Cinder cones are commonly found on the flanks of shield volcanoes, stratovolcanoes, and calderas.
A cinder cone or scoria cone is a steep conical hill of loose pyroclastic fragments, such as either volcanic clinkers, cinders, volcanic ash, or scoria that has been built around a volcanic vent. Cinder cones are made of pyroclastic material. Many cinder cones have a bowl-shaped crater at the summit. During the waning stage of a cinder-cone eruption, the magma has lost most of its gas content. This gas-depleted magma does not fountain but oozes quietly into the crater or beneath the base of the cone as lava. A cinder cone is a steep conical hill of tephra (volcanic debris) that accumulates around and downwind from a volcanic vent.The therefore mentioned Cinder Cone is located in a Valley Near the Columbia River Gorge in Skamania Washington.  Red Mountain, located in the Coconino National Forest of northern Arizona, 25 miles northwest of Flagstaff, is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a U, open to the west, and in lacking the symmetrical shape of most cinder cones.  Another area with a great deal of cinder cone volcanoes is the Raton Clayton volcanic field located in the northeastern portion of New Mexico. This area has around 120 cinder cones that range from 2,300 years old to over a million. Cerro Negro. Cerro Negro is located in Nicaragua and is currently the youngest volcano in Central America. It was first created in April of 1850 and since then has been one of the most active in the country. This volcano is in a group of four cinder cone volcanoes located in the Maribios Range. Cinder Cones. Cinder cones are simple volcanoes which have a bowl-shaped crater at the summit and 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.  Cinder cones are commonly found on the flanks of shield volcanoes, stratovolcanoes, and calderas. For example, geologists have identified nearly 100 cinder cones on the flanks of Mauna Kea, a shield volcano located on the island of Hawaii. Cinder cones are made of pyroclastic material. Many cinder cones have a bowl-shaped crater at the summit. During the waning stage of a cinder-cone eruption, the magma has lost most of its gas content. This gas-depleted magma does not fountain but oozes quietly into the crater or beneath the base of the cone as lava. Cinder cone volcanoes are located all over the world, including the  Amboy in the United States and Pinacate in Mexico. Lava Butte is  another cinder cone volcano in the Uni … ted States, located in  Oregon. Answered. 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 ga … ses carry liquid lava blobs into the atmosphere that fall back to earth around a single vent to form the cone. Cinder Cones. At the high-fountaining end of the spectrum are cinder cones. Cinder cones can be quite large in Hawai'i; those on the summit of Mauna Kea (formed during gas-rich alkalic-stage eruptions) are a few hundred meters high, whereas those on Mauna Loa and Kilauea usually range between 20 and 100 m high. In plan view, cinder cones tend to be roughly circular. They are usually formed later in an eruption when activity has localized to one or more discrete vents. If the precise location of the vent changes during an eruption, the cone loses its simple circular shape, and becomes more complex. Lava Butte. Lava Butte is one of the over 400 cinder cone volcanoes that surround the Newberry volcano. Normal cones in this area are generally 200 feet high while some of the larger ones reach 400 feet. Lava Butte, however, is 4,970 feet high and has created a flow that goes five miles north and three to the west. Cerro Negro. Cerro Negro is located in Nicaragua and is currently the youngest volcano in Central America. It was first created in April of 1850 and since then has been one of the most active in the country. This volcano is in a group of four cinder cone volcanoes located in the Maribios Range. Cinder cone volcanoes are the most common type of volcanoes. They are characterized by steeply angled sides and a conical shape. They are relatively small in size and can rang … e from tens to hundreds of meters in height. They are often found along the flanks of larger, more mountain sized volcanoes. 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 ga … ses carry liquid lava blobs into the atmosphere that fall back to earth around a single vent to form the cone.
https://en.wikipedia.org/wiki/Cinder_cone http://thecindercone.com/about http://pubs.usgs.gov/fs/2002/fs024-02/ http://www.basicplanet.com/cinder-cone-volcano/ http://www.windows2universe.org/earth/interior/cinder_cone.html https://en.wikipedia.org/wiki/Cinder_cone http://www.answers.com/Q/Where_are_cinder_cone_volcanoes_located http://volcano.oregonstate.edu/cinder-cones http://www.basicplanet.com/cinder-cone-volcano/ http://www.answers.com/Q/Where_are_cinder_cone_volcanoes_located
where are cinder cones located