Saguaro N.P., AZ 2010


During December of 2010, I found myself driving through Tucson, Arizona. I took the opportunity to visit the Saguaro-East National Park and the nearby Colossal Cave.

Arizona Parks Map

The Saguaro National Park is part of the Sonora Desert that covers much of southwest America and northwest Mexico.

Picture taken from Catalina State Park, towards Mount Lemmon in the Rincon Mountains; near Tucson, Arizona

Tucson, Arizona actually splits the Saguaro National Park into two separate districts. The geological history of the park is actually a large part of the geological history of the Tucson Basin. The northeastern boundary of the Tucson Basin is formed by the Santa Catalina and Rincon Mountains. Pictured above, the Rincon Mountains have a maximum elevation of just over 3000 m.

Looking south from the Saguaro N.P. near sun-down. The Rincon Mountains towards the east.

The Rincon Mountains are encompassed by the Coronado national Forest and the Rincon Mountain District. They are composed of foliated and folded banded gneiss, as well as schist and the granite which can be dated back to the Precambrian age, with younger colluvial and alluvial deposits draped over the base, often forming a thin cover.

Near Saguaro N.P.

Saguaro National Park is home of the iconic Saguaro cactus, which has an incredibly slow growth rate. It can grow to a height of 15 meters and weigh over 10 tons. The Saguaro Cactus can live up to 200 years, and dominates the scenery of the National Park that bares its name.

I’m posing in the Saguaro National Park, in December of 2010.

Without doubt, the long arms of the Saguaro cactus are the plant’s most distinctive feature.

A quick shot of the sun going down at the Saguaro N.P.

Nearby and 20 km south of Saguaro-East N.P., I explored the Colossal Cave. Colossal Cave is a large cave-system that contains about 5.6 km of mapped passageways. Temperatures inside average 70 °F (21 °C) year-round.

Colossal Cave near Tucson, AZ

The Colossal Cave is an ancient karst cave, classified as “dry”. The meaning of this is that its formations are completely dry, or “dead”, and do not grow. This is because the cave was formed by water depositing limestone, but this source has disappeared.

Colossal Cave

About 300 million years ago much of the American Southwest was covered by a vast sea populated by giant sharks, tetrapods and other primitive amphibians. Eventually the waters receded. Organic material left behind dried out and was compressed to form the limestone. Then 80 million years ago the heaving earth thrust limestone and granite together to create new landforms such as the Rincon Mountains where Colossal Cave is located. After eons of water erosion, the Cave reached a dry state, and today Colossal Cave is one of the largest dry caves in north America.

Drapery Room in the Colossal Cave System near Tucson, Arizona

The earliest inhabitants of the region were the Hohokam, a prehistoric culture who called Arizona home for more than 1,200 years. Subsistence farming was made possible through their highly advanced network of irrigation canals that at its apex stretched more than 150 miles. Archeologists have discovered evidence that the Hohokam used Colossal Cave as temporary shelter as early as 900AD.

Cave formations found in Colossal Cave.
Cave formations in Colossal Cave.
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