What volcanoes form at divergent plate boundaries and hot spots?

Rift volcanoes form when magma rises into the gap between diverging plates. They thus occur at or near actual plate boundaries.

Where do cinder cone volcanoes occur?

Cinder cones are found in many parts of the world, including: Australia, Canada, Chile, France, Iceland, Italy, Japan, Mexico, New Zealand, Peru, the Philippines, Russia, Spain (Canary Islands), Turkey, and the United States.

How are cinder cone volcanoes formed?

Cinder cones form from ash and magma cinders–partly-burned, solid pieces of magma, that fall to the ground following a volcanic eruption. This type of eruption contains little lava, as the magma hardens and breaks into pieces during the explosion.

Why do volcanoes form at plate boundaries and hot spots?

A hot spot is an intensely hot area in the mantle below Earth’s crust. The heat that fuels the hot spot comes from very deep in the planet. This heat causes the mantle in that region to melt. The molten magma rises up and breaks through the crust to form a volcano.

What plate boundary do cinder cone volcanoes form?

Cinder cones form along convergent plate boundaries, divergent plate boundaries, and some types of transform plate boundaries (specifically, those that involve divergence). Basically, anything that gets magma near the surface will create cinder cones, whether through spreading or through subduction.

Is a cinder cone volcano?

Cinder cones are the most common type of volcano in the world. They may look like an idealized depiction of a volcano as they are steep, conical hills that usually have a prominent crater at the top. Cinders at Capulin Volcano. Cinders are small chunks of scoria.

What type of volcano is cinder cone?

Cinder cones are simple volcanoes which have a bowl-shaped crater at the summit and steep sides. They only grow to about a thousand feet, the size of a hill. They usually are created of eruptions from a single opening, unlike a strato-volcano or shield volcano which can erupt from many different openings.

What are the characteristics of cinder cone volcanoes?

The characteristics of cinder cones include:

  • cone shape.
  • made of igneous rock.
  • typically symmetrical; can be asymmetric if wind was blowing during an eruption and rock landed primarily on one side.
  • relatively low altitude (300-1200 ft.)
  • eject fragments of lava (called tephra) from one vent.

What boundary do cinder cone volcanoes form?

What type of volcano is a cinder cone volcano?

Cinder cones are the simplest type of volcano. They are built from particles and blobs of congealed lava ejected from a single vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as cinders around the vent to form a circular or oval cone.