{"id":672,"date":"2009-02-27T12:44:38","date_gmt":"2009-02-27T12:44:38","guid":{"rendered":"http:\/\/geologicalintroduction.baffl.co.uk\/?p=672"},"modified":"2026-04-08T14:24:14","modified_gmt":"2026-04-08T14:24:14","slug":"9-mining","status":"publish","type":"post","link":"https:\/\/geologicalintroduction.baffl.co.uk\/?p=672","title":{"rendered":"9. Mining"},"content":{"rendered":"<h3><strong>9.1 PRIMITIVE EXTRACTION<\/strong><\/h3>\n<p>I include under mining all human activities concerned with the extraction of inert natural materials. As such, the extraction\u00a0of stone for construction, is mining, and at the beginning, perhaps the easiest was the excavation in relatively soft sandstones, to enlarge the original caves where the people dwelt (<a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/?p=323#attachment_324\">fig. 89<\/a>). Also, rock blocks shaped by natural jointing were used originally possibly only for religious purposes (fig. 163B),<\/p>\n<div id=\"attachment_913\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stonehenge.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-913\" class=\"wp-image-913 size-medium\" title=\"stonehenge\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stonehenge-440x258.jpg\" alt=\"\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-913\" class=\"wp-caption-text\"><em>Figure 163B &#8211; Stonehenge, one of the earliest human utilisation of stone.<\/em><\/p><\/div>\n<p>but later they started building wall protections and houses by \u201cdry packing\u201d carefully selected well shaped blocks (fig. 163C).<\/p>\n<div id=\"attachment_3003\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C30S64-1.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3003\" class=\"wp-image-3003 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C30S64-1-600x396.jpeg\" alt=\"\" width=\"600\" height=\"396\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C30S64-1-600x396.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C30S64-1-1024x676.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C30S64-1-768x507.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C30S64-1.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3003\" class=\"wp-caption-text\">Figure 163C &#8211; The remains of a Bronze Age village (Cit\u00e2nia de Briteiros, Portugal).<\/p><\/div>\n<p>As technology progressed people realised \u00a0they could improve on the natural jointing by using very simple chisels for digging grooves along predetermined lines, in order to create an artificial joint through which the rock would fracture. \u00a0A good example can be seen within the Moorish castle at Sintra, Portugal (Fig. 164), \u00a0built during the 8th century.<\/p>\n<div id=\"attachment_676\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/moorcastle.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-676\" class=\"wp-image-676 size-medium\" title=\"Moorish castle, Sintra\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/moorcastle-440x322.jpg\" alt=\"Figure 165 - Wall of the Moorish castle where the block is located (Sintra, Portugal).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-676\" class=\"wp-caption-text\"><em>Figure 164 &#8211; Inner view of the Moorish castle wall\u00a0(Sintra, Portugal).<\/em><\/p><\/div>\n<p>As figure 165 shows, two lines of grooves were chiseled on the granite boulder located within the castle area, and along one of them a neat break had already been accomplished. Surely this is a block in preparation for repairing the wall.<\/p>\n<div id=\"attachment_674\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stonespliting.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-674\" class=\"wp-image-674 size-medium\" title=\"primitive stone splitting\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stonespliting-440x586.jpg\" alt=\"Figure 165 - Granite boulder halfway split to shape a block for the castle wall (Sintra, Portugal).\" width=\"440\" height=\"586\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stonespliting-440x586.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stonespliting-768x1024.jpg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stonespliting.jpg 960w\" sizes=\"auto, (max-width: 440px) 100vw, 440px\" \/><\/a><p id=\"caption-attachment-674\" class=\"wp-caption-text\"><em>Figure 165 &#8211; Granite boulder halfway split to shape a block for the castle wall (Sintra, Portugal).<\/em><\/p><\/div>\n<h3>Just as primitive, is the use of laterite for the construction of houses. This material occurs in regions with high precipitation. India is a great example, with their well known monsoons. There, I saw laterite being mined (<a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/laterite.jpg\">fig. 31D<\/a>) by cutting it in blocks (fig. 166) for the construction of houses. These blocks are rather large, about 0.5 x 0.3 x 0.1 metres but they are not too heavy, so they can be handled reasonably easily. Also, I was told no cementing material is needed since, with time and the enormous amounts of rain they have, the iron in the laterite is mobilised some more and the blocks seal themselves.<\/h3>\n<div id=\"attachment_2272\" style=\"width: 650px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P1010036.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-2272\" class=\"wp-image-2272 size-full\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P1010036.jpg\" alt=\"\" width=\"640\" height=\"480\" \/><\/a><p id=\"caption-attachment-2272\" class=\"wp-caption-text\">Figure 166 &#8211; Laterite construction blocks (Orissa, India).<\/p><\/div>\n<h3><strong>9.2 SIMPLE EXTRACTION<\/strong><\/h3>\n<p>With the present technology, inert materials can be extracted in many sophisticated ways. Here I just refer to some which have been extracted since time immemorial and even today are extracted in a relatively simple manner. River sand dredging (fig. 166) is one of them. This job that initially was done entirely manually is now done in a totally mechanised manner.