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Geology, Landscapes and Eco-Tourism
Badlands are regions in the Midwest of the United States, where the climate is substandard. Terrain varies from extremely cold to extreme warm, with large glaciers in some areas. The experience primarily unincorporated landforms and little vegetation; and experience no significant wildlife. In fact, it is the most desolate place in the entire Midwest, with only a few cities of any size.
Badlands are typically a part of flat, low-lying land that has experienced erosion. They are more defined by sharp, descending cliffs and low-lying clay soils. Geographically, the badlands consist of ten Eastern Corners, including two Wakhan Desert and four taverns deserts. The landscape is highly diverse, with landscapes ranging from heavily eroded sand to heavily vegetated forests.
Badlands has numerous geological features, such as cliffs, canyons, depression, plateaus, and erosion. The landscape appears flat due to lack of any significant elevations.
Geologically, the badlands feature several folds, faults, and folds of earth that have separated over time. In fact, the tectonic forces responsible for the folding and canyoning of the landmass are still present, although at a much reduced rate.
Geographically, badlands show little evidence of recent landform evolution. Most interesting in the geomorphological sites in the badlands are folds and gully erosion that mark the low-lying land surfaces.
Tundra zones in the vicinity of the badlands include an unusual combination of wetlands and arctic tundra. Most of the plants in the area are coniferous or deciduous, with exception of connotes.
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Seismic activity, especially within the last century, has altered the topography, especially along the margins of the major tectonic field. Sedimentary material such as gravels and finer clay soils are exposed in the southern part of the badlands, while in the north most of the badlands vegetation is prevalent.
Most of the erosion takes place in the south Dakota area, although the edge of the Badland Formation also contributes largely to the high salt content of the Badland.
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The tundra regions and the Badland can be utilized as a platform for research and observation of the natural phenomena. During the winter, the blanket of snow covering the ground creates a photographic site. The same phenomenon can be observed in the summer on the opposite side of the spectrum, when the melt water from the ice caps and glaciers on the surface make the land highly visible.
In addition, Badland National Park features a variety of geological and biological wonders, including a variety of salt pans, faulted-concentrated folds and cavities, abundant host plant communities, unique dinosaur mammals, a diversity of vertebrates, and the fossils and nests of millions of winged creatures.
A Badland sightseeing excursion consists mainly of travelling through the numerous escarpments and troughs that are formed on the bed of the Badland. These formations are separated into two parts – the glacial ones which are forming owing to the movement of the earth’s ice over the surface, and the eroding ones, whose formation is a consequence of wind erosion.
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Most of the glacial buttes and mountains are relatively flat. The troughs, on the other hand, begin to form gradually and are filled with gravel or sand as they accumulate. Geologists and archeologists usually distinguish between the glacial and the eroding badlands.
The most prominent feature of the Badlands is the absence of any vegetation. This is because the presence of considerable quantities of clay-rich silt results in the deposition of copious amounts of this sediment, which acts as a sole condition for the existence of the badlands.
The silt, together with the clay, forms a noxious layer that has an unpleasant smell and is dark and smoky. These dark layers which are several kilometres in thickness also help preserve the integrity of the tiniest of the Badland National Park.
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