One hundred and sixty million years ago a deposit of creamy, erosive entrada sandstone was laid down in the shallows of an inland sea in what is now southern Utah. Sixty million years later, along the margins of a younger shore, a harder, more resistent layer of sandstone, called Dakota, came to be deposited over the Entrada. Over time, both layers were covered over with additional strata, which eventually eroded away exposing the Dakota-overlaid Entrada. As this eroded, it produced amazing white columns topped with dark-capped, small-grained, igneous-pebbled conglomerate. Thus were created the amazing Wahweap Hoodoos of the southern edge of the Grand Staircase-Escalante National Monument, where Wahweap Creek empties into the Colorado River now flowing beneath the mudhole of Lake Powell.

A focal length of 292mm from about 30 yards away allowed me to magnify the relatively small hoodoo and compress it with its background, the wall of the Entrada deposit. It also allowed me to control the background and elininate the sky from the composition. An aperture of f/20 provided depth-of-field and a shutter speed of 1/13th second at ISO 100 gave me an overall slightly lighter-than-medium exposure.

Even though the hoodoos of the Wahweap remain within the reduced margins of Grand Staircase-Escalante National Monument, and are thus still afforded some protection, the monument itself has been reduced in size by 47%, from nearly 2 million acres to just over 1 million; and places just as wondrous as the Wahweap have been stripped of protection and laid bare to loosely regulated mining development, expanded grazing, and other forms of exploitation. In the mountains of the Southern Appalachians, the GSENM may seem far away and beyond the need to consider, but our public lands are under attack, and if we wish to continue to have them, we must be willing to fight for their continued existence. Like the Wahweap, they are all special.