Sticky lava, also known as andesitic or rhyolitic lava, is typically found in stratovolcanoes and volcanic arcs, particularly along convergent plate boundaries. This type of lava has a high viscosity due to its higher silica content, which causes it to flow slowly and create steep, conical volcanoes. Notable examples include Mount St. Helens in the United States and Mount Fuji in Japan. Sticky lava can also be found in areas with continental crust, where it can lead to explosive volcanic eruptions.
Thick and sticky lava, known as pahoehoe lava, is typically found in Hawaii and other hot spot volcanic regions. Pahoehoe lava has a smooth, rope-like texture due to its high viscosity and low gas content, which causes it to flow slowly and form characteristic swirls and folds as it cools.
Runny lava contains low amounts of silicon, whereas sticky lava contains high amounts of silicon.
Composite volcanoes are found on destructive plate margins , where the oceanic crust sinks beneath the continental crust. Composite volcanoes have the following characteristics: Acidic lava, which is very viscous (sticky). Steep sides as the lava doesn't flow very far before it solidifies
A lava dome volcano is typically found at convergent plate boundaries, where two tectonic plates are colliding. The magma from the volcano is usually thick and sticky, causing it to build up and form a dome-shaped structure.
It is possible that Mt. Makushin, a stratovolcano in Alaska, may have sticky magma due to its composition and eruptive history. However, detailed studies would be needed to determine the specific properties of its magma.
The typical cone shape of a volcano happens when sticky lava erupts upward. Sticky lava creates a dome shape and the lava cools slowly.
Thick and sticky lava, known as pahoehoe lava, is typically found in Hawaii and other hot spot volcanic regions. Pahoehoe lava has a smooth, rope-like texture due to its high viscosity and low gas content, which causes it to flow slowly and form characteristic swirls and folds as it cools.
well, since basaltic lava is the same material that composes the ocean floor, it is common sense that it would be sticky, not runny.
the most dangerous type of lava is sticky lava because slow moving acid lava is more vicious
Runny lava contains low amounts of silicon, whereas sticky lava contains high amounts of silicon.
Glitter Lava is a sticky colourful lava thing that is save for skinyou can put it on you locker, laptop, shoes, car, ecthope I was helpful
Composite volcanoes are found on destructive plate margins , where the oceanic crust sinks beneath the continental crust. Composite volcanoes have the following characteristics: Acidic lava, which is very viscous (sticky). Steep sides as the lava doesn't flow very far before it solidifies
no, it depends on the type of bridge
A lava dome volcano is typically found at convergent plate boundaries, where two tectonic plates are colliding. The magma from the volcano is usually thick and sticky, causing it to build up and form a dome-shaped structure.
This type of lava can be found at Mt. Ol Doinyo Lengai, Northern Tanzania.
It is possible that Mt. Makushin, a stratovolcano in Alaska, may have sticky magma due to its composition and eruptive history. However, detailed studies would be needed to determine the specific properties of its magma.
free flowing lava