WARNING: This blog contains copious amounts of adult GAY material. If that's offensive to you, please leave now. All pix have been gleaned from the internets so, if you see a picture of yourself that you don't wish to have posted here, please leave a comment on the post and I will remove it with my apologies.

I REPEAT: If you see a picture of yourself that you don't wish to have posted here, please leave a comment on the post and I will remove it with my apologies.

Friday, March 28, 2025

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A blog that I visit once in a while is called "Just For The Gents". Recently he posted:

Important message: I live in Indiana, with that stated - Indiana passed a law to block what [they] deem this site as pornography. If this happens to my blog, I will try to give a heads up before closing my blog. Hopefully, I can find a new site that doesn't have the restriction or they totally ignore the Indiana law.

Here is the link to his blog if you have any suggestions...

https://justforthegents.blogspot.com

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These people are very lucky...

Pilot rescued with 2 girls from icy Alaska lake was not authorized to have passengers, official says



Click on headline to read the articles, there's a second story at the end of the first story.

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Moeraki Boulders, New Zealand









Some 60 million years ago, sediment was accumulating on the sea floor, with small frag­ments such as shells and plants within it. Calcite slowly built up around organic nuclei, forming spherical nodules with harder outer layers while the inner material dehydrated to give cracks which spread radially out to the rim. The cracks themselves filled with varying mineral deposits as groundwater conditions changed. The largest boulders are thought to have taken more than four million years to form. Following uplift onto the landmass of New Zealand in a period of mountain building, erosion was able to expose the Palaeocene mudstone beds that contain the boulders and from which they continue slowly to emerge. The effects of weathering have removed some of the outer layers, allowing the inner structure to be seen and breaking up some boulders. - SOURCE

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