Out of the given statements, Science consists of proven theories that are understood to be true explanations of reality is not consistent with the major hallmarks of science.
Answer: Option A
<u>Explanation:
</u>
Hallmarks of science are the factors that need to be logically acceptable about any given theory for it to be called 'scientific'. These hallmarks are specific, nor absolute neither relative in nature.
For a theory to qualify scientific hallmarks, it can also be at the stage of a proposed hypothesis, not necessarily a true explanation of true reality. For example, the theory of relativity was still considered a scientific theory before Albert Einstein proved it to be true.
My answer -
I believe the correct answer is:
Subduction is the collision between two tectonic plates. It is the
biggest crash scene here on Earth. It is a geological process where one
plate moves under another and is forced down into the mantle.
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Answer:
Movement in the mantle caused by variations in heat from the core, cause the plates to shift, which can cause earthquakes and volcanic eruptions.
The faults in which the hanging wall moves down relative to the footwall is called normal fault.
Explanation:
There are several types of faults based on their characteristics. One of them is the normal fault, or normal dip-slip fault. The main characteristic of this fault is that its hanging wall moves down relative to the footwall, while the footwall tends to move up relative to the hanging wall. The force that creates this type of faults is the vertical compression as the crust of Earth is lengthening.
- These faults can be found all over the world, and they are actually the most common type of faults.
- The normal dip-slip faults are bounding big portion of the mountains, as well as rift valleys.
- As these faults progress with their formation, with the footwall going up, and the hanging wall going down, the footwall becomes a hill or a mountain, while the hanging wall becomes a valley.
- The normal dip-slip faults can be found at all types of tectonic plate boundaries.
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