Geology and Tours

Park Geology

Southern Arizona is a place of rugged linear mountains, called ‘sky islands,’ separated by arid desert plains. Geologically, this area is part of the Basin and Range Province of the Western U.S. The landscape began to form more than 20 million years ago as land masses moved along numerous faults. As the mountains rose, erosion removed an enormous amount of overlying rock, exposing once deeply buried rocks in the highlands while filling the valleys. 

The past 20+ million years of mountain building and erosion is a significant yet brief segment of the extensive history of this area. Major events are preserved in geologic features visible along the Geology Trail at Oracle State Park.

Significant geologic events

A photo showing sedimentary rock known as Pinal Schist in Oracle State Park1.7 billion years ago, this area was part of an island chain located off the coast of a continent during a period of early mountain building. Rock formed from sediments that accumulated at the base of sea canyons. This sedimentary rock was later metamorphosed as Pinal schist, the oldest rock of this area. Fragments of this rock are visible at the park.

1.4 billion years ago, magmatic activity deep beneath the surface enabled the formation of Oracle Granite. It is the basement rock of the area. Oracle Granite’s stacked boulders and balanced rocks dominate the park’s landscape.

Apache group of sedimentary rocks1.0 to 1.4 billion years ago, molten rock intruded into Oracle Granite, forming igneous dikes and sills. Hydrothermal solutions associated with the magma formed minerals like tourmaline. This was also a time of sedimentation from shoreline erosion and sea action. The Apache Group of sedimentary rocks formed during this time, and their fragments are scattered across the park’s bajada. 

252 to 541 million years ago, shallow seas covered this area multiple times.  This created fossil-bearing Paleozoic limestone. These rocks later hosted valuable mineral deposits.

70-80 million years ago, North America was gliding westward, colliding with the crust of the ocean. The downward movement of ocean crust initiated magmatic activity, producing a Laramide Granitic Porphyry rock that intruded into Oracle granite. This time, the hydrothermal solutions were rich in copper and smaller amounts of silver, gold and molybdenum. The porphyry rock related to this mineral deposit is exposed at the surface along trails in the park. Although mining never occurred within the park boundary, Oracle State Park is surrounded by numerous underground and open pit mines that have extracted valuable minerals over the past 100 years.

This history and more can be explored along the park’s Geology Trail. Information about the trail and guided geology hikes can be found below.

Geology Tours

An example of unique merged rock formations at Oracle State ParkIn 2022, Oracle State Park launched a 1.2-mile Geology Trail. Starting at the park’s Group Use Area Trailhead, hikers wind through igneous intrusions, mineral deposits, bedrock pediment, and alluvial fans that showcase the past 1.7 billion years of geologic history. From high points along the trail, there are unobstructed views of the volcanic Galiuro Mountains, the Santa Catalina Mountains, and the San Pedro Valley.  

There are two ways to experience Oracle State Park’s Geology Trail. Join a Geologist/park staff-led tour by calling the visitor center at 520-896-2425 or sign up online here (search Oracle under Places). 

Self-guided Tours

You can also take a self-guided tour using one of the the Geology Trail maps below. Either download the map in advance or pick one up at the Kannally Ranch House.  

Self-guided Geology Tour Map

Geology Tour Map (print version)


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