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Mount Taal is a cinder cone volcano because it has a bowl shaped crater.

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10y ago

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What are the example of cinder cone volcano in the Philippines?

Some cinder cone volcanoes in the Philippines are Musuan, or Calayao Volcano, and Mayon Volcano.


What are the examples of cinder cone volcanoes in the Philippines?

Some examples of cinder cone volcanoes in the Philippines include Mount Malindig on the island of Marinduque and Mount San Carlos in Negros Occidental. These volcanoes are characterized by their steep sides and typically smaller size compared to other types of volcanoes.


How do cinder cone volcanos erupt?

Cinder cone volcanoes erupt explosively, but not as violently as composite volcanoes.


Where does cinder cone volcanoes form?

cinder cone volcanoes usually form around lithospheric plate boundaries.


What are the 3 common types of plutons?

Cinder volcanoes, composite volcanoes, frision volcanoes, and cinder cone volcanoes.


What are three types of volcanoes?

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.


What is the lava of cinder cone volcanoes?

A cinder cone has basaltic lava, which has a fairly low viscosity.


How are cinder volcanoes different from composite volcanoes?

Cinder cone volcanoes are much shorter and a little bit wider.


What are some types of cinder cone volcanoes?

volcanoes in guatemala


What famous volcanoes are cinder cone volcanoes?

Some famous cinder cone volcanoes include Parícutin in Mexico, Sunset Crater in Arizona, and Cerro Negro in Nicaragua.


What type of magma erupts from a cinder cone volcano?

Cinder cone volcanoes are formed by basaltic magma.


Where does Cinder Cone form?

cinder cone volcanoes usually form around lithospheric plate boundaries.