Answer:
In my perspective, Cassie should not have got revenge. I think your essay is perfect if I do say so myself. If you would lie to add more figuretive language, I suggest you give some thing that happened to you, and put it in there, make it even more interesting. It's your decision, but I personally think It's perfect.
Explanation:
Answer:
the answer is c.
to list the information in two categories: clubs and teams
Explanation:
Answer:
he second fire goes out because the man makes a mistake: he builds the fire under a pine tree. ... Eventually, this snow falls onto the fire itself, extinguishing it and leaving in its place “a pile of fresh snow.”
Explanation: look it up lol :)
The best way to write sentences about likes and dislikes of a person is:
- I love playing football.
- I dislike swimming.
- Volleyball is fun, but badminton is too much of a bore.
- I'm a bit scared of long jump, but i prefer athletics.
<h3>What is a Sentence?</h3>
This refers to the collection of words which contains a subject and a predicate and makes meaning.
With this in mind, we made use of both simple sentences and complex sentences to show the likes and dislikes which a person might have for different activities.
Read more about sentences here:
brainly.com/question/781903
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
