Mudslides and landslides.
Kinetic energy can be expressed by the equation: Ek= ½ mv2. Therefore in addition to speed (v), kinetic energy is also dependent on mass (m).
Weight is dependent on mass. Weight is the force exerted on an object due to gravity, and it is directly proportional to an object's mass. Mass, on the other hand, remains constant regardless of location in the universe.
The mass of water at 25 degrees Celsius, without knowing the volume, cannot be determined. Mass is dependent on both volume and density, and without the volume of water given, it is not possible to calculate its mass.
if the steepness of a slope exceeds the stable angle, mass movements become more likely.
kilograms is a measure of weight. Litre is a measure of mass. theyre not compatible terms. also, the weight of water, specifically, is dependent on its temperature.
Mudslides and landslides.
Mudslides and landslides.
The mass movement that makes the most changes in Earth's surface is not air, or water, but a landslide. The four mass movements are landslide, slump, creep, and mudslide.Old Answer: air, water.
Kinetic energy can be expressed by the equation: Ek= ½ mv2. Therefore in addition to speed (v), kinetic energy is also dependent on mass (m).
The mass movement of surface water is typically referred to as runoff, which is the flow of water over land surfaces towards rivers, lakes, and oceans. This movement can occur due to rainfall, snowmelt, or other forms of precipitation. Runoff plays a crucial role in the water cycle and can contribute to erosion and sediment transport.
Rapid mass movements occur suddenly and can travel at high speeds due to factors like steep slopes or heavy rainfall, leading to landslides, rockfalls, or avalanches. Slow mass movements, such as soil creep or solifluction, involve gradual downslope movement of material over an extended period, often influenced by factors like gravity and water infiltration. While rapid mass movements pose immediate risks and can cause significant damage, slow mass movements are generally more subtle but can still contribute to landscape changes over time.
Weight is dependent on mass. Weight is the force exerted on an object due to gravity, and it is directly proportional to an object's mass. Mass, on the other hand, remains constant regardless of location in the universe.
The mass of water at 25 degrees Celsius, without knowing the volume, cannot be determined. Mass is dependent on both volume and density, and without the volume of water given, it is not possible to calculate its mass.
Water and sediment are common substances that can fill the pores in sediments and act as triggers for mass movements. When the pores become saturated with water, it can decrease the strength and stability of the sediment, leading to events like landslides or debris flows.
The three main types of mass movements are landslides (movement of rock, soil, and debris down a slope), mudflows (rapid flow of a mixture of water, rock, soil, and debris), and rockfalls (sudden collapse or falling of rocks from a steep slope). These mass movements can be triggered by factors such as heavy rainfall, earthquakes, or human activities.
Mass movements occur when gravity acts on a large amount of material on a slope, causing it to move downhill. Factors such as steepness of the slope, type of material, amount of water content, and vegetation cover can trigger mass movements like landslides, rockfalls, or debris flows. Once the material becomes unstable and the resisting forces are overcome by gravity, a mass movement occurs.
This depends for intensive (not dependent of mass) and extensive (dependent of mass) properties.