High school essay examples include a variety of short essays such as the narrative essay, persuasive essay and analytical essay and more. Depending on the essay type, the high school essay format can be anywhere from one to five paragraphs in length.
When choosing a high school essay format, the first step is to identify the type of essay you need to write. Generally essays for school students are much focused and concern one topic or one narrative story. Check out some narrative essay examples. High school essays tend to be shorter and simpler than those for university, but an essay for school students should be clear and concise.
As a second step, “how to write a high school essay?” comes into play. The most common type of short essay format is the 5 paragraph essay. Like all essays, the 5 paragraph essay contains an introduction, a body and a conclusion. For this high school essay, the introduction is one paragraph, the body is three paragraphs and the conclusion is one paragraph. It’s simple and easy to work with.
The goal of an introduction is to capture your reader’s interest and explain what the essay is about. The introduction will also contain a thesis statement. A thesis statement is usually one sentence that shares the main point of the essay. Read any list of tips for writing essays and they’ll tell you that the intro is vital. It lets the reader know if they want to continue.
The main part of a short essay is the body. In the 5 paragraph essay, the body is three paragraphs long. Each paragraph should cover a particular point or claim that relates back to the thesis statement. There should be a main sentence that supports the claim in each paragraph. Transition smoothly from one paragraph to the next. The entire high school essay should flow easily and be simple to read.
The conclusion of a short essay is the most memorable part for a reader. In the conclusion, you can summarize your main idea. Rewrite the thesis statement from the first paragraph and leave the reader with something memorable. This is your final chance to tell them something.
After writing, proofread your essay. Proofreading a short essay involves checking spelling, grammar, sentence fluency and checking the overall flow and readability of your ideas.
The following short progress report, written by a student in geology, provides an excellent example of how concrete and affirmative a progress report can be. Note the specificity even in the title, and how sections such as "Remaining Questions" and "Expected Results" demonstrate that the writer, even though he is two months away from the completion of his thesis, is thinking about the work in a professional manner.
Click here to open a sample progress report within this page.
"Stratigraphic Architecture of Deep-Ramp Carbonates: Implications for Deposition
of Volcanic Ashes, Salona and Coburn Formations, Central Pennsylvania"
by John Lerner
SCOPE AND PURPOSE
The Late Middle Ordovician-age Salona and Coburn formations of central Pennsylvania show cyclic patterns on a scale of tens of meters. Little research has been done on sequence stratigraphy of deep-water mixed carbonate/siliciclastic systems, and a depositional model for this environment is necessary to understand the timing and processes of deposition. The stratigraphic position of the bentonites at the base of the larger cycles is significant because it indicates that they accumulated during a time of non-deposition in a deep water environment.
To date, I have described five lithofacies present in the Salona and Coburn formations. Two lithofacies are interpreted as storm deposits and make up the limestone component of the thinly-bedded couplets. Some trends were observed in the raw data; however, because of the "noisy" nature of the data, a plot of the five-point moving average of bed thickness was created to define the cycles better.
Two key tasks are to be completed in the coming weeks. With the results of these tests and the field observations, I will create a model for deposition of a deep-ramp mixed carbonate/siliciclastic system in a foreland basin environment. The model will include depositional processes, stratigraphic architecture, and tectonic setting.
Questions remain regarding the depositional processes responsible for the featureless micrite at the base of the Salona Formation. . . . How rapid was the transition? What record (if any?) remains of the transition? Were bentonites not deposited, or were they selectively removed at certain locations by erosive storm processes?
I expect to find that the large-scale cycles represent parasequences. Flooding surfaces are marked by bentonites and shales, with bentonites removed in some locations. If the cycles are true parasequences, the implication is that eustatic sea level changes and not tectonic influences controlled the depositional changes over the interval.