<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><dc:coverage>United States, Georgia, 32.75042, -83.50018</dc:coverage><dc:creator>Coleman, David C., 1938-</dc:creator><dc:creator>Lee Coursey</dc:creator><dc:date>2018-10-31</dc:date><dc:description>A bare fallow field, composed of sandy soil and clay subsoil, in Vienna, Georgia. Soil, which is composed of minerals, organic material, water, and air, is generally less than a meter in depth and forms through the weathering of the earth's surface.</dc:description><dc:description>Photograph of a barren fallow field, composed of sandy soil and clay subsoil, experiencing wind erosion. An abandoned wooden building sits on the field. Soil, which is composed of minerals, organic material, water, and air, is generally less than a meter in depth and forms through the weathering of the earth's surface.</dc:description><dc:format>image/jpeg</dc:format><dc:relation>http://www.georgiaencyclopedia.org/articles/geography-environment/soils</dc:relation><dc:relation>Forms part of: New Georgia Encyclopedia</dc:relation><dc:rights>https://creativecommons.org/licenses/by/4.0/</dc:rights><dc:source>http://www.georgiaencyclopedia.org/articles/geography-environment/soils</dc:source><dc:source>Forms part of: New Georgia Encyclopedia</dc:source><dc:subject>Fallow lands--Georgia</dc:subject><dc:subject>Erosion--Georgia</dc:subject><dc:subject>Wind erosion--Georgia</dc:subject><dc:subject>Soil erosion--Georgia</dc:subject><dc:subject>Soils--Georgia</dc:subject><dc:subject>Dust--Georgia</dc:subject><dc:title>Fallow Field</dc:title><dc:type>StillImage</dc:type></oai_dc:dc>