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A tectonic boundary where two plates are moving away from each other and new crust is forming from magma that rises to the Earth's surface between the two plates. The middle of the Red Sea and the mid-ocean ridge (running the length of the Atlantic Ocean) are divergent plate boundaries.

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Convergent boundaries are areas on Earth where two or more lithospheric plates collide. One plate eventually slides beneath the other causing a process known as subduction. The subduction zone can be defined by a plane where many earthquakes occur, called the Benioff Zone.

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"This type of convergent boundary happens where two oceanic plates push against one another, causing the colder, denser, older plate to buckle up and sink into the mantle.  Hot magma comes from where the plate sank, creating new crust." (http://gamediv1.weebly.com/convergent.html)

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"This type of convergent boundary happens where an oceanic plate and a continental plate push together causing the oceanic plate to be forced under the continental  plate into the mantle because the oceanic plate is thinner.  This is called a subduction.  When the oceanic plate is pushed under, it melts and turns into hot magma which burns its way through the continental plate, creating a volcano and causing many earthquakes." (http://gamediv1.weebly.com/convergent.html)

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"This type of boundary happens where two continental plates collide and push up creating mountain ranges.  Like colliding icebergs resist downward motion, the same thing happens with colliding continental plates, instead of moving down, they move up." (http://gamediv1.weebly.com/convergent.html)

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Transform boundaries are places where plates slide sideways past each other. At transform boundaries lithosphere is neither created nor destroyed. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges.

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movements along transforms plate boundary

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A transform fault or transform boundary is a plate boundary where the motion is predominantly horizontal. It ends abruptly and is connected to another transform, a spreading ridge, or a subduction zone.

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When a divergent plate boundary is found in the ocean, it will produce new sea-floor by putting lava up and pushing old sea-floor outward.

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Since continental crust is much thicker than oceanic crust, new land usually does not form. Instead rift valleys are formed and eventually they will fill with water.