How do weathering, erosion, and deposition work together to change earth’s surface?

Deposition breaks down rock, erosion moves rocks, and weathering places rocks in a new location.

Weathering breaks down rock, deposition moves rocks, and erosion places rocks in a new location.

Weathering breaks down rock, erosion moves rocks, and deposition places rocks in a new location.

Erosion breaks down rock, weathering moves rocks, and deposition places rocks in a new location.

Weathering breaks down rock, erosion moves rocks, and deposition places rocks in a new location.

Over a period of a hundred years, how could it be determined how the shape of a structure on earth has changed using topographical maps?

The original map would become larger so that more detailed structures could be observed.

The changes will not be able to be determined through topographical maps because the loops will remain the same.

Comparing the two images taken from space of the structure would be how the differences are identified.

The shape of the loops on the map would be changed to imitate the new shape of the structure.

The correct answer is: Weathering breaks down rock, erosion moves rocks, and deposition places rocks in a new location.

Now, let me explain in more detail how weathering, erosion, and deposition work together to change Earth's surface.

Weathering is the process by which rocks are broken down into smaller pieces by various physical, chemical, or biological processes. This can happen due to factors like changes in temperature, moisture, wind, or the action of plants and animals. Weathering can occur through processes such as freezing and thawing, abrasion, or the chemical decomposition of rocks.

Once the rocks have been weathered, erosion comes into play. Erosion is the transportation of the weathered rock fragments or sediments by agents like water, wind, ice, or gravity. For example, water erosion occurs when rivers, streams, or ocean waves carry away sediments, while wind erosion occurs when strong winds sweep away loose soil particles.

Finally, deposition is the process by which the eroded materials are dropped or settled in a new location. This can occur when the velocity of the transporting agent decreases and can no longer carry the sedimentary material. As a result, the sediments settle on the ground or accumulate in bodies of water, such as rivers, lakes, or oceans. Over time, these deposited sediments may become compacted and cemented together, forming new layers of rock.

So, in summary, weathering breaks down rocks into smaller pieces, erosion transports these fragments, and deposition places them in new locations. Together, these processes continuously shape and change the Earth's surface over time.

Comparing the two images taken from space of the structure would be how the differences are identified.