Japan's largest historic eruption was at Towada in 915 AD.

Because Japan is in this zone, people who live in … At an ocean-ocean convergent boundary, one of the plates (oceanic crust and lithospheric mantle) is pushed, or subducted, under the other (Figure \(\PageIndex{1}\)). A destructive plate boundary is sometimes called a convergent or tensional plate … The collision of tectonic plates can result in earthquakes, volcanoes, the formation of mountains, and other geological events. [1] Tectonic erosion along convergent plate boundaries, whereby removal of upper plate material along the subduction zone interface drives kilometer‐scale outer forearc subsidence, has been purported to explain the evolution of nearly half the world's subduction margins, including part of the history of northeast Japan. The Cascade Mountain Range is a line of volcanoes above the melting oceanic plate. The plate collisions that occur in these areas can produce earthquakes, volcanic activity, and crustal deformation. A convergent plate boundary is a location where two tectonic plates are moving toward each other, often causing one plate to slide below the other (in a process known as subduction). Plate boundaries. Here the Nazca Plate is subducting beneath the South American plate. Other articles where Convergent plate boundary is discussed: earthquake: Tectonic associations: …zones, which are associated with convergent plate boundaries, intermediate- and deep-focus earthquakes mark the location of the upper part of a dipping lithosphere slab. Destructive plate boundary. Tephrochronology is commonly used in Japan and allows for a more detailed and balanced view of volcanic activity over the last 10,000 years. The Andes Mountain Range of western South America is another example of a convergent boundary between an oceanic and continental plate.

Tectonic Setting. Japan leads the world's volcanic regions with 1,274 dated eruptions and … Convergent plate boundaries are locations where lithospheric plates are moving towards one another. There are a number of different types of plate boundary. Often it is the older and colder plate that is denser and subducts beneath the younger and warmer plate. For example, the islands of Japan are a great example of a convergent plate boundary, which was formed by two oceanic plates (the Pacific Plate and the Philippine Sea Plate) subducting (Scholz & Kato, 1978). Japan is situated in a complicated plate boundary region where three subduction zones meet. Two of these subduction zones run parallel to the east coast of Japan.