Winter weather makes for more than a pretty picture. Iron oxide minerals have tinged the rock red, orange, and yellow. Most of the rock pictured here is 50-million-year-old limestone from the Claron Formation. As the name implies, the view from Sunset Point is most spectacular near sunset, when the colorful rock formations are illuminated by low-angle light. On February 9, 2017, photographer and writer Ray Boren captured a ground-based photo showing snow extending into Bryce Canyon.īoren shot his photo while looking toward the southeast from Sunset Point, one of the park’s many overlooks accessible from a network of trails. When this satellite image was acquired, snow covered the plateau. Over time, weathering has shaped the series of hoodoo-filled amphitheaters that descend from the east side of the Paunsaugunt Plateau.Ĭompared to Zion Canyon just 80 kilometers (50 miles) away, Bryce Canyon is about 300 meters (1,000 feet) higher in elevation, and the climate is cooler and moister. Unlike canyons sculpted primarily by a river, Bryce Canyon is the result of weather-induced erosion. It shows the north-central part of the park in the vicinity of the main amphitheater. On March 9, 2017, the Operational Land Imager (OLI) on Landsat 8 captured this natural-color image of Bryce Canyon National Park. They are there to capture images of the delicate spires called “hoodoos” that rise from the canyon. But photographers who visit Bryce Canyon National Park are not typically looking for dizzying heights and depth. Arizona’s Grand Canyon, for comparison, measures more than 1,800 meters deep in places. Utah’s Bryce Canyon is not the deepest in the United States its largest “amphitheater” of naturally eroded rock drops 240 meters.
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