
There are three types of plate boundaries; divergent, convergent, and transform. A
divergent boundary is a tectonic plate that is moving away from another plate. These two plates moving away from each other cause rift valleys to form on land and ocean rifts to form in the ocean. A
convergent boundary is when two plates move toward each other and then collide. These boundaries form subduction zones and continental collisions. There are three types of convergent boundaries: oceanic/continental- where an oceanic plate slides underneath a continental plate causing a volcanoe arc and trenches, continental/continental- where one continental plate slides under another continental plate forming mountain ranges and plateaus, and oceanic/oceanic- where one oceanic plate slides under another oceanic plate forming island arcs, underwater volcanoes, and deep sea trenches. The third plate boundary, the
transform boundary, is a boundary where two plates slide horizontally against each other. This causes some of the boundaries to become zigzagged.

There are alos three types of volcanoes; shield, strato, and cinder cone. A
shield volcano is a large volcano with shallow sloping sides. A
stratovolcano is a tall cone-shaped volcano made up of many layers of hardened magma. A
cinder cone is a steep cone shaped volcano. All of these types may be found around the ring of fire which is a volcano hot spot located around plate boundaries in the Pacific Ocean.
Sources:
http://en.wikipedia.org/wiki/Convergent_boundaryWikimedia Foundation Inc.
Wikipedia
Convergent Boundary
May 13, 2008
http://vulcan.wr.usgs.gov/Glossary/ShieldVolcano/description_shield_volcano.htmlUSGS
Shield Volcano
December 28, 2005
Pictures:
http://en.wikipedia.org/wiki/Convergent_boundaryWikimedia Foundation Inc.
Wikipedia
Convergent Boundary - Oceanic/Continental
May 13, 2008
http://vulcan.wr.usgs.gov/Glossary/ShieldVolcano/description_shield_volcano.htmlUSGS
Shield Volcano
December 28, 2005