earthflow & mudflow
Creep and solifluction are examples of slow mass movement processes. Creep is the slow, continuous movement of soil and rock downhill, while solifluction is the slow movement of thawed soil over frozen ground in areas with permafrost.
Water can increase the likelihood of mass movements by weakening the slope material through saturation, leading to landslides and debris flows. For example, heavy rainfall can saturate the soil on a steep slope, triggering a landslide. In another case, melting snow can infiltrate cracks in rocks, expanding them and causing a rockfall.
The two fastest forms of mass wasting are rockfalls and landslides. Rockfalls occur when rocks or debris fall rapidly downhill due to gravity, while landslides involve the sudden movement of a mass of rock, soil, and debris down a slope. Both processes can happen quickly and cause significant damage.
Examples of inputs to Earth's system include solar radiation from the Sun, which provides energy for various Earth processes such as weather and climate dynamics; and external debris like meteoroids and interstellar dust, which occasionally enter the Earth's atmosphere and contribute to the planet's mass.
Two factors that influence mass movements are gravity, which acts as the driving force behind the movement of materials downslope, and the slope angle of the terrain, which determines the stability of the material and the likelihood of it moving. Additional factors can include the presence of water, vegetation cover, and the type of material involved.
Creep and solifluction are examples of slow mass movement processes. Creep is the slow, continuous movement of soil and rock downhill, while solifluction is the slow movement of thawed soil over frozen ground in areas with permafrost.
rapid eyes movement (REM) and non rapid eyes movement (NREM)
Violent motion refers to a forceful or rapid movement. Two examples include a car crash where the vehicles collide with high impact, and a heavy object falling from a height hitting the ground forcefully.
A Mass & A Pendulum
Mass movement and runoff.
two types are movement and reproduction,
Mass: Pound and Gram Volume: Gallon and Litre.
Two factors that affect mass movement are the steepness of the slope and the amount of water present in the soil or rock. Steeper slopes increase the likelihood of mass movement due to gravity, while excessive water can decrease the friction between particles, making the material more unstable.
Some examples would be avalanche, landslide, debris flow, mudflow, and a sinkhole. Gravitational eroson is caused by gravity in contrast to the physical movement of wind and water required for other types of soil erosion. This involvs mass wasting and smaller scale erosion. Two types of mass movements are slump and creep
Your height (centimetres) and mass (kilograms).
Population of a country. Mass of the sun.
Gravity erosion, also known as mass wasting, includes various processes where gravity causes the movement of rock and soil downhill. Examples of gravity erosion include landslides, rockfalls, creep, and slumps. Landslides are rapid downslope movements of rock and soil, while rockfalls involve the free fall of detached rocks. Creep is the slow, continuous movement of soil downhill, and slumps are rotational slides where a mass of rock and soil moves along a curved surface.