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  2. Category : Tourist attractions in Colorado Springs, Colorado

    en.wikipedia.org/wiki/Category:Tourist...

    University of Colorado Colorado Springs (3 C, 3 P) Pages in category "Tourist attractions in Colorado Springs, Colorado" The following 19 pages are in this category, out of 19 total.

  3. Manitou Cliff Dwellings - Wikipedia

    en.wikipedia.org/wiki/Manitou_Cliff_Dwellings

    The Manitou Cliff Dwellings were built at their present location in the early 1900s, as a museum and tourist attraction. Some of the building materials were looted and stolen from a collapsed Ancestral Puebloan site near Cortez in southwest Colorado, shipped by railroad to Manitou Springs, and assembled in their present form as Ancestral ...

  4. Garden of the Gods - Wikipedia

    en.wikipedia.org/wiki/Garden_of_the_Gods

    Garden of the Gods (Arapaho: Ho3o’uu Niitko’usi’i) is a 1,341.3 acre public park located in Colorado Springs, Colorado, United States. [ 1 ] 862 acres (3.49 km 2 ) of the park was designated a National Natural Landmark in 1971.

  5. Category:Tourism in Colorado Springs, Colorado - Wikipedia

    en.wikipedia.org/wiki/Category:Tourism_in...

    Tourist attractions in Colorado Springs, Colorado (4 C, 19 P) Pages in category "Tourism in Colorado Springs, Colorado" The following 4 pages are in this category, out of 4 total.

  6. Seven Falls - Wikipedia

    en.wikipedia.org/wiki/Seven_Falls

    The Broadmoor Seven Falls is a series of seven cascading waterfalls of South Cheyenne Creek in South Cheyenne Cañon, Colorado Springs, Colorado. It has been a privately-owned tourist attraction since it was opened in the early 1880s. There is no parking at Seven Falls. Round trip shuttle service is provided from the Norris Penrose Event Center.

  7. Cave of the Winds (Colorado) - Wikipedia

    en.wikipedia.org/wiki/Cave_of_the_Winds_(Colorado)

    Flowstone & draperies Helictites (Cave of the Winds, Manitou Springs, Colorado, USA) As the water table dropped within the cave system air began to fill the passageways and caverns. Stalactites formed on the cave's ceilings as calcium carbonate-rich water dripped leaving thin calcite rings that grew into icicle-like shapes over thousands of years.

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