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Plate tectonics quiz
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The Magnificent North American Tectonic Plate Even though other global problems are bigger than Plate tectonics, the North American Plate took many years to form, is very divers, and is purely magnifect because a big part of our everyday life and the plate tectonic theory is one of the oldest theories known to man. There are also many different aspects to the North American Plate. There are regular basic facts about the plates, there are specific scientists that gathered and founded information about this plate and many others. There is the location of this plate and the plates surrounding it. There are multiple different types of boundaries that surround this plate. Also, there is the multiple years it took for this and other plates to form. …show more content…
there were many specific scientists that contributed to this idea of the moving continents, some more than others. 2 major contributors to the idea were Alfred Wegener, and Henry Hess. They all contributed to the idea of why the plates are in different place that when the Earth was first born. One of the Scientists, Alfred Wegener, is very well known and his name is related when talking about Plate tectonics. When he first proposed( put out there) his theory ( which later turned out to be right) it was rejected immensely because he did not know how or why the continents moved. He just had a theory, but know facts. When coming up with this idea of plate tectonics, he used many different tools. He used fossils, different rock types, and a bunch of climatic evidence. Henry hess came up with the idea of seafloor spreading( the oceanic plates spreading and moving …show more content…
What kind of boundaries are there, where are the located, and most importantly, what kind of boundaries does the North American Plate have. These plates are constantly sliding past each other with every passing year. There are 3 main plate boundaries that we all need to know. They are convergent, divergent, and transform. They all have different names even though they are all related to boundaries. This is because all of them move the crust in different ways. Weather it be a few tenths of degrees or multiple degrees, the plates are always moving. Sometimes when these plates collide, things like volcanoes can come to form. The boundaries can make things like: folded mountain ranges, volcanoes, earthquakes, trenches, mid ocean ridges, and rift valleys. Convergent boundaries are when the plates collide into each other. Divergent boundaries are when the plates move apart from each other. And lastly, Transform boundaries are when the plates slide laterally past each other.for some examples: Southern California is on the boundary of the North American Plate and the Pacific Plate, therefore making it an easy fault zone. That is why Southern California has so many earthquakes. It is because they are on the a transform boundary. Another examples is that A divergent boundary on iceland between the North American plate and the Eurasian plate is causing iceland to split along a mid ocean
15. The pictures above show how the continents on Earth’s surface have changed position over a very long period of time. What explains this change? (S6E5e, f)
Earthquakes are a natural part of the Earth’s evolution. Scientific evidence leads many geologists to believe that all of the land on Earth was at one point in time connected. Because of plate tectonic movements or earthquakes, continental drift occurred separating the one massive piece of land in to the seven major continents today. Further evidence supports this theory, starting with the Mid-Atlantic ridge, a large mass of plate tectonics, which are increasing the size of the Atlantic Ocean while shrinking the Pacific. Some scientists believe that the major plate moveme...
... plate is now called the Juan de Fuca plate (“Juan de Fuca General”). This happened just before the Laramide orogeny contributing to the building of this huge landmass of geological features.
When the plates mash together on a convergent boundary, they can create an earthquake. A place with a convergent boundary is New Zealand. When the plates pull apart, a divergent boundary, they create a hole in the ocean that causes molten lava to rush up and it causes a volcano to form. A place with a divergent boundary is Iceland. With about 130 volcanoes all together, it has the most volcanoes of any country in the world and is on two tectonic plates. Santorini is currently in an area of earth where the African and Eurasian plate meet, and Atlantis disappeared with a rumble that could have come from a volcano or an
For example when he writes about how the axes of each continent affects how well ideas and domesticated crops and animals flow or spread through the continent. This discussion had made lots of sense for me and is yet another idea that supports his theory. "At the one extreme was its rapid spread along east-west axes: from Southwest Asia both west to Europe and Egypt and east to the Indus Valley (at an average rate of about 0.7 miles per year); At the opposite extreme was its slow spread along north-south axes: at less than 0.5 miles per year, from Mexico northward to the U.S. Southwest; at less than 0.3 miles per year, " This example shows how east to west axes allow for a faster diffusion of crops and animals. But the north to south is very slow compared to the other. This helps explain why Eurasia had developed the quickest and the America and Africa lagged behind." For example, Portugal, northern Iran, and Japan, all located at about the same latitude but lying successively 4,000 miles east or west of each other, are more similar to each other in climate than each is to a location lying even a mere 1,000 miles due south." This line tells us why Eurasia was able to develop so fast. That is because it has an east to west axes which means animals and crops can more wildly thought the same land due to there being large amounts of land with the same latitude. While the Americas
What challenges did explorers and colonists face in what became North America from the 1580’s until the 1630’s? Look at geographical, political, economic, indigenous peoples, climate, diet, etc., anything that presented a challenge to survival and development during this period.
