FIELD TRIP STOP -- BLACK CANYON OF THE GUNNISON, COLORADO (PreCambrian Metamorphic and Igneous Granite including Pegmatites)

LOCATION:  In west-central Colorado, about 8 miles east of Montrose near the intersection of Routes 50 and 347.

GEOLOGIC FEATURES: PreCambrian Metamorphic Gneiss, Schist and Granite; Pegmatites; Unconformities (Non-Conformity); Foliation


DESCRIPTION: The Black Canyon of the Gunnison is composed of 1.8 byo Gneisses and Schists that have been intruded by 1.4 byo granites and granite pegmatites. Mainly outside the park boundaries, the metamorphic and igneous rock are unconformably overlain by Upper Jurassic to Upper Cretaceous strata (160 to 85 myo) which are then overlain in angular unconformity by 30 myo (Oligocene) volcanics.


The greatest depth of the Canyon is 2722 ft at Warner Point while the narrowest width at the rim is 1100 ft.  The Park is named for its steep cliffs which are darkened by a lack of sunlight, as low as 33 minutes per day.


Following deposition of Mesozoic strata, uplift commenced with the Laramide Orogeny (about 70-40 mya). This uplift was also associated with mid-Tertiary volcanic activity. Subsequent erosion, perhaps enhanced by a sporadic uplift of the Colorado Plateau within the past few million years by rivers, eventually exposed the crystalline rocks of the Canyon about two million years ago.


Personal photographs below were taken in April 2021 from the South Rim Visitor Center and nearby Gunnison Point. Both South Rim and East Portal Roads were closed for various reasons during my visit.  A photo of the famous Painted Wall was taken from the Parks brochure.



(01) Describe a Non-Conformity. Where does it occur in the Park and how did it form chronologically?

(02) What are the distinguishing characteristics of a Pegmatite?

(03) What Geologic Process is responsible with the carving of the Canyon?

(04) What is a probable cause of the Laramide Orogeny? What Mountain System was the result of the this orogeny?

(05) CHALLENGE: Describe the geologic history of the area within and near the Black Canyon of the Gunnison.  Beginning in the PreCambrian, include all episodes of Deposition, Metamorphism, Igneous Activity, mountain building, and erosion in the area.


-National Park Service, Black Canyon of the Gunnison National Park Geology. U.S. Department of the Interior (updated Oct. 22, 2019). Accessed April 25, 2021 from


-USGS. Black Canyon of the Gunnison National Park. U.S. Department of the Interior (updated Oct. 22, 2019). Accessed April 25, 2021 from

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Cross-sectional Figure illustrates the geology in and around  Black Canyon of the Gunnison N.P. (from Hanson, Wallace R. 1965. The Black Canyon of the Gunnison, USGS Bulletin 1191.)


Map Figure of the National Park shows roads and notable features (from Park Brochure)


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Figure 1 - Granitic Pegmatites (1.4 byo) intruded parallel to foliation in 1.8 myo Gneiss and Schist photographed from Gunnison Point.

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Figure 2 - View of the Canyon immediately south of the South Visitor Center (Tomichi Point).

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Figure 3 - View from Gunnison Point near South Visitor Center showing the Gunnison River and multiple craggy spires due to weathering.

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Figure 4 - View of Painted Wall illustrating the numerous Granitic Pegmatites (1.4 byo) intruded into the older Metamorphic Rock.  Photo is from the Park Brochure since access to Painted Wall was not available at the time of my visit..

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Figure 5 - Close-up of a Granitic Pegmatites as exposed on the stairway down to Gunnison Point.

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Figure 6 - Stairway near South Visitor Center leading down to Gunnison Point. Note the incredibly steep walls of crystalline rock.