(1) At convergent boundaries (subduction zones), where one plate is being subducted (going beneath) the other.
(2) At hot spots, where a large magma plume has risen from the mantle.
(3) At divergent boundaries, where crust is moving apart, magma is wedging its way between the crust, and often erupts as a volcano.
Some people think that Volcanoes form from Earthquakes, but they don't.
Volcanoes can form at convergent plate boundaries when one tectonic plate subducts beneath another. They can also form at divergent plate boundaries where plates move apart, allowing magma to rise and create new crust. Another way is through hot spots, where magma rises through the mantle and creates volcanoes independent of tectonic plate boundaries.
The three types of volcanoes are cinder cone, composite, and shield. Cinder Cones look like a cone-shaped mountain. A material called tephra (cinder) erupts and forms a cone-shaped mountain. Cinder cones are 100 to 400 meters tall. An example is Krakatoa Island.
Composite Volcanoes have both tephra and lava material that erupt from it. The materials layer themselves and form a huge cone-shaped mountain. Composite volcanoes are 100 to 3500 meters tall. Mount St. Helens is an example of a composite volcano.
Shield Volcanoes look like dome-shaped mountain. The mountain is formed when the lava spills out and gradually creates a dome-shaped mountain. Shield volcanoes are 9000 meters tall. Example: Hawaii Island.
(1) At convergent boundaries (subduction zones), where one plate is being subducted (going beneath) the other.
(2) At hot spots, where a large magma plume has risen from the mantle.
(3) At divergent boundaries, where crust is moving apart, magma is wedging its way between the crust, and often erupts as a volcano.
volcanoes takes place in two ways which are at the hotspot and at the point of weakness which are fault or crack
Land Volcanoes eat lamas and underwater volcanoes eat camals
There are three different types of volcanoes. The types of volcanoes are shield volcanoes, dome volcanoes, and also composite volcanoes.
Plates do not cause volcanoes. Volcanoes generally form at the boundaries between plates. They form at convergent and divergent boundaries.
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.
The two ways to write the plural form of "volcano" are "volcanoes" and "volcanos". The most common and accepted plural form is "volcanoes".
volcanoes takes place in two ways which are at the hotspot and at the point of weakness which are fault or crack
Well one way is when a volcano erupts, the lava dries and then it can make the volcano bigger by building it up.
Glaciers, volcanoes, and erosion, explosion, implosion.
The path of three over two divided
Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.
Press under the earth. Erosion, and volcanoes.
Three types of volcanoes are Cinder Cone Volcanoes, Shield Volcanoes and Composite Volcanoes.
Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.
The plural possessive form of "volcanoes" is "volcanoes'".
there are three and they are Active Volcanoes, Dormant Volcanoes, and Extinct Volcanoes.
Volcanoes usually form where tectonic plates meet.