Plate Boundaries and Their Hazards
Destructive boundaries are where the real drama happens. At subduction zones like the Andes, oceanic plates crash into continental plates. Because oceanic crust is denser, it gets forced underneath, melts, and creates magma that erupts as volcanoes.
When two continental plates collide (like in the Himalayas), neither can sink, so the land gets crushed upwards into massive fold mountains. You get earthquakes here but no volcanoes.
Constructive boundaries work the opposite way - plates pull apart likeattheMid−AtlanticRidge, allowing magma to rise and form new volcanoes. Conservative boundaries are where plates simply slide past each other, like California's San Andreas Fault.
Remember: The type of boundary determines what hazards you'll get - it's all about the direction plates are moving and what type of crust is involved.