<\/p>\n<div id=\"attachment_685\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/sanddredging.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-685\" class=\"wp-image-685 size-medium\" title=\"sand dredging, Portugal\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/sanddredging-440x322.jpg\" alt=\"Figure 168 - Sand dredging (Douro River, Portugal).\" width=\"440\" height=\"322\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/sanddredging-440x322.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/sanddredging-1024x749.jpg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/sanddredging.jpg 1280w\" sizes=\"auto, (max-width: 440px) 100vw, 440px\" \/><\/a><p id=\"caption-attachment-685\" class=\"wp-caption-text\"><em>Figure 167 &#8211; Sand dredging (Douro River, Portugal).<\/em><\/p><\/div>\n<p>Note that this sand is not extracted to permit navigation, but rather for construction. A consequence of this huge and continuous suction of sand, is the rejuvenation of the river&#8217;s energy level, thus increasing enormously its erosional power, with disastrous consequences for \u00a0bridges, etc. To me this is a very short sighted approach because sand of the same quality can be obtained by minor additional processing of the fines which develop at stone crushers, and otherwise has to be discarded as waste, occupying unnecessary space an \u00a0adding costs to the final rehabilitation.<\/p>\n<p>Continuing with rivers, there is also the mining of gold and diamonds, \u00a0which originally was done \u00a0by panning but now, even<span class=\"Apple-converted-space\">\u00a0 <\/span>though done using more mechanical methods, can still be considered a one man operation, with very few helpers.\u00a0 The example I show, is for diamonds along the Vaal River, in South Africa (item 6.4.1, <a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/?p=323#attachment_358\">fig. 99<\/a>), where \u00a0a rather simple but effective mechanical method of grading the clasts is being used (fig. 168),<\/p>\n<div id=\"attachment_688\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/diamondaluvial.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-688\" class=\"wp-image-688 size-medium\" title=\"alluvial diamond mining, SA\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/diamondaluvial-440x292.jpg\" alt=\"Figure 169 - Mechanical grading of the river gravel (Ulco Area, Orange River, South Africa).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-688\" class=\"wp-caption-text\"><em>Figure 168 &#8211; Mechanical size sorting\u00a0of the river gravel (Ulco Area, Vaal River, South Africa).<\/em><\/p><\/div>\n<p>and figure 169 showing the owner of the enterprise doing the final sorting. It was impressive how fast his hand moved, but I do not think many diamonds were missed.<\/p>\n<div id=\"attachment_690\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/diamondsorting.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-690\" class=\"wp-image-690 size-medium\" title=\"diamond hand sorting, SA\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/diamondsorting-440x659.jpg\" alt=\"Figure 170 - Final hand sorting for diamonds (Ulco Area, Orange River, South Africa).\" width=\"440\" height=\"659\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/diamondsorting-440x659.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/diamondsorting-683x1024.jpg 683w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/diamondsorting.jpg 854w\" sizes=\"auto, (max-width: 440px) 100vw, 440px\" \/><\/a><p id=\"caption-attachment-690\" class=\"wp-caption-text\"><em>Figure 169 &#8211; Final hand sorting for diamonds (Ulco Area, Vaal River, South Africa).<\/em><\/p><\/div>\n<p>Another one man operation I came across, was the mining of a gold rich quartz vein in what was \u00a0still Rhodesia. Actually, in this case it was a partnership of two. This time a grader was not necessary, but rather a stamping mill\u00a0 (figure 170) <span class=\"Apple-converted-space\">\u00a0<\/span>to crush the ore, which is also rather simple but very effective.<\/p>\n<div id=\"attachment_692\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldcrushing.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-692\" class=\"wp-image-692 size-medium\" title=\"gold ore crushing, Zimbabwe\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldcrushing-440x642.jpg\" alt=\"Figure 171 - One man gold mine operation, ore stamping mill (Bulawayo region, Zimbabwe).\" width=\"440\" height=\"642\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldcrushing-440x642.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldcrushing.jpg 876w\" sizes=\"auto, (max-width: 440px) 100vw, 440px\" \/><\/a><p id=\"caption-attachment-692\" class=\"wp-caption-text\"><em>Figure 170 &#8211; One man gold mine operation, ore stamping mill (Bulawayo region, Rhodesia).<\/em><\/p><\/div>\n<p>Needed too, was a vibrating table to sort the heavy material (fig. 171). Note the pale, rather thick streak of heavies at the top of the table, on the left hand side. Unfortunately for the owners, this streak was not just gold but rather predominately sulphides with minor gold specks. For the final separation they were still using mercury which makes an amalgam with the gold, and then the mercury was \u201cboiled out\u201d.<\/p>\n<div id=\"attachment_694\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldconcentr.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-694\" class=\"wp-image-694 size-medium\" title=\"gold concentration, Zimbabwe\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldconcentr-440x293.jpg\" alt=\"Figure 172 - Vibrating table (Bulawayo region, Zimbabwe)\" width=\"600\" height=\"400\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldconcentr-440x293.