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4: Plate Tectonics

  • Page ID
    20338
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    World map with plate boundaries illustrated. Lithospheric plates and the mid-Atlantic Ridge are labeled.
    Figure \(\PageIndex{1}\): World map showing the boundaries of the tectonic plates. The North American Continent takes up only part of the North American plate (brown). The Mid-Atlantic Ridge, a spreading center (in other words, a place where plates are moving away from one another) is also labeled. The arrows indicate the directions of plate movement. Convergent boundaries are indicated by arrows pointing toward each other, divergent boundaries are indicated by arrows pointing away from each other, and transform boundaries are indicated by arrows pointed in opposite directions parallel to the plate margin. "This work" by Earth@Home, Paleontological Research Institution is in the Public Domain / A derivative from the original work
    Learning Objectives
    • Describe the geological processes that take place at divergent, convergent, and transform plate boundaries.
    • Describe the physical mechanisms that drive plate movement. 
    • Locate and describe California’s major plate boundaries.

    Introduction

    Plate tectonics is a theory that best explains all available observations concerning the Earth's geological features and their changes over time. As a theory it is constantly being evaluated and refined. More specifically, it is a model that explains the origins of continents and oceans, folded rocks and mountain ranges, igneous and metamorphic rocks, earthquakes and volcanoes, and the movements of the continents. Plate tectonics was first proposed in 1915, but did not become an accepted part of geology until 1965. It took 50 years for this theory to be accepted for a few reasons.

    First, plate tectonics was a paradigm shift in thinking about Earth and it was difficult for many established geologists to accept. While observations made by Alfred Wegener concerning the movement of continents were complete and his hypothesis of ‘drifting continents’ was very astute, he could not explain a driving mechanism that would account for the perceived motion of the continents through time. Many geoscientists would not accept his ideas without an explanation of a plausible driving mechanism. 

    Second, many of Wegener’s observations were from studies of rocks, fossils and landforms in the southern hemisphere and most geologists of the time were in the northern hemisphere (Europe and North America). These Northern Hemisphere geologists were unfamiliar with the rocks and structures in the southern hemisphere. It was difficult for them to independently verify Wegener’s observations and therefore easier to discount them.

    Third, the technology necessary to collect the data to develop the concept of plate tectonics simply did not exist until the middle of the 20th century. Though not covered in depth in this resource, we recommend exploring the development of Plate Tectonics theory in Physical Geology – H5P Edition (Panchuk, 2021).


    4: Plate Tectonics is shared under a CC BY-NC 4.0 license and was authored, remixed, and/or curated by LibreTexts.

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