pressure, heat, time
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.
Limestone, marble, and chalk are all types of sedimentary rocks composed mainly of calcite. Limestone is the precursor to marble when subjected to high pressure and temperature. Chalk is a softer form of limestone made up of microscopic marine organisms.
When pure limestone undergoes metamorphism, it can transform into marble. Marble is a metamorphic rock composed primarily of calcite crystals that have recrystallized under high pressure and temperature conditions.
Marble is a metamorphic rock that forms from the recrystallization of limestone or dolostone under high pressure and temperature conditions. When limestone or dolostone undergoes metamorphism, the calcite or dolomite minerals recrystallize to form marble. Therefore, the primary rocks that change into marble are limestone and dolostone.
Marble is a metamorphic rock formed from limestone that has undergone intense heat and pressure deep within the Earth's crust. The process of metamorphism recrystallizes the original minerals in limestone to create the distinct crystalline structure and smooth texture of marble. Marble is valued for its beauty and is commonly used in architecture and sculpture.
Limestone - sedimentary deposition of calcarious marine organisms. Marble - compressed (metamorphosed) limestone.
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.
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.
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.
Limestone metamorphoses into marble.
The metamorphic form of limestone is marble. Marble is created when limestone undergoes intense heat and pressure within the Earth's crust, causing the minerals in the limestone to recrystallize into a harder, denser rock with a variety of colors and patterns. Marble is commonly used in architecture and sculpture due to its elegance and durability.
Marble is metamorphosed limestone.
When limestone is heated under pressure, it forms marble. This process, known as metamorphism, occurs when the mineral calcite in the limestone recrystallizes into the interlocking calcite crystals that compose marble.
Limestone can metamorphose into marble, a regional metamorphic rock, or into skarn, a contact metamorphic rock.
Marble is made from limestone.
Limestone, marble, and chalk are all types of sedimentary rocks composed mainly of calcite. Limestone is the precursor to marble when subjected to high pressure and temperature. Chalk is a softer form of limestone made up of microscopic marine organisms.
When limestone undergoes metamorphism, it produces the metamorphic rock called marble. This process involves recrystallization of the calcite mineral in limestone to form interlocking crystals of calcite in marble.