Limestone Granite Weathering

The rounded shapes are pillows formed at depth in the granitic magma roots rub against the edges of the granite burrowing animals eat away parts of the granite weathering removes corners and edges as in spheroidal weathering.

Limestone granite weathering.

Hard rocks such as granite weather more slowly than softer rocks such as limestone. Weathering is the breakdown of rock by physical chemical or biological processes. Limestone areas are predominantly affected by chemical weathering when rainwater which contains a weak carbonic acid reacts with limestone. Limestone is a sedimentary rock created from the remains of dead sea creatures and is predominately made up of calcium carbonate.

Mechanical weathering is weathering done by trees ice etc. Granite vs limestone characteristics. Thus limestone is not easily soluble in pure water but carbonated water dissolves the rock effectively. Though some rocks look identical they have certain characteristics which distinguish them from others.

This greatly shows that out of the three rock samples being tested against limestone that granite will most likely show less weathering through the duration of the experiment. B hydration and hydrolysis. Many horizontal and vertical cracks run through limestone. Rainwater can get acidic because of the carbonic acid that it contains.

Limestone being sedementary is sheety and softer than granite which is igneous and harder having less cracks so it weathers more slowly. These two processes indicate the direct attack of atmospheric moisture on the individual minerals of a rock that ultimately affect its structural make up. Carbon dioxide from the respiration of animals and ourselves is one cause of increased carbon dioxide in the atmosphere. Granite vs limestone characteristics assist us to distinguish and recognize rocks.

Karst is landscape formed from the weathering of limestone. Limestone is a rock which is more prone to especially chemical weathering than other types of rocks such as granite. Why does weathering of granite bedrock produce rounded shapes. This causes the limestone to dissolve.

Limestone gets pitted and porous due to chemical weathering. It begins when a crack made larger by freeze thaw and tree roots growing larger until the rock splits. A gravestone made of granite will therefore resist fracturing cracking and chipping longer than a sandstone marker found in the same location. Although the granite is now starting to show some signs of decay it took over a hundred years and exposure to aggressive water to do so.

Differential weathering happens when softer rocks weathers away and leaves harder more resistant rock behind. Granite is extremely hard and less affected by the freeze thaw cycle the forces of abrasion and the surface exfoliation processes that are all a part of physical weathering.