Mississippi has a variety of different soils .The three general soils are 1) the river flood plain, known as the Delta, 2) a loess region, or bands of soils formed in windblown material that adjoins the Delta, and 3) Coastal Plain. The Mississippi Delta is better for growing row crop, while the loess and Coastal Plain region are better for animal production and forestry. The loess and Coastal Plain regions are divided based on similar soils, geology, climate, water resources, and land use called Major Land Resource Areas. The Mississippi Delta’s soil comes from sediments left by flooding various rivers in the region, rather than being a typical Delta formed by the mouth of a river. In the Delta most of the land is farmed, with three-fourths of the cropland to the north. Controlling surface water and drainage are major soil management issues. In the Delta soils are naturally diverse because of their alluvial origin. Particle sizes within the sediment decrease as distance from the originating stream increase. Another factor in Delta soil formation us surface water movement over time, because soils that formed under standing water have different properties than soils formed under moving water. Soils with large amounts of clay particles have unique features. When the soil is dry, small round aggregates form at the surface that look like shotgun buckshot, which is where the popular name for Delta clay soils “buckshot” came from. Soils with large clay content have very slow water filtration rates; this has led to significant aquaculture and rice production in the region. When floodwaters receded in the Delta, strong winds blew some of the dry sediment left by flooded river to the adjacent uplands to form the loess areas. Because of eas...
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...c Research Papers, 1964. Jackson, MS: Mississippi Geological, Economic and Topographical Survey, 1964. 15. Print.
4. Hilgard, Eugene W. "Age of the Orange Sand." Report on the Geology and Agriculture of the State of Mississippi. Jackson, MS: E. Barksdale, State Printer, 1860. 17. Print.
5. Marsh, Bob. "Guide to the Mississippi Barrier Islands." Guide to the Mississippi Barrier Islands. N.p., n.d. Web. 30 Mar. 2014.
6. Krinitzsky, E. L., and Willard Jay Turnbull. Loess Deposits of Mississippi. New York: Geological Society of America, 1967. Print.
7. Huang, Ter-chien. The Sediments and Sedimentary Processes of the Eastern Mississippi Cone, Gulf of Mexico. Tallahassee: Florida State University, Sedimentological Research Laboratory, 1969. Print.
8. Bennett, Frank, and R. A. Winston. Soil Survey of Pontotoc County, Mississippi. Washington, D.C.: G.P.O., 1907. 405. Print.
Marshak, S. (2009) Essentials of Geology, 3rd ed. New York: W.W. Norton & Company, ch. 11, p. 298-320.
The shelf-edge includes carbonate-to-clastic facies transition and tectonic uplift and erosion of the carbonates followed by deposition of the clastics. The Saint Peter Sandstone is a well-sorted, almost pure quartz arenite deposited during a major mid-Ordovician low stand. Clastics spread across an exposed carbonate platform by transportation. This is shown by the well-rounded, frosted texture of the quartz grains.
During the years between 1840 and 1890, the land west of the Mississippi River experienced a wild and sporadic growth. The natural environment contributed greatly to this growth spurt and helped shape the development of the trans-Mississippi west. The natural environment dictated and facilitated the development of the west by way of determining who settled where, how the people survived, why people wanted to settle, and whether they were successful or not.
2000 Rural Communities in the Black Warrior Valley, Alabama: The Role of Commoners in the Creation of the Moundville I Landscape. American Antiquity 65(2):pp. 337-354. Welch,
The Geological history of the Houston area includes surface water present in several types of lakes, rivers, and a wide-ranging system of bayous as well as, manmade canals that all share the rainwater runoff management system. In of Harris County 25%-30% of the land is within a 100 year flood plain. Elevation range of Harris 0'-310', so presently land surface and uppermost sediments in the Houston area are geologically very young strata and research isolates that its ages are measured in tens of thousands, not millions, of years. Distinctly this knowledge concludes it is faulted by a natural process, before significant fluid extraction ha...
Ashton, John. "KENEDY, MIFFLIN." 15 June 2010. Handbook of Texas Online. Web. 5 May 2014. .
Secondly, it is important to discuss the people of the state. According to Wikipedia, the 2010 U.S. census stated, “ Mississippi is an ethnic diverse state with 59% of the residents being White, 37% African American, 0.5% American Indian, 0.9% Asian American and 2% other. With this many ethnic group, the area is filled with cultural activities to promote their ethnic backgrounds. Prior to the 1830s there were many tribes of Indians in Mississippi. However, in the 1830s the Treaty of Dancing Rabbit Creek, most of the Indian population was moved to Oklahoma. Now, the Mississippi Band of Choctaw Indians is located in Philadelphia, Mississippi and the surrounding counties”. According to the same census, “Mississippi has the highest proportion of African American in the nation.
If this culture had survived, European settlement would have taken much longer than it originally did. The Mississippian people would no longer fear the Europeans, because of all the anger and resentment they had towards them for the devastation and despair they caused them. It would have taken a very large and skilled army to take down the Mississippian culture a second time.
The purpose of this paper is to explain and highlight different aspects of the Powder River Basin to include paleogeography, stratigraphy, maturation history of organic material, vitrinite reflectance data, sulfur content, both historical and current production data, as well as the environmental impact in the basin.
Fleeger, Gary M., Bushnell, Kent O., and Watson, Donald W. “Moraine and McConnells Mill State Parks.” Pennsylvania Trail Geology. 2003. The 'Secondary' of the 'Secondary' of the 'Secondary' of the 'Secondary' of the 'Secondary' of the ' Print. The.
Morton, J. W. (n.d.). Metamorphosed melange terrane in the eastern piedmont of north carolina. Retrieved from http://geology.geoscienceworld.org/content/14/7/551.abstract
Davis, J. G., R. M. Waskom, and T. A. Bauder. Managing Sodic Soils. Colorado State
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6. In 2001 it was assumed that soil contamination at the site would be prevented from leaching into the Floridan Aquifer due to the assumed impenetrable nature of thick clay formations (Miocene clays) located between the soil contamination sources and the deeper Floridan Aquifer. Has this turned out to be true? No, this has not turned out to be true because significant levels of dissolved contaminants moved to the deeper zones of the intermediate Hawthorn Group formation and the Floridan Aquifer.