gently sloping sides
Composite - Type / Shapevery steep sides at top
Shield - Viscosity of Magmalow viscosity / fast flowing
Composite - Viscosity of Magmahigh viscosity / slow / thick
Shield - Silicalow silica content
Composite - Silicahigh silica content
Shield - Temperature of Magmahot magma
Composite - Temperature of Magma'cool' magma
Shield - Source of Magmadirectly from mantle
Composite - Source of Magmamelted crust
Shield - Densityhigh density
Composite - Densitylow density
Shield - Eruption Typequiet eruptions / constantly 'oozing'
Composite - Eruption Typeexplosive eruptions / immense pressure / pyroclastic flow
Shield - ExampleHawaii / hot spots
Composite - Examplemt. fuji / convergent boundary
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Pyroclastic materials from shield volcanoes generally consist of basaltic lava flows and minor amounts of tephra, such as ash and cinder. These materials are typically low in silica content and flow easily, producing gentle, broad slopes characteristic of shield volcanoes. Explosive eruptions from shield volcanoes are less common compared to stratovolcanoes due to the lower viscosity of the magma.
Because if you look at them from above, they look like a warrior's shield.
No, shield volcanoes are a specific type of volcano characterized by their broad, gentle slopes and low viscosity lava flows. "Volcano" is a general term that refers to any landform where volcanic activity occurs, encompassing a variety of volcano types such as shield, composite, and cinder cone volcanoes.
The Hawaiian islands are made of two types of volcanoes, shield volcanoes and cinder cone volcanoes. Shield volcanoes have broad bases with gentle slopes. Cinder cone volcanoes have steeper sides, are made from fragments of lava, and are usually located at the base of shield volcanoes.
shield volcanoes are in many places but the most common are the Hawaiian Islands
Cinder volcanoes, composite volcanoes, frision volcanoes, and cinder cone volcanoes.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Pyroclastic materials from shield volcanoes generally consist of basaltic lava flows and minor amounts of tephra, such as ash and cinder. These materials are typically low in silica content and flow easily, producing gentle, broad slopes characteristic of shield volcanoes. Explosive eruptions from shield volcanoes are less common compared to stratovolcanoes due to the lower viscosity of the magma.
Because if you look at them from above, they look like a warrior's shield.
No, shield volcanoes are a specific type of volcano characterized by their broad, gentle slopes and low viscosity lava flows. "Volcano" is a general term that refers to any landform where volcanic activity occurs, encompassing a variety of volcano types such as shield, composite, and cinder cone volcanoes.
No. Compared to composite and cinder cone volcanoes, shield volcanoes are very short. Mauna Loa in Hawaii is a shield volcano.
The Hawaiian islands are made of two types of volcanoes, shield volcanoes and cinder cone volcanoes. Shield volcanoes have broad bases with gentle slopes. Cinder cone volcanoes have steeper sides, are made from fragments of lava, and are usually located at the base of shield volcanoes.
Kilauea is an example of a (shield) volcano.
Three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by low-viscosity lava, while stratovolcanoes are characterized by alternating layers of lava and ash. Cinder cone volcanoes are small, steep-sided volcanoes formed by pyroclastic material ejected during eruptions.
Composite.
No. Shield volcanoes are quite large. Cinder cones are the smallest volcanoes.