How Independent Sample Essays Can Improve Your Test Essay

How Independent Sample Essays Can Improve Your Test EssayWhen writing an essay, you may be interested in knowing more about test samples. You may think that there is no way that you will be able to use these for your essay, but you are mistaken. These can be used to make your essay much more unique and impressive than a typical essay.First of all, these sample essays are by no means like the ones that are offered online. There are a lot of online test websites that offer sample essays, however the content is pretty similar. By using these sample essays, you will be able to get some insight into how to write an essay. Many people make the mistake of getting ready to write the essay before they know what they want to say.When you start looking for sample essays, you will notice that some of them are very simple. Some are even very basic. In this case, it is best to try to use a sample that is really short. If you are trying to get across a point, this will be a good idea.These test ess ays that you find are actually short test papers that you can use to take before taking the actual test. This is great for you if you are not going to be on time for your test. By using these sample essays, you will be able to get an idea of what you need to do when you are going to take the actual test.It is not necessary that you use the same essay that you will be given, however you should keep in mind that the content should be fairly easy to understand. If you try to write it fast, you will end up making some mistakes. It is better to slow down a little bit.Make sure that you learn from the sample essays that you find. This will help youto learn to write a well-written essay. The more you practice, the easier it will be for you to get your essay correct.Writing a good essay is something that is important to do when you are going to take a test. This is what will help you pass the test and go on to further your education. Make sure that you research about writing your essay befo re you get started.

The Erosional and Depositional Landforms that Result from Rivers and Glaciers

The forces that the earth possesses have the ability of moving tectonic plates, in turn, creating volcanoes and ranges. These forces whose energy is obtained from the sun, have the ability of destroying mountain chains. This paper aims at discussing numerous erosional and depositional landforms, which appeared as a result of glaciers and rivers.Advertising We will write a custom essay sample on The Erosional and Depositional Landforms that Result from Rivers and Glaciers specifically for you for only $16.05 $11/page Learn More Some of the erosional landforms are arete, cirque, col, groove, hanging valley, headwall, horn, paternoster lakes, striations, tarn, truncated spur, and u- shaped valley (Peizhen, Peter and William 894). An arete refers to a bedrock ridge that has sharp edges and steep sides. It is formed of two glaciers, which are located on opposite sides of the ridge. A col refers to a little spot that is found either on an arà ªte or cirque. A cirque is a bedrock feature, which can be either in the form of amphitheater or it can be semicircular-shaped. They are formed when glaciers are scouring in the mountains. The ice that leads to the development of the glacier accumulates here first. In other words, a cirque is glacier’s headwaters. The headwall is a cirque’s steep back- wall (Benn et al 380). Paternoster lakes refer to a long sequence of lakes, which are found in a glacial valley. A horn refers to a mountain peak, which is shaped like a pyramid, and which appears as a result of erosion of several glaciers at various sides of a mountain. A tarn refers to a glacial lake, which is formed as a result of scouring. Tarns are usually common in cirques. A truncated spur refers to a split, which is created as glaciers are forming valley. A U- shaped valley is also referred to as a glacial trough, and it is a valley that is eroded glacially. There are several types of moraines, which constitute depositional land forms. A moraine refers to the collection of unconsolidated materials, which result from glaciers. The various types of moraines have different appearances (Fort 107). In end moraines, the material gathers at the schnozzle end. In ground moraines, the material gathers right under the glacier’s foundation. Finally, in medial moraines, the moraine is at the middle and its top. Apart from moraines, other depositional landforms include esker, kame, and outwash fan. A kame is a hillock with an irregular shape. An outwash fan refers to a braided stream, which begins from the front side of a glacier (Milton 4040).Advertising Looking for essay on geology? Let's see if we can help you! Get your first paper with 15% OFF Learn More As opposed to a river, a glacier entirely fills a valley. Therefore, a glacier possesses more eroding power. It is not necessarily that a glacier winds around intertwining spurs. Moreover, its valleys can be subjected to other transformations. A misfit stream refers to an extremely minute stream at a glacial trough’s bottom, which is usually too minute to form the valley. In conclusion, it must be highlighted that there are various types of erosional and depositional landforms that are associated with the creation of glaciers and rivers. Their study is extremely vital taking into consideration the continuous formation of volcanoes. In order to comprehend rivers and glaciers, there is a need to study them comprehensively. This allows the differentiation of minute and stringent characteristics and features. In this regard, geologists have a demanding role in ensuring differentiation of the various landforms. Works Cited Benn, Douglas I., et al. â€Å"Glaciated valley land systems.† Glacial landsystems (2003): 372-406. Print. Fort, Monique. â€Å"Glaciers and mass wasting processes: their influence on the shaping of the Kali Gandaki valley (higher Himalaya of Nepal).† Quaternary International 65 (2000): 1 01-119. Print. Milton, Daniel J. â€Å"Water and processes of degradation in the Martian landscape.†Journal of Geophysical Research 78.20 (1973): 4037-4047. Print. Peizhen, Zhang, Peter Molnar, and William R. Downs.†Increased sedimentation rates and grain sizes 2–4 Myr ago due to the influence of climate change on erosion rates.†Nature 410.6831 (2001): 891-897. Print. This essay on The Erosional and Depositional Landforms that Result from Rivers and Glaciers was written and submitted by user Ares to help you with your own studies. You are free to use it for research and reference purposes in order to write your own paper; however, you must cite it accordingly. You can donate your paper here.