A. The theory could be altered. If new evidence I presented it is the law to take a look at it.
If new evidence challenges a theory, it may lead to the alteration of that theory. This is a key aspect of the scientific method, where theories and hypotheses are continuously tested. The climax of these tests can lead to validation, modification, or discarding of the theory.
If a theory is challenged by new evidence, a possible outcome is that the theory could be altered. In the realm of science, theories are not static; they are dynamic and prone to modifications when new, credible evidence emerges. Theories are always subject to validation and verification. When the theory of evolution was first proposed, for instance, it faced plenty of criticism and disbelief. However, as it was continually supported by emerging evidence, it is now widely accepted.
An assumption or hypothesis is typically tested through experiments. If experimental results contradict the theory or hypothesis, scientists often amend or discard it. This process exhibits that theories aren't absolutes but rather are continually evolving constructs subject to change based on the emergence of new evidence.
This is part of the scientific method, where theories and hypotheses are continuously tested and re-tested using experiments. It's also important to remember that evidence-based science values new findings that can be replicated and verified across multiple experiments, confirming or questioning existing theories.
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Answer:
Explanation:when happens when a parking lot is built in a wetland area? what happens is that the RUNOFF CARRYING POLLUTANT ORGANIC MATERIAL AND EXCESS NUTRIENTS FLOWS DIRECTLY INTO THE LAKE AND RIVERS this is your answer the reason is that when anything especially a parking lot is built in an area that is has the moisture from rain flood ect it pulls everything into a direction towards something that is moving downward into lake or rivers to be connected, give me a 5 star please :)
A downward arching rock layer is called syncline.
Explanation:
Syncline and anticline are words used to design folds based on the analogous ages of folded rock layers. A syncline is a fold in which the modern rocks happen in the core of a fold. Where rock layers have been changed prior to folding, such as by folding about a giant fold with a shallowly inclined axial surface, the dearest rocks now occur in the core of folds where layers slide towards the fold axis.
A downward arching rocklayer is called a syncline. It is a type of fold that is characterized by its downward-facing axis.
Synclines are typically formed when sedimentary rocks are subjected to compressional forces. The compressional forces cause the rocks to bend, forming the downward-facing axis.
Synclines are often found in sedimentary basins, which are areas where sediment has accumulated over time. The sediment is typically deposited in horizontal layers, but the compressional forces can cause the layers to bend, forming synclines.
Synclines can be identified by their characteristic shape. They are typically bowl-shaped, with the axis of the fold running through the center of the bowl.
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