Plate Tectonics: How Do Plates Move?

There are three different types of plate boundaries. The first type of plate boundaries is, the spreading boundary. A spreading boundary is when two plates move apart. The spreading boundary is also known as a divergent boundary. The second type of plate boundary is a colliding boundary. A colliding boundary is when two plates come together, or collide. It is also known as convergent boundary. The third is, a sliding boundary. A sliding boundary is when two plates slip past each other moving in opposite directions. It is also known as transform boundary. Those were the three different types of plate

Each plate is moving a certain direction due to the convection from the Asthenosphere. The meeting of two plates is called a boundary, there are three types of boundaries in the world: Convergent Boundaries, Divergent Boundaries. And Transform Boundaries. In the case of Convergent Boundaries, two plates are pushing against each other, which can create Deep Ocean Trenches, Huge Mountains, and/or Volcanic Mountain chains. An example of this happening is the Mariana Trench, During Convergence, the denser crust, oceanic crust, is subducted below the less dense crust. If the crusts have the same density then the plates are pushed upwards. At Divergent Boundaries, the plates are moving away from each other, this can create Mid-Ocean Ridges and Rift Valleys. An example of this happening is the Mid-Atlantic Ridge. At the final boundary, Transform Boundaries, the plates slide the past one another in the opposite direction, causing shallow earthquakes and offset features. An example of this Boundary is The San Andreas Fault. While the crust moves, there are places called Hot spots in which a hot portion of the mantle rises up beneath the crust for millions of years. An example of this is the Hawaii Island

Plate boundaries are pieces of earths’ crust and upper mantle interacting with each other. There are three ways these plates can interact with each other, transform, convergent, and divergent. When plates transform to each other, they are when two plates slide past each other, currently there are transforming plates in California right now. Convergent plates are two plates going towards each other, one going other the other, and the other overlapping. The final type is divergent plates, two plates going away from each other, one of these is found between North

There are three distinct types of plate boundaries existing, which are supported by geological observation, geophysical data, and theoretical considerations. Their names and categories are based on if adjacent plates move apart from each other (divergent plate margins), toward one another (convergent plate margins), or slip past one another in a direction parallel to their common boundary (transform plate margins) (Pitman, W.C., 2007).

Plate tectonics are very dangerous when they collide,slide,and move apart. They can create mountains like the Appalachian Mountains that used to tower over everything then erosion took place. The Appalachian Mountains were formed by convergent boundaries, convergent boundaries are collide

12. List the three types of plate boundaries and describe the relative motion at each of them.

The seven major tectonic plates comprise mostly on continental plates and the Pacific plate. The seven major plates from greatest to least are called: the Pacific Plate stretching 103,300,000 km2, North American Plate being 75,900,000 km2, Eurasian Plate being 67,800,000 km2, African Plate stretching 61,300,000 km2, Antarctic Plate being 60,900,000 km2, Australian Plate being 47,000,000 km2, and the South American Plate being 43,600,000 km2. With different tectonic plates, there are different ways they can move: divergent, convergent, and transform. Divergent plate movement is when both plates moving away from each other, creating a canyon that has magma pushing out from the bottom, forming new ground. Convergent is usually an oceanic plate and a continental plate are moving into one another, causing the oceanic plate to subducts into the mantle. This causes move active volcanos and earthquakes. Even though all of the plates are in the lithosphere, it's only the where Earth is flexible enough to move rather than flow. The lithosphere flexes when loads of weight are placed on it or

The different tectonic plates rest on the mantle, a very hot layer of earth that is directly beneath the crust. There are seven major tectonic plates, their names are The Pacific Plate, The North American Plate, The Eurasian Plate, The African Plate, The Antarctic Plate, The Australian Plate, and The South American Plate. In addition to these major plates there are also many smaller tectonic plates that make up parts of the Earth's crust. When the boundaries between plates shift, this causes earthquakes. There are three types of movements that cause earthquakes. Divergent is when the plates move away from each other, Subduction is when one plate moves underneath another, and Transform is when the plates grind against each other. The lithosphere is another name for earth's crust and mantle, it is made up of all the tectonic

Explain to the class that another type of plate tectonics, when the plates crash into each other, is called convergent, and that this causes the Earths crust to be pushed into the interior where it is remelted at the same rate the new crust is being made. Discuss the two kinds of surface features associated with them, then describe to them that with oceanic convergence, a deep ocean trench is formed along a line of the

The plate tectonics theory is the theory that the outer rigid layer of the earth is divided into several plates that move around across the earth's surface. There are many topics that support this theory, but I think that continental drift and seismic activity help support it the best. Theories can change over time because people get new understandings of things as time goes by, new knowledge is gained with new technology, and new discoveries can be made.

Earth has many tectonic plates which made out the seven continents. even today there are tectonic plates that are shifting. Some say that California is shifting away from the United States. Although, Earth started out with one continent called Pangaea. There are three major types of tectonic plate boundaries. The first one is divergent, divergent is when the plates move apart from one another. The second one is subduction, subduction is when the oceanic plate moves under a continental plate. Subduction mostly causes the most violent earthquakes and volcanic activity. The last major type of boundary is transform, transform is when the plates slide back and forth against one another. Plates that are located in the Lithosphere are North America, South America, Africa, Europe, Asia, India, Antarctica, Australia and the Pacific

Plate tectonics allows the Earth’s crust to continually change and move. There are seven major plates and many smaller plates making up the Earth’s Lithosphere. I remember from an Astronomy course I took in Muggle school that the major plates roughly correlate to the continents of the world. There major plate names are as follows: North American, South American, African, Antarctic, Australian, the Eurasian (which encompasses both continents of Europe and Asia), and Pacific (which encompasses the entire Pacific Ocean and is actually an oceanic plate whereas the other plates are continental plates). There are three types of boundaries where the different plates meet. The first one is called transform and this is where plates slide past each other. The second one is called divergent and is where plates move away from each other. And the third type of boundary is subduction where an oceanic plate moves under a continental plate. With a subduction boundary the plates continually “bump” into each other causing violent volcanoes and

The plate tectonic theory states that rigid plates slowly ride on the molten mantle. The boundaries between the plates are known to serve as an important mineral resource. Three types of tectonic plate exist: convergent, divergent and transform boundaries. A convergent boundary represents two plates moving towards each other mostly forming a subduction. When two plates move away from each other, a divergent boundary is formed. In transform boundaries, the plates move laterally past each other (Mission, 2016).

The tectonic plates and their movement are the basis of seismology which tries to explain the way in which the mountains and the seas we currently have on the surface of the Earth formed in the geological eras. The Ural Mountains are an example of how tectonic plates determined the formation of the landscape.

Mountains when two plate boundaries collide with each other. This process can also be called orogeny. Mountains form at subduction zones and can form with two oceanic plates, two continental plates, and with one oceanic and continental.