The large rock weathers. Its particles are eroded to a place of deposition. The particles are compacted and cemented together, forming a new sedimentary rock. This is a simplified explanation of the process.
Igneous rock can become sedimentary rock through the process of weathering and erosion, where the igneous rock breaks down into smaller pieces called sediment. These sediments are then transported by water, wind, or ice, and eventually get deposited and compacted to form sedimentary rock through the processes of lithification.
A metamorphic rock can become a sedimentary rock through weathering and erosion, where the existing rock is broken down into sediments. These sediments can then be carried away by water or wind and deposited in layers. Over time, these layers can become compacted and cemented together to form a new sedimentary rock.
Weathering breaks down rocks into smaller pieces, forming sediment. Erosion then transports this sediment to new locations, where it eventually settles and compacts, becoming sedimentary rock through the process of lithification. Over time, layers of sediment build up and solidify to form sedimentary rocks.
Erosion. If a metamorphic rock is exposed above sea level it will erode or weather, the products from this erosion or weathering will be moved by gravity, wind or water to a sea or basin where the products will settle as a sediment. If the conditions are right the sediment will eventually become a sedimentary rock.
The process you are describing is called deposition. When sedimentary material is carried by ice and then melts, the sediment is deposited or dropped in a new location. This can lead to the formation of new landforms, such as moraines or eskers.
The process that changes sedimentary rock into igneous rock is called "melting." When sedimentary rock is subjected to high temperatures and pressures deep within the Earth's crust, it can melt and re-crystallize into igneous rock. This process occurs in the presence of magma and can lead to the formation of new igneous rock.
sedimentary rock formed by the denudational process of various activity. the sediments in sea water may deposited and thus lead to the formation of sedimentary rock
When two tectonic plates collide, one plate may be forced beneath the other in a process called subduction. This subduction can lead to intense pressure and heat which can cause the sediments on the ocean floor to undergo metamorphism and turn into sedimentary rocks. Additionally, the collision can also uplift and expose existing sedimentary rocks to be further cemented and compacted into new sedimentary rock layers.
Sedimentary processes are normally very slow in human terms. The process of lithification of sediments can take millions of years. Chemical sedimentary rocks, on the other hand can be created in a very short period of time even though the processes that lead to them may take much longer.
It is possible for a sedimentary rock to become marble through the effects of environmental conditions such as pressure and temperature. They help to alter the structural and textural characteristics of the rock thereby changing it form and appearance. Limestone is a common sedimentary rock that is transformed in Marble which is a metamorphic rock. The process of changing a sedimentary rock into a metamorphic rock is called Metamorphism.
In the lead chamber process, sulphur dioxide is oxidized to sulphur trioxide using atmospheric oxygen in the presence of a vanadium oxide catalyst. The sulphur trioxide is then absorbed in water to form sulphuric acid. The lead chamber process gets its name from the large lead-lined chambers used in the process to contain the reaction.
Subsidence, the gradual sinking of the Earth's surface, creates environments where sediments can accumulate, such as river valleys or ocean basins. Over time, these sediments layer upon one another, increasing in pressure and temperature. This process can lead to lithification, where sediments are compacted and cemented together, ultimately forming sedimentary rocks. Thus, subsidence plays a crucial role in creating the conditions necessary for sedimentary rock formation.