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Profile picture for user clock
By clock on June 19, 2008.


Microbiologist XX


Gramstain


Botswana Sceptic


Random Thoughts from Bennett Kankuzi

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More by this author

New URL for this blog
July 5, 2011
Earlier this morning, I have moved my blog over to the Scientific American site - http://blogs.scientificamerican.com/a-blog-around-the-clock/. Follow me there (as well as the rest of the people on the new Scientific American blog network
New URL/feed for A Blog Around The Clock
July 26, 2010
This blog can now be found at http://blog.coturnix.org and the feed is http://blog.coturnix.org/feed/. Please adjust your bookmarks/subscriptions if you are interested in following me off-network.
A Farewell to Scienceblogs: the Changing Science Blogging Ecosystem
July 19, 2010
It is with great regret that I am writing this. Scienceblogs.com has been a big part of my life for four years now and it is hard to say good bye. Everything that follows is my own personal thinking and may not apply to other people, including other bloggers on this platform. The new contact…
Open Laboratory 2010 - submissions so far
July 19, 2010
The list is growing fast - check the submissions to date and get inspired to submit something of your own - an essay, a poem, a cartoon or original art. The Submission form is here so you can get started. Under the fold are entries so far, as well as buttons and the bookmarklet. The instructions…
Clock Quotes
July 18, 2010
At bottom every man know well enough that he is a unique being, only once on this earth; and by no extraordinary chance will such a marvelously picturesque piece of diversity in unity as he is, ever be put together a second time. - Friedrich Wilhelm Nietzsche

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As a volcanologist, I am partial to impressive lava flows, especially in volcanoes that erupt material that you'd think wouldn't produce big flows. For example, there are quite a few volcanoes in the Chilean Andes that erupt dacite lavas, which are relatively viscous (sticky), so you might expect it to erupt explosively. However, you can get large dacitic to rhyolitic lava flows, quite commonly,…

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