Nazca and South American boundary (featuring the Andes ranges) Since the African plate was denser, it was subducted under leaving the lighter continental crust above it.ДЄn interesting feature of the Alps is the Matterhorn which has rock materials from both the Eurasian plate and African plate but in different places. They formed from the African and Eurasian tectonic plates colliding together. It features sedimentary rocks which is evidence that it originally emerged from the sea. The Alps are some of the most majestic mountains around.

African Eurasian boundary (featuring the Alps) Source: Wikipedia The Indian plate still maintains its movement northward at 67 mm each year. One of them is Mount Everest which is the earthвЂ™s highest mountain. The collision of the plates has produced the Himalayas Range which has produced 15 of the highest mountains in the world. This boundary is a continent-continent convergent boundary. India plate and Eurasian plate (featuring the Himalayas) Its boundaries border other plates such s the Philippine, North American, Nazca, Indian-Australian, Cocos, Juan de Fuca, and Pacific plates. It has a length of about 40,000 kilometers. ItвЂ™s a ring covering 15 countries which include New Zealand, Papa New Guinea, Indonesia, Philippines, United States, Japan, Chile, Canada, Russia, Guatemala, and Peru.ДЄbout 450 volcanoes occur here which is 75% of all of the volcanoes on earth.ДЄlso, 90% of all earthquakes take place here. This is the most famous boundary because itвЂ™s the most active seismic area in the world. Here are 5 convergent boundary examples in real life. Mountain ranges can also form as well as earthquake action. Typically, no subduction takes place as both plates are less dense than the mantle.ДЄs a result of this boundary, intense faulting and folding can occur. It occurs when two continental plates collide with each other. This type of boundary is not as well understood as the others. The effects of this boundary are the formation of an oceanic trench and an area where earthquakes occur with increasing depth.Д¬hains of volcanic islands are also formed. The sunken plate gets heated in the mantle causing it to melt. So, it is pushed down or subducted beneath the other plate which is warmer and younger. Out of the two, the older or colder plate will be denser. e.g., a lithospheric mantle and an oceanic crust. Two oceanic plates meet under the ocean crust. Ocean trenches can also form as well as volcanic eruptions. The effect of this boundary is that an area of earthquake action is formed. For example, depths of about 160 m can cause the material to reach melting temperatures. Since the oceanic plate is denser than the continental plate, it is pushed or subducted under the continental plate.ДЄs the oceanic plate gets pushed into the mantle, it reaches high-temperature areas. This is where an oceanic and a continental plate collide. These are determined by the area or location on the earthвЂ™s crust where the boundaries are formed. Types of Convergent BoundariesД¬onvergent boundaries are of 3 types. The others are divergent and transform boundaries that are created in a different way.

This is a high activity area that can also literally get too hot to touch!ДЄ convergent boundary marks the area where two tectonic plates collide or meet each other.ДЄs a result of this, dramatic seismic events can follow like earthquakes, volcanic eruptions, or deformation of the crust.Д¬onvergent boundaries are just one of three types of tectonic plate boundaries that can form. You are likely to get some from a convergent boundary. Want a front-row seat to some tension-packed seismic action on earth?

Convergent boundary