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Photo by Renee Snoderly
http://www.black.canyon.national-park.com/images/areamap.jpg   Photo by Renee
                                                               Snoderly
http://www.nps.gov/blca/planyourvisit/upload/blca_map.pdf
All photos on this page by Mike Snoderly
Second Stop- Visitor Center/Gunnison Point
                                                                About 100 yards up the road from
                                                                Tomichi Point you will find the Visitor
                                                                Center. There is ample parking and
                                                                rest facilities or you can simply hike
                                                                the short trail that links the two points.

                                                                The rangers inside are
                                                                knowledgeable about the geography
                                                                of the Black Canyon and are more
                                                                than willing to provide you with a free
                                                                map of the park and discuss in
                                                                greater detail some of the landscape
                                                                features that make up the geography
                                                                of Black Canyon.

                                                                While you are in the Visitor Center be
                                                                sure to check out the free movie on
                                                                the history of the Black Canyon.
                                                                There are some interesting
                                                                geographical tidbits about the
                                                                logistics of diverting the Gunnison
                                                                River through six miles of solid rock
View from the back patio of the Visitor Center                  to reach the arid mesa nearby.



 PLEASE REMEMBER... Collecting rock or plant specimens
 in Black Canyon of the Gunnison National Park is illegal.

    Picture by Mike Snoderly
Click the picture above to play the video
Exit the back door of the Visitor Center to reach the short walkway to Gunnison Point. This vantage offers
sweeping 360 degree views of the canyon. We are able to see the first signs of white colored pegmatite veins
running through the Black Canyon Gneiss. These veins were formed through an extrusion process. The
pegmatite has a much lower melting temperature than the surrounding gneiss. As the rock expanded and
cracked apart during the cooling process, pegmatite was forced into the gaps much like toothpaste through a
tube. As we head north to the next stop, these veins will become more abundant and impressive.




Video by Mike Snoderly
Sub-topic: Geology and Erosion
 On your way back to the Visitor Center, be sure to look on your right side for some excellent geologic
samples. Visible here are tiny, glittering quartz crystals, vivid orange lichen and examples of biological
                and mechanical weathering. The iPhone visible on the left is for scale.
Third Stop – The Painted Wall
         Sub-topic: Geology

                              Continue for about four miles
                              down the road and you will see
                              the signs for the Painted Wall.
                              This is a popular attraction and
                              parking is limited. The darker
                              portions of rock visible on the
                              canyon wall are Black Canyon
                              Gneiss, a combination of
                              gneisses and mica schist formed
                              around 1.7 billion years ago in
                              the middle Proterozoic Era.
                              These metamorphic rocks were
                              deeply folded and subjected to
                              several instances of igneous
                              intrusion beginning about 1.4
                              billion years ago. This resulted
                              in the lighter areas of pegmatite
                              and granite. The area at the top
                              of the cliff is the Great
                              Unconformity, where sediments
                              from the middle Jurassic Era
                              contact the Proterozoic gneiss.
                              This phenomenon represents a
                              gap in the geological record of
                              about 1.2 billion years.
http://coyotegulch.files.wordpress.com/2009/07/gunnisontunnelnps.jpg
Conclusion
The Black Canyon of the Gunnison National Park contains rich
geological treasures found nowhere else on the planet. There are
canyons that are longer, deeper or sheerer but only the Black
Canyon possesses these features in such a magnificent
combination. Through millions of years, the Gunnison River has
scoured the Proterozoic rock tirelessly and at a rate so slow it
overwhelms the mind. The sheer walls of black schist and gneiss
stand in stark contrast to the beautiful pink quartz and granite
crystalline rock. It is easy to get swept up in the amazing views
and thundering sound of the Gunnison River but we must keep in
mind how mankind has affected the environment by changing the
flow of this river. However, only with an understanding of the
geologic principles that shaped the canyon can one truly appreciate
the majesty that is the Black Canyon of the Gunnison National
Park.
References
Author Unknown. "Black Canyon National Park." Black Canyon of the Gunnison
        National Park. Gunnison - Crested Butte Tourism Association, 2008. Web. 27
        Nov 2011. <http://www.gunnisoncrestedbutte.com/area-tour/national-
        parks/black-canyon-gunnison>.
Author Unknown. "Black Canyon of the Gunnison National Park (U.S. National Park
        Service)." U.S. National Park Service - Experience Your America. National Park
        Service, 11 Nov. 2011. Web. 27 Nov. 2011.
        <http://www.nps.gov/blca/index.htm>.
Blakey, Ronald C., and Wayne Ranney. Ancient Landscapes of the Colorado Plateau.
        Grand Canyon, AZ: Grand Canyon Association, 2008. Print.
Jacobson, John. "The Gunnison National Park Visitor Center." Personal interview. 19
        Nov. 2011
Jenkins, John W. The Essential Guide to Black Canyon of the Gunnison National Park.
        Golden, CO: Colorado Mountain Club, 2004. Print.
Spooner, Alecia M. Geography for Dummies. Hoboken, NJ: Wiley, 2011. Print.

