12.11.2014 Views

Download Guidebook as .pdf (2.2 Mb) - Carolina Geological Society

Download Guidebook as .pdf (2.2 Mb) - Carolina Geological Society

Download Guidebook as .pdf (2.2 Mb) - Carolina Geological Society

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

______________________________________________________________________________________<br />

2008 annual meeting – Spruce Pine Mining District: Little Switzerland, North <strong>Carolina</strong><br />

______________________________________________________________________________________<br />

STOP No. 1 – The Sink Hole at Bandana: A Blue Ridge mica mine<br />

reveals Its prehistoric p<strong>as</strong>t<br />

By: Peter R. Margolin<br />

Ple<strong>as</strong>e see paper located in front part of this guidebook.<br />

STOP No. 2 – Spruce Pines mines – Overlook and handout<br />

By: Samuel E. Swanson, Department of Geology, University of Georgia<br />

Athens, GA 30602<br />

Ple<strong>as</strong>e see paper located in front part of this guidebook.<br />

STOP No. 3 -- Vulcan Materials Company -- Spruce Pine Quarry<br />

By: Jim Stroud and Marion Wiggins, and Jeff Panther<br />

Vulcan Materials Company’s Spruce Pine Quarry in Spruce Pine, North <strong>Carolina</strong> w<strong>as</strong><br />

originally called the Bear Creek Quarry or Mayland Stone and w<strong>as</strong> opened in 1978. It is<br />

located in the Blue Ridge Mountain Province. The topography at Spruce Pine Quarry<br />

consists of relatively steep terrain with high relief, typical of the Blue Ridge Province of<br />

North <strong>Carolina</strong>.<br />

Spruce Pine Quarry is underlain by the Late PreCambrian Ashe Metamorphic Suite of the<br />

Spruce Pine thrust sheet. This thrust sheet is part of the Blue Ridge thrust complex and<br />

consists of amphibolite facies met<strong>as</strong>edimentary rocks. These rocks are described <strong>as</strong><br />

amphibolite, biotite schist, biotite-amphibole gneiss, and biotite-amphibole schist.<br />

Quartz veining is widespread.<br />

The major minerals observed in these rocks are feldspar, amphibole, biotite, and quartz.<br />

Garnet and pyrite are also evident in trace (

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!