How Science Works: One Anomaly Versus A Mountain of Evidence

:slight_smile: Well, for starters, their very close proximity to one another!

You find bits of leaves and insects that were swept into the lake and settled to the bottom, and then measure the ratios of carbon isotopes in those samples. You then compare those ratios to their depth in the varve record.

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What about it? Why can’t lakes close to one another have different conditions, some of which are not conducive to varve formation?

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Well, apparently they can! But why would they demonstrate this? That is the question not being addressed.

You have already been given those answers:

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Not at all. There is no reason that Lake H should show that much variance in varve count given your list of requirements for varve formation.

By the way, are you possibly stating that if all of those requirements are not met in other locations, then YEC’s don’t have to listen to your conclusions?

To be fair, there have been times when a YEC has posted a response of “Google it for yourself” and I’ve criticised them harshly for it. So I think it’s only fair to give YECs the treatment that I expect to receive from them.

Accordingly, @r_speir, here is a link to Roy’s post.

Based on what evidence?

I’m not stating that at all. What I am saying is that there needs to be specific conditions for annual varves to form.

Now we are getting somewhere. What are those?

Already given to you. Here it is again:

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It’s worth pointing out that nowhere does the citation claim that there are only 3000 years worth of varves in Lake Hiruga. It says they took a 2.45m core sample, and dated the bottom of that core at 3300 years old. It doesn’t tell us if the core consists entirely of varves, or how many varves may be found if deeper core samples were taken.

Their focus was more recently formed laminations, apparently caused by the construction of the artificial Saga tunnel that connected Lake Hiruga to Lake Suigetsu.

From the 19th century, the lake basin shows high sedimentation rate, and distinct lamina sediments are formed. It is considered that this is caused by the construction of the Saga tunnel.

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Of course I’m happy to provide citations for my claims, but it bugs me when people ask questions that are so incredibly basic it really reveals that they haven’t bothered spending any time whatsoever trying to find out the answer on their own. In this case, r_speir even refused to scroll up in the thread.
I’m not going to spoon-feed people who aren’t really interested in learning.

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And here is my question again:

So let me get this straight. If there is a lake somewhere else that doesn’t have the right conditions to form varves you think this allows you to ignore the varves found in lakes with the right conditions? Do I have that right? If so, this is one of the most ludicrous things I have seen you write, and that is saying something.

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You’re absolutely right there. After all, I did make the point on a different thread that I thought he was trolling.

This is not “straight” and you know it. You twist words of others and put a spin on them to try and make them look ignorant or confused.

Question: what is your list of requirements for annual varves? Plain and simple. List them here.

It is the features of the varves that evidence their annual nature. In the case of Lake Suigetsu, annual varves have a layer predominately made of diatoms and a layer predominately made up of fine grained clay. This is consistent with the passing of seasons over a single year.

But we may not find that elsewhere where you are claiming annual varves, so you have a problem already.

We may find other features that indicate an annual cycle. Why is that a problem? Different geologic formations are going to contain different evidence.

Two problems 1. You have no idea what standard you want to use for annual varve count, 2. you still have not told us why two lakes side by side have such different varve counts