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldconcentr-1024x684.jpg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/goldconcentr.jpg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-694\" class=\"wp-caption-text\"><em>Figure 171 &#8211; Vibrating table (Bulawayo region, Rhodesia)<\/em><\/p><\/div>\n<h3><strong>9.3 OPEN CAST<\/strong><\/h3>\n<p>As the name indicates, open cast means mining on the surface. Of these, the simplest is the extraction of stone for construction and since there is construction everywhere, stone quarries also exist everywhere. Here I only want to show not so much the importance of the health regulations but rather, their implementation. Figure 172 shows an entirely dustless loading operation in a granite quarry in South Africa,<\/p>\n<div id=\"attachment_696\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/quarryclean.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-696\" class=\"wp-image-696 size-medium\" title=\"clean quarry operation \" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/quarryclean-440x324.jpg\" alt=\"Figure 173 - Dustless dump loading operation in a quarry (Halfwayhouse, South Africa).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-696\" class=\"wp-caption-text\"><em>Figure 172 &#8211; Dust free dump loading operation in a quarry (Halfwayhouse, South Africa).<\/em><\/p><\/div>\n<p>and figure 173 shows a limestone quarry in Portugal with so much dust, that one has difficulty in distinguishing the crusher unit on the right hand side. Probably, because Portugal belongs to the EU, its mining laws are actually more strict than those in South Africa but, obviously in Portugal there is no apparent law enforcement, since the photo was taken from a moderately important road with considerable traffic of all sorts.<\/p>\n<div id=\"attachment_698\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/quarrydust.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-698\" class=\"wp-image-698 size-medium\" title=\"quarry dust, Portugal\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/quarrydust-440x273.jpg\" alt=\"figure 174 - Quarry without any dust prevention (Serra de Janeares, Portugal)\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-698\" class=\"wp-caption-text\"><em>Figure 173 &#8211; Quarry with no dust prevention (Serra de Janeares, Portugal).<\/em><\/p><\/div>\n<p>This is sad because quarry dust is easily prevented by simply spraying the haul roads, the blast heaps, as well as all the crushing units. That is, all the sectors where dust may develop, with the exception of course, of the dust caused by the blast (fig. 174).<\/p>\n<div id=\"attachment_700\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/blast.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-700\" class=\"wp-image-700 size-medium\" title=\"blast in progress, SA\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/blast-440x335.jpg\" alt=\"Figure 175 - Blasting in progress (Ulco, South Africa).\" width=\"600\" height=\"440\" \/><\/a><p id=\"caption-attachment-700\" class=\"wp-caption-text\"><em>Figure 174 &#8211; Blasting in progress (Ulco, South Africa).<\/em><\/p><\/div>\n<p>For obvious reasons, this regulation is extremely important and, in Portugal, where water is abundant, it is not even expensive to implement. On the other hand this is not so in many parts of South Africa like Ulco, which has a very arid climate and consequently where water is difficult to obtain. Even then however, for the workers\u2019 health sake, the quarries are maintained dust free.\u00a0Going still further, at Ulco there is not only a stone quarry, but also a cement and lime factory, that is, additional potential sectors of large quantities of dust development but, as figure 175 shows, there is none.<\/p>\n<div id=\"attachment_702\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/limestonequarry.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-702\" class=\"wp-image-702 size-medium\" title=\"limestone quarry, SA\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/limestonequarry-440x290.jpg\" alt=\"Figure 176 - Ulco from the air, with the township on the right, the quarry in the middle, and the factory complex on the left (South Africa).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-702\" class=\"wp-caption-text\"><em>Figure 175 &#8211; Ulco from the air, with the township on the right, the quarry in the middle, and the factory complex on the left (South Africa).<\/em><\/p><\/div>\n<p>Still to do with construction and ornamental stone we look now at the extraction of marble. The interesting aspect here is that technology has already managed to do away with blasting, which used to cause a lot of wastage due to excessive and uncontrolled cracking of the rock, even under very cautious controlled methods. Nowadays a <strong><span id=\"diamond\">diamond wire\u00a0<\/span><\/strong><span id=\"diamond\">is used<\/span>, that is, a wire line impregnated with diamond chips. Figure 176 shows the control unit as well as the two sides of the wire loop. On the far side, out of the picture, there is a pulley positioned in such a fashion that the wire is in continuous contact with the marble to be cut. In other words it is a \u00a0sort of band saw.<\/p>\n<div id=\"attachment_704\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/marblecutter.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-704\" class=\"wp-image-704 size-medium\" title=\"marble wire cutter\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/marblecutter-440x289.jpg\" alt=\"Figure 177 - Wire cutter in a marble quarry (Porto Alegre region, Portugal).