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THE GREAT SAND DUNES
      By Amalia McCoy
           GEO 111
          Spring 2012
   The Great Sand dunes of Colorado are the tallest in
    North America.
   Rising about 750 feet
   Covering roughly 30 square miles
EARTH’S NATURAL PROCESS
   Formed by sand and soil deposits of the Rio Grande
    and other streams and smaller rivers which flow into
    the Rio Grande

   Western winds picked up the sand and soil deposits
    from the River’s flood plain

   The wind loses power right before crossing the
    Sangre de Cristo Range

   The sand was deposited on the eastern edge of the
    valley

   The wind changes the formation and shapes of the
    dunes daily
AEOLIAN DEPOSITION

Definition: Sand and dust moved by the wind
 are eventually deposited when the wind dies
 down.




          Image taken from: http://web.ncf.ca/jim/sand/overview/grainflowAnimation.gif
SLIP FACE
    The steeper leeward face of a sand dune
•Wind erodes the windward
side of the dune which force
the grains of sand up and over
the crest to be deposited on
the other side

•Maintains an angle of 32
degrees- 34 degrees.



                            Image taken from: http://www.geocaching.com/seek/cache_details.aspx?guid=c93e835c-617b-
                            4c33-bc61-1e2b484e267a
STAR DUNES                                                           BARCHAN DUNES

• Formed by multidirectional winds                                      • form in places where there is
                                                                        limited sand and a constant wind
•Have 3 or 4 arms                                                       direction

•Large pyramid shape dunes                                              •crescent-shaped dunes that
                                                                        concave downwind

                                                                        •Face the prevailing wind




Image taken from:
http://www.nps.gov/grsa/naturescience/images/star_dune_form   Image taken from: http://www.indiana.edu/~geol116/Week11/dunes2.jpg
ation.jpg
TRANSVERSE DUNES                                                       SEIF DUNES
•become aligned together along a plane                     •Linear or longitudinal dune
perpendicular to the wind
                                                           •Represents an intermediate direction
•Occur where the supply of sand is greater                 between 2 dominate wind directions, blowing
than that of where barchans are formed                     from one direction part of the year and
                                                           another direction the rest of the year
•Face the prevailing wind
                                                           •Usually parallel




                                                            Image taken from: http://icons-
                                                            ak.wunderground.com/data/wximagenew/e/Eaglz/196.jpg
Image taken from:
http://giltphoto.com/images/Colorado/Great%20Sand%20Dune
s%20National%20Park/GreatSandDunes35w.jpg




Image taken from:                                              Image taken from: http://digital-desert.com/natural-formations/SDGfig4.gif
http://web.arc.losrios.edu/~borougt/DesertDiagrams.htm
FLUVIAL PROCESS
•The Medano Creek that flows next to the Sand
dunes, is an Intermittent Stream


•Intermittent stream- is known as a seasonal stream
where water flows for ONLY part of the year.

•When the water level is low the stream has braided
channels

•Braided channels- consisting of multiple interwoven
and interconnected channels that are separated by
low bars or islands of sand, gravel and other lose
debris.

•During the winter and wet seasons the stream fills up

•The stream carries and deposits sand

•Deposition- whatever is picked up must be set down
BIBLIOGRAPHY
   http://en.wikipedia.org/wiki/Great_Sand_Dunes_National_Park_and_Preserve
   http://www.indiana.edu/~geol116/Week11/wk11.htm
   http://mycolorado.org/sand_dunes.html
   http://www.americansouthwest.net/colorado/great_sand_dunes/national_monument.html
   http://web.ncf.ca/jim/sand/overview/grainflowAnimation.gif
   http://www.geocaching.com/seek/cache_details.aspx?guid=c93e835c-617b-4c33-bc61-
    1e2b484e267a
   http://www.nps.gov/grsa/naturescience/images/star_dune_formation.jpg
   http://www.indiana.edu/~geol116/Week11/dunes2.jpg
   http://giltphoto.com/images/Colorado/Great%20Sand%20Dunes%20National%20Park/Gre
    atSandDunes35w.jpg
   http://web.arc.losrios.edu/~borougt/DesertDiagrams.htm
   http://icons-ak.wunderground.com/data/wximagenew/e/Eaglz/196.jpg
   http://digital-desert.com/natural-formations/SDGfig4.gif

