Most of the lava is liquid. Has very LOW viscosity
it wil have thin lava because the lava is "runny" and shield volcanoes are made from nonexplosive eruptions so they will be quiet when they erupt.
the Philippines volcano's form thin layer of cooled lava but not really cold like freezing
silica content
No, shield volcanoes typically have relatively thin, fluid lava that can flow over long distances. This type of lava, often basaltic in composition, allows for the gentle, broad slopes characteristic of shield volcanoes. The low viscosity of the lava contributes to the volcano's shield-like shape, as it spreads out instead of piling up.
A basic volcano, often referred to as a shield volcano, is formed by the gradual accumulation of low-viscosity basaltic lava that flows easily over long distances. As the lava erupts from a central vent or fissure, it spreads out in thin layers, creating a broad, gently sloping structure. Repeated eruptions build up the volcano over time, resulting in its characteristic shield-like shape. These volcanoes typically produce non-explosive eruptions due to the low gas content and fluid nature of the basaltic lava.
it wil have thin lava because the lava is "runny" and shield volcanoes are made from nonexplosive eruptions so they will be quiet when they erupt.
the Philippines volcano's form thin layer of cooled lava but not really cold like freezing
No
silica content
A+ answer : shield volcano
No, shield volcanoes typically have relatively thin, fluid lava that can flow over long distances. This type of lava, often basaltic in composition, allows for the gentle, broad slopes characteristic of shield volcanoes. The low viscosity of the lava contributes to the volcano's shield-like shape, as it spreads out instead of piling up.
A basic volcano, often referred to as a shield volcano, is formed by the gradual accumulation of low-viscosity basaltic lava that flows easily over long distances. As the lava erupts from a central vent or fissure, it spreads out in thin layers, creating a broad, gently sloping structure. Repeated eruptions build up the volcano over time, resulting in its characteristic shield-like shape. These volcanoes typically produce non-explosive eruptions due to the low gas content and fluid nature of the basaltic lava.
A large, dome-shaped volcano is known as a shield volcano. These volcanoes are characterized by their broad, gently sloping profiles built up by many thin, fluid lava flows. Mauna Loa in Hawaii is a famous example of a shield volcano.
Kilauea is a shield volcano. Its low viscosity lava flows spread out in thin layers, creating a broad and gently sloping shield-like shape. It is one of the most active volcanoes in the world, located on the Big Island of Hawaii.
Shield volcanoes are likely to form at hot spots where magma wells up from the mantle and erupts through the crust. They often occur in areas with thin crust, such as oceanic regions, and are characterized by broad, gently sloping profiles due to the flowing and relatively low-viscosity lava. Examples include the Hawaiian Islands and the Galápagos Islands.
Thin lava
Kilauea volcano primarily produces basaltic rock, which is a type of volcanic rock that is low in silica content and flows easily when molten. The lava flows from Kilauea are typically thin and hot, allowing them to travel long distances before solidifying.