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-704\" class=\"wp-caption-text\"><em>Figure 176 &#8211; Wire cutter at a marble quarry (Portalegre region, Portugal).<\/em><\/p><\/div>\n<p>I can not resist going back to the problem of heritage misusage. The background of figure 176 is completely occupied with waste dumps, which is another example of shortsightedness, since nature is a human heritage to be preserved and not to be abused.<\/p>\n<h3><strong>9.4 UNDERGROUND<\/strong><\/h3>\n<p>Naturally mining is cheaper at the surface than underground. Hence, mining will only go underground if the desired material can no longer be extracted from the surface, or if that material does not outcrop.<\/p>\n<h4><strong>9.4.1 Marble<\/strong><\/h4>\n<p>I visited the quarry\/mine shown in figure 177, in November of 1998. It is apparent that the exploitation is still within day light. In fact it is a case of cutting inwards from a central open pit. Going underground reduces the need to remove the thick overburden constituted by very weathered and broken marble, thus reducing waste removal. One can have an idea on how close the surface is, because the weathering effect is still noticeable on the upper section of the central portion, which is a structural support pillar. By the way, this pilar also shows how well the wire cutting mechanism mentioned above works.<\/p>\n<div id=\"attachment_716\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/marbleunderground.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-716\" class=\"wp-image-716 size-medium\" title=\"underground marble operation, Portugal\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/marbleunderground-440x696.jpg\" alt=\"Figure 178 - Underground mining of marble (Porto Alegre region, Portugal).\" width=\"440\" height=\"696\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/marbleunderground-440x696.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/marbleunderground-647x1024.jpg 647w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/marbleunderground.jpg 809w\" sizes=\"auto, (max-width: 440px) 100vw, 440px\" \/><\/a><p id=\"caption-attachment-716\" class=\"wp-caption-text\"><em>Figure 177 &#8211; Underground mining of marble (Porto Alegre region, Portugal).<\/em><\/p><\/div>\n<p>Naturally, as the picture shows, this is a case of very high quality white marble, hence allowing the possibility of going underground. However, even with all these possible cost advantages, I wonder if the venture is still going. I do not have much faith in it.<\/p>\n<h4><strong>9.4.2 Rock Salt<\/strong><\/h4>\n<p>Perhaps a rather interesting and important example of early mining underground is rock salt. Obviously outcrops of such a material would not last at all, since salt is so soluble. However, salt diapers (<a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/?p=323#eva256\">item 6.5.2<\/a>) are very abundant for example, in Europe, and I&#8217;m sure it has been mined since time immemorial, because it was so useful in areas away from the coast, and it is so easily mined (fig. 178).<\/p>\n<div id=\"attachment_3005\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/PB030259-1.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3005\" class=\"wp-image-3005 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/PB030259-1-600x450.jpeg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/PB030259-1-600x450.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/PB030259-1-1024x768.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/PB030259-1-768x576.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/PB030259-1.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3005\" class=\"wp-caption-text\"><em>Figure 178 &#8211; Mining a rock salt diaper (Loul\u00e9, Portugal).<\/em><\/p><\/div>\n<p>Of these diapers, Portugal has a very unusual example in the vicinity of Rio Maior. Its extraction method is quite unique because that diaper is located in a rather large aquifer within a limestone succession.\u00a0The water in this aquifer has diluted the rock salt to a concentration seven times greater than the one of the Atlantic Ocean, approximately 30km W of this deposit. Thus, instead of having to mine the rock salt underground, the saturated water is simply drawn from a well (fig. 178B),<\/p>\n<div id=\"attachment_3007\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271320.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3007\" class=\"wp-image-3007 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271320-600x450.jpeg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271320-600x450.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271320-1024x768.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271320-768x576.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271320.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3007\" class=\"wp-caption-text\">Figure 178B &#8211; Rock salt extraction (Rio Maior, Portugal).<\/p><\/div>\n<p>and the much cleaner salt is collected from the evaporation pans around it (fig. 178C). Supposedly this deposit has been exploited on and off since 1177.<\/p>\n<div id=\"attachment_3009\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271321.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3009\" class=\"wp-image-3009 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271321-600x450.jpeg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271321-600x450.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271321-1024x768.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271321-768x576.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8271321.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3009\" class=\"wp-caption-text\">Figure 178C &#8211; The salt pans around the well.