wind water ice gravity
All rocks can form from sedimentary because the rock cycle is endless.
weathering of preexisting rocks form clastic sedimentary rocks, Oversaturated water basins form chemical sedimentary rocks after the water evaporates and dead sea organisms settle at the bottom forming biochemical sedimentary rocks.
Are meatmorphic rocks and also perhaps soil.
The rock cycle consists of three major groups of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling and solidification of molten material (magma or lava). Sedimentary rocks develop from the accumulation and compaction of mineral and organic particles, often in water. Metamorphic rocks arise when existing rocks are subjected to heat and pressure, causing them to transform into new forms. These rocks can transition between groups through various processes, such as erosion, melting, and metamorphism, illustrating the dynamic nature of the rock cycle.
drag and momentum
Igneous, metamorphic, and existing sedimentary rocks can weather and erode to form sedimentary rocks. Igneous and metamorphic rocks can break down into sediments through processes like weathering and erosion, which then may accumulate and lithify into sedimentary rocks. Existing sedimentary rocks can also be reworked and lithified to form new sedimentary rocks through processes like compaction and cementation.
The three major types of rocks are igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling and solidification of magma or lava. Sedimentary rocks are formed from the accumulation and compression of sediment over time. Metamorphic rocks are formed from the alteration of existing rocks due to high heat, pressure, or chemical processes.
One process that is not a major part of sedimentary rock formation is metamorphism. Metamorphism involves the alteration of existing rocks through heat and pressure, leading to the formation of metamorphic rocks, rather than sedimentary ones. Sedimentary rocks typically form through processes such as weathering, erosion, deposition, and lithification.
Sediments in sedimentary rocks are often caused by precipitation.
Sedimentary rocks are the type of rocks that can only form on or very near Earth's surface. Sedimentary rocks form from weathering processes that occur on Earth's surface.
Igneous and metamorphic rocks can form sedimentary rocks when they undergo weathering. As these rocks break down into smaller particles through physical and chemical processes, they can be transported and deposited, eventually lithifying into sedimentary rock. Additionally, pre-existing sedimentary rocks can also contribute to the formation of new sedimentary layers through similar weathering and erosion processes.
Biochemical sedimentary rocks form from sediment derived by biological processes. A type of sedimentary rock primarily comprising deposits resulting.
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.
Chemical sedimentary rocks form from solutions (water with something in it).
There are two processes in which sedimentary rocks form. One is chemical, and the other is by deposition (sediment being deposited and then cemented together). Examples of chemical sedimentary rocks are limestone, dolomite, and rock salt.
Sedimentary rocks form at or near the Earth's surface through the accumulation and compression of sediments. These sediments can come from the weathering and erosion of pre-existing rocks, as well as from the remains of plants and animals. Over time, these sediments are compacted and cemented together to form sedimentary rocks.
lava cooling