Calcite.
Sedimentary rock and igneous rock would most likely have a zone of contact metamorphism between them. When molten magma intrudes into the surrounding rock, the heat and fluids released can alter the mineral composition of the adjacent rocks, leading to contact metamorphism.
Sedimentary rock, such as sandstone, is most likely formed from the compaction and cementing of particles together. As layers of sediment accumulate and are compressed over time, the particles are gradually cemented together by minerals, creating a solid rock.
Sedimentary rocks, such as sandstone, shale, and limestone, are most likely to result from the compaction and cementation of particles. These rocks form through the accumulation and lithification of sediments that have been weathered and eroded from pre-existing rocks.
Yes, rocks are typically formed through the process of compaction and cementation. This involves the settling and compression of mineral or organic particles over time, leading to the formation of solid rock through the binding of these particles by natural cementing agents.
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Calcite is the most likely mineral to display effervescence when treated with dilute acid. The acid reacts with the calcium carbonate in calcite, releasing carbon dioxide gas, which causes the mineral to bubble or fizz.
The mineral that is colorless and fizzes with acid is likely calcite, which is a type of carbonate mineral. When calcite comes into contact with acid, such as vinegar, it will bubble or effervesce due to the carbon dioxide gas being released.
Sandstone. Sandstone is a sedimentary rock - which is the only type of rock which can contain fossils.
As sandstone is a sedimentary rock formed from grains of sand over millions of years), applying heat and pressure is likely to pulverise the sandstone.
yes
Sedimentary rock and igneous rock would most likely have a zone of contact metamorphism between them. When molten magma intrudes into the surrounding rock, the heat and fluids released can alter the mineral composition of the adjacent rocks, leading to contact metamorphism.
Sedimentary rocks are most likely to contain minerals that have not been changed, as they are formed from the accumulation and cementation of materials without undergoing high temperatures or pressures that could alter their mineral composition. Examples include sandstone and limestone.
Sedimentary rock like sandstone
More than likely................a fart.
Big Foot
shale and sandstone
The internal atomic structure of a mineral most likely determines its physical and chemical properties, such as hardness, color, cleavage, and crystal shape. It also influences how the mineral interacts with its environment and how it behaves in different conditions.