Natural Processes:

* Wind Erosion: Wind can pick up and transport small soil and rock particles, especially in arid or dry environments. This is called aeolian transport and can lead to the formation of dunes and loess deposits.

* Water Erosion: Moving water, such as rivers and streams, can erode and carry away soil and rock particles. This can lead to soil loss and the formation of canyons and valleys.

* Glacial Erosion: Glaciers can pick up and carry large amounts of soil and rock, transporting them great distances and depositing them as they melt. This creates glacial valleys, moraines, and other landforms.

* Volcanic Activity: Volcanic eruptions can eject ash, rock fragments, and other materials into the atmosphere, which can settle on the surrounding land.

* Tectonic Plate Movement: Earthquakes and volcanic activity associated with plate movements can cause rocks and soil to shift and rise.

Human-Induced Processes:

* Construction: Construction activities, such as excavation and grading, can disturb the soil and cause particles to become airborne.

* Agriculture: Agricultural practices, such as tilling and harvesting, can lead to soil erosion and the movement of particles.

* Mining: Mining operations can create large piles of loose soil and rock, which can be easily dispersed by wind or water.

* Pollution: Air and water pollution can affect soil and rock composition, making them more susceptible to erosion and lifting.

Other Factors:

* Gravity: While not directly causing particles to rise, gravity plays a role in erosion by pulling soil and rock downhill, where they can be picked up by wind or water.

* Particle Size: Smaller particles, such as silt and clay, are more easily lifted by wind and water than larger rocks.

It's important to note that the specific cause of soil and rock particle rise depends on the context and specific conditions.