Ash and pumice are common materials.
In volcanoes that have lower amounts of volcanic gases in the magma. A good example is the volcanoes in the Hawaiian islands. Volcanoes with more gases in the magma tend to erupt explosively (Mt. St. Helens, Vesuvius) and have a thicker, slower moving lava.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
Active volcanoes on islands create more land area through the deposition of lava, ash, and other volcanic materials. When volcanoes erupt, the flowing lava solidifies and cools, forming new land masses on the island. Over time, repeated eruptions can contribute to the growth and expansion of the island.
Volcanoes with high levels of water in their lava produce ash, those with dry lava produce no ash.
The three major types of volcanoes are shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Shield volcanoes have broad, gently sloping sides and are primarily composed of basaltic lava. Cinder cone volcanoes are small, steep-sided volcanoes that erupt primarily cinder-sized fragments. Stratovolcanoes are tall, conical volcanoes composed of alternating layers of lava flows, volcanic ash, and other materials.
Lava, ash, pumice and molten debris.
Magma and lava also crust?
Gaseous matter such as H2O, SO2, CO2. Solid materials such as ash, lava, bombs.
When lava spews out of it.
Fissures usually erupt basaltic lava.
volcanoes will erupt and let out lava then the lava will harden and that will be new land.
When Volcanoes erupt the surface is melted by the lava
Volcanoes can erupt ash, gas, and pumice in addition to or instead of lava.
No. Volcanoes also release ash and a variety of gasses.
In volcanoes that have lower amounts of volcanic gases in the magma. A good example is the volcanoes in the Hawaiian islands. Volcanoes with more gases in the magma tend to erupt explosively (Mt. St. Helens, Vesuvius) and have a thicker, slower moving lava.
by pressure of molten lava of the dence viscocity.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.