Santrouis
1. Are bedrock channels more likely to be found near the head or near the mouth of stream?
Wiki User
∙ 14y agoBedrock channels are more commonly found near the head of a stream where the gradient is steeper and erosion is more significant. As a stream flows downstream, the energy decreases, and sediment deposition can cover and mask the bedrock, leading to fewer bedrock channels near the mouth of a stream.
Bedrock channels are more likely to be found near the head of a stream where the gradient is steeper and erosion processes are more active. As the stream flows downstream and the gradient decreases, the likelihood of encountering bedrock channels decreases as well.
A fossil that is likely to be found in the same age bedrock as Centroceras is a marine organism such as other types of algae, foraminifera, or marine invertebrates like brachiopods or ammonites. These organisms lived in similar environments and time periods as Centroceras, making them common in the same age bedrock layers.
Aquifers are typically found below the bedrock. Bedrock acts as a barrier that holds the water in the aquifer, with layers of soil, sand, and gravel above the bedrock helping to recharge the aquifer with water.
A resurgent stream is typically formed in a limestone area because limestone is a soluble rock that can be easily eroded by water. As water flows through the limestone, it creates underground channels and caves. When these channels become blocked or the water table drops, the water is forced to resurge back to the surface, creating a resurgent stream.
Unweathered bedrock is typically found in the bedrock layer of the Earth's crust, which is known as the lithosphere. This layer is located beneath the soil, regolith, and weathered rock layers.
Bedrock channels are more likely to be found near the head of a stream where the gradient is steeper and erosion processes are more active. As the stream flows downstream and the gradient decreases, the likelihood of encountering bedrock channels decreases as well.
The processes most likely formed a burial and compaction which the shale bedrock is found near Ithaca, New York.
The efflux of potassium ions is maintained by passive potassium channels.
The efflux of potassium ions is maintained by passive potassium channels.
A fossil that is likely to be found in the same age bedrock as Centroceras is a marine organism such as other types of algae, foraminifera, or marine invertebrates like brachiopods or ammonites. These organisms lived in similar environments and time periods as Centroceras, making them common in the same age bedrock layers.
A chalk stream is a type of river or stream that flows over chalk bedrock or through chalk hills. These streams are known for their clear, alkaline water and are usually rich in flora and fauna. Chalk streams are found mainly in southern England.
everyone, the answer to this question is burial and compaction
There is not a specific type of bedrock found along the rocky shores. The types of bedrock found depend on the ecosystem at the different rocky shore sites.
Assuming you are not referring to the 'Flintstones - town of Bedrock' and are referring to geological bedrock then any rock that is not part of the soil or an erosional clast (of any size) is bedrock. Bedrock is therefore found everywhere.
Aquifers are typically found below the bedrock. Bedrock acts as a barrier that holds the water in the aquifer, with layers of soil, sand, and gravel above the bedrock helping to recharge the aquifer with water.
in the tug hill plateau
yes example:I dug really deep and found the bedrock beneath the soil.