Clastic or detrital rocks, depending on size.
Sedimentary rocks. Sandstone is a common example of a sedimentary rock that is formed from the accumulation and cementation of sand-sized grains of mineral and rock fragments.
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.
Any rock (igneous, sedimentary or metamorphic) may be broken into fragments that may later be formed into sedimentary rock.
A sedimentary rock is formed when rock fragments are compacted and cemented together by pressure and minerals. Examples of sedimentary rocks include sandstone, shale, and conglomerate.
No, sedimentary rocks formed from broken fragments are called clastic sedimentary rocks. Organic sedimentary rocks are formed from the accumulation of organic material such as plant debris or remains of marine organisms.
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.
Sedimentary rock formed from rock fragments is called clastic sedimentary rock. These rocks are made up of pieces of other rocks that have been weathered, transported, and then deposited and cemented together. Examples include sandstone, shale, and conglomerate.
Sedimentary rock is formed when small rock fragments are cemented together. This happens through a process called lithification where sediments are compacted and cemented together over time. Sandstone and conglomerate are examples of sedimentary rocks formed in this way.
Sedimentary rocks made of weathered rock fragments are called clastic sedimentary rocks. These rocks are formed from the accumulation and cementation of fragments that have been weathered, eroded, and transported from their original source. Examples include sandstone, shale, and conglomerate.
Some examples of clastic sedimentary rocks include sandstone, conglomerate, shale, and breccia. These rocks are formed from the accumulation of fragments of pre-existing rocks and minerals, which are then compacted and cemented together over time.
The main types of sedimentary rocks are clastic (formed from fragments of other rocks), chemical (formed from minerals precipitated from water), and organic (formed from the remains of once-living organisms). Examples include sandstone, limestone, and shale.
Both sandstone and siltstone are clastic sedimentary rocks formed by broken fragments of rock being deposited and then turned into solid rock by heat and pressure. The main difference is in grain size. Sandstone has larger grains than siltstone.