<\/p><\/div>\n<h4><\/h4>\n<h4><strong>9.4.3 Chrome<\/strong><\/h4>\n<p>The chrome mine at Boula, India, is a good example of a mine which started at the surface, but due to the space constraints with depth, it had to opt and go underground (fig. 179).<\/p>\n<div id=\"attachment_706\" style=\"width: 650px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/mineheadgear.jpg\" target=\"_blank\" rel=\"noopener noreferrer\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-706\" class=\"wp-image-706 size-large\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/mineheadgear-1024x768.jpg\" alt=\"\" width=\"640\" height=\"480\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/mineheadgear-1024x768.jpg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/mineheadgear-440x330.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/mineheadgear.jpg 1280w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><p id=\"caption-attachment-706\" class=\"wp-caption-text\"><em>Figure 179 &#8211; Boula chrome mine (Orissa, India).<\/em><\/p><\/div>\n<p>Three chrome rich zones exist in this mine. The richest, originally mined at the pit on the left, is named Shankar. To the right within a shallower pit, is the next chrome rich zone, named Lakshmi and to the right of that, outside of the picture, there is the third chrome rich zone named Durga. The Shankar section is the deepest portion of the open cast development, at the far end of which the small little building is the engine house for the hauling of ore along an inclined shaft. On the right, within the Lakshmi pit we have the more obvious headgear of a vertical shaft. It is via these two shafts that the underground mining is done. This mine has interesting features which deserve mentioning. Notice at the centre, of picture 179, the flat portion at the higher point separating the Shankar from the Lakshmi pits. That is where the ore is sorted (fig. 180)<\/p>\n<div id=\"attachment_709\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/handsorting.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-709\" class=\"wp-image-709 size-medium\" title=\"ore hand sorting, Orissa, India\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/handsorting-440x330.jpg\" alt=\"Figure 179 - Hand ore sorting (Chrome mine, Boula, India)\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-709\" class=\"wp-caption-text\"><em>Figure 180 &#8211; Hand ore sorting (Chrome mine, Boula, India).<\/em><\/p><\/div>\n<p>and piled (fig. 181). Female laborers do the sorting by hand and they are also the ones who, manually and meticulously, pack the ore on an exactly dimensioned four sided prism. This is a natural consequence of cheap labour. Note that a mechanical ore sorting machine would be far too expensive, making this venture not viable. In the same way, the packed ore does not need to be weighed, saving on the expense of such a machine. The volume of the prism is measured by tape and the tonnage is calculated using the predetermined SG of the packed ore.<\/p>\n<div id=\"attachment_711\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/orepile.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-711\" class=\"wp-image-711 size-medium\" title=\"chromite ore pile, Orissa, India\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/orepile-440x327.jpg\" alt=\"Figure 180 - Manually packed ore pile (Chrome mine, Boula, India)\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-711\" class=\"wp-caption-text\"><em>Figure 181 &#8211; Manually packed ore pile (Chrome mine, Boula, India).<\/em><\/p><\/div>\n<p>Now, the naming of the ore zones;\u00a0figure 179 is facing S and the picture was taken from a ridge formed by a fault zone with an apparent uplift to the N. On the N side of the fault, that is, behind the photographer, only one ore zone exists which was named Ganga. I find the reasoning behind the naming fascinating. If I understood it correctly, Shankar is a very important god whose wife is Lakshmi and they have a daughter called Durga. In other words, the thickest \u00a0and best developed ore zone gets the name of an important god. Next to it but not as well developed, is his wife and the weakest of the ore zones is the daughter. More, supposedly Ganga is Shankar\u2019s lover. The affair must not be obvious so Ganga is separated by a fault, but she is important and so she is at a higher level than Lakshmi\u00a0and Durga.<\/p>\n<h4><strong>9.4.4 Diamond Pipe<\/strong><\/h4>\n<p>The Kimberly pipe (<a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/?p=3#attachment_71\">fig. 17<\/a> ) is the one which started the diamond rush in South Africa and gave the name to the rock that forms it (kimberlite). This is another example of surface mining having to go underground due to lack of space.\u00a0By 1875, within the 38 acres encompassing the outcrop area of the pipe, there were hundreds of independent miners working in their separate claims as can be observed in figure 181B, showing not only the web made by the numerous cables of the active individual rock hoists, but also the depth at which they were already working.<\/p>\n<div id=\"attachment_3011\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/scan1875.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3011\" class=\"wp-image-3011 size-medium\" title=\"kimberley Mine\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/scan1875-600x388.jpeg\" alt=\"\" width=\"600\" height=\"388\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/scan1875-600x388.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/scan1875-1024x662.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/scan1875-768x497.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/scan1875.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3011\" class=\"wp-caption-text\"><em>Figure 181B &#8211; The historic Kimberley Pipe in South Africa. Photo taken in 1875, showing the existing individual rock hoists (photo obtained in the Kimberley Museum \u201csold in the aid of the Red Cross\u201d).