The process of breaking down the rock material without changing its chemical composition is called mechanical weathering.
Physical weathering!
The changing of a liquid to a gas without boiling is called evaporation. It occurs at the surface of the liquid when molecules gain enough energy to break free and become a gas.
The amount of pressure an object can handle without changing is called its elastic limit. Beyond this point, the object will undergo permanent deformation or break.
tie break
Mechanical weathering refers to the process where rocks break down physically without changing their chemical composition. This can include processes like freezing and thawing, abrasion, or root wedging.
The energy required to create a phase change without changing the temperature is known as latent heat. This energy is needed to break the intermolecular forces holding the molecules in a particular phase, such as solid to liquid or liquid to gas, without increasing the temperature of the substance.
The process of changing from a solid to a gas directly is called sublimation. It occurs when the solid absorbs enough heat energy to break the intermolecular forces holding its particles together, allowing them to escape into the gaseous state without passing through the liquid phase.
Because of the distributive property of multiplication over addition.
Brittleness refers to the tendency of a material to fracture or break when subjected to stress, whereas malleability is the ability of a material to deform under compression without breaking. In simple terms, a brittle material breaks easily under pressure, while a malleable material can be shaped without breaking.
Gas changing into a solid is called deposition, where gas molecules lose energy and come together to form a solid. On the other hand, solid changing into a gas is called sublimation, where solid molecules gain enough energy to break free and become a gas without passing through the liquid state.
The process is called mechanical weathering. It involves the physical breakdown of rocks into smaller fragments without altering their chemical composition. Factors such as temperature changes, frost action, and abrasion contribute to this type of weathering.
Spiders.