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Tectonic plate boundary types, diagram

Tectonic plate boundary types, diagram


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Tectonic plate boundary types, diagram

Tectonic plate boundary types. Diagram showing three types of movement (arrows) at tectonic plate boundaries. Tectonic plates moving parallel to each other (bottom) lead to strike-slip earthquakes with relatively little deformation. At a divergent boundary (middle), such as a mid-ocean ridge or rift valley, the plates move apart and molten rock (orange) rises to form new land. At a convergent boundary (top), such as a subduction zone, one plate moves under the other as they collide (thrust or reverse faulting). This also leads to the formation of mountain ranges and volcanoes along the boundary as the subducting plate melts

Science Photo Library features Science and Medical images including photos and illustrations

Media ID 9241947

© HENNING DALHOFF/SCIENCE PHOTO LIBRARY

Block Diagram Boundaries Convergent Destruction Diagram Divergent Earth Science Earthquake Fault Formation Geological Land Mid Ocean Ridge Mountain Range Movement Parallel Ridge Rift Rift Valley Rock Seismology Subduction Zone Tectonic Plate Tectonic Plates Trio Type Volcanic Volcano Volcanoes Volcanology Vulcanology Cutouts Earthquakes Mountain Ranges Orogeny


EDITORS COMMENTS
This print from Science Photo Library showcases the various types of movement that occur at tectonic plate boundaries. The diagram beautifully illustrates three distinct boundary types, each with its own unique geological processes and consequences. At the bottom, we see parallel movement between tectonic plates, resulting in strike-slip earthquakes with minimal deformation. This type of boundary leads to fascinating seismic activity but relatively little change in landforms. In the middle, a divergent boundary is depicted where plates move apart, creating a mid-ocean ridge or rift valley. Molten rock rises to form new land as an awe-inspiring display of nature's creative power. Finally, at the top of the image lies a convergent boundary like a subduction zone. Here, one plate moves beneath another during their collision through thrust or reverse faulting. This intense interaction not only forms mountain ranges but also triggers volcanic activity along the boundary as melting occurs. The artwork expertly captures these dynamic processes while emphasizing destruction and formation within Earth's geology. With its white background and cut-out style presentation, this illustration stands out as an informative visual aid for anyone interested in earth science and seismology.

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