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Geography Final Project by Mike Snoderly

  • 1. Photo by Renee Snoderly
  • 4.
  • 5. All photos on this page by Mike Snoderly
  • 6. Second Stop- Visitor Center/Gunnison Point About 100 yards up the road from Tomichi Point you will find the Visitor Center. There is ample parking and rest facilities or you can simply hike the short trail that links the two points. The rangers inside are knowledgeable about the geography of the Black Canyon and are more than willing to provide you with a free map of the park and discuss in greater detail some of the landscape features that make up the geography of Black Canyon. While you are in the Visitor Center be sure to check out the free movie on the history of the Black Canyon. There are some interesting geographical tidbits about the logistics of diverting the Gunnison River through six miles of solid rock View from the back patio of the Visitor Center to reach the arid mesa nearby. PLEASE REMEMBER... Collecting rock or plant specimens in Black Canyon of the Gunnison National Park is illegal. Picture by Mike Snoderly
  • 7. Click the picture above to play the video Exit the back door of the Visitor Center to reach the short walkway to Gunnison Point. This vantage offers sweeping 360 degree views of the canyon. We are able to see the first signs of white colored pegmatite veins running through the Black Canyon Gneiss. These veins were formed through an extrusion process. The pegmatite has a much lower melting temperature than the surrounding gneiss. As the rock expanded and cracked apart during the cooling process, pegmatite was forced into the gaps much like toothpaste through a tube. As we head north to the next stop, these veins will become more abundant and impressive. Video by Mike Snoderly
  • 8. Sub-topic: Geology and Erosion On your way back to the Visitor Center, be sure to look on your right side for some excellent geologic samples. Visible here are tiny, glittering quartz crystals, vivid orange lichen and examples of biological and mechanical weathering. The iPhone visible on the left is for scale.
  • 9. Third Stop – The Painted Wall Sub-topic: Geology Continue for about four miles down the road and you will see the signs for the Painted Wall. This is a popular attraction and parking is limited. The darker portions of rock visible on the canyon wall are Black Canyon Gneiss, a combination of gneisses and mica schist formed around 1.7 billion years ago in the middle Proterozoic Era. These metamorphic rocks were deeply folded and subjected to several instances of igneous intrusion beginning about 1.4 billion years ago. This resulted in the lighter areas of pegmatite and granite. The area at the top of the cliff is the Great Unconformity, where sediments from the middle Jurassic Era contact the Proterozoic gneiss. This phenomenon represents a gap in the geological record of about 1.2 billion years.
  • 10.
  • 12. Conclusion The Black Canyon of the Gunnison National Park contains rich geological treasures found nowhere else on the planet. There are canyons that are longer, deeper or sheerer but only the Black Canyon possesses these features in such a magnificent combination. Through millions of years, the Gunnison River has scoured the Proterozoic rock tirelessly and at a rate so slow it overwhelms the mind. The sheer walls of black schist and gneiss stand in stark contrast to the beautiful pink quartz and granite crystalline rock. It is easy to get swept up in the amazing views and thundering sound of the Gunnison River but we must keep in mind how mankind has affected the environment by changing the flow of this river. However, only with an understanding of the geologic principles that shaped the canyon can one truly appreciate the majesty that is the Black Canyon of the Gunnison National Park.
  • 13. References Author Unknown. "Black Canyon National Park." Black Canyon of the Gunnison National Park. Gunnison - Crested Butte Tourism Association, 2008. Web. 27 Nov 2011. <http://www.gunnisoncrestedbutte.com/area-tour/national- parks/black-canyon-gunnison>. Author Unknown. "Black Canyon of the Gunnison National Park (U.S. National Park Service)." U.S. National Park Service - Experience Your America. National Park Service, 11 Nov. 2011. Web. 27 Nov. 2011. <http://www.nps.gov/blca/index.htm>. Blakey, Ronald C., and Wayne Ranney. Ancient Landscapes of the Colorado Plateau. Grand Canyon, AZ: Grand Canyon Association, 2008. Print. Jacobson, John. "The Gunnison National Park Visitor Center." Personal interview. 19 Nov. 2011 Jenkins, John W. The Essential Guide to Black Canyon of the Gunnison National Park. Golden, CO: Colorado Mountain Club, 2004. Print. Spooner, Alecia M. Geography for Dummies. Hoboken, NJ: Wiley, 2011. Print.