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  • Understanding Rift Valleys, Volcanoes & Fault Scarps at Divergent Plate Boundaries
    When continental plates pull apart at divergent boundaries on land, the following forms:

    * Rift Valleys: These are large valleys that form as the land is pulled apart. They are often characterized by steep sides and a flat floor.

    * Volcanic Activity: As the plates separate, magma from the Earth's mantle rises to the surface, creating volcanoes.

    * Fault Scarps: These are steep cliffs that form along the edges of the rift valleys, where the land has been broken apart.

    * Grabens: These are blocks of land that have been pulled down between two faults.

    * Horsts: These are blocks of land that have been pushed up between two faults.

    * New Ocean Basins: Over time, if the plates continue to pull apart, the rift valley may eventually widen and fill with water, forming a new ocean basin.

    The East African Rift Valley is a prime example of a divergent boundary on land. This vast valley system stretches for thousands of kilometers, and it is home to some of the world's most active volcanoes.

    Here's a simplified breakdown:

    1. Continental Plates Pull Apart: The force of the plates moving apart causes the land to crack and break.

    2. Rift Valley Forms: The broken land sinks, creating a rift valley.

    3. Magma Rises: As the plates pull further apart, magma rises from the Earth's mantle to fill the gap.

    4. Volcanoes Form: The magma erupts at the surface, forming volcanoes.

    5. New Ocean Basin Forms: Over millions of years, the rift valley can widen and fill with water, eventually becoming a new ocean basin.

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