Heat and pressure
A what rock...?Limestone is sedimentary - the other two classes are igneous and metamorphic.Limestone will metamorphose in suitable conditions of heat and pressure, into marble.
Limestone and dolostone can metamorphose into marble.
No, granite cannot become marble. Granite and marble are two distinct types of rocks formed under different geological conditions. Granite is an igneous rock formed from the cooling of molten rock, while marble is a metamorphic rock formed from the recrystallization of limestone.
Limestone and marble.
Limestone and marble are two types of rock that are easily weathered by carbonic acid, which is a common acid found in rainwater. Over time, carbonic acid dissolves these rocks, leading to the formation of caves, sinkholes, and other karst topography features.
Limestone and marble are primarily composed of calcite, a mineral that reacts with acid by producing bubbles. This reaction is commonly used to identify these rocks in the field.
Marble is a metamorphic rock with a parent rock of limestone or dolostone and is formed by natural processes by heat and pressure. The heat may be derived by proximity to a magmatic intrusion or from depth of burial.
The two rocks that are primarily composed of a mineral that bubbles with acid are limestone and marble.
Two types of limestone are chalk, which is a soft, white sedimentary rock composed of the skeletal remains of marine organisms, and travertine, which is a form of limestone deposited by mineral springs, often found in caves and near hot springs.
The two most common non-foliated metamorphic rocks are marble, formed from the metamorphism of limestone, and quartzite, formed from the metamorphism of quartz sandstone.
Limestone and marble are two types of rocks that can be easily weathered by carbonic acid. This is because carbonic acid reacts with the calcium carbonate in these rocks, leading to the formation of calcium bicarbonate and ultimately causing dissolution and erosion of the rock.
Limestone and marble are two types of rocks that are easily weathered by carbonic acid due to their high calcium carbonate content. Over time, carbonic acid dissolves these rocks, leading to the formation of caves, sinkholes, and other karst landscapes.