Answer :
The correct answer is: Shale is typically found in marine environments, such as the bottom of oceans or marshes.
Explanation:
Shale is a type of sedimentary rock that is formed from the compaction and cementation of fine-grained sediments, such as clay, silt, and mud. These sediments are typically deposited in low-energy, quiet water environments, such as the bottom of oceans, lakes, or marshes.
The conditions that favor the formation of shale include:
1. Slow, steady deposition of fine-grained sediments: Shale forms when small particles of clay, silt, and organic matter are slowly deposited over time, often in deep, calm water environments.
2. Anoxic (low-oxygen) conditions: Shale often forms in environments with limited oxygen, such as the bottom of deep oceans or stagnant bodies of water, where organic matter can be preserved.
3. Burial and compaction: As the sediments are buried under additional layers of sediment, the weight and pressure cause the sediments to compact and cement together, forming the layered structure of shale.
Therefore, the conditions that are most likely to be associated with the formation of shale are the bottom of oceans or marshes, where fine-grained sediments can accumulate in a low-energy, anoxic environment. Mountain streams and desert environments are not typical locations for the formation of shale.
Explanation:
Shale is a type of sedimentary rock that is formed from the compaction and cementation of fine-grained sediments, such as clay, silt, and mud. These sediments are typically deposited in low-energy, quiet water environments, such as the bottom of oceans, lakes, or marshes.
The conditions that favor the formation of shale include:
1. Slow, steady deposition of fine-grained sediments: Shale forms when small particles of clay, silt, and organic matter are slowly deposited over time, often in deep, calm water environments.
2. Anoxic (low-oxygen) conditions: Shale often forms in environments with limited oxygen, such as the bottom of deep oceans or stagnant bodies of water, where organic matter can be preserved.
3. Burial and compaction: As the sediments are buried under additional layers of sediment, the weight and pressure cause the sediments to compact and cement together, forming the layered structure of shale.
Therefore, the conditions that are most likely to be associated with the formation of shale are the bottom of oceans or marshes, where fine-grained sediments can accumulate in a low-energy, anoxic environment. Mountain streams and desert environments are not typical locations for the formation of shale.