Several events can occur. The Himalayas are where the thickest crust is found on Earth; roughly 60km thick.
… Convergent boundaries include when two continental plates collide, two oceanic plates converge or when an oceanic plate meets a continental plate. Generally, when the oceanic plate hits a continental one, the continental plate uplifts, and the oceanic plate goes beneath it or subducts. As with oceanic-continental convergence, when two oceanic plates converge, one is usually subducted under the other, and in the process a trench is formed. Wow, that’s thick; we wouldn’t want to get caught under one of these! The Indo-Australian Plate includes the majority of the Indian Ocean. 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 … Continental drift means that plates are never idle. A subduction zone is formed at a convergent plate boundary when one or both of the tectonic plates is composed of oceanic crust. • There are three types of convergent plate boundaries: oceanic-oceanic boundaries, oceanic-continental boundaries, and continental-continental … It borders the Eurasian Plate in the north, the Antarctic Plate in the south and the Pacific Plate in the east. It borders the Eurasian Plate in the north, the Antarctic Plate in the south and the Pacific Plate in the east.

Eurasia is a large landmass covering about … Tectonic plate interactions are of three different basic types:.

The African Plate's speed is estimated at around 2.15 cm (0.85 in) per year. 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. These are also known as compressional or destructive boundaries. Oceanic – oceanic plates are made of an oceanic crust called ‘sima’.

Subduction of one of the oceanic plates occurs because one plate is likely to be older and denser than the other. It has been moving over the past 100 million years or so in a general northeast direction. Another interesting geologically active area on the Eurasian continent is southern China. Over time, they move at a snail’s pace. An oceanic plate is a tectonic plate at the bottom of the oceans. 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). Continental drift means that plates are never idle.

Some part of the plate is adjacent to an area of sea floor spreading where oceanic crust is being created, so even though they are thought of as "Continental" plates....they contain portions of continental crust as well as oceanic crust. The Indo-Australian Plate includes the majority of the Indian Ocean. This is a list of tectonic plates on the Earth's surface.Tectonic plates are pieces of Earth's crust and uppermost mantle, together referred to as the lithosphere.The plates are around 100 km (62 mi) thick and consist of two principal types of material: oceanic crust (also called sima from silicon and magnesium) and continental crust (sial from silicon and aluminium). Start studying Oceanic-Oceanic, Continental-Continental, and Oceanic-Continental Convergence. Ask for details ; Follow Report by Kyimonmonshein 26.01.2020 Log in to add a comment 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. This is drawing it closer to the Eurasian Plate, causing subduction where oceanic crust is converging with continental crust (e.g.