<\/em><\/p><\/div>\n<p>The corresponding statistics shown in figure 182, gives a rather nice summary.<\/p>\n<div id=\"attachment_719\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/kimberlysection.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-719\" class=\"wp-image-719 size-medium\" title=\"kimberley pipe explanatory panel, SA\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/kimberlysection-440x291.jpg\" alt=\"Figure 182 - Diagrammatic section and statistics of the Kimberley diamond pipe (South Africa).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-719\" class=\"wp-caption-text\"><em>Figure 182 &#8211; Diagrammatic section and statistics of the Kimberley diamond pipe (South Africa).<\/em><\/p><\/div>\n<h4><\/h4>\n<h4><strong>9.4.5 Witwatersrand<\/strong><\/h4>\n<p>I think this is the best example of the influence of mining on the surface morphology and on the important differences between surface and underground mining. Figure 183 shows Johannesburg from the air, seen from the South. Notice in the background numerous large buildings. In the mid ground, with practically no buildings, there is a reasonably sized lake and two barren portions, one close to the left extremity, which is a remaining waste dump and the other of considerably larger dimension, near to the lake is a slimes (tailings) dam. This central area is where the gold bearing sedimentary horizons of the Witwatersrand Supergroup outcrop and most of that ground still belonged to the mining houses in 1984, when this picture was taken.<\/p>\n<div id=\"attachment_721\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/jhbair.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-721\" class=\"wp-image-721 size-medium\" title=\"Johannesburg from the air\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/jhbair-440x279.jpg\" alt=\"Figure 183 - Johannesburg from the air (South Africa).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-721\" class=\"wp-caption-text\"><em>Figure 183 &#8211; Johannesburg from the air (South Africa).<\/em><\/p><\/div>\n<p>These gold bearing sediments dip southwards at about 25\u00ba and the mining started going underground by about where the lake is. In other words, the houses in the foreground of the picture were built over ground mined pretty close to the surface. That is why, by municipal law, no houses of more than one floor were allowed on that sector. Nowadays all the Witwatersrand gold mines are underground and their head gears are characteristic of the region (fig. 184).<\/p>\n<div id=\"attachment_723\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/mineshaft.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-723\" class=\"size-medium wp-image-723 \" title=\"Winklehaak mine headgear, SA\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/mineshaft-440x295.jpg\" alt=\"Figure 184 - Winklehaak Gold Mine no 1 shaft and reduction works, Evander, SA\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-723\" class=\"wp-caption-text\"><em>Figure 184 &#8211; Winklehaak Gold Mine no 1 shaft and reduction works, Evander, SA.<\/em><\/p><\/div>\n<p>The haulage levels are approximately 30 vertical metres apart and the staff as well as the materials are transported by very fast lifts with stations at every level (fig. 185).<\/p>\n<div id=\"attachment_725\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/undergrstation.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-725\" class=\"size-medium wp-image-725 \" title=\"Witwatersrand gold mine underground station\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/undergrstation-440x278.jpg\" alt=\"Figure 185 - Underground lift station, East Driefontein Gold Mine (Carletonville South Africa)\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-725\" class=\"wp-caption-text\"><em>Figure 185 &#8211; Underground lift station, East Driefontein Gold Mine (Carletonville South Africa).<\/em><\/p><\/div>\n<p>All the development of the haulages used to be done by drilling and blasting (fig. 186),<\/p>\n<div id=\"attachment_727\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/undergrdrilling.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-727\" class=\"wp-image-727 size-medium\" title=\"underground drilling team\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/undergrdrilling-440x594.jpg\" alt=\"Figure 186- Underground drilling team. B - Raise borer hole (East Driefontein Gold Mine, Carletonville South Africa).\" width=\"440\" height=\"594\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/undergrdrilling-440x594.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/undergrdrilling-757x1024.jpg 757w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/undergrdrilling.jpg 947w\" sizes=\"auto, (max-width: 440px) 100vw, 440px\" \/><\/a><p id=\"caption-attachment-727\" class=\"wp-caption-text\"><em>Figure 186- Underground drilling team (East Driefontein Gold Mine, Carletonville South Africa).<\/em><\/p><\/div>\n<p>but by the time I left, 1975, boring machines were starting to be used in main haulages and raises (fig. 187).<\/p>\n<div id=\"attachment_729\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/raiseborer.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-729\" class=\"size-medium wp-image-729 \" title=\"raise borer hole\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/raiseborer-440x292.jpg\" alt=\"Figure 187 - Raise borer hole (East Driefontein Gold Mine, Carletonville South Africa).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-729\" class=\"wp-caption-text\"><em>Figure 187 &#8211; Raise borer hole (East Driefontein Gold Mine, Carletonville South Africa).