Did you change the feed yet?
September 21, 2010
If you’re getting this in your RSS feed reader it’s because you are still getting the old Clastic Detritus feed! I’ve already posted a handful of posts at the blog’s new home.
Here’s the new info:
URL: http://www.wired.com/wiredscience/clasticdetritus/
RSS: http://www.wired.com/wiredscience/category/clastic-detritus/feed
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2 Comments
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I need your help, please. I’ve been trying to submit my ‘experience’ to the Accretionary Wedge 27, but every time I try to post it or get it to Lockwood it mysteriously disappears after I see it on the screen under comments. If it is not suitable I’m fine with that but I just want to know why it is NOT ACCEPTABLE. Could you please review it and give me your opinion as to why it isn’t being included. And if you find it acceptable to forward it to him. I respect the hosts job of editing what they want too and they can leave what they want in or out. I can accept that but I do feel like a response back is in order as to when there are multiple inquiries as to whether they got it or not. I haven’t even gotten that much. Please go to ‘Ann’s Musings on Geology and Other Things’. http://annsmusingsongeologyotherthings.blogspot.com/ . I can be contacted at amowillis@yahoo.com.
Ann O’Brien Willis
I don’t know about your log in problems, but I wanted to leave a comment on the Lava Delta erosion topic and it never seemed to come on….. it just keeps on ticking and does’nt take a licking. Ha OK anyway it does’nt seem to log me in.
Very Cool Video, it appears obvious from the extreme amount of heating and cooling that the materials in the lave are extremely stressed and very brittle just as a peice of neon glass that needs to anneal in order not to shatter. Although there is volcanic rock that is glass “Obsidian” (spelling ??;) it has ample time to cool whereas this delta volcanic rock does not. Therefore brittle highly stressed rock….my theory.
thanks
Stephanie R
memphissigncompany.com