ID: 1106
rec_id: 1106
site_name: Ketcherside Gap deposit
oremin: Actinolite exhibits colour-zoned prismatic to fibrous grains replacing clinopyroxene, garnet, and early scapolite"" (Lowell and Noll, 2001, p. 379). ""Colour-zoned prismatic to fibrous amphibole with colourless to pale green pleochroism is the dominant late skarn phase in both volcaniclastic and dolomite protoliths"" (Lowell and Noll, 2001, p. 388).
devel: small former copper mine
json: {"id":"http:\/\/mrdata.usgs.gov\/asbestos\/record\/1106","type":"Feature","geometry":{"type":"Point","coordinates":[-90.660120491735,37.513249845331]},"properties":{"state":"MO","county":"Iron","site_name":"Ketcherside Gap deposit","devel":"small former copper mine","latitude":"37.5132","longitude":"-90.66","oremin":"Actinolite exhibits colour-zoned prismatic to fibrous grains replacing clinopyroxene, garnet, and early scapolite\"\" (Lowell and Noll, 2001, p. 379). \"\"Colour-zoned prismatic to fibrous amphibole with colourless to pale green pleochroism is the dominant late skarn phase in both volcaniclastic and dolomite protoliths\"\" (Lowell and Noll, 2001, p. 388).","assocmin":"numerous minerals reported--see Lowell and Noll (2001)","hostrock":"scapolite skarn","reference":[{"citation":"Sides (1981)","onlink":"http:\/\/gsabulletin.gsapubs.org\/content\/92\/9\/686.full.pdf+html","source":"ofr20061211","reference":"Sides, R.J., 1981, Geology of the Ketcherside Mountain area, southeastern Missouri, and the source of Grassy Mountain Ignimbrite: Geological Society of America Bulletin, v. 92, p. 686-693."},{"citation":"Lowell and Noll (2001)","source":"ofr20061211","reference":"Lowell, G.R., and Noll, P.D., Jr., 2001, Fe-Cu-Au-bearing scapolite skarn in moat sediments of the Taum Sauk Caldera, southeastern Missouri, USA: Mineralogical Magazine, v. 65, no. 3, p. 373-396."}]}}
url: https://mrdata.usgs.gov/asbestos/show-asbestos.php?rec_id=1106