Detritus can be organic or inorganic. Organic detrital rocks form when parts of plants and animals rot in the soil, leaving behind biological material that is compressed and becomes rock. Coal is a sedimentary rock formed over millions of years from compressed plants. Inorganic detrital rocks, on the other hand, are formed from broken pieces of other rocks, not living things. These rocks are often referred to as clastic sedimentary rocks. One of the most famous clastic sedimentary rocks is sandstone. Sandstone is formed from layers of sandy sediments that are compacted and lithotified. Sedimentary rock can be found anywhere on Earth. When sedimentary rocks are heated and pressed, they become metamorphic rocks. Magmatic rocks have a volcanic origin. Over a very long period of time, rocks are recycled in two ways. When marine sediments are lifted above sea level, they are altered and the pieces are transported into the sea. On a much longer time scale, continental plates can collide.
Then one plate passes under the other (is subducted), and all its material is recycled and occurs much later. Sedimentary rock is formed when sand, mud and pebbles settle in layers. Over time, these layers are pressed under more and more layers. Finally, the layers are lithotified – in rock. Sedimentary rock can form in deserts, lakes, rivers and seas. Between each group of characters, the face of the rock was dotted with mysterious signs and crudely lowered weapons of war and hunting. Consolidated rocks may be slightly altered by water infiltration or by heat and extreme pressure. Density contrasts can also cause small-scale faults, even as sedimentation progresses (synchronous sedimentary fault).  Such a fault can also occur when large masses of unlithified sediment settle on a slope, for example .B. at the front of a delta or on the continental slope.
Instabilities in such sediments can cause the deposited material to subside, creating cracks and wrinkles. The resulting structures in the rock are synsedimentary folds and faults that are difficult to distinguish from wrinkles and faults formed by tectonic forces acting on lithified rocks. Some sedimentary rocks consist of a single type of sediment, all of which are about the same size, such as . B sand. Other sedimentary rocks have large and small tufts and pieces of different types of rocks. The well-known sedimentary rocks are sandstone and limestone. When sediment accumulates in a deposition environment, older sediments are buried by younger sediments and undergo diagenesis. Diagenesis includes all chemical, physical and biological changes, with the exception of surface weather, that a sediment undergoes after its first deposition. These include sediment compaction and lithification.  The early stages of diagenesis, called eogenesis, take place at shallow depths (a few tens of meters) and are characterized by bioturbation and mineralogical changes in sediments with only minor compaction.  The red hematite that gives red bed sandstones their color is likely formed during eogenesis.   Certain biochemical processes, such as bacterial activity, can affect minerals in a rock and are therefore considered part of diagenesis.
 Relatively small changes in the orientation of the Earth`s axis or the length of the seasons can have a major impact on the Earth`s climate. An example is the ice age of the last 2.6 million years (Quaternary), which is believed to have been caused by astronomical cycles.   Climate change can affect global sea level (and thus the amount of housing space in sedimentary basins) and sediment supply in a given region. Finally, small changes in astronomical parameters can cause large changes in the sedimentary environment and sedimentation. The descendants of the wicked will not produce many branches and will make a sound like impure roots at the top of a rock. Clastic sedimentary rocks are divided according to the size of the dominant particles. Most geologists use the Udden-Wentworth particle size scale and divide unconsolidated sediments into three fractions: gravel (>2 mm in diameter), sand (1/16 to 2 mm in diameter) and mud (<1/16 mm in diameter). The sludge is then divided into silt (1/16 to 1/256 mm in diameter) and clay (<1/256 mm in diameter). The classification of clastic sedimentary rocks corresponds to this scheme; Conglomerates and breccias are mainly made of gravel, sandstones are mainly made of sand, and clay rock consists mainly of mud.
This tripartite subdivision is reflected in the broad categories of rudits, arenites and lutites in older literature. The environment in which sedimentary rock forms is called the deposition environment. Each environment has a characteristic combination of geological processes and circumstances. The type of sediment deposited depends not only on whether the sediment is transported to a place (origin), but also on the environment itself.  The shape of the clasts may reflect the origin of the rock. For example, coquina, a rock composed of clasts of broken shells, can only form in energetic water. The shape of a syringe can be described using four parameters: These sedimentary processes – weathering, transport and deposition – reach three final products: quartz sand, shale (from clay) and limestone (CaCO3). Most sedimentary rocks are variations of this general pattern. The rate at which sediment is deposited varies by location. A channel in a mudflat can see the deposition of a few meters of sediment in a day, while only a few millimeters of sediment accumulates on the deep seabed each year. A distinction can be made between normal sedimentation and sedimentation by catastrophic processes.
The latter category includes all kinds of sudden extraordinary processes such as mass movements, falling rocks or floods. Catastrophic processes can see the sudden deposition of a large amount of sediment at once. In some sedimentary environments, most of the entire column of sedimentary rock has been formed by catastrophic processes, although the environment is usually a quiet place. Other sedimentary environments are dominated by normal and persistent sedimentation.  Sediment refers to small particles or grains of minerals or altered rocks that have been broken by the forces of nature. These sediments can vary in size and shape. Sedimentary rock is formed when these particles settle and combine to form a larger whole by lithification. Lithification occurs either by sediment compaction or by cementation caused by minerals that bind the particles together. Otherwise, the water can be extracted from the stones, but remains for a long time with an unchanged character. There are many quarries with unconsolidated deposits where sand and gravel are removed for the construction industry. Such quarries can extract sand that has existed in the form of sand since the Jurassic period. But consolidated sand, sandstone, can be a very hard rock.
My ball bounced and the stone rolled a little forward. .