Large rocks are left behind and dry soil is transported away. B- Dry soil is transported away in a process called deflation
Erosion can wear away all types of rocks, but it is more effective on softer rocks such as sandstone and limestone compared to harder rocks like granite and basalt. The rate of erosion depends on the rock's hardness, composition, and resistance to weathering.
When hard rocks break and wear away, they often form sediment particles that can be carried and deposited by water, wind, or ice. These sediments can then accumulate and compact over time to form new sedimentary rocks.
Scientists discovered that rocks farther away from the mid-ocean ridge were older than those closer to it through radiometric dating of the rocks. By analyzing the age of the rocks using isotopes with known half-lives, they were able to determine that the rocks get progressively older as you move away from the ridge due to the process of seafloor spreading.
The process called weathering is responsible for the breaking up and wearing away of the Earth's rocks. The broken up rocks are then carried away by the process of erosion.
Erosion and it eroded away
Rocks wear away because slowly,wind/water take away tiny pieces of dust and slowly it gets worn away.
No, though they are often confused. Here are the definitions:Weathering: the wearing away of rocks in situErosion: the wearing away and taking away of rocks
Wearing away of rocks is called weathering.
A canyon can be formed where the water eats away on the rocks.
The wind, can soften rocks and blow it away also acid rain can erode rocks with acid and eventually melt it away.
wears them away
Erosion
Abrasion
Rocks get eaten away by weathering and erosion
Large rocks are left behind and dry soil is transported away. B- Dry soil is transported away in a process called deflation
Scientists discovered that rocks farther away from the mid-ocean ridge were older through radiometric dating of the rocks. By analyzing the age of the minerals within the rocks, researchers found that the rocks closest to the ridge were younger, while those farther away were older, supporting the theory of seafloor spreading.