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A rift valley is where plate tectonics move apart or rift. They are created by the movement of tectonic plates. Tectonic plates are constantly moving shifting against each other in zones. It is "huge rocky slabs of Earth's lithosphere-- it's crust and upper mantle. A real life example is "The Great Rift Valley."

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Oceans are a result of tectonic plate activity, which describes the movement of the earth's lithosphere. At many convergent plate boundaries, dense lithosphere melts or slides beneath less-dense lithosphere in a process called subduction, creating a trench. An example would be the Mariana Trench which is the largest trench in the world it is in the western pacific ocean.

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Mid-Ocean Ridge is a chain of a formation of mountains under water, it's a mountain range. Basically its mountain ranges under water formed the same way they do on land. When beneath the ocean floor the mantle rises and sinks and creates convection currents and forms the under water mountain.
Reykjanes Ridge

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Himalaya Mountains
Rocky Mountains
Appalachian Mountains
Alps
Andes
Sierra Nevada
Atlas Mts.

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Volcanoes are found in the same place as earthquakes, and sometimes they are related but they are still independent events. When a volcano erupts the magma forcing its way through the crust it activates earthquakes.

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This picture shows the location of earthquakes. As you can see the earthquakes are happening right along the edges of the tectonic plates. Earthquakes are formed but the plates colliding, subduction or transforming. One of the largest eartquake "The Great Chilean Earthquake" was located right along the South American plate

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Mountains Form when the tectonic plates collide and one piece of the land goes under and the other plate starts going over the other plate, Mountain or volcano's form when this happens

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Broad belts are when boundaries are not well defined and the effects of plate interaction are unclear. They tend to have complicated geological structures and earthquake patterns.

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Transform Boundaries are when no crust is destroyed or created but the plates are just sliding against each other.An example of transform boundaries is the Alpine Fault of New Zealand.

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There are fragments that make up the world. Tectonic plates are when plates move and (could have) caused continental drift.

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Convergent Boundaries are when two or more tectonic plates are moving toward each other.The Washington-Oregon coastline of the United States is an example of this. Convergent boundaries form strong earthquakes, as well as volcanic mountains or islands, when the sinking oceanic plate melts.

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Plate Boundaries on the Map Earthquake's and Volcano's

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Plate Boundaries on the Map Earthquake's and Volcano's

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plate boundaries mark the area where a lot of earth quakes and volcano's can form. Usually there are many on the boundaries. There is a place called Ring of Fire, it is on the U.S. coast and goes into the ocean. This Ring of Fire contains the most earthquakes and Volcano's in the world, it has so many they gave it a name. It is also very dangerous in the area. So basically where ever you see mountains like the Rocky Mountain or the App. Mountain or the Nevada Mountain They all formed because of plate collision, wherever you see mountain's and volcano's or a record of earthquake's they are on a boundary line.

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A divergent boundary is when to plates are moving away from each other. The mid-Atlantic ridge is a example of this. This divergent boundary formed a underwater mountain range that is forever growing as a new crust is formed. mid-oceanic mountains/ridges are formed from Divergent Boundaries. Divergent boundaries also form volcanic islands which occur when the plates move apart to produce gaps which molten lava rises to fill.

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There  4 different types of plate boundaries that result in different outcomes:
Divergent boundaries-where new crust is generated as the plates pull away from each other.
Convergent boundaries -where crust is destroyed as one plate dives under another.
Transform boundaries - where crust is neither produced nor destroyed as the plates slide horizontally past each other.
Plate boundary zones - broad belts in which boundaries are not well defined and the effects of plate interaction are unclear.