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The great sand dunes

  • 1. THE GREAT SAND DUNES By Amalia McCoy GEO 111 Spring 2012
  • 2.  The Great Sand dunes of Colorado are the tallest in North America.  Rising about 750 feet  Covering roughly 30 square miles
  • 3. EARTH’S NATURAL PROCESS  Formed by sand and soil deposits of the Rio Grande and other streams and smaller rivers which flow into the Rio Grande  Western winds picked up the sand and soil deposits from the River’s flood plain  The wind loses power right before crossing the Sangre de Cristo Range  The sand was deposited on the eastern edge of the valley  The wind changes the formation and shapes of the dunes daily
  • 4. AEOLIAN DEPOSITION Definition: Sand and dust moved by the wind are eventually deposited when the wind dies down. Image taken from: http://web.ncf.ca/jim/sand/overview/grainflowAnimation.gif
  • 5. SLIP FACE  The steeper leeward face of a sand dune •Wind erodes the windward side of the dune which force the grains of sand up and over the crest to be deposited on the other side •Maintains an angle of 32 degrees- 34 degrees. Image taken from: http://www.geocaching.com/seek/cache_details.aspx?guid=c93e835c-617b- 4c33-bc61-1e2b484e267a
  • 6. STAR DUNES BARCHAN DUNES • Formed by multidirectional winds • form in places where there is limited sand and a constant wind •Have 3 or 4 arms direction •Large pyramid shape dunes •crescent-shaped dunes that concave downwind •Face the prevailing wind Image taken from: http://www.nps.gov/grsa/naturescience/images/star_dune_form Image taken from: http://www.indiana.edu/~geol116/Week11/dunes2.jpg ation.jpg
  • 7. TRANSVERSE DUNES SEIF DUNES •become aligned together along a plane •Linear or longitudinal dune perpendicular to the wind •Represents an intermediate direction •Occur where the supply of sand is greater between 2 dominate wind directions, blowing than that of where barchans are formed from one direction part of the year and another direction the rest of the year •Face the prevailing wind •Usually parallel Image taken from: http://icons- ak.wunderground.com/data/wximagenew/e/Eaglz/196.jpg Image taken from: http://giltphoto.com/images/Colorado/Great%20Sand%20Dune s%20National%20Park/GreatSandDunes35w.jpg Image taken from: Image taken from: http://digital-desert.com/natural-formations/SDGfig4.gif http://web.arc.losrios.edu/~borougt/DesertDiagrams.htm
  • 8. FLUVIAL PROCESS •The Medano Creek that flows next to the Sand dunes, is an Intermittent Stream •Intermittent stream- is known as a seasonal stream where water flows for ONLY part of the year. •When the water level is low the stream has braided channels •Braided channels- consisting of multiple interwoven and interconnected channels that are separated by low bars or islands of sand, gravel and other lose debris. •During the winter and wet seasons the stream fills up •The stream carries and deposits sand •Deposition- whatever is picked up must be set down
  • 9. BIBLIOGRAPHY  http://en.wikipedia.org/wiki/Great_Sand_Dunes_National_Park_and_Preserve  http://www.indiana.edu/~geol116/Week11/wk11.htm  http://mycolorado.org/sand_dunes.html  http://www.americansouthwest.net/colorado/great_sand_dunes/national_monument.html  http://web.ncf.ca/jim/sand/overview/grainflowAnimation.gif  http://www.geocaching.com/seek/cache_details.aspx?guid=c93e835c-617b-4c33-bc61- 1e2b484e267a  http://www.nps.gov/grsa/naturescience/images/star_dune_formation.jpg  http://www.indiana.edu/~geol116/Week11/dunes2.jpg  http://giltphoto.com/images/Colorado/Great%20Sand%20Dunes%20National%20Park/Gre atSandDunes35w.jpg  http://web.arc.losrios.edu/~borougt/DesertDiagrams.htm  http://icons-ak.wunderground.com/data/wximagenew/e/Eaglz/196.jpg  http://digital-desert.com/natural-formations/SDGfig4.gif