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North and South America have joined, Africa and Eurasia are divided. This, folks, is our earth

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This is the stage closest to our own. You can clearly indenting the different structures we know today. Note however how north and South America aren't connected.

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The time of the dinosaurs! Here continents drift yet again (or to be more accurate, continue drifting).

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This is the second stage of the formation of land as we know it today. Here, Pangea divided into two supercontinents: Laurasia in the north and Gondawa in the south.

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Millions of years ago, all land was clumped together into one extra large continent, called Pangea. The next stages depict the ways in which this continent divided and spread due to the movement of tectonic plates.

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The rift is a narrow zone that is a developing divergent tectonic plate boundary,in which the African plate is in the process of splitting into two tectonic plates,called the Somali plates and the nabian plates at the rate of 6-7mm annually as extension continues ,lithosphere  will occur within 0 million years, the somaliplate will bfreak off,and a new ocean basin will form

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The rift is a narrow zone that is a developing divergent tectonic plate boundary,in which the African plate is in the process of splitting into two tectonic plates,called the Somali plates and the nabian plates at the rate of 6-7mm annually as extension continues ,lithosphere  will occur within 0 million years, the somaliplate will bfreak off,and a new ocean basin will form

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A continental carton:is an old old and stable part of the continental lithosphere,where the lithosphere consists of the earth tw top most layer,the crust and the upper most mantle.
Ocean basin:This are areas found under the sea.They are relatively inactive areas where deposits of sediment slowly collect and active areas where tectonic plates meet.
Volcanic arc:volcanic arts result from the subduction of an oceanic tectonic plate under another tectonic plate, and often parallel an oceanic trench.
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This is the transfer of heat by the mass movement of heated particles into an area of cooler fluid

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There is a very hot center made of iron (at least, we think it is iron because 1. it is very dense and 2. it creates a magnetic field, or atmosphere, without which life would be impossible). It is surrounded by several layers of magma. The actual crust on which we live  is tiny and superthin  compared to the rest of the earth.

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This is the same as the previous post, only that as mentioned, it causes mountains and earthquakes. One sample of mountains is the Himalaya Range, and an earthquake: the one in Nepal.The Washington-Oregon coastline of the United States is an example of convergent boundaries on land

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This is sometimes called the 'destructive boundary' as  is the causer of earthquakes. Here two plates collide against each other. One slips under the other and then it finally collides back. This image is of sea,  and one thing convergent boundaries can cause in the sea are volcanoes.

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When this happens (convergent boundaries in sea, underwater volcanoes happen.An example is he Cascade Mountain Range is a line of volcanoes above the melting oceanic plate.

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A divergent boundary is a linear feature that is found between two tectonic plates that are moving away from each other. This  can cause rifts that can eventually cause Rift Valleys.

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Transform boundaries are places where plates slide sideways past each other. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges. Their sliding motion causes lots of earthquakes. The strongest and most famous earthquake along the San Andreas fault hit San Francisco in 1906. Many buildings were shaken to pieces by the quake, and much of the rest of the city was destroyed by the fires that followed.

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Plate onics explains the features and movement of Earth's surface in the present and the past.
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.