Water deposits the clay particles in thin, flat layers.
Shale rocks turn into clay. The pressure make shale into clay.
It is more accurate to say it is formed from clay and silt.
the type of rock made mostly from clay is the shale rock
Clay minerals, quarts, feldspar
It smells like clay because that is what it's made out of.
Silt and clay size sediments form shale.
First, a layer of clay that would turn to shale was deposited. Next, a layer of plant life that would become coal was deposited, then another layer of clay. Over time, the clay became shale, and the plants became coal. Sort of like how did the blanket on your bed get between the sheets and the bedspread? You put on the sheets, then the blanket, then the bedspread.
Shale beaches are formed from the deposition of sediment form nearby shale cliffs which are eroded. The shale can also be deposited at a beach due to longshore drift.
Shale, a sedimentary rock.
Clay is a type of fine-grained natural soil material that is composed of mineral particles smaller than silt. Shale is a fine-grained sedimentary rock that is formed from the compaction of clay, silt, or mud over time. Essentially, shale is the hardened form of clay.
Shale started as mud. Mud is deposited in the bottom of lakes and seas.
Shale rocks turn into clay. The pressure make shale into clay.
Silt and clay size sediments form shale.
George S. Austin has written: 'Directory of clay and shale producers and ceramic plants in Indiana' -- subject(s): Clay industries, Shale 'Clay and shale resources of Indiana' -- subject(s): Shale, Clay 'Geology of clay deposits' -- subject(s): Clay, Geology
Shale is made from layers of mud and clay pressed together. :)
Shale is non foliated, as foliation is a rock texture caused by metamorphism; fluid drag or crystal settling in igneous magmas and lavas, whereas shale is a sedimentary rock typically deposited in lacustrine or other low energy environments. The banding in shale is called lamination and is due in part to variations in the energy of the depositional environment, leading to fluctuations in the size of grains being deposited and also due to the presence of large numbers of clay minerals which are typically plate like (termed phyllosilicates) and therefore on compaction form parallel layers.
Shale.