A sedimentary rock formed from sand deposits is called a 'Sandstone' or generically a 'Psammite'.
Sedimentary rock is the rock formed as a result of deposits from weathering and erosion. Sedimentary rock can be millions of years old.
The sedimentary rock formed from tiny particles of clay in thin, flat layers is called shale. I hope this was helpful:)
The sedimentary rock formed from clay deposits is called shale. Shale is composed of very fine particles of clay minerals that have been compressed and compacted over time. It commonly has a layered structure due to the alternating sequences of clay-rich and silt-rich layers.
Sedimentary rock, such as sandstone or shale, is often formed from soil deposits carried by moving water from rivers or streams. These sediments accumulate, compress, and cement over time to form rock layers.
Clastic sedimentary rock is sedimentary rock that is formed from rock particles.
claystone
shale
A rock formed for sedimentary deposits is called a sedimentary rock. A sedimentary rock which has then undergone metamorphism is called a meta-sediment.
Claystone, and shale are sedimentary rocks formed from lithified deposits of clay.
Sandstone.
Sandstone!
Sedimentary rock is the rock formed as a result of deposits from weathering and erosion. Sedimentary rock can be millions of years old.
A sedimentary rock formed from deposits of shells is called limestone. Limestone is made up primarily of calcium carbonate, which is derived from the shells of marine organisms like coral or shellfish.
I think you are referring to a classification of rock called sedimentary. the other two main types are metamorphic and igneous.
The sedimentary rock formed from tiny particles of clay in thin, flat layers is called shale. I hope this was helpful:)
Sedimentary rock formed from sand is called sandstone.
The sedimentary rock formed from clay deposits is called shale. Shale is composed of very fine particles of clay minerals that have been compressed and compacted over time. It commonly has a layered structure due to the alternating sequences of clay-rich and silt-rich layers.