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  • Rift Valleys: Formation at Divergent Continental Plate Boundaries
    When two continental plates diverge, a rift valley forms.

    Here's a breakdown:

    * Divergent Boundaries: These are areas where tectonic plates move apart.

    * Continental Plates: These are the thick, less dense plates that make up the continents.

    * Rift Valley Formation: When continental plates pull apart, the crust stretches and thins. This thinning causes the land to sink, forming a valley.

    Additional Features Associated with Rift Valleys:

    * Volcanic Activity: As the plates separate, magma rises from the mantle, often leading to volcanic eruptions within the rift valley.

    * Earthquakes: Frequent earthquakes occur as the plates move apart and the crust readjusts.

    * Fault Lines: The boundary between the diverging plates is marked by prominent fault lines.

    * Graben: A series of parallel fault lines can create a graben, a downthrown block of crust that forms the central part of a rift valley.

    Examples of Rift Valleys:

    * East African Rift Valley: A major rift valley system stretching for thousands of kilometers across eastern Africa.

    * Rio Grande Rift: A rift valley extending from Colorado to Texas in the United States.

    * Baikal Rift Valley: Located in Siberia, Russia, it is the deepest freshwater lake in the world.

    Remember that the formation of a rift valley is a long and slow process, taking millions of years.

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