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<p>from a more roughly planar surface above it, such as at <a href="page.php?w=Canyonlands_National_Park">Canyonlands National Park</a> in <a href="page.php?w=Utah">Utah</a>. When sheets of water on a roughly planar surface first enter a depression in it, this erodes the top edge of the depression. The stream is forced to grow longer at the very top of the stream, which moves its origin back, or causes the canyon formed by the stream to grow wider as the process repeats. Widening of the canyon by erosion inside the canyon, below the canyon side</p><p>
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