Bearded Geology

A new project I've been working on is now on the blog: the Arkansas Paleozoic Stratigraphy Database . This is a searchable database of the Paleozoic lithostratigraphic nomenclature in Arkansas with some related information. Within this database, you can search for stratigraphic names that not only are currently in use, but names that are now abandoned and replaced, as well as some that have recently been proposed. For each name you can find its age, any sub-divisions, proper usage as used by the USGS and AGS, historical usage (including past and present names), type locality or type area, type section location (if available), primary reference section location (if available), geographic distribution, etymology of the name, and citation of the original publication the name was used in. Also included for each name is a downloadable stratigraphic chart (PDF file) of either the Ozark or Ouachita/Arkansas River Valley region (whichever the unit is best exposed in) that illustrates the s

People looking at folds. Faces obscured to protect identities. ¡Mas folding!. Action shot of man pointing at a fold Normal fault in sandstones and shales Recently, I got to join a field trip to the Ouachita Mountains to discuss a spectacular structural event that took place in the Late Paleozoic. The strata of the Ouachita Mountains are dominantly sandstone and shale beds from the Cambrian to the Pennsylvanian that were deposited in an offshore, deep water environment somewhat similar to the deep water regime of the Gulf of Mexico. Beginning in the Mississippian Subperiod, a compressional event initiated as proto-North America collided with a small land mass (volcanic arc) to the south creating the Ouachita Mountains, a

I just ran across this really good Associated Press article titled " AP: At least 1,680 dams across the US pose potential risk ," from last month about dam hazards and recent dam failures. Here's a brief summary: A more than two-year investigation by The Associated Press has found scores of dams nationwide in even worse condition, and in equally dangerous locations. They loom over homes, businesses, highways or entire communities that could face life-threatening floods if the dams don’t hold. A review of federal data and reports obtained under state open records laws identified 1,688 high-hazard dams rated in poor or unsatisfactory condition as of last year in 44 states and Puerto Rico. The actual number is almost certainly higher: Some states declined to provide condition ratings for their dams, claiming exemptions to public record requests. Others simply haven’t rated all their dams due to lack of funding, staffing or authority to do so.  Deaths from dam failures

In 1857, twenty-one years after Arkansas gained statehood, the Arkansas legislature approved funding for the first geological survey of the state. Governor Elias N. Conway commissioned Dr. David Dale Owen to lead the survey beginning in 1857 to 1859 with funds of $4,800 per year, plus a salary of $1,800, and continuing from 1859 to 1860 with $6,000 per year, plus $2,500 salary. Owen was no stranger to government surveys; he also served as the State Geologist of Indiana (1837-1838) and Kentucky (1854-1857), as well as a geologist for the U.S. Government on a survey of Iowa, Minnesota, Wisconsin, and parts of Illinois and Nebraska (1839-1840, 1847-1850). David Dale Owen (image credit: Smithsonian Archives/ Wikimedia ) Owen commenced the Arkansas survey in Greene County with laboratory and field assistance of William Elderhorst - professor of chemistry and mineralogy at Rensselaer Polytechnic Institute, Edward T. Cox - who later would be State Geologist of Indiana, Robert Pete

While between rain storms earlier this week, I was able to get out into the field to do some outcrop work near Yellville, Marion County, Arkansas. I visited a roadcut near the US Hwy 412/AR Hwy 125 junction that is made of Lower Ordovician age  dolostone rock with some shale intervals. Interestingly, it has a couple thrust (reverse) faults on display: Thrust fault through carbonate rock (Facing north. Scale: 1.5 m staff with 10 cm intervals) A closer look at the fault in the lower-right corner of the previous image An even closer look at the fault. Lots of fault gouge. Notice the clasts that have rotated. Another thrust fault at the same roadcut (Facing north. Scale: 1.5 m staff) Some weeks ago, I was visiting a roadcut near Cotter, Arkansas  where I left with buckets of samples to analyze. One such sample was a large cobble that I slabbed on the rock saw and found these beautiful normal faults, with a baby graben flanked by two horsts: Faulted rock wi

