it changes to marble....
No. Limestone changes to Marble when it undergoes intense heat and pressure.
Oh, dude, limestone metamorphoses into marble. It's like the glow-up of rocks, you know? Limestone is just like, "I'm tired of being basic, I'm gonna become fancy marble now."
The formation of the Superior limestone and the Columbia limestone likely involved significant geological processes such as changes in sea levels, sedimentation patterns, and tectonic activities. Over time, the environment shifted from the conditions that produced the Superior limestone, characterized by shallow marine environments, to the Columbia limestone, which may have developed under different sedimentary conditions or during a different geological period. These transitions often reflect broader climatic changes and evolving ecosystems that influenced the deposition of limestone in various geologic settings.
erosion, acid rain...
Limestone is considered the parent rock of marble because marble forms from the metamorphism of limestone. Under heat and pressure, the mineral composition of limestone changes, resulting in the formation of marble. This transformation gives marble its distinct crystalline structure and unique appearance while retaining some of the original characteristics of limestone.
When limestone, which is composed of calcium carbonate, reacts with vinegar (which contains acetic acid), a chemical reaction occurs that produces carbon dioxide gas. This gas bubbles through the solution and breaks the limestone down into calcium acetate, water, and carbon dioxide. The physical appearance of the limestone changes to a powdery form due to the breakdown of the solid structure as it dissolves.
Limestone is cooled in a dry argon atmosphere to prevent any unwanted reactions or changes in the limestone due to exposure to moisture or oxygen. The dry argon atmosphere helps maintain the integrity of the limestone and ensures that the cooling process is conducted under controlled conditions.
The formation of Superior Limestone and Columbia Limestone represents a significant geological transition during the Late Mississippian to Early Pennsylvanian periods. The Superior Limestone was primarily deposited in a shallow marine environment, characterized by warm, clear waters that favored the accumulation of carbonate materials. In contrast, Columbia Limestone formed later under different conditions, influenced by changes in sea level and sediment supply, leading to a more varied depositional environment that included both marine and non-marine influences. This shift reflects broader tectonic and climatic changes occurring during this time in Earth's history.
Limestone changes into marble through a process called metamorphism. This process involves the recrystallization of the calcite mineral in limestone due to high pressure and temperature deep within the Earth's crust. This transforms the limestone into a more compact, harder, and denser rock known as marble.
Snow itself does not directly affect limestone; however, the freeze-thaw cycles associated with snow and cold temperatures can lead to weathering of limestone. Water can seep into cracks in the limestone, freeze, and expand, causing the rock to break down over time. Additionally, the acidity of snowmelt can contribute to the chemical weathering of limestone, especially if it contains pollutants. Overall, while snow doesn't harm limestone directly, its effects through temperature changes and chemical processes can lead to deterioration.
When vinegar is spotted onto chalk or limestone, it creates a chemical reaction that dissolves the calcium carbonate in the rock. This reaction is not reversible as it breaks down the structure of the rock and changes it permanently.
concrete is formed from limestone by the combustion of the limestone (heating of the limestone)!