Alien Earth Moon

originally posted by: lunarrover
The following image proves that the moon is an alien space station.

Crooks crater from apollo 8.

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Check Korolev crater images from Apollo 17 to see reptilian architecture.

Life is but a dream.

I thought I was looking at a hornets nest. Layer upon layer.... That is some very old core mindset there...

a reply to: lunarrover

Calling it rocks just does not wash anymore

Actually, I believe you are on to something here. None of the craters are logical. No cone shape. The impact blows the dust away to reveal a flat bottomed crater.

I'm thinking of something like concrete, only the main element in this concrete, is titanium.

Interesting....

thread getting shoved in the ass by jim oberg or onebigmonkey in 3.2.1

oh wait its you lunar rover!
i was wondering where you went
seems you are back to your old tricks

a reply to: lunarrover

i see a bunch of rocks making weird shapes

a reply to: lunarrover

same

a reply to: lunarrover

1: the weird crater in the far right is caused by the asteroid that made it entering in an oblique angle
2: craters

a reply to: lunarrover

bunch of stuff in there but nothing anomalous

a reply to: lunarrover

thats an blotch in the image

a reply to: lunarrover

first is rocks
the superstruture is an common transmission glitch

a reply to: humanoidlord

The problem for you H is that no matter how much you think your opinion counts it in fact does not.

You are wasting your time, everybody knows it, you fool no-one.

All things bright and beautifil the lizards created all.

We cant but an 11bln year old civilisation can and have.

www.flickr.com...@N04/04058L

As many others have complained, you have done nothing but post images and go "LOOK, SEE!"

This does not demonstrate the superior research skills and intelligence you mistakenly think you possess.

I have better things to do with my time than waste it on this.

a reply to: OneBigMonkeyToo

Great go do them then.

Heres a pic of JO emptying a bin.

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a reply to: OneBigMonkeyToo

Look, see.

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