Dead Zone: Mouth Of The Mississippi River In The Gulf Of Mexico

Most of the precipitation is around the Gulf Coastal region near Austin and Galveston Island because that is the farthest point of southeast in Texas. Most of the Great Plains will not get nearly as much rain as the Gulf Coastal region because the elevation is a bit higher. The Mountains and Basins region will get little if not no rain at all because of the elevation of that region. The population in North Central is higher than most regions because of the few major cities we have and the growing cities. The regions Gulf Coastal and Great Plains are related because the weather is alike and the population of both regions are close together. The Great Plains and the Mountains and Basins are close related because the Great Plains has big hills

Dead zones develop due to excess nutrients getting into water causing eutrophication, which means over-enrichment. River runoff deposits these nutrients, which come from upstream, a large amount from agriculture of the Midwest. Nitrogen and phosphorus, the primary excess nutrients, are limiting nutrients to primary producers, such as phytoplankton, that live in the surface oceans. Since those elements are limiting nutrients, an elevated influx of them will cause an explosion of productivity called an

The great flood of the Mississippi river in 1927 prompted the severing of class divisions and the extension of racial oppression. The flood caused over $350 million in property damage, 246 flood-related deaths, and a home loss of 130,00. Many african americans fled north to escape the racial oppression that resulted from the disastrous flood. Police held black african americans at gun point until they agreed to help raise the levees to protect buildings and houses from rising flood waters. After African americans started refusing to work, one got shot in the back and all the african americans fled north to escape the hardships that were brought about when the river flooded. After Hoover won presidency, he did not keep his promises to ensure

Lastly, I will explain the dead zone of the chesapeake Bay. Excessive Nitrogen and Phosphrous pollution from human activities cause “Dead Zones” , which are areas with low amounts of oxygen. With little or no oxygen, fish, crabs, oysters, and other aquatic animals literally suffocate. Further excess in nutrients also fuels the growth of dense algae blooms that block sunlight that underwater grasses need to grow in order to continue providing food for waterfowl and shelter for blue crabs and juvenile fish. (Chesapeake Bay Foundation) (Dead Zones)

The Mississippi Delta has many good aspects: heavenly food, ideal land for farming, the culture, and being the home of the Blues are just a few. However, there are many downsides to living in the delta, such as the racial segregation that still exists today, the poverty levels, the percentage of people alcohol and drugs, and health issues. These health issues include obesity, cancer due to the pesticides used in farming, drug/alcohol abuse, and diabetes. Diabetes is such a problem in the South that that it affects majority of the population, Dr. Joseph Assini said, “The Delta is the epicenter of the worldwide diabetes epidemic.” There are nearly twenty seven million people in the United States with Type 2 Diabetes, the disease prohibits the

The Atchafalaya Basin could be perceived as the embodiment of the Cajun Culture within the southern Louisiana region. It has not only been a home to the growing Cajun population but a safe haven for Native American settlers and French colonist that have been exiled. The Basin has existed for hundreds of years dating back to the 15th century. The basin itself is one of the most ecologically varied regions within the United States and has provided for over hundreds of different species. The benefits of the Atchafalaya Basin are endless and have continually provided the inhabitants of the area with bountiful resources, hunting grounds, homes, and transportation.

Louisiana’s Gulf Coast is eroding into the sea, and by 2100 most of Southeast Louisiana could be completely underwater. Not only does this threaten human and animal habitats, but also the energy, shipping, fishing, and tourist industries that have made this region of the U.S. a valuable part of the national economy (Marshall, 2014). In the past 200 years, half of the nation’s wetland habitats have been lost due to natural and manmade processes. Louisiana’s wetlands make up 40 percent of the total wetlands in the continental United States. 80 percent of losses, nationally, are of Louisiana’s coast (Williams).

The formation of the Atchafalaya River is nothing short of remarkable. Alongside the regulatory systems, the Atchafalaya is responsible for the delicate water balance of the Atchafalaya and the Mississippi River. The Atchafalaya River is one of the largest tributaries to the Southern Louisiana swamps and bayous.

Ali Ware Mrs. Buckley English I 14 February 2018 The Evolution of the Mississippi Delta The Mississippi Delta is a region 200 miles long and 85 miles wide. Home to the most fertile soil in the world, the Delta-Yazoo Basin Region is a rare place.

The Arkoma Basin is one of several foreland basins that formed along the Ouachita Orogenic Belt during the Mississippian and Pennsylvanian time periods. It covers approximately 33,800 square miles and extends from southeastern Oklahoma to central Arkansas (Perry, 1997). The Arkoma Basin is bounded to the north by the Ozark Uplift, to the south by the Ouachita Mountains, to the northwest by the Anadarko Basin, to the southwest by the Arbuckle Uplift, and to the southeast by the Mississippian Embayment (Figure 5). The red box in figure 5 denotes the general location of the study area, which is in the eastern Arkoma section.

The Colorado RIver is best known for being the principal river of the southern United States and Mexico, but it soon could lose that title. Running about 1,500 miles long, the river is a vital source of water for agricultural and urban areas in the southern desert lands of North America. However over the past decade or so, the river has begun to deteriorate. There are many causes and solutions to the deterioration of the Colorado River.

How was life up and down the Mississippi river? Life on the Mississippi was no cakewalk. The first settlers had to endure floods, war and disease. Many died coming West to start a new life for their families. It was hard for them, but they made it work and more people followed suit and came to settle along the banks of the Mississippi.

The Atchafalaya River was created over 1000 years ago. It was formed because of the mighty Mississippi river. It plays a very important role in the everyday lives of the Louisiana people. The conceivable redirection of the Mississippi River and man1s push to oppose it, present one of the best stream designing issues ever experienced. The proof that backings the case that catch of the Mississippi by the Atchafalaya is inevitable, is accessible and plentiful. Information on the decay of the limit of the Mississippi underneath Old River and the expanding limit of the Atchafalaya has been gathered and validated. Geotectonic movement a1 so shows that the inclination toward preoccupation is expanding.

Could you imagine what happened to translucent and glistened Florida’s springs? Florida was floating on the water, it has more than 900 freshwater springs (Guest, 2014). Unfortunately, many studies show there are several threats such as drawing out tremendous amount of water, and the absent of regulation laws, lead to Contamination of Florida’s springs, loose business.

Dead zones in the ocean are so called because of the lack of oxygen in the seawater according to Karstensen. Oxygen is obviously needed to support all marine life in these areas. The article also mentions dissolved oxygen is