sand
The cementing material could be calcite, clay minerals, iron minerals, or quartz in a clastic sedimentary rock.
Sand is a solid due to its molecular arrangement.
The metamorphic rock that lacks mineral grains with long axes in one direction is called marble. Marble is formed from the metamorphism of limestone or dolomite, and its grains do not exhibit a preferred orientation or alignment. It often has a smooth and uniform appearance, making it a popular material for sculptures and architectural purposes.
when a material changes from a solution into another material what is thes prosses called
A consolidated rock is called a "lithified" rock. This means that loose sediment has been compacted and cemented together to form a solid rock mass.
Loose rock material is called detritus.
Sand
Talc
Talc
coal and limestone
Loose rock material is called detritus.
Sedimentary rock, though that category also includes rocks formed when a cementing material precipitates out of groundwater between the grains.
The particles of minerals or other rocks that make up a rock are called grains or crystals. These grains can vary in size and shape based on how the rock was formed and the types of minerals present within it.
The loose material is called sediment. It may include bits of rock, minerals, and organic material like plant and animal remains. This sediment can accumulate in layers over time and eventually become sedimentary rock through processes like lithification.
The loose material on the surface of the Earth is called "regolith." Regolith includes soil, sand, gravel, and other broken rock particles that cover solid rock.
It is false that the loose material on Earth's surface that contains weathered rock particles and humus is bedrock. The loose weathered material on Earth's surface in which plates can grow is soil.
Rock