Buffalo River Research Paper

The acidic ground water was necessary due to the fact that pure water could not dissolve the limestone and marble. The acidic ground water absorbed some carbon dioxide from the air and the decaying vegetation located in the soil and formulated carbonic acid. The carbonic acid was able to dissolve out “cavities” (3) in the bedrock and when the level of the water dropped, the passageways were ready for the next step of the development of caves. There is water that seeps into the cave at a slower rate. The acid is weak but it is able to dissolve the bedrock above the cave and is able to redeposit the minerals, which in this case is calcite, on the floors, ceilings, and walls of the Lehman Caves in the form of “cave decorations” (3). These are still growing today, and because of it they are very

There is one day that will always stick out in my mind. I was down at the Wabash River with my family and friends celebrating Labor Day. I was doing what any second grader would be doing, riding my bike, enjoying the outside. I had no care in the world while I was riding my bike. I only cared about two things, having fun and the wonderful weather.

Starved rock and St. Peter Sandstone are an erosional remnant of Ordovician period. These remnants contain Pennsylvanian clastics that survived the washing out of the Illinois River at the end of the Ice Age. Evidence for swift, turbulent, and deep water includes gravel bars and erosional features as high as 160 feet above the current level of the river, massive cross bedded sand, and gravel deposits along the river course.

Six years ago, my family and I went to Turner Falls Park in Davis, Oklahoma. We arrived at the park early in the morning and got ready to go swimming. I went to the restroom and got changed. When we were ready, we left to go swimming we walked on a bridge to get to the swimming area, there was a huge waterfall and we went swimming under it. After that we went to another swimming area that had two big slides, we swam there for about and hour then went to our camping area to eat. The next day we went hiking on trails and also went to a castle that was made of stone. We spent the rest of the day swimming and looking around the park. It was a great experience and It would be great to go again. In this essay you will be reading about history, a physical description

Limestone and dolomite are most susceptible to solution processes because the water, which is slightly acidic, reacts with rock and dissolves the co2 gas carrying away or dissolving some of the sediment.

This early in the football season, it's still difficult to get a clear idea about the strength of any given team. Most of major conference teams have been playing against lesser competition, making it precarious to pinpoint exactly where the team sits as far as talent is concerned. It's kind of like doing a 5 Dimes review without ever visiting the website.

Suwannee River is the place where strangers are turned into friends. Suwannee River has been around for many years, Suwannee River was formed in December 21st, 1858. Stephen Foster never visited, but, named the Suwannee River “ Swanee River” after his song “Old Folks at Home” written in 1851. “Old Folks at Home” became Florida’s official state song in 1913.

The Buffalo Creek flood of West Virginia is believed to be the most devastating coal relate disaster in West Virginia history. The flood occurred in the Buffalo Creek area of Logan County on February 26, 1972 when three dams broke and released 132 million gallons of water and coal waste known by miners as “gob,” and is a thick sludge-like material. The gob contains many toxic chemicals and pollutants such as mercury and arsenic that are left behind from the coal mining process. The wastewater would lie in settling ponds and dams until it could be properly disposed of. The water that was left over from processing coal would be disposed of in two different ways. Some of the water would be pumped from the dam back to the “tipple”, otherwise

The quadrangle is considered to be a part of the Allegheny Plateau, so the rocks in this region are mostly of Carboniferous age. Carboniferous rocks are subdivided into two series: the Pennsylvanian and Mississippian. The rocks of both series mainly consist of alternating beds of shale and sandstone, but Mississippian rocks on southern parts of the plateau include thick limestones (Phalen 1). Both series are represented in the Johnstown quadrangle. The Pennsylvanian series, however, covers most of the region, while Mississippian rocks appear only at the surface along deeply eroded anticlines.

The karst terrain which creates the geomorphic conditions for sinkholes is a broad topic in the field of geology, and encompasses the study of groundwater, drainage, chemical processes, and many other considerations. Essentially, karst regions are located where the rock below the earth can be dissolved by the acidic groundwater which percolates through it (The Science of Sinkholes). These areas are underlain by soluble rocks such as gypsum, limestone, and dolomite which typically react with carbonic acid (H2CO3) from groundwater to dissolve the rock. Presence of limestone is

At the beginning of the month we stopped at the sweetwater river crossing because the land was ideal for camping and lavish for the animals. At nightfall we were attacked by another tribe of native americans, this battle was faster although more meaningful because 7 of my close friends died in the battle. Joseph and Tom both died in the battle leaving Tom, Dave and I left in the council. Joseph's death was early on in the battle, him and his family were slaughtered horrifically as joseph was fighting off the indians he watched as his daughter was decapitated and wife's throat was cut open as she screamed and pleaded, Joseph upon watching was distracted from the task at hand and was stabbed in the stomach and was left to bleed to death on the

It has came to mind that the Big Sioux River located in the Eastern Part of South Dakota is a very polluted river. It is so polluted that its the 13th highest polluted water source in the United States. Therefore the people around this river, this is a very important to the people around because this is there main water source. People may ask why is this river so polluted and its because of the toxic waste from us humans. Every time you go to the bathroom all this waste ends up going into the river and even when you take a shower all the chemicals that go in your hair or for your body from the soap end up going into the river.

Multiple Japanese settlements started to increase in rustic communities of the Columbia River Basin, despite the Issei’s harsh labor in the early 20th century, the discrimination led to growing anti-Japanese arrogances on the West Coast, even the feeling had developed against the seeming Chinese competition. Nampa, and Caldwell Idaho drove out the Japanese workers this led to white mobs around Coeur d’ Alene and in Poland to threaten the Japanese railroad workers. Pressures led to the (“Gentleman’s Agreement”) between the U.S. which effectually limited the numbers of laborers that could travel from Japan in 1908.

“What’s the Boneyard Creek?” was the response I got from several my friends as I asked them about the trench located on the Engineering Quad. Honestly, if not for FOS I don’t think I would have paid much attention to the creek. It is not exactly beautiful and not particularly important to a students running by it to get to class. However, after a quick google search, I discovered that the Boneyard Creek is an extremely fascinating historic landmark of the University of Illinois.

The Illinois River has a lot of attractions nearby. The attractions are very popular amongst college students and hikers.One of the most popular attractions is the Sparrowhawk Primitive Area Trail which allows you to view the beautiful scenery of northeast Oklahoma.The J.T. Nickle Preserve is another attraction in Oklahoma which allows you to