Eric Roston on Dot Earth
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Labels: blogs, books, climate change, india
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MAK was there too, but for some reason I don't have him in any of my photos... Sorry!
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I hereby initiate a geoblogosphere meme...
What are ten things that every geology major ought to know about? The only restriction is you're not allowed to list anything that has already been listed by a previous geoblogger. You don't have to list everything, just ten important things.
My ten:
Please, add to these... So far Mel at Ripples in Sand, Chris at GoodSchist, Eric at The Dynamic Earth , Lockwood at Outside the Interzone, Bryan at In Terra Veritas, Kim at All My Faults..., Garry at Geotripper, and the Short Geologist at Accidental Remediation have added their top tens. Plus, Silver Fox at Looking For Detachment posted 4, and the comments section on this post has another suggestion from Michael Welland (of Through the Sandglass) and others. That's 85 things to know... and counting...
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The western half of the Arabian Peninsula contains not only large expanses of sand and gravel, but extensive lava fields known as haraat (harrat for a named field). One such field is the 14,000-square-kilometer Harrat Khaybar, located approximately 137 kilometers to the northeast of the city of Al Madinah (Medina). The volcanic field was formed by eruptions along a 100-kilometer, north-south vent system over the past 5 million years. The most recent recorded eruption took place between 600-700 AD.
Harrat Khaybar contains a wide range of volcanic rock types and spectacular landforms, several of which are represented in this astronaut photograph. Jabal ("mountain" in Arabic) al Qidr is built from several generations of dark, fluid basalt lava flows. Jabal Abyad, in the center of the image, was formed from a more viscous, silica-rich lava classified as a rhyolite. While the 322-meter high Jabal al Qidr exhibits the textbook cone shape of a stratovolcano, Jabal Abyad is a lava dome; a rounded mass of thicker, more solidified lava flows. To the west (image top center) is the impressive Jabal Bayda'. This symmetric structure is a tuff cone, formed by eruption of lava in the presence of water. The combination produces wet, sticky pyroclastic deposits that can build a steep cone structure, particularly if the deposits consolidate quickly.
White deposits visible in the crater of Jabal Bayda' and two other locations to the south are sand and silt that accumulate in shallow, protected depressions. The tuff cones in the Harrat Khaybar suggest that the local climate was much wetter during some periods of volcanic activity. Today, however, the regional climate is hyperarid - little to no yearly precipitation - leading to an almost total lack of vegetation.
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The scenic Wit Mfolozi River Gorge in South Africa displays unique and spectacularly preserved sedimentary structures caused by microbial mats that colonized a sandy coastal area that are 3 billion years old. A comparison with modern microbial mats in a similar setting today suggests that the mat-constructing microbiota may have been cyanobacteria, possibly the oldest known in Earth history (GSA Today, October 2008).
In collaboration with the Society for Sedimentary Geology (SEPM), the Geological Society of America (GSA) and as part of the Year of the Planet Earth (IYPE), the Geological Society of South Africa (GSSA) is establishing the "Wit Mfolozi River Area" as a Geoheritage Site. This Geoheritage Site will serve visiting scientists, students and the interested public in leaning more about the Archean world and Earth's earliest life.
With the support of funds raised around the world, GSSA will set up the logistical and administrative infrastructure necessary to preserve and make this site available to all. This includes, for example, the construction of secure access to the site, installment of signs explaining the details of biogenic sedimentary structures at different spots in the outcrop and also measures to protect the site from damaging flooding by the river.
For further information about the site contact Roger Price (Geosite Conservation Committee, GSSA - rprice@geoscience.org.za), Nora Nofke (Old Dominion University and GSA Division of Geobiology and Geomicrobiology - nnofke@odu.edu) or Wesley Hill (GSA - hill@geosociety.org).
For donations to the fund for the site please contact Theresa Scott (SEPM - tscott@sepm.org).
Thank you very much,
Nora Noffke
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"(1) It is easy to obtain confirmations, or verifications, for nearly everyPopper concluded that "One can sum up all this by saying that the criterion of the scientific status of a theory is its falsifiability*, or refutability, or testability."
theory - if we look for confirmations. (2) Confirmations should count only
if they are the result of risky predictions ... (3) Every "good" scientific
theory is a prohibition: it prohibits certain things to happen ... (4) A theory
that is not refutable by any conceivable event is non-scientific.
Irrefutability is not a virtue of a theory (as people often think) but a
vice. (5) Every genuine test of a theory is an attempt to falsify it, or
to refute it. ... (6) Confirming evidence should not count except when it is the
result of a genuine [italics his] test of the theory; and this means that it can
be presented as a serious but unsuccessful attempt to falsify the theory."
"This was a theory of trial and error - of conjectures and refutations... IIt goes without saying that the initial conjecture must be triggered by some observations; It is not something pulled out of thin air.
thought ... that scientific theories were not the digest of observations, but
that they were inventions - conjectures boldly put forward for trial, to be
eliminated if they clashed with observations; with observations which were
rarely accidental but as a rule undertaken with the definite intention of
testing a theory by obtaining, if possible, a decisive refutation."
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As for why geobloggers bother with blogging, the most common response was that they wanted to share information and perspectives with others, followed closely by the sense of connecting with other interested individuals and public outreach. A significant minority also mentioned the pleasure they take in the act of writing, or a desire to practice/improve their writing skills. Some comments from the survey on why geobloggers blog:
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Where are these people coming from? What's the referring page that links them to NOVA Geoblog? Turns out SiteMeter can tell me that too! A lot of visitors were brought here by web searches, including a lot of image searches. People searched on Google or Yahoo for "biofuels cartoon," "totem pole tasmania," "unconformities in the grand canyon," "geoblog," and many more. Others were linked to my site from other geology blogs, and a few came from my NOVA website and my Blackboard courseware platform.
If this sort of stuff interests you (and I can't imagine why it should), you can explore details of each of these searches on the SiteMeter's "NOVA Geoblog" page (click on the SiteMeter icon below the counter in the right column, or click here).
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If you don't have time to sift through all of them, a "best of" list of 21 maps is compiled here.

Labels: blogs, global warming, humor
Labels: blogs
