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  • Melissa Harrington

    Antelope Canyon is one of the most breathtaking places on earth. It is also known as a “slot canyon” or “Corkscrew Canyon” and has been described as the most photogenic in the world. (Road Trip 2009)

  • Sara Scates

    In Arizona, near the border with Utah, in the United States, you can find a stunning sandstone rock formation called The Wave. The Wave is on the slopes of the Coyote Buttes, which are in turn located in the Paria Canyon-Vermilion Cliffs Wilderness, on the Colorado Plateau. This formation is actually sand dunes calcified in vertical and horizontal layers, and the fascinating color bands are iron oxides, hematite, and goethite. The Jurassic-age Navajo sandstone making up The Wave is estimated to be 190 million years old.

  • Nikki Strait

    Lake Powell area, Arizona, Antelope Canyon near Lake Powell in Arizona, on my bucket list of places to see in person.

  • Angela Hart

    Located near yet little known attractions of the Lake Powell area, Arizona, Antelope Canyon is one of the most beautiful places on earth. It is also known as a “slot canyon” or “Corkscrew Canyon” and has been described as the most photogenic in the world.

  • Susan Kennedy

    Lower Antelope Canyon near Page, Arizona, and Knaab, Utah. On the slopes of the Coyote Buttes, which are in turn located in the Paria Canyon-Vermilion Cliffs Wilderness, on the Colorado Plateau. This formation is actually sand dunes calcified in vertical and horizontal layers, and the fascinating color bands are iron oxides, hematite, and goethite. The Jurassic-age Navajo sandstone making up The Wave is estimated ...

Tags:
Lakes Powell, Buckets Lists, Color, Beautiful Places, Places I D, Roads Trips, The Waves, United States, Antelop Canyon

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Antelope Canyon Antelope Canyon is the most photographed slot canyon in the world, and for good reason. There are two sections, separated by a couple of miles. Upper Antelope Canyon is known as Tsé bighánílíní – “the place where water runs through rocks” – in the Navajo language; and the Lower Canyon Hazdistazí, or "spiral rock arches". The canyon was formed by erosion of Navajo sandstone, mainly due to flash flooding and the slow wear of water and grains of sand rushing through its steadily

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