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This is something I've been meaning to do for a few weeks, and I think I will shortly have brain for it. It arises because I often joke that, actually, as a geologist it's remarkably easy to get away with talking about work at parties - because while what I actually do is quite dull, every igneous geologist has their Top Five Volcanoes, and what's not to like about that. So! The idea is a series of posts on Cool Geological Shite, in (approximately) lay terms.
Stuff already on the list:
... and so on, and so forth. Is there anything you'd like me to add? I am very willing to take requests for this series!
Stuff already on the list:
- how we know how many days there were in a year three billion years ago
- top five volcanoes
- ENORMOUS MILLIPEDES (with gammy legs)
- how we could tell meteorites were from Mars before we'd ever been to Mars
- trilobites with eyes on stalks
- unravelling continental motion over geological history
- magnetic stripes IN THE OCEAN
- plate tectonics
- core polarity reversals
... and so on, and so forth. Is there anything you'd like me to add? I am very willing to take requests for this series!
(no subject)
Date: 2013-05-26 12:11 am (UTC)(no subject)
Date: 2013-05-30 01:17 am (UTC)(no subject)
Date: 2013-05-26 07:58 am (UTC)(no subject)
Date: 2013-05-30 01:16 am (UTC)(no subject)
Date: 2013-05-26 04:24 pm (UTC)(no subject)
Date: 2013-05-26 06:33 pm (UTC)(no subject)
Date: 2013-05-26 06:35 pm (UTC)(no subject)
Date: 2013-05-26 06:38 pm (UTC)Friends and Lavas
Date: 2013-05-26 07:59 pm (UTC)Re: Friends and Lavas
Date: 2013-05-30 01:16 am (UTC)Most of my favourites are currently active, but I am yet young. :-)
(no subject)
Date: 2013-05-26 09:47 pm (UTC)Or was the thing that told me that wrong?
(Something tells me that the actual answer to this may be more materials science / physics than geology, but hey, any insight welcome :-))
ETA: Incidentally, I'm guessing that the answer to your first question is relevant to my field... :-)
(no subject)
Date: 2013-05-30 01:15 am (UTC)The answer to your question requires distinction to be made between chemical division of the Earth (into crust, mantle and core) and rheological/mechanical division (lithosphere vs asthenosphere, i.e. brittle deformation vs ductile deformation/solid-state convection). Will happily natter about it but may have to do a technical version and a less technical version :-)
(no subject)
Date: 2013-05-28 09:14 am (UTC)(no subject)
Date: 2013-05-30 01:13 am (UTC)(no subject)
Date: 2013-05-30 08:19 am (UTC)(no subject)
Date: 2013-05-30 01:13 am (UTC)