<h2>Answer:</h2>
C) build playgrounds,not shopping malls.
<h2>Explanation:</h2>
A persuasive essay is an essay which is used to convince a reader about a particular idea or plan that he believes in. A persuasive essay can be based on anything about which a person may have an opinion or that one can make a clear argument about. Since the C option tells us about an opinion and persuading us to build playgrounds rather than shopping malls that is why this can be put under the category of persuasive essays.
Answer:
It explores the way that telling stories simultaneously recalls the pain of the war experience and allows soldiers to work through that pain after the war has ended. O'Brien and Bowker illustrate how speaking or not speaking about war experience affects characters.
Answer: In this sentence, the word fancied means trusted or liked.
Explanation:
Fancied can mean either mean a regard something or to feel a liking for someone or something. In this case, she had trusted/liked the shadows.
Compacted meaning i do believe
Answer:
Explanation:
1. There are three main types of glacial erosion - plucking, abrasion and freeze thaw.
2. A nunatak is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They are also called glacial islands. Examples are natural pyramidal peaks.
3. A lateral moraine forms along the sides of a glacier. As the glacier scrapes along, it tears off rock and soil from both sides of its path. This material is deposited as lateral moraine at the top of the glacier's edges. Lateral moraines are usually found in matching ridges on either side of the glacier
4. These scratches, "striations," can be used to understand past ice flow. ... Over time, the glacier moves over rock and sediment, leaving striations or striae, on the rock surfaces that can reveal the direction that the glacier was flowing
5. They form in bowl-shaped depressions, also known as bedrock hollows or cirques, located on the side of, or near mountains. They characteristically form by the accumulation of snow and ice avalanching from upslope areas
