The answer is B) <span>Don't look forward to the day you stop suffering, because when it comes you'll know you're dead.
Please vote Brainliest!
Silvera ^_^</span>
Answer:
C
Explanation:
The alternative C is correct. <em>YOU'RE</em><em> </em>is describing what you are doing, going to do, or what you did or want.
Make a quick, subconscious determination as to whether the consequence in question is important - how will it affect my life, the future, if it will affect the people in my life and how.
If it does not affect others or myself that much, I follow my instinct about whether the action is right or wrong. After that act on it and the results automatically modifies my mentality for future decisions.
If the consequence in question is likely to be high then I think long and hard about the decision. I do not make a snap decision in this case (as above), instead I take responsibility and make sure I get information in order to make the best choice.
Then process the information to determine whether the action will affect the happiness and survival of the people involved, whether it will affect the dynamic of my family, whether it will be against a cultural norm, whether it breaks any laws, whether anyone will be physically harmed and so forth.
After determining all these factors I weigh the costs against the benefits to those same categories (as well as to myself) and then I will take action.
I deal with any consequences and then (as above) evaluate the results and let that information guide future decisions.
Answer:
answer other people's questions and how it answer your questions
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
