4000 x 3000 px | 33,9 x 25,4 cm | 13,3 x 10 inches | 300dpi
Aufnahmedatum:
4. Juli 2011
Ort:
Page Arizona USA
Weitere Informationen:
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways are eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock. Flooding in the canyon still occurs. It has been accessible by permit only since 1997, when the Navajo Tribe made it a Navajo Tribal Park. Upper Antelope Canyon, called Tse bighanilini, "the place where water runs through rocks" by the Navajo
