User talk:Lusilier

Welcome aboard!
Welcome - always glad to see geo-knowledgeable new editors. I've tweaked a few of your edits for image sizing and some link fixes. Normal illustrative images should be set to default size (no size given in the image link) as Wiki users can set their preferences for image size. Other images such as diagrams & graphs with text should in general be large enough to make them readable, but not too large to avoid overwhelming the page view. Note that I set my browser at 200x for viewing ease (vision problems plus distance to my screen from my recliner :). Anyway, enjoy editing and feel free to drop me a note if the wiki gets confusing or you hit a rough spot. Cheers, Vsmith (talk) 00:12, 18 December 2012 (UTC)
 * Thank you very much. I was just wondering about that. Default setting does make sense (a principle i now remember from HTML programing way back then!). Tx also for your offer to help - I may take you up on it. --Lusilier (talk) 00:36, 18 December 2012 (UTC)

WikiProject
Hi Luilier! I hope you are having a fun time contributing to Wikipedia! I was wondering if you would like to join WikiProject_Geology to stay in contact with like-minded editors. all the best! --Tobias1984 (talk) 11:07, 14 June 2013 (UTC)
 * Hi Tobias. Thanks very much for the invitation. I appreciate. Interestingly, years ago when I still called myself a structural geologist, I did my graduate work on ice to shed light on rock deformation. In the geological community, ice was considered a rock analogue, even though it is as rock. But my research did not qualify as geo-relevant so I was forced to move into an unusual field where ice did matter and funding was available: offshore engineering in cold regions. My contributions to Wikipedia deal mostly with sea ice and engineering (as opposed to sedimentological/depositional) aspects of the seabed. Although still a geologist at heart, I don't feel I can contribute to any geo-relevant topics. --Lusilier (talk) 14:10, 14 June 2013 (UTC)
 * I do think that we should think of Geology in the broadest sense. It would be helpful to have people like you on board so we can stay flexible enough in topics and opinions. By the way, I have student-assisted a course about brittle and ductile deformation in thin-sections a couple of years. We watched a movie about ice deformation every year, because it can be deformed and filmed at the same time. Really interesting topic. --Tobias1984 (talk) 14:33, 14 June 2013 (UTC)
 * The movie was probaly Chris Wilson's work (if you remember a thick Australian accent in the commentator's voice...). The processes described take place at relatively low strain rates, more akin to what happens inside glaciers (compared to, say, when floating ice crashes into a bridge pier). The key feature with ice is that it happens to melt at relatively low temperature (0 deg. C), hence no need for a oven to make these observations, just a cold room. I'll have a closer look at your WikiProject. --Lusilier (talk) 15:13, 14 June 2013 (UTC)
 * I think that's the movie. We compared it to the deformation of quartz-rich rocks. Both minerals have different deformation mechanisms at different temperatures. The movie showed that very nicely. --Tobias1984 (talk) 16:29, 14 June 2013 (UTC)

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November 2013
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A barnstar for you!

 * Tx Blkutter. Nice to get some feedback on this. I'll browse around and see if I can add some more links. As for geotechnical engineering, it already has a subsection dedicated to offshore. Lusilier (talk) 00:25, 15 February 2014 (UTC)

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