No.
Depends, all volcanoes have different amounts of lava.
No. Lava flow in a volcanic eruption is a factor of the temperature, chemistry, and amount of trapped gas in the lava. Highly viscous, felsic, gas charged magmas tend to explode upon eruption. Low viscosity, basaltic magmas tend to flow upon eruption.
I only know four they are shield volcanoes, composite volcanoes, and lava plateaus thats all I know
No, not all volcanoes shoot out the same lava. There are four different kinds of lava. 1.) Volcanic 2.) magma 3.) sedimentary 4.) diesel hope this helps!
No. Large explosive eruptions do not produce lava, but rather produce clouds of hot ash, gas, and pumice. This is a result of gas-rich magma getting blasted into the air with such violence that the molten rock does not get a chance to flow as a liquid on the surface. These eruptions can produce towering ash columns that rain down on the country side, and pyroclastic flows, superheated avalanches of ash, rock, and gas that race down the sides of a volcano. Some explosive eruptions are phreatic, consisting of steam explosions from groundwater coming in contact with magma or rocks heated by magma.
Lava emissions are found with all active volcanoes, although some volcano emit more lave than others.
All volcanoes do have lava (magma), mostly in their young and early (ie, active) stages.
Shield volcanoes erupt in a flowing, non-explosive manner, the lava flowing for extremely long distances creating the gentle shield shaped form. Eruptions at shield volcanoes are only explosive if water somehow gets into the vent, otherwise they are characterized by low-explosive fountaining that forms cinder cones and spatter cones at the vent. In a shield volcano, 90% of the volcano is lava rather than pyroclastic material. Due to high magma supply rates, the lava is hot and changes very little after it is generated. A common product of hotspot volcanism, shield volcanoes can also be found along subduction-related volcanic arcs or all by themselvesShield volcanoes usually erup by fountaining or extruding lava.
All types of volcanoes involve the eruption of molten rock (magma) from beneath the Earth’s surface. They can also release gases, ash, and lava during the eruption, impacting the surrounding environment. Additionally, they are shaped by the accumulation of erupted materials over time.
The main types of volcanoes are stratovolcanoes (composite volcanoes), shield volcanoes, cinder cone volcanoes, and lava dome volcanoes. Stratovolcanoes have steep slopes due to the alternating layers of lava flows, ash, and other volcanic debris. Shield volcanoes have gentle slopes due to the low-viscosity lava flows. Cinder cone volcanoes are small and steep-sided, formed from explosive eruptions. Lava dome volcanoes are formed from slow, viscous lava flows piling up near the vent.
VOLCANOES Volcanoes are also like super duper hot hotubs! And also the lava from a volcano can reach up to 2000 degrees Fahrenheit! The volcanoes can produce ash, magma (which is a gooey substance), and last but not least lava (lava is a very hot substance which is also made from a volcano). Volcanoes can build land after it erupts it goes"kaboom"! When the red molten cools from the lava it turns into rock. Volcanoes are very useful because the lava from a volcano can heat cold hotubs during the winter.When the lava dries it will turn into a special rock called "Obsidian" that is very useful for carving spears and making knifes. Volcanoes can help you if you are in the middle of a power outage and to create flowers from its ash that it produces. There is also a volcanic ash called "Tuff". A long time ago this ash was used by ancient Romans to build solid buildings.
Basically because the type of lava they are made from is runnier and therefore spreads out more.