weathering, cementation, deposition
In clastic (or detrital) sedimentary rock:Weathering of an existing body of igneous, metamorphic, or sedimentary rock by natural mechanical or chemical means.Erosion of the weathered particles by wind, water, ice, and gravity.Deposition of the particles after transportation.Compaction of the particles by the weight of overlying sediments.Cementation of the particles by mineral precipitation from surrounding fluids.
The correct order of processes involved in sedimentary rock formation is weathering, erosion, deposition, compaction, and cementation. Weathering breaks down rock into smaller pieces, erosion moves the sediments, deposition deposits the sediments into layers, compaction squeezes the sediments together, and cementation binds the sediments into rock.
A metamorphic rock can form from either a sedimentary rock or an igneous rock. When subjected to high heat and pressure, existing rocks can recrystallize and change into new types of rocks, resulting in the formation of metamorphic rocks.
Correct, porphyritic texture is typically associated with igneous rocks and is not a common feature of sedimentary rocks. It is characterized by larger crystals, known as phenocrysts, surrounded by a fine-grained or glassy matrix. Sedimentary rocks are formed through the accumulation and lithification of sediments, which do not typically undergo the same crystallization processes as igneous rocks.
The presence of organic matter is not important in the formation of minerals. Minerals are inorganic substances that form through processes such as crystallization, precipitation, and solidification from molten rock. Organic matter may be present in the environment where minerals form, but it is not a necessary factor in mineral formation.
In clastic (or detrital) sedimentary rock:Weathering of an existing body of igneous, metamorphic, or sedimentary rock by natural mechanical or chemical means.Erosion of the weathered particles by wind, water, ice, and gravity.Deposition of the particles after transportation.Compaction of the particles by the weight of overlying sediments.Cementation of the particles by mineral precipitation from surrounding fluids.
In clastic (or detrital) sedimentary rock:Weathering of an existing body of igneous, metamorphic, or sedimentary rock by natural mechanical or chemical means.Erosion of the weathered particles by wind, water, ice, and gravity.Deposition of the particles after transportation.Compaction of the particles by the weight of overlying sediments.Cementation of the particles by mineral precipitation from surrounding fluids.
The correct order of processes involved in sedimentary rock formation is weathering and erosion, transport, deposition, and lithification. First, existing rocks are broken down into smaller particles through weathering. These sediments are then transported by water, wind, or ice to new locations where they are deposited. Finally, the sediments undergo lithification, which involves compaction and cementation, turning them into solid sedimentary rock.
In clastic (or detrital) sedimentary rock:Weathering of an existing body of igneous, metamorphic, or sedimentary rock by natural mechanical or chemical means.Erosion of the weathered particles by wind, water, ice, and gravity.Deposition of the particles after transportation.Compaction of the particles by the weight of overlying sediments.Cementation of the particles by mineral precipitation from surrounding fluids.
The correct order of processes involved in sedimentary rock formation is weathering, erosion, deposition, compaction, and cementation. Weathering breaks down rock into smaller pieces, erosion moves the sediments, deposition deposits the sediments into layers, compaction squeezes the sediments together, and cementation binds the sediments into rock.
Sedimentary rocks are formed through a series of processes that typically occur in the following order: first, weathering and erosion break down existing rocks into sediments. Next, these sediments are transported and deposited in layers through processes such as sedimentation. Over time, the accumulated sediments are compacted and cemented together, leading to the formation of sedimentary rocks.
In clastic (or detrital) sedimentary rock:Weathering of an existing body of igneous, metamorphic, or sedimentary rock by natural mechanical or chemical means.Erosion of the weathered particles by wind, water, ice, and gravity.Deposition of the particles after transportation.Compaction of the particles by the weight of overlying sediments.Cementation of the particles by mineral precipitation from surrounding fluids.
Caliche is the correct spelling for the sedimentary rock.
meiosis...fertilization...mitosis
The process involved in sedimentary rock formation includes weathering and erosion, which break down existing rocks into smaller particles. These sediments are then transported by wind, water, or ice and eventually deposited in layers. Over time, the accumulated sediments undergo compaction and cementation, transforming them into solid sedimentary rock. This process often preserves fossils and other geological features, providing insights into Earth's history.
A metamorphic rock can form from either a sedimentary rock or an igneous rock. When subjected to high heat and pressure, existing rocks can recrystallize and change into new types of rocks, resulting in the formation of metamorphic rocks.
Fertilization, cleavage, blastulation, gastrulation, organogenesis.