Maintenance window scheduled to begin at February 14th 2200 est. until 0400 est. February 15th

(e.g. yourname@email.com)

Forgot Password?

    Defense Visual Information Distribution Service Logo

    Geology of Boulder, Colorado: Image of the Day

    Issued by: on

    VIRIN:
    Date Created:
    City:
    State:
    Country:
    Geology of Boulder, Colorado: Image of the Day

    WASHINGTON, DISTRICT OF COLUMBIA, UNITED STATES

    07.11.2011

    Courtesy Photo

    NASA

    On a hillside west of Boulder, Colorado, the National Center for Atmospheric Research www.ncar.ucar.edu/ (NCAR) straddles the boundary between two different types of landscape. To the east is the relatively flat terrain of the Boulder Valley. The mountains to the west are the stony archives of hundreds of millions of years of changing landscapes.

    The Advanced Spaceborne Thermal Emission and Reflection Radiometer asterweb.jpl.nasa.gov (ASTER) on NASA's terra.nasa.gov Terra satellite captured this simulated true-color image of NCAR and its surroundings on December 12, 2003, after a snowstorm blanketed much of the area. Snow covers the ground near the research center, as well as lawns in the nearby city, and parts of the mountain slopes where evergreen trees poke skyward through the snow.

    Among the most prominent features west of Boulder are the www.flickr.com/photos/jtowns/104578322/ Flatirons -- giant slabs of red sandstone leaning toward the west. Although ''flatiron'' can be applied to some rock formations well north and south of Boulder, the rocks most visible from the city are northwest of NCAR. Snow seldom lingers long on these giant rocks; the Sun quickly melts it away in all but the coldest temperatures. So while much of the rest of the area is snowy in this picture, the Flatirons are largely bare. East of the Flatirons is the Dakota Hogback, nicknamed for its resemblance to a razorback hog.

    The Flatirons and the Dakota Hogback are just two examples of remains of ancient landscapes. By examining evidence in Boulder and elsewhere, geologists have been able to piece together a complex puzzle of changing land surfaces, elevations, and climates in the area over millions of years.

    Colorado was not always above sea level, and some 600 million years ago, sea water flooded the area. Seas alternately invaded and retreated over the next few hundred million years, but if any rocks from that era were deposited, they later eroded away. About 300 million years ago, mountain ranges known as the www.dmnh.org/main/minisites/ancientDenvers/fountain.html Ancestral Rockies rose in central and western Colorado. As wind and water gradually eroded these mountains, the resulting sandstone sediments flowed off to the east and west. Near Boulder, these sediments lay buried underground, eventually turning into the maroon sandstones known today as the Fountain Formation. Besides the Boulder Flatirons, the Fountain Formation appears in www.redrocksonline.com/index.asp Red Rocks Amphitheatre, parks.state.co.us/Parks/roxborough Roxborough Park, and www.gardenofgods.com/home/index.cfm?flash=1 Garden of the Gods.

    After the sediments that would become the Fountain Formation were deposited, seas returned to Colorado, starting a 150-million-year cycle of floodplain and desert landscapes. Throughout the cycle, rock sediments of alternating hardness and durability were laid down. During the Jurassic, the area was a warm, wet swamp where www.dmnh.org/main/minisites/ancientDenvers/longneck.html sauropods munched the local vegetation. During the Cretaceous, shallow seas once again invaded, and the area became a coastline where dinosaurs roamed along the www.dmnh.org/main/minisites/ancientDenvers/dakota.html shore. Over time, sandy beaches can turn into erosion-resistant rock, like the sandstone of the Dakota Hogback. Just east of the hogback are the remains of an ancient www.dmnh.org/main/minisites/ancientDenvers/pierre.html sea floor, known as the Pierre Shale. NCAR itself sits atop this rock formation.

    All this evidence of ancient landscapes might still be underground were it not for a mountain-building episode beginning about 70 million years ago. At that time, the current Rocky Mountains began to rise. As the mountains rose, old sandstones comprising the Fountain Formation and Dakota Sandstone pushed out of the ground, making them hallmarks of today's Colorado Front Range.

    You can download a eoimages.gsfc.nasa.gov/images/imagerecords/8000/8307/boulder_ast_2003346.kmz 15-meter-resolution KMZ file of the Flatirons suitable for use with earth.google.com/ Google Earth.

    • earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=17126 Red Rocks and Dinosaur Ridge from the Earth Observatory.
    • bcn.boulder.co.us/basin/watershed/geology/ Geology of the Boulder Area from the Boulder Area Sustainability Information Network.
    • www.coloscisoc.org/fieldtrips/ft1.html The Geology Along the Trails West of NCAR by Emmett Evanoff and Sue E. Hirshfeld, Colorado Scientific Society.
    • www.dmnh.org/main/minisites/ancientDenvers/index.html Ancient Denvers from the Denver Museum of Nature and Science.
    • en.wikipedia.org/wiki/Flatirons Flatirons from Wikipedia.
    • www.periclespress.com/geology_Flatirons.html A Geological Tour of Denver, Golden, and Colorado's Front Range by Jack Barkstrom

    NASA image created by Jesse Allen, using data provided courtesy of NASA/GSFC/METI/ERSDAC/JAROS, and U.S./Japan asterweb.jpl.nasa.gov/ ASTER Science Team.



    NASA Identifier: boulder_ast_2003346

    IMAGE INFO

    Date Taken: 07.11.2011
    Date Posted: 10.19.2012 18:32
    Photo ID: 761019
    Resolution: 2000x2000
    Size: 4.13 MB
    Location: WASHINGTON, DISTRICT OF COLUMBIA, US

    Web Views: 45
    Downloads: 6

    PUBLIC DOMAIN