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Plate boundaries are the scene of much geological action - earthquakes, volcanoes, and a dramatic topography such a mountain ranges like Himalaya.

Map 1: Map showing earthquakes from 2003-2011 with magnitude greater than 3. Colors indicate depth of hypocenter, or origin of the earthquake: Red is 0-33 km, yellow is 33-100 km, green is 100-400 km, and blue is >400 km depth. Data are from the Advanced National Seismic System.

Map 2: Map showing volcanoes that have been active in the last 10,000 years. Colored triangles indicate different volcano types: Red triangles are primarily calderas; green triangles are stratovolcanoes; blue triangles are shield volcanoes and fissure vents. Data are from the Smithsonian Institution, Global Volcanism Program.

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-Divergent Boundaries: Is a linear feature that exists between two tectonic plates that are moving away from each other. Divergent boundaries within continents initially produce rifts.
-Convergent Boundaries: Are tectonic plates or fragments of the lithosphere move toward one another and collide. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries.

Depending of the plates involved, there are three types: Continental-Continental, Oceanic-Continental, Oceanic-Oceanic.

-Transform plate boundaries: Two plates sliding past each other forms a transform plate boundary.

Diferent boundaries in the Earth.

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To do this map we answer some questions and with the help of each other and a little bite of internet, we were able to do it.
In the map you can find:
- Divergent boundaries (Age of rocks on the seafloor, distribuation of volcanos, Landforms and hypocenter depths)
- Distribuation of volcanos
- Convergent boundaries (Distribuation of volcanos)
- Hotspots

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The theory of plate tectonics states that the Earth's outermost layer is fragmented into large and small plates that are moving relative to one another as they ride over hotter, more mobile material.
The following picture shows all the plate tectonics in the planet: