The processes would be, in order of their occurrence: weathering, erosion, deposition, compaction, and cementation.
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.
Heating to melting point and coolingAPEX - Erosion & LithificationAPEX students should be advised that using wiki.answers.com is a bad idea because copying and pasting is plagerism and your teachers will notice. Put responses in your own words.
The two processes that result in the formation of igneous rocks are cooling and solidification of molten magma, and crystallization of magma within the Earth's crust or on the surface. These processes lead to the solidification of molten material, which then forms igneous 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.
Amphibolite is typically formed from the metamorphism of basalt or gabbro, which are both mafic igneous rocks. The high temperatures and pressures during metamorphism lead to the formation of amphibole minerals, giving rise to the rock type known as amphibolite.
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.
The statement is not correct because igneous rock can undergo various processes in the rock cycle that do not necessarily lead to sedimentary rock. Instead, igneous rocks can be subjected to weathering and erosion, becoming sediments that may later form sedimentary rock, or they can be transformed into metamorphic rock through heat and pressure. Additionally, igneous rocks can also be recycled back into magma through subduction processes, bypassing sedimentary rock entirely. The rock cycle is a complex system with multiple pathways, not a linear sequence.
Melting and solidification!
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.
Heating to melting point and coolingAPEX - Erosion & LithificationAPEX students should be advised that using wiki.answers.com is a bad idea because copying and pasting is plagerism and your teachers will notice. Put responses in your own words.
Sedimentary rocks are formed on or near the Earth’s surface, in contrast to metamorphic and igneous rocks, which are formed deep within the Earth. The most important geological processes that lead to the creation of sedimentary rocks are erosion, weathering, dissolution, precipitation, and lithification.
The two processes that result in the formation of igneous rocks are cooling and solidification of molten magma, and crystallization of magma within the Earth's crust or on the surface. These processes lead to the solidification of molten material, which then forms igneous rocks.
Zinc is a mineral in its natural state as sphalerite (ZnS), which is a compound of Zinc and Sulphur. It is normally found along with other igneous type minerals such as copper, lead and iron.
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.
There are seven major mineral formation systems, which are igneous, sedimentary, metamorphic, hydrothermal, weathering, soil, and biological. Each system involves specific processes that lead to the creation of different types of minerals.
Not every rock goes through the complete rock cycle in a linear fashion. While the rock cycle describes the processes through which rocks can transform from one type to another—igneous to sedimentary to metamorphic and back—many rocks may not experience all these stages. Environmental conditions, geological processes, and the specific rock's history can lead to various pathways, meaning some rocks may remain in one form or undergo only certain transformations.
Clastic sedimentary rocks are formed by the weathering, erosion, deposition, compaction and cementation of other rocks. Chemical sedimentary rocks however may be precipitated directly from saturated solutions (examples incldue the evaporitic rocks and certain types of carbonates such as oolitic limestones). Some other sedimentary rocks may be biogenic in origin (such as the linmestones that are formed of coral reefs).