At divergent boundaries, crustal features primarily include mid-ocean ridges, where tectonic plates are moving apart, allowing magma to rise and create new oceanic crust. This process often leads to the formation of rift valleys on land, characterized by steep-sided, elongated depressions. Additionally, volcanic activity is common in these regions, resulting in underwater volcanoes and hydrothermal vent systems. Overall, divergent boundaries are marked by unique geological formations and dynamic geological processes.
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