Subduction Zone
Veteran Member
As to deposition, we can observe how sediments are deposited today. We can also observe what happens when deposition is interrupted or sped up.
For example shale is made of very fine clays. We can observe that being deposited in deeper waters, after all of the coarser sediments have settled out. Not vey much can be deposited in a year since water does not hold that much pure lay. If you speed up the rate of deposition you also increase the amounts of coarse materials. The same applies to chalk and coral reef growth. Chalk is made when tiny coccolithophores die and sink to the bottom of the sea. That has to be well away from land sources that would contaminate it with clay or coarser sediments. And only a certain population can exist at a time. Algal blooms are limited events and can only again produce a limited amount of sediments. People who say maybe the flood would have made a massive bloom have it backwards. They need a specific environment to do well. The flood would have been the worst thing for them. There is no way to massively increase their rate of production.
But as I said, if deposition is interrupted there usually is some sort of evidence. A line that shows erosion. Cross bedding in wind blown sands, there are quite a few different ways that such changes manifest. The sedimentary rocks that we see are from slow and continual deposition for the most part. Again, there are some rather interesting exceptions. But the signs are clear.
For example shale is made of very fine clays. We can observe that being deposited in deeper waters, after all of the coarser sediments have settled out. Not vey much can be deposited in a year since water does not hold that much pure lay. If you speed up the rate of deposition you also increase the amounts of coarse materials. The same applies to chalk and coral reef growth. Chalk is made when tiny coccolithophores die and sink to the bottom of the sea. That has to be well away from land sources that would contaminate it with clay or coarser sediments. And only a certain population can exist at a time. Algal blooms are limited events and can only again produce a limited amount of sediments. People who say maybe the flood would have made a massive bloom have it backwards. They need a specific environment to do well. The flood would have been the worst thing for them. There is no way to massively increase their rate of production.
But as I said, if deposition is interrupted there usually is some sort of evidence. A line that shows erosion. Cross bedding in wind blown sands, there are quite a few different ways that such changes manifest. The sedimentary rocks that we see are from slow and continual deposition for the most part. Again, there are some rather interesting exceptions. But the signs are clear.