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A Destructive Plate Margin and Constructive Plate Margin :: Papers

destructive plate margin diagram

Remember that at divergent boundaries, new crust is being made, but the earth is not getting larger. Some of this molten material can work its way up through the continental crust through fissures and cracks in the crust to collect in magma chambers. Iceland owes its existence to this ridge. The friction between the two plates is often so great that the two sliding margins become 'stuck' together, allowing stresses to build up, which are then relieved by large earthquakes. Similarly, the Scotia arc in the southern Atlantic is terminated in the north by a long transform fault along the North Scotia Ridge that marks the boundary between the South American Plate and the Scotia Plate. Sometimes the plates get stuck and pressure builds and builds until eventually they suddenly jerk forwards. Molten rock inside the earth is called lava.

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Plate Boundaries: Convergent, Divergent, and Transform Boundaries

destructive plate margin diagram

Rising and diverging convection currents drag on the bottom of the plates causing them to shift apart. When it does, an earthquake occurs. The map above may seem confusing at first, but the main thing is that the colored lines show the lines where the crust is broken up into many different plates. A convergent boundary is a boundary where two separate plates are pushing into each other. When the oceanic crust begins to melt as it goes down into the hot mantle it starts to float back up, because it is made up of lighter material than the mantle.

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Constructive Plate Margins

destructive plate margin diagram

This is often s ome distance from the margin where magma can eventually re-emerge at the surface to create a range of mountains. There are other smaller plates however, such as the Philippines and Cocos plates. Originally, there used to be a sea called the Tethys sea between India and Asia, but over time India has collided into Eurasia creating huge fold mountains rich in marine sea fossils! They float on the semi-molten mantle rocks, and are moved around by convection currents within the very hot rocks. Does it result in Earthquakes or volcanoes? Molten rock and magma immediately rises to fill any possible gap and froms new oceanic crust. Does it result in Earthquakes or volcanoes? On the ocean floor the plates are spreading. Different plates move at a different rate. By not entertaining the argument, a positive person can diffuse the situation quickly.

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Plate Boundaries

destructive plate margin diagram

Rift valleys develop when a continent is broken apart by a divergent boundary. Note the location of the earthquake is beneath the offshore shelf and not in the trench. The Earth does have a solid core of Iron and Nickel, which is solid despite temperature of 3700°C because of the intense pressure there. In cross-section the convergent margin would look something like this: Diagram showing the tectonic plate movement beneath Japan. If continental crust pulls apart from continental crust then the same process occurs.

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Destructive Plate Margins

destructive plate margin diagram

The Daily Dish has a good of media relating to the effects of the quake, including footage of the tsunami inundating coastal areas. Anyone can learn for free on OpenLearn, but signing-up will give you access to your personal learning profile and record of achievements that you earn while you study. These rocks are fractured into huge segments called Tectonic plates. It is still the first model to neatly explain all the pieces of data scientists couldn't explain when they thought the surface of the earth was stationary. Only those sections of transform faults between two segments of constructive boundaries e. Would you expect to find earthquakes here? Small chains of islands are created in some places as new crust is created it builds into a small volcano that sometimes breaks the surface of the water. Watch an C ollision al At these margins 2 plates of similar density are forced toward each other.


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Constructive Plate Margins

destructive plate margin diagram

The Pacific plate is moving westward and being subducted beneath the northern part of Japan, which is on the Okhotsk Plate. As it sinks below the continental plate the oceanic plate melts due to friction in the subduction zone. Leave a Reply You must be to post a comment. This then builds up until the volcano gets higher and higher. This type of transform boundary produces shallow earthquakes and accompanying ground faulting. Volcanoes are a sign of a divergent boundary.

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What Happens At A Destructive Plate Boundary Bv

destructive plate margin diagram

Remember that this piece of North America is on a different plate, and the whole thing is moving. Even though, humans have existed on Earth for around 200,000 years, humans have been responding to the challenges of living on a planet with a constantly changing surface by using scientific evidence and technology to help them adapt to a constantly changing environment. Copy out the sentences you think are correct. Convergent boundaries form strong earthquakes, as well as volcanic mountains or islands, when the sinking oceanic plate melts. The Himalayas are still growing today as the plates continue to be pushed together at about 1 or 2cm a year! As they move past each other friction builds as the plates snag and grind on one another. This magma fills the gap and eventually erupts onto the surface and cools as new land.

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Plate Tectonics: 3.8 Conservative plate boundaries and transform faults

destructive plate margin diagram

Examples of plate margin types are linked to the map. This happens because oceanic crust is more dense than continental crust, making it more likely to be pushed back into the mantle. The crust becomes molten called magma. If a continent happens to be a place where a divergent boundary occurs, then the continent will begin to be torn apart as the sides of the plates separate, creating a rift valley. It is the Oceanic crust which sinks down into the mantle because it is denser heavier. The process of how constructive plate margins are formed : 1.


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