Примери за използване на Convergent boundary на Английски и техните преводи на Български
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What is a Convergent Boundary?
A convergent boundary might also feature two oceanic plates.
Future activity is expected because the Alaska peninsula is on an active convergent boundary.
To the East is a convergent boundary with the Okhotsk plate.
These mountains were formed as a result of the collision between the Eurasian Plate andthe Indo-Australian Plate at the convergent boundary.
An example of this type of convergent boundary is the Washington-Oregon coastline of the US.
When two tectonic plates approach each other,subduction zones might be created at the convergent boundary between these two tectonic plates.
This is a convergent boundary and eventually the ocean will disappear and all that is left is a remnant ocean basin.
The northeasterly side is a complex but generally convergent boundary with the Pacific Plate.
At the subduction zone of a convergent boundary, the denser tectonic plate slides underneath the relatively less dense plate.
The Himalayas were born as a result of the collision between two continental plates(the Indo-Australian Plate andthe Eurasian plate) at the convergent boundary between these plates.
The tectonic activity at this convergent boundary has led to the formation of the volcanic Cascade Mountain Range.
The formation of Himalayas dates back to 70 million years ago,when a collision occurred between India and Asia, along the convergent boundary, via the Indo Australian and Eurasion Plates.
To answer the question“What Is A Convergent Boundary?”, we first need to understand the meaning of tectonic plates.
According to the modern theory of plate tectonics, their formation is a result of a continental collision ororogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate.
The northerly side of the Plate is a convergent boundary with the Eurasian Plate forming the Himalaya and Hindu Kush mountains.
Instead, subduction might happen to some extent if the heavier lithosphere below the crust might break free from it due to the forces of friction andpressure created at the convergent boundary.
Along the border with the Philippine Sea Plate is a convergent boundary that transitions into a rift.
The northern side is a convergent boundary subducting under the North American Plate forming the Aleutian Trench and the corresponding Aleutian Islands.
When a continental andan oceanic plate collide at the convergent boundary of the two plates, subduction zones often develop.
The eastern margin is a convergent boundary subduction zone under the South American Plate and the Andes Mountains, forming the Peru- Chile Trench.
The western side, the plate is bounded by the Okhotsk Plate at the Kuril-Kamchatka Trench and the Japan Trench,forms a convergent boundary by subducting under the Philippine Sea Plate creating the Mariana Trench, has a transform boundary with the Caroline Plate, and has a collision boundary with the North Bismarck Plate.
The south-east boundary, along the Manus Trench,is a convergent boundary, but in the absence of active volcanoes and earthquakes, is not a subduction zone at present.
In the south-west, the Pacific Plate has a complex but generally convergent boundary with the Indo-Australian Plate, subducting under it north of New Zealand forming the Tonga Trench and the Kermadec Trench.
Convergent boundaries are highly unstable areas of the lithosphere of the Earth.
Where Are Convergent Boundaries Located?
There are three types of convergent boundaries depending on the nature of the tectonic plates converging with each other.
Such types of convergent boundaries are also subjected to extensive faulting and folding of the rocks within the two plates that are colliding with each other.
At convergent boundaries that involve two continental plates, the plate tectonics is a bit more complex than in the other two types of convergent boundaries.
Convergent boundaries, also referred to as destructive plate boundaries, are locations on the lithosphere where two or more tectonic plates move towards each other leading to high levels of tectonic activities.