Fay Canyon, Arizona

This is the end of Fay Canyon near Sedona, Arizona. The trail divides at this point to go up two other valleys. The large bolders are from the Schnebly Hill Sandstone Formation, which is the source of the sand.

Definition/Function:

The Schnebly Hill Sandstone Formation is the main redstone formation in the Sedona area. It is 800 to 1000 feet thick and was formed about 270 million years ago.

Significance in the Environment:

Characteristic Features:

Associated Particles:

References:

Greenberg, Gary, A GRAIN OF SAND: NATURE'S SECRET WONDER, Voyageur Press, 2008.

Welland, Michael, SAND: THE NEVER ENDING STORY, University of California Press, 2009.

http://www.microscopy-uk.org.uk/mag/indexmag.html?http://www.microscopy-uk.org.uk/mag/artjun01/clsand.html
(Good Information on the microscopy of sand, Great site for more information on microscopy in general)

http://www.scientificamerican.com/article.cfm?id=a-grain-of-sand-natures-secret-wonder
(Good Information on Sand with links to more information on sand)

http://www.sciencelive.org/component/option,com_mediadb/task,play/idstr,Open-feeds_fsc_exploring_sedimentary_processes_fsc02_02_m4v/vv,-2/Itemid,97
(Brief, very informative video on what can be learned from the shape of a sand grain.)