If gas pressure drops, the final stage cinder cone construction may be a lava flow that breaks through the base of the cone. If a lot of water in the environment has access to the molten magma, their interaction may result in a maar volcano rather than a cinder cone. If you found this answer helpful, please recomend me.
Cinder cone volcanoes are formed by the buildup of debris from magma ruptures in the earth. Koko Crater is an example of an extinct cinder cone.
Example of Cinder Cone volcanoes can be seen here:
http://en.wikipedia.org/wiki/Cinder_cone Or here:
http://en.wikipedia.org/wiki/Volcano#Cinder_cones
Paricutin, in Mexico.
Paricutin in Mexico
Cinder cone volcanoes are the most common kind of volcanoes. they are steep sided cones of basaltic fragments and are smaller and simpler than composite volcanoes. Streaming gases carry liquid lava blobs into the atmosphere that fall back to earth around a single vent to form the cone. The volcano forms when ash, cinders and bombs pile up around the vent to form a circular or oval cone. Cinders are melted volcanic rock that cooled and formed pebble-sized pieces when it was thrown out into the air. They are ejected from a single vent and accumulate around the vent when they fall back to earth. Bombs are melted volcanic rock that cooled and formed large pieces of rock when it was thrown out into the air before landing on the ground. Cinder cones are chiefly formed by Strombolian eruptions. They grow rapidly and soon reach their maximum size. Cinder cones can occur alone or in small to large groups or fields. Most have a bowl-shaped crater at the summit. The longer the eruption, the higher the cone. They rarely exceed 250 meters in height and 500 meters in diameter, although some may rise to as high as 650 meters or more. If gas pressure drops, the final stage cinder cone construction may be a lava flow that breaks through the base of the cone. If a lot of water in the environment has access to the molten magma, their interaction may result in a maar volcano rather than a cinder cone. The shape of a cinder cone can be modified during its life. When the position of the vent alters, aligned twin cones develop. Nested, buried or breached cones are formed when the power of the eruption varies. A great example of a cinder cone is Paricutin in Mexico. In Iceland, Surter I and Surter II cinder cone volcanoes created an island named Surtsey.
It is good to be interested in this sort of question, and the answers to it are available to you if you search the web or look in Wikipedia (it will help you to get answers more quickly if you learn how to do this) - for instance the answer to this question is to be found on the link I am placing below.
Cinder cones are usually not that deadly because they usually don't cause any loss of life. They are the smallest type of volcanoes, of all the volcanoes that there are(Composite Volcano, Shield Volcano, and Cinder Cone Volcano). Some dangers of the Cinder Cone volcano are listed below: 1.)Lava sprays out deadly 2.)The hot magma erupts 3.)Lava spills out,sometimes causing deaths 4.)The volcano rumbles 5.)The lava splashes everywhere 6.)Ash and molten rock burst out of the volcano
A conical volcano is the name given to a land form that has the shape of a volcano. A hill could be call a conical volcano when it is formed due to the debris from an eruption that forms the same shape as the volcano.
It is hard to distinguish between a dormant and extinct volcano, but it will be considered dormant if it has not showed signs of eruption over several spans of its recharge period. For example, a volcano that has been known to erupt every twenty years might be considered dormant if it goes sixty years without erupting. Signs that a volcano might be dormant and is not nearing an eruption include: -Does not produce smoke or sulfuric smell from vents or crater -Lava cannot be viewed in or near the volcano, or can only be found very deep inside the crater -No tremors or small earthquakes have been detected in the area around the volcano for a long period of time -Small plants and trees have grown naturally on the cone. (More plant life than moss or lichen)
Cinder cone volcanoes are the most common kind of volcanoes. they are steep sided cones of basaltic fragments and are smaller and simpler than composite volcanoes. Streaming gases carry liquid lava blobs into the atmosphere that fall back to earth around a single vent to form the cone. The volcano forms when ash, cinders and bombs pile up around the vent to form a circular or oval cone. Cinders are melted volcanic rock that cooled and formed pebble-sized pieces when it was thrown out into the air. They are ejected from a single vent and accumulate around the vent when they fall back to earth. Bombs are melted volcanic rock that cooled and formed large pieces of rock when it was thrown out into the air before landing on the ground. Cinder cones are chiefly formed by Strombolian eruptions. They grow rapidly and soon reach their maximum size. Cinder cones can occur alone or in small to large groups or fields. Most have a bowl-shaped crater at the summit. The longer the eruption, the higher the cone. They rarely exceed 250 meters in height and 500 meters in diameter, although some may rise to as high as 650 meters or more. If gas pressure drops, the final stage cinder cone construction may be a lava flow that breaks through the base of the cone. If a lot of water in the environment has access to the molten magma, their interaction may result in a maar volcano rather than a cinder cone. The shape of a cinder cone can be modified during its life. When the position of the vent alters, aligned twin cones develop. Nested, buried or breached cones are formed when the power of the eruption varies. A great example of a cinder cone is Paricutin in Mexico. In Iceland, Surter I and Surter II cinder cone volcanoes created an island named Surtsey.
It is good to be interested in this sort of question, and the answers to it are available to you if you search the web or look in Wikipedia (it will help you to get answers more quickly if you learn how to do this) - for instance the answer to this question is to be found on the link I am placing below.
it is a cone
They could, but it really doesn't happen all that often.
Cinder cones are usually not that deadly because they usually don't cause any loss of life. They are the smallest type of volcanoes, of all the volcanoes that there are(Composite Volcano, Shield Volcano, and Cinder Cone Volcano). Some dangers of the Cinder Cone volcano are listed below: 1.)Lava sprays out deadly 2.)The hot magma erupts 3.)Lava spills out,sometimes causing deaths 4.)The volcano rumbles 5.)The lava splashes everywhere 6.)Ash and molten rock burst out of the volcano
a top (the toy..) i think is an oblique cone.
An old fashioned DUNCE hat!
A cone could be a party hat && a sphere couldd be a bowling ball.
One example I know is an ice cream cone.
cyclinder = soda(can) cone = ice-cream cone rectangular (3d) = shoe box circle = beach ball
A conical volcano is the name given to a land form that has the shape of a volcano. A hill could be call a conical volcano when it is formed due to the debris from an eruption that forms the same shape as the volcano.
a flow that is in cone like shape. HAVE FUN WITH YOUR LIfE