You're possibly looking for an Andesite volcano. Characterized by periodic eruptions of ash and pumice, and prone to highly explosive eruptions. Some of these are just explosion craters - Yellowstone and Taupo would be a couple of examples where at the end of the eruption, a lake; or series of lakes; are left behind, but without an obvious cinder cone.
The name comes from the Andes mountains of S America, where there are exceptional examples of their cones.
A cinder cone volcano
Parasitic cone volcanos and cinder cone volcanos are not the same when classifying. Cinder cone volcanos are the most popular type of volcano, named for its cone shaped formation. Cinder cone volcano are also considered the smallest type of volcanos and can stand alone or grow on the flanks of other volcanos. The parasitic cone volcanos are similar to the cinder cones, however, the volcano is found on the flanks of other volcanos, hence, the name. It is created by flank eruptions of larger volcanos.
Some famous cinder cone volcanoes include Paricutin in Mexico, Sunset Crater in Arizona, and Capulin Volcano in New Mexico. These volcanoes are characterized by their small size and steep-sloped cones composed of loose volcanic fragments known as cinders.
Cinder cone volcanoes are named because they are composed primarily of loose volcanic fragments called cinders. These cinders are ejected during eruptions and accumulate around the vent, eventually forming the cone-shaped structure we see today.
shield volcano- volcano with whide crater developing from layers of lavacinder cone- small volcano with steep sides and explosive eruptions made of ash and rocks.composite volcano- tall volcano formed from eruptions of ash and rock followed by quiet lava flows.
A cinder cone volcano
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Parasitic cone volcanos and cinder cone volcanos are not the same when classifying. Cinder cone volcanos are the most popular type of volcano, named for its cone shaped formation. Cinder cone volcano are also considered the smallest type of volcanos and can stand alone or grow on the flanks of other volcanos. The parasitic cone volcanos are similar to the cinder cones, however, the volcano is found on the flanks of other volcanos, hence, the name. It is created by flank eruptions of larger volcanos.
The closest thing I can think of is a Cinder Cone Volcano. They look like conical mountains
Some famous cinder cone volcanoes include Paricutin in Mexico, Sunset Crater in Arizona, and Capulin Volcano in New Mexico. These volcanoes are characterized by their small size and steep-sloped cones composed of loose volcanic fragments known as cinders.
El cheesestick boner. It's a cinder cone volcano.
Cinder cone volcanoes are named because they are composed primarily of loose volcanic fragments called cinders. These cinders are ejected during eruptions and accumulate around the vent, eventually forming the cone-shaped structure we see today.
The cinder cone volcano located in New Mexico is called Capulin Volcano. It is part of the Raton-Clayton Volcanic Field and is known for its well-preserved shape and accessibility. Capulin Volcano offers visitors scenic views and hiking opportunities around its rim and down into the crater. It is also designated as a national monument, highlighting its geological significance.
shield volcano- volcano with whide crater developing from layers of lavacinder cone- small volcano with steep sides and explosive eruptions made of ash and rocks.composite volcano- tall volcano formed from eruptions of ash and rock followed by quiet lava flows.
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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.
When a secondary vent opens on a volcano the name can depend based on the type of eruption as well as the type of volcano. If a Shield Volcano has a secondary vent eruption it is called a rift eruption. This is demonstrated in the current eruption on Kileaua volcano in Hawaii. In a stratovolcano a secondary vent can either be a rift vent, or a cinder cone. This depends on the nature of the eruption. If it is a moderate explosive eruption with minor lava effusion than it would develope into a cinder cone, while if it is a constant lava spatter it would be deemed a rift zone eruption. There are several other minor terms of events, however they are extremely rare and are associated with both of these types of eruptions.