Answer:
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Answer:
c) on the outer banks of the meander loops
Explanation:
The meandering streams form in places that have low elevation and are flat, covered with softer sediments. The stream starts as mostly straight, but as time passes it erodes one of the banks, while depositing on the opposite bank, become very curvy, snake-like in shape, thus a meandering stream. In the meandering streams, the water has the most velocity at the outer banks. This results in greater erosion of the outer banks, and this part constantly moves outwards. In the same time, the water has the least velocity at the inner bank, resulting in deposition of the material that it has been carrying with it, so this part constantly grows inwards.
Law of lateral horizontality or law of original horizontality.
The law of primordial horizontality states that all rock formations are initially deposited (deposited) horizontally and can be deformed later. from this, we can conclude that something must have happened to the rock that caused it to tilt. These include orogenic events, earthquakes, and faults.
Laws of geology?
- Uniformity: the present is the key to the past.
- Pure horizontality: sedimentary layers are deposited first in horizontal strata.
- Superposition: the lowest layer is the oldest, and it gets younger as it accumulates.
The term, coined by William Whewell, was first proposed by English naturalists in the late 18th century as an antidote to catastrophe. It originated with geologist James Hutton starting his research in many of his books, including his theory of the earth.
Learn more about Geological Process here brainly.com/question/17159824
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Answer:
answer is b X,y to -X,-y
Explanation:
The rule for a rotation by 180° about the origin is (x,y)→(−x,−y) .
There are many ways to determine what minerals are present in a sample. You can observe its color, streak, luster, magnetism, cleavage and hardness. Obviously, you can see what color it is and whether it is metallic or cloudy, but other tests may be required. Streak is tested by rubbing the mineral onto a streak slab of concrete to see what color the powder is. Magnetism is determined by putting a magnet next to the sample, or placing it next to a dish of iron filings. Cleavage is determined by cracking the sample to see the way it fractures. Finally, to determine hardness, you scratch test rocks with the sample, like as controls. I hope this answered your question. (Also, questions like this would best fit under chemistry, because geography is the study of political land)
