<u>If your asking about what interactions mean in </u><em><u>Science</u></em><u> then this is the definition</u> --> a mutual or reciprocal action; interacting.
<u>If your asking for the </u><em><u>physics</u></em><u> definition for interactions mean then this is the definition</u> --> transfer of energy between elementary particles or between an elementary particle and a field or between fields; mediated by gauge bosons.
<u>Or, if your asking for what interactions mean </u><em><u>in general</u></em><u> then this is the definition </u>--> 1 : mutually or reciprocally active. 2 : involving the actions or input of a user especially : of, relating to, or being a two-way electronic communication system (such as a telephone, cable television, or a computer) that involves a user's orders (as for information or merchandise) or responses (as to a poll).
<em>Hope this helps you, and I hope you have a wonderful weekend and a wonderful Thanksgiving bye! Your welcome.</em>
<h3>- Sadie ❤</h3>
The answer is: The personification makes the setting more vivid to the reader.
Figurative language is a nonliteral, metaphorical or symbolic choice of words, and personification occurs when something nonhuman possesses human qualities, or when an abstract attribute takes human shape.
In the passage from "Morte d'Arthur," by Alfred Lord Tennyson, personification is used to offer readers a more forceful or powerful description of the scene. For example, <em>mighty bones, the wind-sea sang shrill</em> and <em>flakes of foam.</em>
The correct answer is definitely the historical method.
You should observe words and their usage as it developed throughout history.
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
