Any rock (igneous, sedimentary or metamorphic) may be broken into fragments that may later be formed into sedimentary rock.
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.
A rock made entirely of seashell fragments is known as a coquina. Coquina rocks are formed from the accumulation and compression of broken seashells, creating a unique and porous sedimentary rock that is often found along coastal regions.
Clastic sedimentary rocks are made of fragments from rocks, minerals, and shells. These fragments, called clasts, are compacted and cemented together over time to form rocks like sandstone, shale, and conglomerate.
Breccia refers to a rock that is composed of the broken fragments of the rocks or minerals that have been cemented together. The broken fragments of the rocks or minerals are usually cemented together to form a fine grained matrix.
Sedimentary rocks form from fragments through the processes of weathering, erosion, transportation, deposition, and lithification. Weathering breaks down solid rock into smaller fragments, which are then transported by water, wind, or ice, and eventually deposited in layers. Over time, the pressure from additional sediment layers can compact and cement the fragments together to form sedimentary rock.
Any rock (igneous, sedimentary or metamorphic) may be broken into fragments that may later be formed into sedimentary rock.
Any rock can be broken up and later form a sedimentary rock.
When broken pieces of minerals and rock fragments accumulate, they form sediment. Over time, this sediment can undergo processes such as compaction and cementation, ultimately leading to the formation of sedimentary rock. Sedimentary rocks often contain layers and may preserve fossils, providing insights into Earth’s history.
sedimentary
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.
A rock made entirely of seashell fragments is known as a coquina. Coquina rocks are formed from the accumulation and compression of broken seashells, creating a unique and porous sedimentary rock that is often found along coastal regions.
No, sedimentary rocks formed from fragments of other rocks are called clastic sedimentary rocks. Chemical sedimentary rocks form from minerals that are dissolved in water and precipitate out to form rocks like limestone or halite.
Clastic sedimentary rocks are made of fragments from rocks, minerals, and shells. These fragments, called clasts, are compacted and cemented together over time to form rocks like sandstone, shale, and conglomerate.
If the original rock is eroded or broken away and then returned to sedimentary-forming conditions, it will form another sedimentary.
Breccia refers to a rock that is composed of the broken fragments of the rocks or minerals that have been cemented together. The broken fragments of the rocks or minerals are usually cemented together to form a fine grained matrix.
Sedimentary rocks form from fragments through the processes of weathering, erosion, transportation, deposition, and lithification. Weathering breaks down solid rock into smaller fragments, which are then transported by water, wind, or ice, and eventually deposited in layers. Over time, the pressure from additional sediment layers can compact and cement the fragments together to form sedimentary rock.
Sedimentary rocks made from fragments of rocks, minerals, and shells are known as clastic sedimentary rocks. Examples include sandstone, shale, and conglomerate. These rocks form when pre-existing rocks are weathered, eroded, transported, and deposited in layers.