Recent earthquake (orange dot) on Sept. 12, 2019 (via  USGS ) After a slow start with my research, I'm hoping that things will begin to move along much faster this fall. To help with the momentum, I've scheduled a meeting with my PhD committee, however, the best day to do so is tomorrow - Friday the 13th. Now, I'm not a superstitious person. After all, when has anything bad happened to me on Friday the 13th? I'll take my chances. However, early this morning - at 1:42am for those who are sticklers for precision - I had just woken up as I was rolling over in bed when suddenly an earthquake rumbled through. I heard my window blinds rattle and felt my bed vibrate, which brought me into a state of sleepy confusion unsure if it was an earthquake or just my neighbors on the other side of my wall. It was initially recorded as a 3.7 by the USGS with an epicenter 19 km (11.8 miles) south-southeast of Gassville, Arkansas just east of the Buffalo River in Baxter County. On

Hidden in the woods of Union County, Arkansas, a large unassuming sinkhole housing a small pond called the Norphlet Crater was added to the National Register of Historic Places in 2008. Although it's easy to overlook, this hole in the ground has quite a story to tell about the early days of the oil and gas industry in Arkansas and a gas well that could not be tamed. Topographic map view of Norphlet Crater In 1922, two years following the Hill No. 1 gas well drilled by Constantine Oil and Refining Company near El Dorado, Arkansas, oil and gas production in the area expanded dramatically and El Dorado became the hub for the petroleum industry in Arkansas. Small independent oil companies and major companies with internationally recognized names, such as Shell and Standard Oil, were all drilling in Union County, Arkansas. In the pine covered hills and farmland about eight miles northwest of El Dorado, near the small town of Norphlet, a cotton field [1] on a farm own

At 2:10 pm on Thursday, April 22, 1920, the small town of El Dorado, in Union County, Arkansas was busily going about its day. Over a dozen miles northwest, a drilling rig had just finished drilling the first productive oil well in Arkansas six days prior, the Hunter No. 1. However, just two miles [1]  southwest of town was another well being drilled that was going to make headlines as the first productive gas well in southern Arkansas.  Top left: land owners, Mr. and Mrs. Frank Hill. Center: the Hill No. 1 well blowing water, gas, and mud into the air. Bottom right: Constantine Oil and Refining geologist, J. J. Victor. [2] The Hill No. 1 well (Sec. 1, T.18S., R.16W.) operated by Constantine Oil and Refining Company of Tulsa, Oklahoma drilled to 2,226 feet, when it became an "unexpected 'gusher'" and a "great 'gasser'" [3] . The Monroe News-Star newspaper of Monroe, Louisiana reported that it received a kick (i.e. anomalous influx of

Measuring section and bagging samples in Marion County, Arkansas looking for clues from the Ordovician in some cherty dolostones. When you can't find a Jacob's staff in the office, you grab a broom stick and make your own...with black, semi-goth duck tape! Now to figure out how to cut slabs, make thin sections, and make sense of these weird tan lines.

Of all of the many types of maps that have been made for one purpose or another, I find one of the most enjoyable kind to look at are the old USGS topographic maps. These types have been made since 1879  (which also was the year that USGS was established) and thus, depict the human world that once was. This is particularly interesting since many localities have been mapped three or more times and we can see the evolution of human geography. For this reason and because I grew up within two miles of two towns that were abandoned during the 1960s as a dam was constructed and flooded the town sites, I'm easily fascinated by old maps that show towns and other old settlements and structures that have been abandoned. Old topo maps from across the country can be viewed and downloaded for free (in JPEG, TIFF, or PDF formats) from the USGS ( click here for more ). Admittedly, this USGS site is a huge rabbit hole for me to fall into and I've downloaded several topo maps from it, incl