Tennessee Field Diamonds

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Tennessee Field Diamonds. A treasure 485 million years in the making. Similar crystals are found in many places throughout the world. See Quartzpage.de. Douglas Dam (locality 5) One of the most prolific sites yet found: Veins and breccia zones in the upper part of the Mascot Dolomite. - PowerPoint PPT Presentation

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  • Tennessee Field Diamonds

    A treasure 485 million years in the making.

  • Similar crystals are found in many places throughout the world.See Quartzpage.de

  • Douglas Dam(locality 5)One of the most prolific sitesyet found:Veins and breccia zones in the upper part of the Mascot Dolomite

  • FeaturesExposed by winter draw-down

    Stratigraphy fossils structure

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • 36.5625, -83.889722

  • Weathering of carbonate bedrock Crystals freed from carbonate bedrock now in residual clay.

    Crystal from Pakistan. The inclusions are brown in transmitted light.Crystals sold to me as being from Tibet. Double terminated crystals are illustrated on the internet from cracks in Septarian nodules from the French Alps (http://www.quartzpage.de/dia_text.html), and northern Ohio (http://www.vasichkominerals.com/Lamereaux1.html). The famous Herkimer diamonds occur in irregular vugs and cavities within undeformed Cambrian dolomites in upstate New York. Many images can be found online, for example http://www.quartzpage.de/her_text.html. Phases of SiO2, with typical geothermal gradient ranges. High Pressure phases coesite and stishovite not shown. Note that increasing pressure is downQuartz crystal showing typical morphology, and stereo plot.Index map of known locations with Herkimer type quartz, along with barite and zinc deposits, andmajor faults. Basemap from the Geologic Map of Tennessee, 1:250,000, with shaded relief overlay.*Brief geologic history of East Tennessee, in four stages.Stratigraphic units of the Valley and Ridge Province of East Tennessee.Time Line, with age range for crystals relative to potential open space. Crystals found in the Knox breccias had all the time from shortly after the formation of the unconformity to the relatively recent geologic past, while those in the Sevier Shale and any younger rocks could not have formed in the interval before the orogeny. There were good images available of karstic processes and paleokarstic collapse breccias at Zeng, H., Wang, G., Janson, X., Loucks, R., Xia, Y., Xu, L., and Yuan, B. (2011). Characterizing seismic bright spots in deeply buried, Ordovician Paleokarst strata, Central Tabei uplift, Tarim Basin, Western China. GEOPHYSICS, 76(4), B127B137

    Douglas Dam area at high water.Douglas dam area at mid water.Mapping features and shoreline on the day I was there.Mapping features.Interpretative geologic map.Lets go down and look at some of the geologic outcrops and features.Outcrop with post-Knox unconformity contact. Lenoir Limestone on top.Unconformable surface, detail.Fossiliferous Lenoir Limestone just above the unconformity.Orthocone (Michelinoceras) beds above the Lenoir Limestone.Sevier Shale along shore farther to the south.Dolomite veins in brecciated dolomite.Universality of breccias. This one is on Mars.Outcrop with the pyrobitumen, where I washed it off.Closer view of pyrobitumen vein.Close up, wet.Dry. You can see the quartz crystals better.Calcite-filled vugs as a growth medium, a potential explanation for some of the things we see in these crystals.Closer view.Large strange chert and calcite nodular feature.Close-up of massive calcite