mid-ocean ridges, where tectonic activity allows magma to rise easily to the surface. In contrast, continental plates often host more viscous lava due to the higher silica content, resulting in more explosive volcanic eruptions.
The lavas erupted from mid-oceanic ridges are called basalts. This lava contains quarts, feldspathoid, and plagioclase. Basalts has gray to black color.
Magma is molten rock deep below the surface of the Earth. Lava is the same stuff when it comes to the surface from a volcano or mid-oceanic ridge. NOW... LOOK UP "mid-oceanic-ridge" AND learn something wonderful! JCF
Mid-ocean ridges typically produce basaltic magma, which is low in silica content and flows easily. This type of magma is associated with fast-spreading divergent plate boundaries and results in the formation of oceanic crust.
mid ocean ridges
Shield volcanoes are typically located at hot spots and divergent plate boundaries, such as in Hawaii or Iceland. These volcanoes have a low profile with gentle sloping sides due to the low-viscosity lava they erupt. Shield volcanoes are characterized by their broad, dome-like shape formed by repeated eruptions of fluid basaltic lava flows.
Volcanoes that form along a mid-ocean ridge are called volcanic islands. These volcanoes occur when the plates move apart to produce gaps which molten lava rises to fill.
Volcanoes on land tend to be more explosive and have thicker lava flows, while underwater volcanoes, known as submarine volcanoes or seamounts, are typically less explosive and produce pillow lava formations due to rapid cooling in water. Underwater volcanoes also contribute to the formation of new oceanic crust as they erupt along mid-ocean ridges.
Volcanoes at spreading centers is referred to as spreading center volcanism. This usually takes place on mid-oceanic ridges where the plates diverge.