Magma or Lava
Metamorphic rocks can form from the transformation of pre-existing rocks under high temperatures and pressures. Common parent rocks include shale, limestone, and granite. The minerals present in the parent rocks determine the types of metamorphic rocks that can form.
Sedimentary rocks, such as sandstone and shale, form from layers of materials that accumulate and undergo compaction and cementation over time. These rocks typically contain fossils and provide important clues about Earth's history.
Intermediate materials in the rock cycle include sedimentary rocks like sandstone and shale, which are formed through the deposition and compaction of sediments. These rocks can undergo metamorphism to form metamorphic rocks like marble and schist. Metamorphic rocks, in turn, can melt to form magma that solidifies into igneous rocks like granite and basalt.
rocks
Sedimentary
Increased temperatures and or decreased pressures.
Detrital Sedimentary Rock
rocks
Minerals and inorganic materials that form soil come from the weathering of rocks and minerals present in the Earth's crust. Through processes like mechanical weathering (breakdown of rocks into smaller pieces) and chemical weathering (breakdown of rocks through chemical reactions), these materials eventually mix with organic matter to form soil. The composition and fertility of the soil are influenced by the types of minerals present in the parent rock.
sediment gets compressed together over long periodsmof time and with heat they get compacted into rocks
Sedimentary rocks such as sandstone and shale can form when materials are squeezed together due to pressure from overlying sediments and compaction. Igneous rocks can also form from intense pressure transforming existing rocks, such as with the formation of gneiss from granite under high pressure and temperature conditions.
The main types of rocks that form from the deposition of different materials on Earth are sedimentary rocks. These rocks are created from the accumulation and compression of sediments, such as sand, silt, and clay, typically through processes like erosion and deposition. Examples of sedimentary rocks include sandstone, shale, and limestone.