Acid rain
An example of a non-physical weathering process is chemical weathering, where rocks are broken down by chemical reactions rather than physical forces like temperature changes or abrasion.
Mechanical weathering is physical changes that break down and/or cracks the rock, such as ice wedging, temperature changes, root growth, or animal activity. Chemical weathering is a chemical change that changes the chemicals of the substance to make a new one. Examples of chemical weathering include oxidation, acid rain, hydration, and carbonation.
Chemical weathering is the type of weathering caused by chemical reactions in water. This process involves the breakdown of rocks and minerals through chemical reactions with water, leading to the alteration of the rock's composition. Examples of chemical weathering processes in water include hydration, hydrolysis, and oxidation.
Chemical weathering is the breakdown of rocks through chemical reactions. Examples include dissolution, oxidation, and hydrolysis. It is likely to occur in humid climates with warm temperatures and abundant rainfall, as these conditions promote faster chemical reactions.
Mechanical weathering examples include frost wedging, where water seeps into cracks in rocks and freezes, expanding and breaking the rock. Chemical weathering examples include acid rain, where pollutants in the atmosphere react with water to form acidic precipitation that can erode rock surfaces over time.
Chemical weathering is the type of weathering that involves a chemical change in some of the minerals in a rock. This process breaks down the rock into smaller pieces by altering its mineral composition through chemical reactions with substances like water, oxygen, or acids.
There are two types of weathering: chemical and physical. Chemical weathering is said to occur when the chemical compounds of rocks are changed. Physical weathering happens due to wind, rain, or other natural occurrences.
Two examples of weathering are mechanical weathering, such as when rocks are broken down into smaller pieces by physical forces like wind or water, and chemical weathering, which occurs when rocks are broken down by chemical reactions like oxidation or dissolving.
well it is very hard to break up bedrock, but the main process that does is weathering. You have two seperit kinds of weathering. The first one is Chemical Weathering. Chemical weathering is when weathering effects the exterior. two examples are rust and leaching. The second type of weathering is Mechanical Weathering. This effects rocks physically. two examples are abrasion and erosion.SO THE MAIN ANSWER WOULD BE WEATHERING. THE TYPE OF WEATHERING, MECHANICAL WEATHERING, THE PROCESS, ABRASION (well there is more than that but that is the most common situation)
mechanical weathering and chemical weathering are related because their both are types of weathering
Weathering I think
Some examples of chemical weathering include the breakdown of rocks through processes such as oxidation, hydrolysis, and dissolution. This can result in the formation of new minerals or the weakening of rock structures over time. Acid rain can also contribute to chemical weathering by dissolving minerals in rocks.