Oceanic crust divergent plate boundary features:
Continental crust divergent plate boundary features:
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At divergent plate boundaries, geologic features include mid-ocean ridges, rift valleys, and fissures. Mid-ocean ridges are underwater mountain ranges formed by the upwelling of magma from the mantle, creating new oceanic crust. Rift valleys form on land where the Earth's crust is being pulled apart, leading to the development of new crust and volcanic activity. Fissures are cracks in the Earth's crust where lava can erupt during volcanic activity.
Mid-Ocean Ridges are the geological features that occur at divergent boundaries. Mid-Ocean Ridges are mountains that form on the ocean floor and with a total length over forty thousand miles.
No. Sea floor trenches are found at convergent boundaries. divergen boundaries form mid-ocean ridges.
Around divergent boundaries, land features such as rift valleys, volcanic mountains, and mid-ocean ridges can be found. These features are a result of tectonic plates moving apart, leading to the creation of new crust through volcanic activity and the stretching and thinning of the lithosphere.
Divergent boundaries are found primarily along mid-ocean ridges, where tectonic plates are moving away from each other. Additionally, divergent boundaries can also occur on continents, leading to the formation of rift valleys.
At divergent boundaries, three features that can be found include mid-ocean ridges where new oceanic crust is formed through volcanic activity, rift valleys that form on land as tectonic plates pull apart, and shallow earthquakes caused by the movement of the plates.
Yes, volcanism is found at both convergent and divergent boundaries of tectonic plates. At convergent boundaries, subduction zones can result in the formation of volcanoes due to the melting of subducted crust. At divergent boundaries, magma rises to the surface to create new crust, leading to volcanic activity as seen in mid-ocean ridges.