Garden of the Gods

Garden of the Gods

Glen Eyrie Castle & Conference Center & Garden of the Gods
3820 N 30th St, Colorado Springs, CO 80904-5001

Overview

The garden’s red rock formations were created millions of years ago during a geological upheaval event called the Laramide Orogeny. Archaeological evidence shows that prehistoric people visited Garden of the Gods about 1330 BC. At about 250 BC, Native American people camped in the park; they are believed to have been attracted to wildlife and plant life in the area and used overhangs created by the rocks for shelter. Many native peoples have reported a connection to Garden of the Gods: Apache, Cheyenne, Comanche, Kiowa, Lakota, Pawnee, Shoshone and Ute people.
Multiple American Indian Nations traveled through Garden of the Gods. The Utes’ oral traditions tell of their creation at the Garden of the Gods, and petroglyphs have been found in the park that are typical of early Utes. The Utes found red rocks to have a spiritual connection and camped near Manitou Springs and the creek near Rock Ledge Ranch bordering Garden of the Gods. The Old Ute Trail went past Garden of the Gods to Ute Pass and led later explorers through Manitou Springs. Starting in the 16th century, Spanish explorers and later European American explorers and trappers traveled through the area, including Lt. John C. Frémont and Lt. George Frederick Ruxton, who recorded their visits in their journals.
The outstanding geologic features of the park, including Steamboat Rock, the Three Graces, and Balanced Rock, are the ancient sedimentary beds of deep-red, pink and white sandstones, conglomerates and limestone that were deposited horizontally, but have now been tilted vertically and faulted into “fins” by the immense mountain building forces caused by the uplift of the Rocky Mountains and the Pikes Peak massif. The following Pleistocene Ice Age resulted in erosion and glaciation of the rock, creating the present rock formations. Evidence of past ages can be read in the rocks: ancient seas, eroded remains of ancestral mountain ranges, alluvial fans, sandy beaches and great sand dune fields.

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