The choices were:Eurasian, continental South American, oceanic African, oceanic North American, continentalBased on the… The Indo-Australian Plate includes the majority of the Indian Ocean. Tectonic plate interactions are of three different basic types:. Oceanic – oceanic plates are made of an oceanic crust called ‘sima’. These are also known as compressional or destructive boundaries. The Indian plate is located in the northeast hemisphere and it’s bounded by four major plates; Eurasian plate (North), Australian Plate (South East), African plate (South West) and Arabian plate (West).The Indian plate moves northward relatives to the Eurasian plate wich a … A subduction zone is formed at a convergent plate boundary when one or both of the tectonic plates is composed of oceanic crust. Marianas Trench is 10.911 km deep and 1580 miles long. Tectonic plates are nearly 100km thick. Or is it both? The African Plate's speed is estimated at around 2.15 cm (0.85 in) per year. Convergent boundaries include when two continental plates collide, two oceanic plates converge or when an oceanic plate meets a continental plate. An oceanic plate is a tectonic plate at the bottom of the oceans. I found the image and the given choices. This caused the continental crust to thicken due to folding and faulting by compressional forces pushing up … • There are three types of convergent plate boundaries: oceanic-oceanic boundaries, oceanic-continental boundaries, and continental-continental … The mountains are the result of the Indian plate colliding into the Eurasian plate during the Eocene, approximately 50 million years ago (Prakash et al., 2007). Subduction of one of the oceanic plates occurs because one plate is likely to be older and denser than the other. Ask for details ; Follow Report by Kyimonmonshein 26.01.2020 Log in to add a comment It borders the Eurasian Plate in the north, the Antarctic Plate in the south and the Pacific Plate in the east. There are actually two main types of tectonic plates, which are oceanic and continental. The volcanic activity the subduction causes (the same as in oceanic/continental destructive margins) leads to the formation of a chain of volcanic islands- like the Mariana Islands. Another interesting geologically active area on the Eurasian continent is southern China. It has been moving over the past 100 million years or so in a general northeast direction. The Earth's crust lies on top of the plates - the continental crust - the relatively thick part of the earth's crust which forms the large land masses. The Indo-Australian Plate includes the majority of the Indian Ocean. which includes most of the continent of EurasiaEurasia. Eurasia is a large landmass covering about … Generally, when the oceanic plate hits a continental one, the continental plate uplifts, and the oceanic plate goes beneath it or subducts. The Eurasian Plate is a tectonic plateTectonic Plate. Start studying Oceanic-Oceanic, Continental-Continental, and Oceanic-Continental Convergence. Several events can occur. Key Takeaways: Convergent Plate Boundaries • When two tectonic plates move toward each other and collide, they form a convergent plate boundary. ... What geological feature was created when the Pacific and Eurasian plate collided. Divergent boundaries are areas where plates move away from each other, forming either mid-oceanic ridges or rift valleys.These are also known as constructive boundaries. Continental drift means that plates are never idle. Learn vocabulary, terms, and more with flashcards, games, and other study tools. Eurasia and Australia to be exact, but you see also if you have a map of these plates.....the the plate is larger than the continent itself. Convergent boundaries are areas where plates move toward each other and collide. Over time, they move at a snail’s pace. It borders the Eurasian Plate in the north, the Antarctic Plate in the south and the Pacific Plate in the east. The Himalayas are where the thickest crust is found on Earth; roughly 60km thick. The Eurasian plate was partly crumpled and buckled up above the Indian plate but due to their low density/high buoyancy neither continental plate could be subducted.