Yes
True. Cinder cone volcanoes are formed from the accumulation of volcanic ash, cinders, and small volcanic rocks that are ejected during explosive eruptions. These materials pile up around the vent in a steep, conical shape, resulting in the characteristic structure of cinder cone volcanoes.
shield volcanoes
Lava
Shield volcanoes are not hot spots but they are associated with them. However, such volcanoes can also form at rift zones.
A combination volcano develops from repeated lava eruptions and the accompanying tephra deposits Tephra is the debris from the eruption..
Cinder cone volcanoes are made of pyroclastic material and most often form from moderately explosive eruptions.
Cinder Cone
at hot spots(a place where volcanoes are very active)
Both shield volcanoes and stratovolcanoes can form islands.
An underwater volcano. The volcano that made Hawaii was a shield volcano.
Cinder cone volcanoes form from the accumulation of cinders and tephra during an explosive volcanic eruption. This material is ejected from the volcano and falls around the vent, building up a cone-shaped structure. Examples of cinder cone volcanoes include Paricutin in Mexico and Sunset Crater in Arizona.
Shield volcanoes.