Erosion
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.
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.
Metamorphism is the process where existing rocks are changed by heat, pressure, or fluids. This process causes the minerals in the rocks to rearrange and form new crystals, creating metamorphic rocks.
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.
The erosion of a mountain range would primarily lead to the formation of sedimentary rocks. These rocks are formed from the accumulation and compaction of sediments that erode from the mountains and are deposited in layers over time. Magma could also be formed if the eroded sediments are subjected to high temperatures and pressures deep within the Earth, leading to the formation of igneous rocks. Metamorphic rocks could form from existing rocks within the mountain range that undergo changes due to heat and pressure during the mountain-building process.
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.
An increase in temperature can lead to the formation of metamorphic rock from either igneous or sedimentary rock. When existing rocks are subjected to high temperatures and pressures, their mineral composition and structure can change, resulting in metamorphic rock. This process, known as metamorphism, does not involve melting but rather the recrystallization of minerals. Thus, both igneous and sedimentary rocks can transform into metamorphic rocks under the right conditions.
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 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.
Extreme pressure and temperature can alter a sedimentary rock by causing it to metamorphose into a new rock type known as metamorphic rock. This can lead to changes in mineral composition, texture, and structure of the original sedimentary rock.
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.
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.
One thing that is not a metamorphic agent is sediment. Metamorphic agents include heat, pressure, and chemically active fluids, which facilitate the transformation of existing rocks into metamorphic rocks. Sediment, on the other hand, refers to fragments of rock and minerals that accumulate and can lead to the formation of sedimentary rocks rather than metamorphic ones.
Sedimentary rock can be transformed into metamorphic rock primarily through heat and pressure. Increased temperature can cause the minerals within the sedimentary rock to recrystallize, while elevated pressure can lead to foliation and changes in texture. These conditions often occur deep within the Earth's crust during tectonic activity. Additionally, the presence of chemically active fluids can also facilitate metamorphic processes.
Metamorphism is the process where existing rocks are changed by heat, pressure, or fluids. This process causes the minerals in the rocks to rearrange and form new crystals, creating metamorphic rocks.
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.
When a metamorphic rock is weathered, it undergoes physical and chemical breakdown due to exposure to the elements. This can lead to the rock breaking apart into smaller pieces or being chemically altered, potentially forming new minerals. Over time, the weathering process can transform the metamorphic rock into sediment that may eventually become part of a sedimentary rock.