i think it is limestone
It is called sedimentary rock.
When layers of sediment get squeezed together, they form a rock type called sedimentary rock. This process, known as lithification, involves the compression and cementation of sediment particles over time. Sedimentary rocks can include materials such as sandstone, shale, and limestone.
It is called sedimentary rock.
It is called sedimentary rock.
Sediment becomes solid rocks through a process called lithification, which involves compaction and cementation. Compaction occurs when sediment is squeezed together by the weight of overlying layers, while cementation happens when minerals precipitate out of water and bind grains of sediment together to form a solid rock.
The two primary causes of lithification are compaction, where sediments are squeezed together by the weight of overlying layers, and cementation, where minerals precipitate and bind sediment grains together. These processes transform loose sediment into solid rock.
Sediment layers are squeezed from above by the weight of overlying sediment, causing compaction. Compaction squeezes out air and water between the sediment particles. Minerals form as the air and water is squeezed out, cementing the particles together, and forming sedimentary rock.
The process where sediment becomes glued together is called lithification. It involves compaction and cementation of sediment particles to form sedimentary rocks over time. Pressure from overlying layers and the presence of mineral-rich fluids help bind the sediment grains together.
When layers of sediment are squeezed together to form rocks, it is called lithification. This process involves compaction and cementation of sediment particles to create solid rock formations.
It is called sedimentary rock.
Sediment layers are squeezed from above by the weight of overlying sediment, causing compaction. Compaction squeezes out air and water between the sediment particles. Minerals form as the air and water is squeezed out, cementing the particles together, and forming sedimentary rock.
Sediment becomes solid rocks through a process called lithification, which involves compaction and cementation. Compaction occurs when sediment is squeezed together by the weight of overlying layers, while cementation happens when minerals precipitate out of water and bind grains of sediment together to form a solid rock.
The two primary causes of lithification are compaction, where sediments are squeezed together by the weight of overlying layers, and cementation, where minerals precipitate and bind sediment grains together. These processes transform loose sediment into solid rock.
The process that presses sediments together is compaction. Thick layers of sediment build up gradually over millions of years. These heavy layers press down on the layers beneath them. The weight of new layers further compacts the sediments, squeezing them tightly together. The layers often remain invisible in sedimentary rock.
Sediment layers are squeezed from above by the weight of overlying sediment, causing compaction. Compaction squeezes out air and water between the sediment particles. Minerals form as the air and water is squeezed out, cementing the particles together, and forming sedimentary rock.
The process where sediment becomes glued together is called lithification. It involves compaction and cementation of sediment particles to form sedimentary rocks over time. Pressure from overlying layers and the presence of mineral-rich fluids help bind the sediment grains together.
The process you're referring to is called compaction. Compaction occurs as the weight of overlying sediment squeezes the grains of sediments together and reduces the volume of pore space between them.
The process you are referring to is called compaction. Compaction occurs when the weight of overlying sediments forces out water and air, reducing the volume of the sediment and causing grains to come closer together.
The squeezing of layers of sediment is called compaction. This process reduces the volume of sediment and removes water between particles, resulting in the formation of sedimentary rocks.
folded mountains