Correa Neto
Philosopher
- Joined
- Aug 4, 2003
- Messages
- 8,548
Buzz, you can do a quick study by yourself, But you will have to keep an open mind for the results. Yes, an open mind, exactly what you claim we don't have.
Go to a beach and/or a stream, grab some sand samples. Look at them under magnifying glasses. Examine the grains. See how rounded or angular they are, how much they deviate from sphericity.
At
http://www.cmis.csiro.au/ismm2002/proceedings/PDF/28_drevin.pdf
you will find a template for sphericity (table 1). Don't let the math intimidate you. All you will need is that table.
At
http://www.eos.ubc.ca/courses/eosc221/sed/sili/siligsize.html
tables for sorting
At
http://www.eos.ubc.ca/courses/eosc221/sed/sili/siligrshap.html
tables for roundness.
Check how many different mineral types you can identify. If the sandstone you think is composed by scales is, say, from a fluvial environment, try looking more closely at recent fluvial sands.
Do the same with your alleged serpent sandstone. Fragment the "scales" down to the individual grains. Study samples from other nearby layers, without the "scales".
At
http://pubs.usgs.gov/of/2003/ofr-03-420/Figure1-Ternary.pdf
You will find a mineralogy-based sandstone classification triangular graph. I really do not think you will be able to recognize the minerals from your samples by yourself (needs some training in mineralogy). Aniway, at
http://www.eos.ubc.ca/courses/eosc221/sed/sili/sedclue1.html you'll find some tips.
In the end, you will be able to see that:
1. Sandstone composition is variable (its not just quartz).
2. The mineral composition of your samples will fall at some places in those graphs.
Note that there will be variations due to different beds bein deposited at different conditions. The deposits of a stream will different at dry and rainy seasons, for example. Even the location within the stream (bars, channels, etc.) system will determinate differences in the sediments. In doubt? Look at a river.
Your next step is to consider your results. You will have to answer these questions (among others):
How much compositional, roundness, etc. variability would be expected at scales from a creature? How does this fits with the observed variability in sandstones?
If the composition, roundness, etc. of what you think are "scales" are similar to those from nearby sandstones that are not composed by "scales", what should you conclude?
If the material from the alleged scales is very similar to recent loose sand grains, what should you conclude?
So, Buzz, sorry, your idea is nothing but a fantasy. And some people already had some similiar fantasies. And there are fictional books, tv series, etc. about it...
Go to a beach and/or a stream, grab some sand samples. Look at them under magnifying glasses. Examine the grains. See how rounded or angular they are, how much they deviate from sphericity.
At
http://www.cmis.csiro.au/ismm2002/proceedings/PDF/28_drevin.pdf
you will find a template for sphericity (table 1). Don't let the math intimidate you. All you will need is that table.
At
http://www.eos.ubc.ca/courses/eosc221/sed/sili/siligsize.html
tables for sorting
At
http://www.eos.ubc.ca/courses/eosc221/sed/sili/siligrshap.html
tables for roundness.
Check how many different mineral types you can identify. If the sandstone you think is composed by scales is, say, from a fluvial environment, try looking more closely at recent fluvial sands.
Do the same with your alleged serpent sandstone. Fragment the "scales" down to the individual grains. Study samples from other nearby layers, without the "scales".
At
http://pubs.usgs.gov/of/2003/ofr-03-420/Figure1-Ternary.pdf
You will find a mineralogy-based sandstone classification triangular graph. I really do not think you will be able to recognize the minerals from your samples by yourself (needs some training in mineralogy). Aniway, at
http://www.eos.ubc.ca/courses/eosc221/sed/sili/sedclue1.html you'll find some tips.
In the end, you will be able to see that:
1. Sandstone composition is variable (its not just quartz).
2. The mineral composition of your samples will fall at some places in those graphs.
Note that there will be variations due to different beds bein deposited at different conditions. The deposits of a stream will different at dry and rainy seasons, for example. Even the location within the stream (bars, channels, etc.) system will determinate differences in the sediments. In doubt? Look at a river.
Your next step is to consider your results. You will have to answer these questions (among others):
How much compositional, roundness, etc. variability would be expected at scales from a creature? How does this fits with the observed variability in sandstones?
If the composition, roundness, etc. of what you think are "scales" are similar to those from nearby sandstones that are not composed by "scales", what should you conclude?
If the material from the alleged scales is very similar to recent loose sand grains, what should you conclude?
So, Buzz, sorry, your idea is nothing but a fantasy. And some people already had some similiar fantasies. And there are fictional books, tv series, etc. about it...




