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Situated in northern Arizona at an elevation of 4500 feet, the famous Red Rocks of Sedona are one of the most beautiful
natural sites in the United States. Part of the eroding Mogollon Rim of the vast Colorado plateau, Sedona’s canyon walls
show nine layers of stone from different geological periods spanning hundreds of millions of years. There are six layers of
sandstone, two thin layers of limestone and atop all of these, one igneous layer of basalt stone. The different sandstone
and limestone layers were formed by wind blown sand dunes or mud deposited by inland seas. The red colors of some of the sandstone
layers are the result of iron oxide staining the rocks over great periods of time. The uppermost igneous layer was deposited
by volcanic eruptions 14.5 million years ago and once covered the entire Verde Valley several meters deep in lava. The Verde
Valley, meaning Green Valley, is so named because of the natural copper, appearing green when extracted from the ground, which
had long been mined in the nearby hills and not because of the colors of local vegetation. The waters of Oak Creek come from
the many natural springs along the course of the creek and not, as is commonly assumed, from melting snow of the nearby sacred
mountain of Kachina Peak.
Evidence of human presence in the Sedona region begins around 4000 BC when hunter-gatherers roamed through the Verde Valley.
As early as 300 BC the dry desert soils were being farmed by the Hohokam people, who developed systems of irrigation canals
by 700 AD but then mysteriously abandoned the area, perhaps because of a regional volcanic eruption in 1066 AD. Next to arrive
were the agrarian Sinagua Indians, whose Spanish name means ‘without water,’ this being an indication of their
ability to farm in the dry environment. Settling in the area from about 1000 to 1400 AD, they built pueblos and cliff dwellings,
perhaps influenced by the architecturally more sophisticated Anasazi Indians, and made baskets, pottery and jewelry. They
also established trading relationships with tribes from the Pacific coastal regions and northern Mexico, and exported the
high grade copper which they mined west of Sedona. Traces of the Sinagua may be found in the remains of their ruined pueblos
scattered around the Sedona area. Sites such as Palatki, Honanki, and Wupatki had dozens of rooms in double story buildings
and were decorated with intriguing pictographs and petroglyphs depicting clan affiliations, mythological beings and astronomical
observations. Archaeologists theorize that the Sinagua may have conducted religious celebrations during particular periods
determined by their celestial observations. Early in the 15th century, the Sinagua disappeared from the area for reasons which
remain a mystery and about this time the Yavapai and Apache Indians began to settle along the sides of Oak Creek canyon.
Europeans first arrived in the region in 1583, when a group of Spanish explorers came in search of gold and silver. Following
the end of the Civil War and the creation of the Territory of Arizona in 1863, homesteaders began to settle in the Verde Valley
and along Oak Creek from the 1870’s. Growth was slow at first because of the remoteness of the region and in 1902 the
small town was named Sedona after the name of the local postmaster’s wife. The first spurt of development came during
the 1940’s and 50’s when Hollywood began filming western movies amidst the red rocks, such as the classics Billy
the Kid, Apache and Broken Arrow. In the 1960s and '70s the beauty of the red rocks began attracting retirees, artists and
an increasing number of tourists. Currently more than four million visitors pass through Sedona each year. While there is
no evidence that the area of Sedona was a highly venerated sacred site in antiquity, it has since the late 1980’s become
the most visited ‘new-age’ pilgrimage destination in the United States. Various local tour guides speak about
‘vortexes’ or specific sites of concentrated energy at different places in the Sedona landscape but geologists
and highly experienced dowsers strongly refute these notions. The general area of the red rocks does seem to have an inspirational
effect upon some people, including the present author, but this effect cannot be attributed to particular places in the landscape.
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