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When rick is weathered and transported downstream, this process exemplifies the conservation of mass. As material breaks down and is carried away, the total mass remains constant, even as it changes form and location. This principle underscores the idea that matter is neither created nor destroyed but merely transformed and redistributed in the environment.

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When rock is weathered and transported downstream is best seen as an example of the conservation of?

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When rock is weathered and transported downstream this is best seen as an example of the conservation what?

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When rock is weathered and transported downstream this is best seen as as example of the conservation of?

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When rock is weathered and transported downstream this is best seen as example of the conservation of?

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When rock is weathered and transported downstream this best seen as an example of the conservation of?

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When rock is weathering and transported downstream this is best seen as an example of the conservation of?

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When rock is weathered and transported downstream this is best seen as an example of conversation of?

This process is best seen as an example of the conversion of mechanical energy into potential energy. The kinetic energy of the moving water impacts the rocks, breaking them down into smaller pieces. These pieces are then transported downstream where they accumulate as sediment, storing potential energy until they are deposited elsewhere.


Sediments eroded from mountainsides and transported in streams are an example of the conservation of?

Sediments eroded from mountainsides and transported in streams are an example of the conservation of mass. The total amount of sediment that is eroded from the mountainside remains constant as it is transported by streams to other locations.


Where can you find weathered mountains?

The American Appalachian mountains a a good example of weathered mountains.


What process changes sedimentary rock into igneous rock?

Physical and chemical erosion/weathering, followed by transport and finally sedimentation. Transport is not always occuring, it is possible that eroded particles are sedimentated in situ. Also, it is higly likely that during transportation, eroded particles are even further significantly eroded/weathered. For example, when a boulder is transported downstream, it's roundness increases with time/distance travelled.