/amaanswers.com/do-earths-plates-move-fast"> //amaanswers.com/what-is-tectonic-depression"> /amaanswers.com/do-transform-boundaries-cause-earthquakes"> Convergent boundaries occur between oceanic-oceanic lithosphere, oceanic-continental lithosphere, and continental-continental lithosphere. The geologic features related to convergent boundaries
vary depending on crust types. Plate tectonics
is driven by convection cells in the mantle.
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Ever, where in America is there a divergent plate boundary?
Tectonic Features of Western North America A divergent plate boundary runs through the Gulf of California in Mexico. The divergence is pulling Baja California and mainland Mexico apart. Just north of there, around the US-Mexico border, in California, there is a transform boundary.
Eventually, where can plate boundaries be found? Plate boundaries are found at the edge of the lithospheric plates and are of three types, convergent, divergent and conservative. Wide zones of deformation are usually characteristic of plate boundaries because of the interaction between two plates. The three boundaries are characterized by their distinct motions.
At least, what are examples of convergent boundaries?
Examples of ocean-continent convergent boundaries are subduction of the Nazca Plate under South America (which has created the Andes Mountains and the Peru Trench) and subduction of the Juan de Fuca Plate under North America (creating the Cascade Range).
What is an example of a convergent plate boundary?
The Washington-Oregon coastline of the United States is an example of this type of convergent plate boundary. ... The Andes Mountain Range of western South America is another example of a convergent boundary between an oceanic and continental plate. Here the Nazca Plate is subducting beneath the South American plate.
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Answer. Explanation: Most of the hazards that characterize a divergent plate boundaries lie under the ocean but on land the hazards are faults, volcanoes , and the most obvious one; earthquakes. These are also known as conservative boundary because the plates grind past one another, not destroying the lithosphere.
If two tectonic plates collide, they form a convergent plate boundary. Usually, one of the converging plates will move beneath the other, a process known as subduction. ... The new magma (molten rock) rises and may erupt violently to form volcanoes, often building arcs of islands along the convergent boundary.
Divergent boundaries -- where new crust is generated as the plates pull away from each other. Convergent boundaries -- where crust is destroyed as one plate dives under another. Transform boundaries -- where crust is neither produced nor destroyed as the plates slide horizontally past each other.
A divergent boundary occurs when two tectonic plates move away from each other. ... Magma rises into and through the other plate, solidifying into granite, the rock that makes up the continents. Thus, at convergent boundaries, continental crust is created and oceanic crust is destroyed.
Examples of Divergent Boundaries The mid-Atlantic ridge is an example of a divergent boundary, where the Eurasian Plate that covers all of Europe separates from the North American Plate. This underwater mountain range is constantly growing as new crust is formed.
Explanation: Examples of non-convergent boundaries include “Mid-Atlantic Ridge and Great Rift Valley”. Iceland is an example of country undergoing continental non-convergent boundaries. Convergent boundaries are the boundaries between “two or more tectonic plates” which are coming towards each other.
There are three main types of plate boundaries:
- Convergent boundaries: where two plates are colliding. Subduction zones occur when one or both of the tectonic plates are composed of oceanic crust. ...
- Divergent boundaries – where two plates are moving apart. ...
- Transform boundaries – where plates slide passed each other.
Convergent boundaries are boundaries where two plates are pushing into each other. They are formed when two plates collide, either crumpling up and forming mountains or pushing one of the plates under the other and back into the mantle to melt.
Earthquakes at convergent plate boundaries mark the location of the subducting lithosphere. The motion of the lithosphere as it plunges through the mantle causes the quakes (Figure below). At greater depths, the plate heats up enough to deform plastically.
Reverse faults occur at convergent plate boundaries, while normal faults occur at divergent plate boundaries. Earthquakes along strike-slip faults at transform plate boundaries generally do not cause tsunami because there is little or no vertical movement.
Transform boundaries represent the borders found in the fractured pieces of the Earth's crust where one tectonic plate slides past another to create an earthquake fault zone. Linear valleys, small ponds, stream beds split in half, deep trenches, and scarps and ridges often mark the location of a transform boundary.
Transform boundaries are also known as conservative plate boundaries because they involve no addition or loss of lithosphere at the Earth's surface.
What is the difference between a divergent and convergent plate boundary? A divergent (constructive) plate boundary is one where the two plates are moving APART from each other in opposite directions. ... A convergent (destructive) plate boundary is one where the two plates are moving TOWARDS each other.