Divergent boundaries in continents (land) create rifts, which grow into rift valleys. Divergent boundaries create volcanic islands and can be found active in the mid-ocean ridge tectonic plate. The rifts of the oceanic ridge system are representative examples of divergent boundaries in the oceanic lithosphere.
Land and oceans is the right answer. Between the spreading centres of two separating tectonic plates, divergent borders, often referred to as constructive barriers, are a feature with a liner-like shape where magma coming from the mantle also builds a new crust.
There are three different kinds of plate tectonic borders. They change plate boundaries and are divergent and convergent. When two tectonic plates diverge, a divergent boundary is created. A constructive boundary is another name for a divergent boundary.
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