Tag Archives: Jacupirangite

AGS Magnet Cove Field Trip with the Texas A&M Geology and Geophysics Society

AGS Magnet Cove Field Trip with the Texas A&M Geology and Geophysics Society
By Lea Nondorf

On Saturday, January 18, 2014, Bill Prior and I met up with sixteen students, ranging in age from freshman to seniors, from the Texas A&M Geology and Geophysics Society. We started the morning at 9 a.m. with a brief introduction on the geology of Magnet Cove at the Sinclair gas station along Highway 51 in Magnet Cove. Everyone was freezing, but you could tell they were super excited to start the day.

Magnet Cove is an area of unusual petrologic and mineralogic interest that derives its name from the presence of lodestone in the soil and from its basin-like shape. It is located in northern Hot Spring County, Arkansas, about 12 miles east of the city of Hot Springs. The diameter of Magnet Cove is about 3 miles (running northwest to southeast) with an overall area of less than 5 mi2 (Howard, 2007).

The Cove is an intrusive igneous body created by mantle-derived magma that pierced through existing Paleozoic sedimentary rocks (Figure 1, listed as Sm, MDa, and Ms) of the Ouachita Mountains approximately 100 million years ago (Late Cretaceous).

clip_image002

Figure 1. Generalized geologic map of Magnet Cove.

Stop 1

Our first stop was along HWY 270 (Figure 2) looking at the Mississippian Stanley Shale (359-323 million years old). The Stanley Shale is composed primarily of sandstones and shales deposited in a deep ocean basin. These deposits were later faulted, folded, and uplifted during the Ouachita Orogeny (Ouachita Mountains) approximately 323-307 million years ago (early to middle Pennsylvanian Period).

clip_image004

clip_image006

Figure 2. Looking at the Mississippian Stanley Shale. Everyone was clearly excited.

Stop 2

Our second stop was along Ross Cuttoff Road where we looked at the Garnet Pseudoleucite Nepheline Syenite (GPNS). Now say that mouth full five times fast. Although there were just a few boulders in the ditch, the phenocrysts of pseudoleucite were very prominent.

clip_image008

Figure 3. A sample of the Garnet Pseudoleucite Nepheline Syenite.

While learning all about GPNS, one particular nice gentleman stopped by to show us his great garnet, rutile, magnetite, and possibly brookite crystals that he collected from his yard. These crystals were absolutely amazing. As we were looking at his collection, another enthusiastic gentleman pulled up telling us all about his beautiful property and all of the different rocks for us to collect. Well of course we were excited, so we jumped in our vehicles and took off. As we were driving, Bill and I noticed how we were traversing over the syenite rim and out of the basin-Oops. When we arrived at his property, we were amazed by the beautiful view, particularly the view of the Magnet Cove basin. And, he did have a variety of rock, but mostly of red, white, and gray Arkansas Novaculite.

clip_image010

clip_image012

Figure 4. All smiles and thumbs up for Magnet Cove (background).

Stop 3

Here we stopped at the old American Titanium Pit where rutile (chemical composition of TiO2, or titanium oxide) was mined during WWII. We collected pyrite cubes and rutile from this pit. It was pretty muddy, but everyone managed. What troopers!

Stop 4

After lunch, we headed to the old Kimzey Magnetite Pit along Highway 51 where we collected lodestone, rutile, and garnet. A few also found pieces of possible Kidney-Ore hematite and phlogopite. This spot seemed to have it all. Plus, everyone enjoyed using the compass to determine whether or not they had lodestone. A stronger lodestone will really spin the compass needle. Also, the highly magnetic soils in this area make it almost impossible for anyone to use a compass in Magnet Cove.

Stop 5

About a quarter-of-a-mile west of stop 4 along Highway 51, we stopped to collect coarse-grained garnet, biotite ijolite. Ijolite is a feldspar-free, nepheline-rich igneous rock. At this location, we were able to pick up smaller biotite booklets that had weathered out of the boulders present in the ditch.

clip_image014

Figure 5. Checking out the garnet, biotite ijolite. Unfortunately, we needed a pick and sledge to break off pieces of the boulder for collecting, which no one had.

Stop 6

Adjacent to the old Kimzey Calcite Pit about one half mile west from Stop 5, a great carbonatite outcrop is exposed here just west of the bridge. This particular carbonatite looks identical to calcite, but is different in the fact that this carbonatite is an igneous rock derived from the mantle. Carbonatite even fizzes like calcite. Some other minerals that can be found with the carbonatite include carbonate-fluorapatite (light yellow-green), monticellite (brown), biotite, magnetite, pyrite and perovskite. Also, this is the type locality for kimzeyite, a dark brown zirconium-rich garnet (Howard, 2007).

clip_image016

clip_image018

Figure 6. Getting up close and personal with the carbonatite. Check out those rhombs.

Stop 7 and 8

Our last and probably most exciting stop was located IN Cove Creek. Although the day had warmed up quite nicely, the creek was still very frigid (and deep). After Bill showed off his awesome pyrite cubes with molybdenite that he had found in the creek 30 years ago, there was no turning back, we were finding pyrite cubes with molybdenite. Only Bill and I were lucky enough to have waders and boots, but that didn’t stop some of the others from jumping in. We trudged up the creek with no luck and quickly came back to where we started only to find nice pyrite pieces in the creek (of course). A few in the group pulled out nice hand-sized specimens with the molybdenite coating. How awesome!

clip_image020

Figure 7. Leaving the creek with gold in hand, fool’s gold that is.

clip_image022

Figure 8. Success in the cove with nice samples of pyrite.

clip_image024clip_image026

clip_image028 clip_image030

Figure 9. Close-ups of the pyrite found in Cove Creek.

Our final stop was just a few hundred feet past the pyrite area. Here we were able to venture to Cove Creek once again to look at jacupirangite, a dark-colored igneous rock composed primarily of pyroxene and magnetite (yes, jacupirangite does slightly attract a magnet). Some brave souls crossed the creek once again to get a closer look at the igneous rock and the lighter-colored syenite dikes. Just FYI, jacupirangite can become very slippery when wet. 😉

clip_image032

Figure 10. Jacupirangite in the creek.

References

Howard, J.M., 2007. Magnet Cove, A Synopsis of its geology, lithology, and mineralogy. Arkansas Geological Survey. AGES, Brochure Series 004. 11 p.

Advertisements