After Reading pages 42-47, answer the following questions in complete sentences.
1. What is Earth’s solid outer shell called? Earth's outer shell is called the lithosphere.
2. What do the Earth’s plates carry (3)? The earth's plates carry the lithosphere,oceans,the crust. -1 3. Explain the Theory of Plate Tectonics. The theory of plate tectonics is that plate tectonics is what moved pangea, a supercontinent with all the continents combined away from each other.
4. What makes Earth’s plates move? convection currents in the mantle is what moves the plates.
5. Name 3 ways that Earth’s plates interact with each other. Earth's plates interact with each other by colliding,splitting up,merging -2
6. What
Short went into depth when talking about the nine main plates of the Earth. The movement of these plates have caused land to separate and changed the location of continents. A great example of the power that these plates hold is when the Indo-Australian plate and the Eurasian plate came together.
Tectonic plates are powered by convection currents, which is the circular movement of magma within the mantle. These currents are powered by the core, which heats the magma, causing it to rise, cool and fall back down. This circular motion causes the plates, which float on the mantle, to
Plate Tectonics is a scientific theory which study how the Earth’s plates are driven and shaped by geological forces to keep them in constant movement. The theory explains the present-day tectonic behavior of the Earth, particularly the global distribution of mountain building, earthquake activity, and volcanism in a series of linear belt. (Pitman, W.C., 2007)
Plate tectonics is a theory that Earth’s crust is broken up into plates that float along the mantle. The plates act like a broken egg shell around the yolk or mantle, outer core, and inner core. Scientist Alfred Wegener didn’t have a scientific reason to explain how the continents moved. These plates are moving very slowly and in a very, very, very long time, Earth will look different than what the continents look like now. The Nazca Plate is moving southeast and will cause a collision with the South American Plate.
The theory of plate tectonics states that Earth’s outer shell is divided into plates. The crust and upper mantle is broken into plates that move around on the mantle, changing in size throughout time. The lithosphere makes up the crust and upper mantle and the asthenosphere a plastic like layer beneath the lithosphere. There are three types of plate boundaries. Divergent boundaries where two plates move away from each other. The ocean widens and new crust forms at the mid-oceanic ridge. Convergent boundaries has three types of converging, moving two plates towards each other. First we have an ocean floor plate that collides with a less dense continental plate. Next an ocean floor plate collides with another ocean floor plate. Finally a continental plate collides with another continental plate. Transform boundaries were two plates slide past one another. The resulting effects of plate tectonics is landforms such as rift valleys,
Plate tectonics is the scientific theory that attempts to explain the movements of the Earth's lithosphere that have formed the landscape features we see across the globe today” (Briney). Geology defines “plate” as a large slab of solid rock, and “tectonics” is part of the Greek root word for “to build.” Together the words define how the Earth’s surface is built up of moving plates. The theory of plate tectonics dictates that individual plates, broken down into large and small sections of rock, form Earth’s lithosphere. These fragmented bodies of rock move along each other atop the Earth’s liquid lower mantle to create the plate boundaries that have shaped Earth’s landscape. Plate tectonics originated from meteorologist Alfred Wegener’s theory, developed in the early 20th century. In 1912, he realized that the east coast of South America and the west coast of Africa appeared to piece together like a jigsaw puzzle. He further examined the globe and deduced that all of Earth’s continents could somehow be assembled together and proposed the idea that the continents had once been linked in a single supercontinent called Pangaea. To explain today’s position of the continents, Wegener theorized that they began to drift apart approximately 300 million years ago. This theory
From Visualizing Earth Science, by Merali, Z., and Skinner, B. J, 2009, Hoboken, NJ: Wiley. Copyright 2009 by Wiley. Adapted with permission.
The three major types of tectonic plates are divergent, subduction and transform. Divergent plates tend to move apart from each other. Subduction plates are when oceanic plate moves under a continental plate. This can cause volcanos to erupt and large sized earthquakes. Transform plates slide back and forth against one another. The Lithosphere consists of the Earths crust and uppermost mantle. The North American plate and the South American plate are the major plates of the lithosphere. The lithosphere also consists of the Pacific plate, the African plate and the Eurasian plate. The Pacific plate is the only major plate that is mainly underwater and is also the largest plate in the lithosphere. The Earth was once one large continental body called Pangea, before the plates started
Tectonic activity varies due to geographical location and position of tectonic plate boundaries. The Earth's crust is made up of continental and oceanic plates, which move across the surface of the planet, meeting at plate boundaries. Plate tectonics cause volcanic activity, tsunamis and
7. What is the relationship between plate tectonics and the ocean floor—seafloor spreading, for example?
On our home planet, there are eight major tectonic plates- African, Indo-Australian, Eurasian, Antarctic, North American, South American, Nazca and the Pacific. These plates are all separate and floats completely independently upon the Earth's mantle, which is much hotter than the crust of the planet. The locations where these plates meet each other are usually places that are extremely prone to large earthquakes and volcanic
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
The plates in our planets surface move on account of the serious warmth in the Earth's center. This causes liquid rock in the mantle layer to move. It moves in a way called a convection cell that structures when warm material ascents, cools, and finally sink down. As the chilled material sinks off, it is warmed and rises once
The pieces that make up the crust and mantle are called tectonic plates. They’re always slowly moving, and they can slide past each other or even bump into one another. The edges of these pieces, or plates, are called plate boundaries. They have lots of faults, which are the surfaces where they slip past each other, and these faults are where most earthquakes happen.