As I said, those are confirmed garbage.
No they are not. The only people calling them garbage are laymen who have no idea what they are talking about.
ALMOST ALL craters would be elongated.
No they wouldn't since it requires a rare and special set of circumstances. You didn't read the link, did you?
But if ignoring the observable facts, evidence, scientific method, and statistical impossibilities is your definition of science, we'll clearly never see eye to eye.
You're ignoring the observable facts, evidence, scientific proof, scientific method, statistical analyses, and passing off unfalsifiable tinfoil hat theories as the explanation.
You clearly don't understand the topic. I've read much on both sides. I didn't read the link because I've previously read the bogus point. The fact you don't understand what you're talking about is the issue.
The fact you're claiming the defacto occurrence is rare and rare is the defacto occurrence, is why you don't understand.
Before you reply, take a second to think about orbital periods and rotation and statistical angles of incidence. Now, stop dishonesty inserting bullshit like atmospheres (which you begrudgingly admit). As the topic is clearly the moon and other such bodies on which craters are well documented.
Ignoring all this, bluntly, only an idiot would choose half baked theories which ignore massive elements of facts in lieu of a theory which explains everything, which is bolstered by experiment, and precisely reproduces the observable facts. Which is why I can easily declare you care not for science.
You clearly don't understand the topic.
I clearly do since you do not even possess a basic understanding of both the position you're arguing against and the position your arguing for.
Ignoring all this, bluntly, only an idiot would choose half baked theories
There's no need to call yourself an idiot. You fell for some bullshit and you're having a hard time changing your mind. That's all. You'll get through it, eventually, and realize this was quite the stupid hill to die on.
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