<\/em><\/p><\/div>\n<p>Stopes are the section of the mine from where the ore is extracted. Since we are dealing with a sedimentary horizon, mine-wise speaking, it has a limited thickness but an unlimited length and width. Thus, wherever the grade is economical that layer of the rock sequence is entirely removed.\u00a0 Figure 188 shows a stope face with the ore exposed.<\/p>\n<div id=\"attachment_731\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stopeface.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-731\" class=\"size-medium wp-image-731 \" title=\"stope face\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stopeface-440x293.jpg\" alt=\"Figure 188 - Stope face (East Driefontein Gold Mine, Carletonville South Africa).\" width=\"600\" height=\"400\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stopeface-440x293.jpg 440w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stopeface-1024x682.jpg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stopeface.jpg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-731\" class=\"wp-caption-text\"><em>Figure 188 &#8211; Stope face (East Driefontein Gold Mine, Carletonville South Africa).<\/em><\/p><\/div>\n<p>To use rock pillars, is to reduce the amount of extractable ore. Thus they used wood log mats (fig. 189). The picture shows two pillars already in place and in the middle a loose pile of mats.<\/p>\n<div id=\"attachment_733\" style=\"width: 610px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stopepillars.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-733\" class=\"size-medium wp-image-733 \" title=\"stope pillars \" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/stopepillars-440x287.jpg\" alt=\"Figure 198 - Sotpe pillar support (East Driefontein Gold Mine, Carletonville South Africa).\" width=\"600\" height=\"400\" \/><\/a><p id=\"caption-attachment-733\" class=\"wp-caption-text\"><em>Figure 189 &#8211; Sotpe pillar support (East Driefontein Gold Mine, Carletonville South Africa).<\/em><\/p><\/div>\n<p>Finally, observation of my assistant, Z\u00e9 (fig. 188), shows how hot it is in those mines. This picture was taken at about 1800m below surface and the rock temperature was close to 50\u00baC. Work is only possible because the ventilation is refrigerated.<\/p>\n<h1 style=\"text-align: center;\">10 Rehabilitation<\/h1>\n<p>As mentioned above, we should not abuse of what nature gives us, and it is our duty to rehabilitate the places destroyed by exploitation. In fact, this is a subject of grate importance, requiring a particularly detailed study. However, I know far too little about it, and all I dare to do here, is give a very brief introduction.<\/p>\n<p>For underground mines, the only example I have is the Witwatersrand gold mines in South Africa (item 9.4.5), where what comes to the surface, is the waste rock, deposited in dumps, and the ore, which is crushed to a very fine mesh, the gold is removed using cyanide, and what remains, a very fine grained sterile mush, is deposited in slimes dams. The waste rock consists of very hard quartzite, and that is reprocessed as gravel for construction. However, the rehabilitation of the slimes dams was much more complex. The slimes dry to a fine dust which, on windy days used to cover the nearby houses. Eventually, the solution encountered was to cover those dams with thick layers of fertile soil and vegetate them as quickly as possible.<\/p>\n<p>Regarding open cast mining, often it is nature that has to do most of the work, because the quarries, most often, \u00a0are simply abandoned (fig. 190),<\/p>\n<div id=\"attachment_2799\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8042994.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-2799\" class=\"size-medium wp-image-2799\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8042994-600x450.jpg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8042994-600x450.jpg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8042994-1024x768.jpg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8042994-768x576.jpg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8042994-1536x1152.jpg 1536w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/P8042994.jpg 1632w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-2799\" class=\"wp-caption-text\">Figure 190 &#8211; <i>Abandoned granite pegmatite quarry (Azias, Portugal)<\/i><\/p><\/div>\n<p>or the area is merely fenced off, when the site is within an inhabited area (fig. 191). Fortunately nature is very resilient and recovers quite well, but it is a very slow process.<\/p>\n<div id=\"attachment_3015\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_1969-1.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3015\" class=\"wp-image-3015 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_1969-1-600x450.jpeg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_1969-1-600x450.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_1969-1-1024x768.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_1969-1-768x576.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_1969-1.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3015\" class=\"wp-caption-text\">Figure 191 &#8211; Fenced off abandoned limestone quarry within the town of Maceira (Portugal).<\/p><\/div>\n<p>However, in the case of sulphide ores, rehabilitation becomes much more complex because the oxidation of the sulphides (fig. 192),<\/p>\n<div id=\"attachment_2803\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02766.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-2803\" class=\"size-medium wp-image-2803\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02766-600x450.jpg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02766-600x450.jpg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02766-1024x768.jpg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02766-768x576.jpg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02766.jpg 1296w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-2803\" class=\"wp-caption-text\">Figure 192 &#8211; S. Domingos Copper Mine, Portugal &#8211; One of the pit&#8217;s faces.