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Mercury Plate Structure

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1. Mercury

The surface of Mercury is rather geologically barren. When looking at the surface of Mercury using a magical telescope (as the muggle telescopes are not as powerful), the planets surface looks very similar to Earth's moon. Grey colored dust covers the planet. Because of being pelted with meteors during the Late Heavy Bombardment period 3.8 billion years ago, thousands of impact craters cover the surface. The largest known crater on Mercury is called the Caloris Basin and is about 1550 km across with its ring being nearly 2 km in height. Along with the numerous craters, the surface of Mercury also has escarpments, mountains and valleys that were likely formed due to volcanic activity.

2. Venus

The atmosphere of Venus, consisting …show more content…

These large sections between he cracks are called tectonic plates. Most of the major tectonic plates are in the Lithosphere- Earth's outermost layer. The major plates in the Lithosphere are the African plate, Antarctic plate, Eurasian plate, Indo-Australian plate, North American plate, Pacific plate and South American plate. The cracks in between these plates are boundaries. There are three main types of boundaries between the tectonic plates. The first is a divergent boundary, which occurs when two tectonic places move away from each other. Volcanic activity is common along this boundary A rift valley can also be created from this type of boundary The next is a convergent boundary, which happens when two tectonic plates come together. There are two kinds of surface feature that are associated with a convergent boundary, deep ocean trenches and volcanic and non-volcanic mountain ranges. The last is a transform boundary, when is when two plates slide against each other. The transform boundary is more commonly known as the fault boundary The most common surface activity associated with this boundary are

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