Sedimentary--Limestone Metamorphic--Marble
Limestone is a sedimentary rock that is highly susceptible to chemical weathering by acid rain due to its high calcium carbonate content. Marble, a metamorphic rock derived from limestone, is also highly affected by acid rain because of its similar composition. Both rocks can undergo dissolution and erosion when exposed to acidic rainwater.
The metamorphic rock marble would react with hydrochloric acid.
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.
The sedimentary rock that forms calcium carbonate and fizzes in acid is likely limestone. Limestone is a common sedimentary rock primarily composed of calcite, a form of calcium carbonate. When exposed to acids such as vinegar or hydrochloric acid, limestone will fizz or effervesce due to the release of carbon dioxide gas.
Limestone is a sedimentary rock that is highly susceptible to chemical weathering by acid rain due to its high calcium carbonate content. Marble, a metamorphic rock derived from limestone, is also highly affected by acid rain because of its similar composition. Both rocks can undergo dissolution and erosion when exposed to acidic rainwater.
metamorphic rocks sedimentary rocks and igneous
Dolomite can be chemically weathered by rainwater through a process called carbonation. Rainwater, which is slightly acidic due to dissolved carbon dioxide, reacts with dolomite to form carbonic acid. This acid then reacts with the dolomite, dissolving it and releasing calcium and magnesium ions into the rainwater.
Quartzite is a common metamorphic rock that does not react with hydrochloric acid due to its high quartz content. This rock forms from the metamorphism of sandstone and is composed primarily of quartz grains that are chemically resistant to acid.
Rainwater is naturally slightly acidic. The acid in rainwater reacts chemically with the calcium carbonate of limestone, dissolving it. The result is chemically weathered limestone, karst terrains, and cave structures.
Carbonic acid
air oxidation, groundwater, and acid precipitation
No. Only sedimentary rocks containing carbonate minerals will bubble with acid.
Limestone is the type of rock that is chemically weathered by acidic groundwater, leading to distinctive features such as karst landscapes, sinkholes, and caves. The acidic groundwater, often containing carbonic acid formed from carbon dioxide in the soil, dissolves the calcium carbonate in limestone, resulting in the erosion and creation of these geological formations. Over time, this process can lead to significant alterations in the landscape.
Limestone and chalk get easily weathered by acid.
living organism and acid rain?
Pure Hydrochloric Acid is a gas.