<\/p><\/div>\n<p>makes the water acidic (fig. 193), completely inhibiting the growth of vegetation. The example I show is of a very small open pit copper mine in Portugal, which ceased its work in 1965, and as can be seen in figure 192 taken in 2010, there are no signs of any vegetation whatsoever. Worst still, these sulphide open pit mines tend to be very large indeed, and it must be incredibly difficult to rehabilitate them.<\/p>\n<div id=\"attachment_3019\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02765.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3019\" class=\"wp-image-3019 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02765-600x450.jpeg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02765-600x450.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02765-1024x768.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02765-768x576.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/DSC02765.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3019\" class=\"wp-caption-text\">Figure 193 &#8211; S. Domingos Copper Mine, Portugal &#8211; The water at the bottom of the pit.<\/p><\/div>\n<p>Returning to simpler cases, it may also happen that nature is eventually assisted, like in Jardim da Alagoa (fig. 194) where, much later, after the quarry ceased its work, an imaginative person adapted the almost finished nature&#8217;s work into a park for the benefit of the local community.<\/p>\n<div id=\"attachment_3021\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_2095-1.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3021\" class=\"wp-image-3021 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_2095-1-600x450.jpeg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_2095-1-600x450.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_2095-1-1024x768.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_2095-1-768x576.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/IMG_2095-1.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3021\" class=\"wp-caption-text\">Figure 194 &#8211; Old abandoned gravel quarry eventually rehabilitated into a public park (Jardim da Alagoa, Carcavelos, Portugal)<\/p><\/div>\n<p>On the other hand, there are numerous other cases where creative people transform sights scarred by quarrying, into wonderful spots, of which I have only been fortunate to visit two, one in South Africa where the quarry was transformed into a water bird sanctuary (fig. 195),<\/p>\n<div id=\"attachment_3024\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C15S28-1.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3024\" class=\"wp-image-3024 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C15S28-1-600x387.jpeg\" alt=\"\" width=\"600\" height=\"387\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C15S28-1-600x387.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C15S28-1-1024x661.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C15S28-1-768x496.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C15S28-1.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3024\" class=\"wp-caption-text\">Figure 195 &#8211; Old gravel quarry rehabilitated into a bird sanctuary (Umgeni Bird Park, South Africa).<\/p><\/div>\n<p>and the other in Cornwall, the Eden Project, my favourite, where the Earth&#8217;s main natural biomes are displayed in two plastic domes within a large open garden representing the temperate climate (fig. 196).<\/p>\n<div id=\"attachment_3027\" style=\"width: 610px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C36S10-1.jpeg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3027\" class=\"wp-image-3027 size-medium\" src=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C36S10-1-600x403.jpeg\" alt=\"\" width=\"600\" height=\"403\" srcset=\"https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C36S10-1-600x403.jpeg 600w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C36S10-1-1024x687.jpeg 1024w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C36S10-1-768x515.jpeg 768w, https:\/\/geologicalintroduction.baffl.co.uk\/wp-content\/uploads\/2009\/02\/C36S10-1.jpeg 1280w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><\/a><p id=\"caption-attachment-3027\" class=\"wp-caption-text\">Figure 196 &#8211; Old clay pit rehabilitated into an Earth&#8217;s Biome exhibit (Cornwall, Great Britain).<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>9.1 PRIMITIVE EXTRACTION I include under mining all human activities concerned with the extraction of inert natural materials. As such, the extraction\u00a0of stone for construction, is mining, and at the beginning, perhaps the easiest was the excavation in relatively soft &hellip; <a href=\"https:\/\/geologicalintroduction.baffl.co.uk\/?p=672\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3,12],"tags":[],"class_list":["post-672","post","type-post","status-publish","format-standard","hentry","category-geology","category-mining"],"_links":{"self":[{"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=\/wp\/v2\/posts\/672","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=672"}],"version-history":[{"count":253,"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=\/wp\/v2\/posts\/672\/revisions"}],"predecessor-version":[{"id":3028,"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=\/wp\/v2\/posts\/672\/revisions\/3028"}],"wp:attachment":[{"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=672"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=672"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/geologicalintroduction.baffl.co.uk\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=672"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}