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Virginia Polytechnic Institute and State University

Manganese mineralization hosted by the Rocky Gap Sandstone in Bland County, Virginia

Abstract

dc:description.abstract

The Stange Mine was one of the largest and most important manganese mines in Virginia . The mineralization is hosted by the Rocky Gap Sandstone of Devonian age. It is a medium to coarse grained sandstone deposited on a shallow marine shelf in a warm water environment. Conodont color indexes indicate the host was buried as deeply as 4 km and heated to 150°C. Romanechite, goethite, and pyrolusite are the three most important oxides, and can coexist at 25°C and 1 bar. In polished section romanechite has three textures: (1) microcrystaline patches, (2) fibers. Pyrolusite occurs as occurs in three textures : botryoidal bands, and (3) interwoven psuedomorphs after manganite. Goethite (1) a mottled and spotted variety characteristic of hand samples with sedimentary layering, (2) a homogeneous goethite , and (3) a banded goethite that occurs as a microbreccia. The paragenesis of the minerals was determined using polished sections, hand samples, and field relationships. Electron microprobe analyses were used to find a nominal chemical formula for romanechite. This formula was used to estimate the Gibbs free energy of formation for romanechite. Manganese deposits in sedimentary rocks are formed by sedimentary processes, submarine volcanic activity, diagenetic activity, residual weathering, and ground water deposition. The stratabound nature, regional extent, burial history, and proximity to fractures on the crest of an anticline indicate the deposit at the Stange Mine was formed by ground water at the interface between deeply-percolating, oxygenated meteoric water and reducing manganese and iron bearing, formation waters where the iron and manganese were precipitated by oxidation .

Degree

thesis:*
Name thesis:degree_name
M.S.
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geological Sciences
Department dc:contributor.department
Geological Sciences
Grantor dc:publisher
Virginia Polytechnic Institute and State University
Year dc:date.issued
1985

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Levy, David J.

Rights

dc:rights
Statement dc:rights
  • In Copyright
Language dc:language.iso
en

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/10919/104304
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/104304

Chain of custody

source
Harvested from
Virginia Tech
Base URL
vtechworks.lib.vt.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
related terms
citation

Levy, David J.. Manganese mineralization hosted by the Rocky Gap Sandstone in Bland County, Virginia. masters thesis, Virginia Polytechnic Institute and State University, 1985. http://hdl.handle.net/10919/104304