its going to brake
The type of weathering that does not alter the chemical composition of the rock is called physical weathering. The acid weathering usually alter the chemical composition of a rock.
Rock exposed to very high temperature and pressure will soften or melt.
Weathering tends to attack the outermost layer of a rock, known as the rock surface or rind, most rapidly. This layer is more exposed to the elements and is therefore more susceptible to weathering processes such as erosion, chemical weathering, and physical weathering.
Pressure on them is released, which can cause pressure-release mechanical weathering. Exposure of an uplifted rock to the surface will fully expose the rock to the effects of mechanical and chemical weathering--basically a rock rot.
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.
Chemical Weathering.. because as rocks exposed to acid rains like limestones, it slowly dissolve and change into a new form
The answer will depend on what the chemical is! A rock exposed to nitrogen, under normal temperature and pressure will be no different from what it would be otherwise!
Chemical Weathering.. because as rocks exposed to acid rains like limestones, it slowly dissolve and change into a new form
it will be influenced, because chemical happens in warm wet area, while are only happens in cold areas :) :) :) :) ONLY A DIRECTIONER WILL IMPROVE IT FOR PUTTING DIRECTIONER FOREVER AND PAULWAYS :) :) :) :) ~Alexia Escutia
Fracturing increases the surface area of a rock exposed to weathering.
Chemical weathering of rock occurs when minerals within the rock are broken down or altered through chemical reactions. This can lead to the formation of new minerals, decomposition of the rock's structure, or dissolution of the rock into smaller particles. Over time, chemical weathering can weaken the rock and cause it to disintegrate.
Physical weathering breaks rock down into much smaller pieces and gives the original rock a much greater surface area which, when exposed to chemical agents such as carbonic acid, reacts at a much faster rate than it would had the larger rock not undergone physical weathering.
Warm, wet, tropical climates speed chemical weathering of rock.
When a rock is exposed to weather, it can undergo weathering processes like physical breakdown due to temperature changes, chemical alteration from rainwater or acids, and biological weathering from plant roots or burrowing animals. Over time, these weathering processes can cause the rock to erode and break down into smaller pieces.
The surface area of an exposed rock directly impacts its rate of weathering. A rock with a larger surface area will weather more quickly because there is more area for chemical and physical weathering processes to act upon. As the surface area increases, the rock is more vulnerable to breakdown and erosion processes, leading to faster weathering.
The process that creates soil from bare rock is called"weathering". The chemical and physical processes of [weathering] transform igneous rock.
Unloading contributes to weathering by relieving pressure on rock layers, which can cause expansion and fracturing of the rock. This can lead to the breaking off of outer layers of rock, increasing surface area exposed to weathering processes such as erosion and chemical weathering.