I am always on the lookout for “strange” minerals or at least something rather unfamiliar to my limited mineralogical knowledge. Therefore, while attending the recent Rocky Mountain Federation show in Sandy, Utah, I nabbed a single and isolated specimen labeled “turgite” that was in the “sale bin”. After all, what is a frugal collector to do when something interesting and “cheap” pops out in front of you?
Graves Mountain Goethite var. Turgite. Note bladed and mammillary goethite covered by hematite. Golden-colored material in upper right is pyrophyllite. Length of specimen ~12 cm.
After returning home I begin to inquire about turgite in my reference books and on various web sites (esp. www.mindat.org). It turns out that turgite is not recognized as a true mineral since it is a mixture of both hematite and goethite. Some rockhounds continue to use the term as a variety of hematite [Fe2O3] and/or goethite [Fe+3O(OH)] as in “goethite var. turgite”.
Whatever the case, turgite usually appears as mammillary, botryoidal, stalactitic or bladed goethite that has its surface covered by hematite. Or perhaps the goethite has even partially altered to hematite. What makes turgite “famous” and quite collectable is the fact that the hematite often displays a beautiful spectrum of colored iridescence and resembles a fire agate (at least to me). Good specimens often are quoted for hundreds of dollars. Now my specimen cost me a couple of bucks and only has a few spots of golden iridescence—until closely examined under a binocular microscope!
As a bonus, my turgite specimen has some nice crystals/exposures of golden-colored pyrophyllite, an aluminum silicate [Al2(Si4O10)(OH)2]. There are also “spots” where tiny crystals of quartz are very loosely cemented and contain microcrystals of pyrite and rutile (both almost impossible to photograph).
Graves Mountain, where my specimen was collected, is perhaps Georgia’s best known collecting locality and is especially noted for specimen minerals (besides turgite and pyrophyllite) of kyanite [Al2(SiO4)O], pyrite [FeS2], rutile ([TiO2] world-class), lazulite [(MgFe+2)Al2(PO4)2(OH)2], and numerous others. In fact, the Mountain was originally mined for the aluminum-rich, refractory kyanite used in such items as spark plug insulators and later as insulated space shuttle tiles (T. Hanley, 2005).
It appears, from my limited knowledge, that the geology of Graves Mountain is quite complex! It lies in the “foothills” of the Appalachian Mountains, and is thrown into the Piedmont Physiographic section of the mountains. In introductory terms, the great Appalachian Belt resulted from the collision of parts of Gondwana (Africa and South America) with Laurentia (North America). The tectonic events started in the Ordovician (Taconic Orogeny), hit another high point in the Devonian (Acadian orogeny) and culminated in the Alleghenian Orogeny (Mississippian through Permian). These events were compressional in nature and produced the: 1) gently folded late Paleozoic rocks of the inner region, the Appalachian Plateau; 2) more steeply folded and faulted early to middle Paleozoic rocks of the Valley and Ridge (sandstone producing ridges; shale producing valleys); 3) the badly deformed metamorphic terrane of Precambrian and earliest Paleozoic rocks of the Blue Ridge; and 4) the complicated and varied terrane of faults, metamorphic rocks and igneous intrusions known as the Piedmont.
One section of the greater Piedmont is the Carolina Slate Belt, essentially an old volcanic terrane (rocks ~560 Ma; right around the Precambrian-Cambrian boundary) that has been subjected to later metamorphism. These rocks originated in an island arc system that was part of the proto-Atlantic Ocean. As proto-North America banged into Gondwana the island arc was “squeezed” and accreted (stuck onto) to North America (Allard, 1999). Perhaps this island arc appeared something like the modern Philippine Islands in the Sea of Japan.
Graves Mountain itself has a unique geology in that the principle rocks are pyritiferous kyanite granofels and sericite (type of muscovite) schist. Allard (1999) believes these rocks are the result of metamorphism of a hydrothermal alteration system---a subsurface hot water vent! I presume the surficial goethite (stable Fe+3) formed from the oxidation of pyrite (and perhaps lazulite) with the unstable Fe+2.
So, if you have not seen an iridescent goethite/hematite from Graves Mountain, take a look on the web. They can be beautiful specimens for your cabinet.
Allard, G. O., 1999, Graves Mountain, Slate Belt, Georgia Geology in Graves Mountain and Magruder Mine, Wilkes and Lincoln Counties Georgia, M. V. Hurst and C. Winkler III. Eds.: Southeastern Geological Society Guidebook Number 38. http://segs.org/wp/wp-content/uploads/2010/01/SEGS-Guidebook-38.pdf
Hanley, T., 2005, The New Georgia Encyclopedia: www.georgiaencyclopedia.org.