WebSeafloor Topography Continents fit together along the edges of their continental shelves. Mid-ocean ridges and deep-sea trenches develop at the boundaries of the moving plates. Volcanic islands and seamounts develop where a plate moves over a stationary hotspot. The new earthquake data revealed three startling observations. WebWhen the water depth decreases to one half of a wave’s wavelength, the wave starts to “feel the bottom”. That means that the deepest water molecules set into circular motion by the wave’s energy run into the …
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Web4. Describe how convection current affects plate movement. 5. how the convection current affects the movement of; 6. how the convection current affects the movement of tectonic; 7. how the convection current affects the movement of techtonics plate 8. How the convection current affects the movement of tectonic plates? 9. WebJan 17, 2024 · Seafloor Spreading Most transform boundaries consist of short faults on the seafloor occurring near mid-ocean ridges. As the plates split apart, they do so at differing speeds, creating space—anywhere from a few to several hundred miles—between spreading margins. As the plates in this space continue to diverge, they do so in opposite … tnpsc dashboard login
High School Earth Science/The Seafloor
WebAs seafloor spreading continues the new rocks move away from the spreading zone. Here, in GeoMapApp, we analyze seafloor age data and calculate spreading rates in … WebDivergent (Spreading):This is where two plates move away from each other. Molten rock from the mantle erupts along the opening, forming new crust. The earthquakes that occur … WebMay 6, 2024 · Plates move apart at mid-ocean ridges where new seafloor forms. Between the two plates is a rift valley. Lava flows at the surface cool rapidly to become basalt, but deeper in the crust, magma cools more slowly to form gabbro. So the entire ridge system is made up of igneous rock that is either extrusive or intrusive. penna holstein association