a seashell doesn't teachnally turn in to a limestone if it didit would take a lot of minerals and heat,pressure
Marble is the rock that results from the metamorphism of limestone. Through the process of heat and pressure, the calcium carbonate in limestone recrystallizes to form marble with a characteristic crystalline structure and unique patterns.
A limestone scar is a natural geological feature formed by the erosion of limestone rock, typically in upland areas. It often results in a steep cliff or slope that is characterized by rocky outcrops and ledges. Limestone scars form over long periods of time due to the dissolution of the rock by chemical weathering processes.
Marble can turn back into limestone through a process called metamorphism. When subjected to high pressure and temperature underground over long periods of time, the minerals in marble can recrystallize and rearrange to form limestone. This transformation occurs in the Earth's crust, where the conditions favor the alteration of marble back into limestone.
The metamorphic form of limestone is marble. Marble is created when limestone is subjected to high pressure and heat over time, causing it to recrystallize into a harder and denser rock with a characteristic crystalline texture.
Yes, limestone is a carbonate rock composed mainly of the mineral calcite, which is a form of calcium carbonate.
How long does it take to drive from limestone maine to quebec canada
it takes thousands of years for acid rain to corrode limestone.
it takes about 15 to 20 min to dissolve
it depends on the amount of rain received in the area because of soil erosion but it has known to be up to 100,000 years in the limestone caves in Naracoorte
Chemical limestone can form when calcite is dissolved.
That's extremely variable and specific to each cave, but you have to think in tens or hundreds of thousands of years.
it rains and sinks into limestone and over to starts to corrode at the vulnerable limestone
limestone forms from skeletons and shells
Limestone - sedimentary deposition of calcarious marine organisms. Marble - compressed (metamorphosed) limestone.
Grikes form through the chemical and physical weathering of limestone bedrock by the dissolving action of water. Over time, this weathering process creates deep grooves or crevices in the limestone, resulting in the characteristic appearance of grikes in limestone pavement landscapes.
Chert, a form of quartz, can form as beds or nodules in limestone or dolostone.
Limestone is the rock that is squeezed and heated to form marble. The high pressures and temperatures cause the limestone to recrystallize and become the metamorphic rock known as marble.