Shale can metamorphose through heat and pressure into slate.
Sandstone: formed by the cementation of sand grains. Conglomerate: formed by the cementation of rounded pebbles. Siltstone: formed by the compaction of silt-sized particles. Shale: formed by the compaction of clay and silt particles.
No, shale is a type of sedimentary rock formed from the accumulation of silt and clay particles. It is not formed from the skeletons of ancient coral animals, which are typically preserved in rocks such as limestone.
Claystone, and shale are sedimentary rocks formed from lithified deposits of clay.
Shale rocks are formed in the deep waters of swaps, oceans and lakes where the water is still and the fine clay and silt particles are able to settle to the floor. Shale rocks can easily erode due to weathering.
Clastic sedimentary rock is formed from the compaction and cementation of particles of other rock. Examples are shale, sandstone, and conglomerate.
Rocks formed from sediment deposits are called sedimentary rocks. They are formed from the accumulation and lithification of sediment, which can include fragments of pre-existing rocks, minerals, and organic material. Examples include sandstone, shale, and limestone.
Rocks that are formed by layers of sediments that are compacted over time are appropriately named sedimentary rocks.
Rocks formed from broken rocks are known as sedimentary rocks. These rocks are formed from the accumulation and lithification of sediments, which can include fragments of other rocks, minerals, and organic material. Common examples of sedimentary rocks formed from broken rocks include sandstone, conglomerate, and shale.
Shale Rock
They are all clastic sedmimentary rocks formed mainly of silicate minerals.
Sedimentary rocks like sandstone, shale, and limestone are formed when layers of sediments are compacted and cemented together over time. This process is known as lithification.
Clay deposits can form sedimentary rocks like shale or mudstone through compaction and cementation over time. These rocks are characterized by fine grains and typically exhibit layering due to the gradual accumulation of sediments in depositional environments such as lakes, rivers, or oceans.