Well it depends on how bad the lava flow is. If the lava is flowing slow then the shape of the volcano won't change much, But if it flows with force then bits of the volcano will fall off and change the shape of the volcano.
Hope this answer helps!!
The shape tells a geologist how viscous (thick and sticky) the lava was. A taller volcano, such as a cone, was formed by thicker lava; a low volcano, such as a shield volcano, was formed by very runny lava.
Montserrat volcano is a stratovolcano, also known as a composite volcano. This type of volcano is characterized by steep slopes and a conical shape formed by layers of lava flows, ash, and volcanic rocks. Stratovolcanoes are capable of producing explosive eruptions.
There are two types of volcanoes formed by liquid rock (lava/magma), one being a shield volcano that are spread out over a large area but are not very tall because of the lava being mafic in nature (very liquid lava) such as the types of volcanoes that formed Hawaii, and the other being a composite volcano which is formed by felsic (thick) lava, making them steep and tall.
Lava. When the lava comes out of the volcano, gravity pulls the lava down the cone of the volcano, and depending the the viscocity of the lava, it forms a 'cone' or 'shield' as it cools. Thinner lava forms a shield volcano; thicker lava forms a steeper cone shape.
A conical volcano is a volcano with a classic triangular shape, formed from layers of lava, ash, and other volcanic debris. These types of volcanoes, such as Mount Fuji in Japan, typically have steep slopes and a conical appearance due to their eruptive style.
A volcano rock is rock formed from ash or lava erupted from a volcano.
The shape tells a geologist how viscous (thick and sticky) the lava was. A taller volcano, such as a cone, was formed by thicker lava; a low volcano, such as a shield volcano, was formed by very runny lava.
shield volcanoes are formed by lava flows or low viscosity lava that flows easily...
Montserrat volcano is a stratovolcano, also known as a composite volcano. This type of volcano is characterized by steep slopes and a conical shape formed by layers of lava flows, ash, and volcanic rocks. Stratovolcanoes are capable of producing explosive eruptions.
SGV
The typical cone shape of a volcano happens when sticky lava erupts upward. Sticky lava creates a dome shape and the lava cools slowly.
There are two types of volcanoes formed by liquid rock (lava/magma), one being a shield volcano that are spread out over a large area but are not very tall because of the lava being mafic in nature (very liquid lava) such as the types of volcanoes that formed Hawaii, and the other being a composite volcano which is formed by felsic (thick) lava, making them steep and tall.
shield volcano
Lava. When the lava comes out of the volcano, gravity pulls the lava down the cone of the volcano, and depending the the viscocity of the lava, it forms a 'cone' or 'shield' as it cools. Thinner lava forms a shield volcano; thicker lava forms a steeper cone shape.
The amount of lava and the thickness of the hole in which the lava rises up. Also the steepness of the actual volcano
No. A shield volcano is a large volcano with broad, shallow slopes formed from layers of lava flows formed by non-explosive eruptions. A cinder cone volcano is a small, steep-sloped volcano composed of pieces of rock formed by lava that was ejected explosively into the air.
A conical volcano is a volcano with a classic triangular shape, formed from layers of lava, ash, and other volcanic debris. These types of volcanoes, such as Mount Fuji in Japan, typically have steep slopes and a conical appearance due to their eruptive style.