There have been many influential moments throughout North America that has helped it become what it is today. I have only touched on the ones the book spoke of, to write about all the moments, it would be the length of a book. It’s amazing to see how one action has such a major effect on not just one country but all three. North America has had many similarities in its development and also many differences as well.
Before examining the Northridge event, understanding the naturally occurring hazard that is an earthquake will help to better understand exactly what happened and why it was such an important geological event. With four distinct layers, two layers, the crust and upper portion of the mantle, compose the skin that is the surface layer of the Earth. The crust is not a single, continuous piece. It is actually several different pieces, or plates, that come together to form the puzzle that comprises the surface of the Earth. These plates are in constant motion rubbing against one another. These areas, known as fault lines, where the plates rub up against one another have spots where one plate ”gets stuck while the rest of the plate keeps moving. When the plate has moved far enough, the edges unstick and is how most of the earthquakes around the world occur” (Wald, 2012). The energy stored from the friction of the two plate...
Pangaea or Pangea is the name given to the supercontinent that existed during the Paleozoic and Mesozoic eras, before the process of plate tectonics separated each of the component continents into their current configuration. The movement of Earth’s tectonic plates formed Pangaea and ultimately broke it apart.
Volcanism is a major part of the Galapagos and their formation. The island chain is positioned on the Nazca Plate, which is subducting beneath the South American Plate at a geologically rapid pace of 2.5 inches per year. In addition, this Nazca Plate is located directly on top of the Galapagos Hotspot. It is here that mantle plumes melt Earth’s crust, creating volcanoes as a product. The oldest island was first shaped by this ...
One way Alfred Wegener proved his theory of continental drift was through land features. He realized that the coal fields, mountain ranges, and continents matched, and he attempted to put the continents together (like a puzzle). The second way Wegener proved his theory was through fossils. He found three fossils called Glossopteris (a fern like plant), Mesosaurus, and Lystrosaurus. Glossopteris was found in rocks in Africa, South America, Australia, India, and Antarctica, while Mesosaurus and Lystrosaurus were found on continents separated by oceans. Finally, the third way Wegener proved his theory continental drift was through climate zone. Wegener looked at climates from the past, and had found tropical plants living in Spitsbergen (an island in the arctic). He assumed that a island in the arctic, used to have a warm climate. In conclusion, the three ways Wegener proved his theory continental drift was through land features, fossils, and climate
Since California had previously been mentioned, it is a great place to begin explaining the complex geological impacts starting with the San Andreas Fault. The San Andreas is what geologists know as a strike-slip fault, meaning that when two pl...
Convection currents deep in the mantle of the earth, begin to well up towards the surface. As the pressure increases, it sets the crustal plates in motion. There are different kinds of mountains - Volcanic, Folded, Fault-block, and Dome mountains. Volcanic mountains are formed when magma comes up through cracks in the Earth’s crust and explodes out of lava and ash. The Hawaiian volcanoes, Mt. Hood, Mt. Etna, Vesuvius, and Mt. Saint Helens is an example of volcanic mountains.
They are the earth’s crust; they move very slowly every year. As the tectonic plates slide over each other they cause earthquakes. Earthquakes produce various damaging effects this includes damage to structures of buildings, bridges and other standing formations which then...
The concurrent convective circulations in the mantle leads to some segments of the mantle moving on top of the outer core which is very hot and molten in nature. This kind of movement in different segments occurs as tectonic plates. These tectonic plates are basically seven on the earth surface as major ones, although, several small ones exist also. The plates motions are characterized by varying velocities, this variance results to sub sequential collision of two plates (leading to formation of a mountain in a convergent boundary), drift of two plates (leading to formation of rifts in a divergent boundary), or parallel movement in a transform boundary(Webcache 3).