// Copyright (c) mindat.org 1993-2009 function j(lat,long) {var point = new GLatLng(lat,long); map.setCenter(point, 16);} function cm(lat,long,html,name) { var point = new GLatLng(lat,long); var marker = new GMarker(point,{icon:icon, title:name}); GEvent.addListener(marker, "click", function() { marker.openInfoWindowHtml(jsunpack(html)); // // map.panTo(marker.getPoint()); var zoom = map.getZoom(); if(zoom<9) zoom=9; map.setZoom(zoom); map.setCenter(marker.getPoint(), zoom); }); GEvent.addListener(marker,"mouseover", function() { marker.setImage("kml-gm-o.png"); }); GEvent.addListener(marker,"mouseout", function() { marker.setImage("kml-gm.png"); }); clus.AddMarker(marker,name); } function jsunpack(txt) { txt=txt.replace(/~~/,"
"); txt=txt.replace(/~!/,""); txt=txt.replace(/~\)/,"
Reference: "); return (txt); } function loadPoints() { cm(40.6916666667,-76.3,"~~4079.html\">Forestville, Schuylkill Co., Pennsylvania, USA
~)Finkelman, R.B. & Mrose, M.E. (1977) American Mineralogist: 62,316-320.
","Forestville, Schuylkill Co., Pennsylvania, USA"); cm(40.7666666667,-76.5583333333,"~~23693.html\">Burnside, Northumberland Co., Pennsylvania, USA~)Mineralogy associated with burning Anthracite deposits of Eastern Pennsylvania, D. M. Lapham, J. H. Barns, W. Downey Jr. and R. B. Finkelman, Min. Rescs. Report #78, 1980
~$~!0401575001208276518.jpg\">Downeyite
© Ł Kruszewski 08

2 mm rock sample covered by very small white crystals of downeyite - natural selenium dioxide. The mineral is a coal-fire byproduct, formed by gas desublimation on a burning coal dump. The mineral is surprisingly unstable - its so extremely ...~%","Burnside, Northumberland Co., Pennsylvania, USA"); }