Here’s the video of yesterday afternoon’s Geology Office Hours Google+ Hangout. Our main topic was advice for geology undergrads looking to apply to grad school, but we also began to answer a really big question about how the Earth has differentiated.
A reminder that the Geology Office Hours hangouts are now on holiday break. Next one is scheduled for Thursday, January 5, 2012.
By now, you’re probably well aware that I’ve been holding “Geology Office Hours” hangouts on Google+ most Monday and Thursday afternoons at 4:00pm CST (2200 GMT). The topics are usually unplanned and tend to go wherever the participants interests lie on any given day. We’ve had some great conversations on topics as diverse as the unfolding eruption sequence at El Hierro, approaches toward teaching geologic time to diverse audiences, the likelihood of fracking causing the early Movember Oklahoma earthquakes, and whether submarine volcanic eruptions could go Plinian, to mane just a few. I’ve been very pleased with the results and I intend to continue these hangouts for the forseeable future (after a holiday recess – more below).
After last Thursday’s hangout +Brian Schrock commented: “Maybe we could do an office hour sometime regarding grad school for us undergrads. I always seem lost in the grad school process despite all the help my professors are giving me.” I think that’s a great topic for one (or more) of these hangouts, so I’m designating it as the primary topic for this Monday’s hangout. Ideally I’d like to have a couple of other geology profs and/or current grad students share their experiences and insights, in addition to as many undergrads with questions as possible. I’ll plan to record the Hangout for those that can’t make it. Also, if there’s enough interest, possibly we’ll repeat this topic sometime in the new year.
For those interested in participating, you’ll need a Google Plus account and a computer (desktop/laptop/Android smartphone), ideally with either a built-in or USB webcam (I’ve had great results with a Logitech 720p Webcam Pro 9000). If you haven’t done a hangout before, read up on Hangouts and make sure to install the required Google Talk add-ons ahead of time (you’ll be prompted to do this).
Finally, I’m going to take a two week break for the holidays from my regularly scheduled hangouts after Monday’s hangout. If there are big geological events in breaking news I may hold an ad hoc hangout or two, as necessary. Otherwise, hangouts will resume on Thursday, January 5, 2012.
Although my specialty in geology is not as a sedimentologist, I did do my Ph. D. thesis in a basin full of turbidites (looking at provenance of conglomerate clasts). Thus, the news of yesterday’s passing of Arnold Bouma gives me a reason to tack on one more set of geology field photos of the Bouma Sequences I knew best. In memoriam…
It’s all fine and good to enjoy the breathtaking geological vistas of our National Parks, but what drives the student of the Earth is reading her rocks to attempt to understand her past. So go ahead and get your noses up against this outcrop and do your best to interpret what you can see here. This is a “no hammer” outcrop. Take as much time as you need and place your answers in the comments.
Back in June 2005, before I owned a GigaPan (indeed, before GigaPans even existed), I passed through Bryce Canyon National Park just in time for an afternoon cloudburst. So for my Wednesday entry in Evelyn Mervine’s Geophoto Week I present you with some squeaky clean hoodoos.
“This color view of a mineral vein called “Homestake” comes from the panoramic camera (Pancam) on NASA’s Mars Exploration Rover Opportunity. The vein is about the width of a thumb and about 18 inches (45 centimeters) long. Opportunity examined it in November 2011 and found it to be rich in calcium and sulfur, possibly the calcium-sulfate mineral gypsum.” –NASA Image Credit: NASA/JPL-Caltech/Cornell/ASU
Back here on Earth you may be more familiar with veins filled with quartz or calcite. But make no mistake, if you find an environment on Earth that resembles Mars, you can find plenty of gypsum veins here, too. I had the good fortune to GigaPan just such an area on the south side of the San Rafael Swell two summers ago. The GigaPan below (and subsequent photographs) illustrate a variety of gypsum veins, as well as some nice faults, crosscutting the Jurassic Summerville Formation (itself composed mostly of shale and bedded gypsum evaporites).
A little over a month ago, while my geoblogging juices were really flowing, a late night rumble inadvertently inspired the theme for this month’s Accretionary Wedge. My own blogging pace has slacked off since then and perhaps yours has too, what with the pressures of the end of the semester and #AGU11. With any luck though, we’ll all have a chance to take a little time between final exams and the holidays to revisit our geoblogs and spread some geological holiday cheer.
Right, then. Your mission, should you choose to accept it, is to relate the story of the most memorable or significant geological event that you’ve directly experienced.
What we seek for Accretionary Wedge #41 is an account of a geologic event that you experienced firsthand. It could be an earthquake, a landslide, a flood, a volcanic eruption, etc. (but don’t feel compelled to stick to the biggies – weathering, anyone?) – some geologic process that you were able to directly observe and experience. The event itself need not have been dramatic or life threatening, or it may have been. The event may have taken place before you were trained as a geologist or since (or maybe you don’t have any geologic training at all). Ideally, it’s something you can describe from firsthand experience, even if you didn’t experience it at ground zero. Events that my have happened while you were at a safe distance, but of which you were able to directly experience the aftermath (while the geologic evidence was still fresh) are certainly acceptable (perhaps you’ve been involved in relief or research efforts immediately following a major geological event). And by all means, don’t limit yourself to a single event if you’ve experienced more that one!
The story you weave is, of course, up to you. Pictures are always a plus (bonus points for audio or video) – you know we’re all adrenaline junkies on one level or another. I’m posting this call during the waning hours of the Paleozoic (time’s almost up, trilobites) but you have until the beginning of the Anthropocene to get your submissions posted. I’ll do my best to gather it all together sometime before Pangea Ultima gets together.