No, Mount Vesuvius is not classified as a cinder cone volcano; it is actually a stratovolcano.
Stratovolcanoes are characterized by their tall, conical shapes and are built up from multiple layers of lava, ash, and other volcanic debris. Mount Vesuvius has a long history of explosive eruptions, which contribute to its stratified structure.
Cinder cone volcanoes, on the other hand, are typically smaller and formed from the eruption of volcanic ash and debris that accumulate around a single vent. These tend to have steeper slopes and a simpler structure compared to stratovolcanoes.
In summary, while Vesuvius has features seen in cinder cone volcanoes, it is primarily recognized as a stratovolcano due to its size, shape, and eruptive history.