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  • Understanding Active Mountain Ranges: Formation & Growth
    There are no mountains that are currently "growing" in the sense of actively increasing in height at a rate noticeable in a human lifetime. Mountain building, or orogenesis, is a slow and gradual process that happens over millions of years.

    However, there are mountains that are still actively rising due to ongoing tectonic plate movement and collisions. These include:

    * The Himalayas: The Himalayas are the youngest and highest mountain range on Earth, formed by the ongoing collision of the Indian and Eurasian tectonic plates. The mountains are still rising at a rate of about 5mm per year.

    * The Andes Mountains: These mountains are formed by the subduction of the Nazca Plate under the South American Plate. The Andes are still rising in some sections.

    * The Alps: The Alps are formed by the collision of the African and Eurasian plates. While the mountains are no longer rising as rapidly as they once did, some sections are still experiencing uplift.

    * The Rocky Mountains: The Rocky Mountains are formed by the subduction of the Farallon Plate under the North American Plate. The mountains are still rising, though at a slower rate than the Himalayas.

    While these mountain ranges are not "growing" in the literal sense, the ongoing tectonic activity means they are still being uplifted and shaped. This process will continue for millions of years, creating new peaks and changing the landscape as we know it.

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