Depending on the minerals in their composition, some rocks are harder than others. Rocks that contain minerals with higher ratings on the Mohs scale are harder, and would erode more slowly than other rocks.
Because of different heights & positions, environments, situations & conditions, angles directions velocities etc of the weather/etc, the seeming randomness of weather & activity in space affecting the weather, etc.
Differential weathering occurs when rocks made of different minerals weather at different rates, resulting in uneven surfaces or shapes. This process is common in regions with varied mineral composition and can lead to the formation of unique landscapes, such as hoodoos in desert environments.
Erosion rates depend on the composition of the rocks and how they are attacked by the environment.Different kinds of rocks have different composition and will erode at different rates.Rocks in different places will be affected differently by wind, water, ice, rain, pollutants, etc. and so they will erode at different rates.
Rocks cool at different rates due to how they were formed if they were formed intrusively or extrusively Examples of different igneous rocks that form differently is Granite and Gabbro form the same but different from Rhyolite.
Strike slip fault
Erosion rates depend on the composition of the rocks and how they are attacked by the environment.Different kinds of rocks have different composition and will erode at different rates.Rocks in different places will be affected differently by wind, water, ice, rain, pollutants, etc. and so they will erode at different rates.
because they didn't now why the weather would affect the rocks. and they didn't now about this at the time
Because of different heights & positions, environments, situations & conditions, angles directions velocities etc of the weather/etc, the seeming randomness of weather & activity in space affecting the weather, etc.
Differential weathering causes rocks of different hardness to weather at different rates. If a rock is softer than the surrounding rock, it will weather more quickly, resulting in differential erosion that highlights the contrast in hardness. Over time, this pattern can help in determining the relative hardness of the rocks.
depends on conditions and type of rock
One main factor that causes bedrock to weather at different rates is the type of rock it is made of. Rocks like limestone and sandstone are more susceptible to weathering compared to harder rocks like granite. Additionally, climate plays a role, with areas experiencing more frequent freeze-thaw cycles or higher rainfall typically experiencing faster weathering.
Erosion rates depend on the composition of the rocks and how they are attacked by the environment.Different kinds of rocks have different composition and will erode at different rates.Rocks in different places will be affected differently by wind, water, ice, rain, pollutants, etc. and so they will erode at different rates.
Differential weathering occurs when rocks made of different minerals weather at different rates, resulting in uneven surfaces or shapes. This process is common in regions with varied mineral composition and can lead to the formation of unique landscapes, such as hoodoos in desert environments.
strike slip fault
The two factors that cause differential weathering are variations in rock composition and variations in rock structure. Rocks with different mineral compositions and structures will weather at different rates, leading to differential weathering processes.
Rocks cool at different rates due to how they were formed if they were formed intrusively or extrusively Examples of different igneous rocks that form differently is Granite and Gabbro form the same but different from Rhyolite.
Rocks at the peak of a mountain are exposed to more extreme weather conditions, like temperature fluctuations, intense sunlight, and strong winds, leading to increased physical and chemical weathering processes. In contrast, rocks at the base of a mountain are usually shielded from such harsh conditions, resulting in slower weathering rates.