Sedimentary rock formation begins with igneous, metamorphic, or other sedimentary rocks. When these rocks are exposed at the earth's surface they begin the long slow but relentless process of becoming sedimentary rock.
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
A major process in the formation of sedimentary rock is lithification, which involves the compaction and cementation of sediments. Over time, layers of sediment accumulate and are buried under additional layers, increasing pressure. This pressure compacts the sediments, while minerals precipitate from groundwater and act as a glue, binding the particles together to form solid rock. Other processes involved include erosion, transportation, and deposition of sediments.
It is more likely that igneous and metamorphic, or igneous and sedimentary rocks would have something in common than sedimentary and metamorphic. The reason is because the processes involved in making metamorphic rocks is completely different than the processes needed to make sedimentary rocks. Only high temperature, high pressure minerals such as olivine, pyroxene, amphibole can withstand these kinds of conditions. Take quartz and feldspar, two of the most abundant minerals found in sedimentary rocks, these minerals would not be found in abundance in metamorphic rocks because they are not high temperature, high pressure rocks. But the most simple answer is that all the major groups of rocks are made of minerals. Metamorphic has high pressure and Igneous does to and both made from a particle called magma.
Melting.
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
The major processes involved in the formation of sedimentary rocks are weathering, erosion, transportation, deposition, compaction, and cementation. Weathering breaks down rocks into smaller particles, which are then transported by water, wind, or ice. The sediments are deposited in layers, compacted by the weight of overlaying sediments, and cemented together over time to form sedimentary rocks.
Igneous Rock Metamorphic Rock Sedimentary Rock
Gypsum is actually a major rock forming mineral. Rock gypsum is a chemical sedimentary rock.
The five major processes involved in the formation of sedimentary rocks are weathering, erosion, transportation, deposition, and lithification. Weathering breaks down rocks into smaller particles, erosion moves these particles, transportation carries them to new locations, deposition settles the particles in layers, and lithification compacts and cements the sediments into solid rock over time.
wind water ice gravity
Calcium carbonate (known as calcite CaCO3) is a common carbonate rock-forming mineral.
Sedimentary rocks require two processes to be formed. The first is weathering. Weathering is the disintegration/decomposition of rocks. Erosion is the process by which the weathered material is moved from one place to another. Erosion occurs when, for instance, a moving stream picks up a weathered pebble and moves it miles downstream to the mouth of a river. Erosion can also take place with ice, wind, etc.
Pathway 2 includes the major groups of sedimentary and metamorphic rocks. Sedimentary rocks are formed from the accumulation and consolidation of sediments, while metamorphic rocks are formed from the alteration of existing rocks through heat and pressure. Both of these rock types are commonly involved in the rock cycle and can contribute to the formation of other rock types.
Igneous rocks are the major group of rocks involved in Pathway 1. This pathway involves the formation of rocks from the cooling and solidification of magma or lava. Examples include granite and basalt.