Mining Operations at Mount Mica & Orchard Pit Mines, Oxford County, Maine.

Coromoto Minerals Mining Operations at Mount Mica,
March, April and May 2006

Pocket 6 Gem
Gem green tourmaline from pocket 7-06

Early 2006 work may have revealed why they call it Mount Mica

We resumed work at Mount Mica pretty much on schedule March 20th. Richard had gotten a head start the prior week on hauling out the ice and pumping the water. Or plan was to take up again trying to get around and behind pocket 11-05. Pocket 11-05 was not completely dug out. Portions of the pocket were nearly impossible to work. The bottom tapered and dropped quickly along the southern edge and in this taper some of the best gem was found.  The grand plan then was to get along side of the pocket, a little below it and work some of this narrow space from the back (down dip) side.  To accomplish this we would be mining in a southerly direction. The next week was spent on  another 3m advance. Once we had cleaned out the muck and washed the face down, we could see schist on the left had side of the advance. I had been concerned for sometime that the emergence of the collection of xenoliths was not a good sign. On the other hand, pocket 11-05 had developed within centimeters of the western edge of once of these huge xenoliths.  The near 3 months of effort to get to where we werein this effort had been in essentially barren pegmatite. So to avoid yet even more input without output, we decided to drill an number of 3m exploratory holes. At best this is a 'hit or miss' business. For example, we had very good luck mining down dip of the 1979 Dagenais pocket. Rene Dagenais, on one of his  many recent visits to Mount Mica, explained how they had similarly probed beyond his pocket in 1980 and concluded there was not much there.  His huge pocket was essentially barren of tourmaline yet we found nice tourmaline within feet of the down dip side of the pocket.  So when our  exploratory holes hit schist within meters of where we were working  in almost every direction , it was time to entertain a radical  re-working of our mining plan and .  We'll return to this area just to makeDagenais Pocket sure we have not made a similar miscalculation to Rene's.

The Mount Mica pegmatite thickens in a stepwise fashion from west to east

So far our work at Mount Mica we have intercepted 4 steps in the pegmatite. Our mining started on the far western end of the pegmatite  on step 'A' as indicated in Figure 1. 'A' proved thin at only 1.5-2.0m. Step 'A' produced pockets but no tourmaline.  As we moved closer to the main pit, we intercepted step 'B'. This step was thicker and produced pockets 1-04 through 11-04. With the exception of 1-04, all contained elbaite. Mining further to the east we entered into step 'C'.  The 1979  pocket of Rene Dagenais, pocket 28-04 and pocket 11-05 was  in each case just east of  interface between steps 'B' and 'C'. (In the image to the right the portal of the 1979 pocket can be seen just to the left (east) of the BC steps in the pegmatite.  It is clear now we spent the majority of '05 mining along the interface between steps C and D. (Dashed area in Figure 2)  There the pegmatite appeared to be quite thick, but was in fact the area where step 'C' ascended to 'D'. 

Offset Map
Figure 1:  Map of Mount Mica showing the trend of the 4 steps in the pegmatite encountered thus far
Figure 2: East- West cross section of the pegmatite detailing the 4 steps.

May under ground

Figure 3: Diagram of the under ground workings

As the pegmatite rises from step to step there is zone of enrichment in Li minerals between the steps consisting of principally of lepidolite,  spodumene, and montebrasite  with masses of pollucite,a cesium silicate. In this zone  pocketing all but ceases. Reviewing our records we could see that pockets only seemed to occur in the areas where the pegmatite has 'flattened out' and not within the interface between steps.  In Figure 3 above most of the pockets we found in '05 were aligned along the down dip side of our drift.  Once we had  mined beyond pocket 3-05 there emerged two clear garnet lines.  We followed the lower line while another seemed to go up into the ceiling of our drift.New drift Later this line descended and merged with the lower line. Eventually the combined lines to pocket 11-05. These garnet lines are also illustrated in the Figure 2 above. Since our attempt to get behind 11-05 seemed to be leading us into less productive pegmatite, we decided in late March to try to mine up to step 'D'. This would require us to drive an advance almost due north and at the same time make a steep ascent to the flatter part of  'D'. We knew the early part of this new cut would be in  pegmatite barren of pockets but we were now confident in our understanding of the structure and its relationship to pocketing not to be too worried by a few dry weeks. ( The start of the new drift is visible in the image to the right)
We chose a point to start this new cut  at the point were the Li enrichment appeared to taper out in the left wall of our workings. To get up to the flat part of 'D' as quickly as possible, an ascnet of more than 4m,  Eyewe set a goal of completing one 3m advance each week.  The purchase of a mini excavator, a Komatsu K-73, greatly assisted us in the mucking and preparation of our muck pile as a drill platform needed to rise. By April 19th we had completed 2 advances placing us somewhat behind our schedule. Though running a week late, we were pleased to see the emergence of a mineralized 'eye' on the back wall of our 2nd advance. We had seen this pattern before and we interpreted it as the margin of a zone of more enriched mineralization. So far in our new cut we had encountered little schorl or mica. This then was a slight hint at  improvement.  On the next advance our burn round exposed some colored tourmaline in cleavelandite and a little lepidolite. It seemed our gamble was paying off. (The burn is a tight drill pattern that is heavily loaded in order to open the rock in the direction of the advance. Once our burn has been successfully completed, we are left with a cavity about 1.5m square and 3m long. This cavity is then enlarged to complete the advance.)  As we were expanding the burn we hit our first pocket of 2006. Small elbaites were visible within the pocket.  Things were looking up.  ( In the image at the left the 'eye' is over Richard's shoulder. The drilled burn pattern is just to the left of the 'eye'.)

Our first pocket of 2006,  MMP1-06.
Blue elbaite
Small elbaite crystals in cookeite-MMP1-06
This 1st pocket was relatively clean and yielded a small amount of fine blue elbaite. These crystals were arrayed around a central schorl that penetrated the pocket from ceiling to floor. The schorl  was more than 12 cm in diameter and the part that was within the pocket had developed a bluish green rind. Lepidolite rimmed mica books, with points down,  projected from the ceiling.
Lepidolite Mica
Lepidolite rimmed mica books project from the ceiling.
MMP1-06 Gem in quartz
Fine gem elbaite in quartz
 The pocket, though small, took us nearly a day and a half to fully clean out. Most of the best gem was locked in  cookeite and required care to extract. 

As we expanded the advance and fanned the side walls to widen the cut, we found 3 other small clean pockets. Each had some tourmaline. Pocket 4, on the left wall of our advance contained several tourmalines locked in the pocket wall. Each started as small schorls but as the emerged into the cavity they converted to blue and green elbaite. An unusual feature of  this pocket was the quartz. A few of the quartz crystals were so included with blue tourmaline they were blue.
Pocket 2 of '06 contained large but badly fractured elbaite
MMP2-06 Included quartz
'Blue' quartz from pocket 4

  The mineralization we encountered ascended on the left wall of the advance climbing nearly to the roof of the cut near the center of the back wall and then descend rapidly into the right side wall forming an arch like pattern. This feature allowed us to make the next burn, the 4th , on the right side of the advance and above the mineralization where it would do no damage. After the burn was completed we expanded the advance on the right side above the mineralization. As we began to widen the advance left of the centerline, we drilled into a space. After shooting the holes above the drill hole that had intercepted the space, we were able to use our CP9 chipping hammer to open pocket another pocket (MMP5-06). 5 contained  elbaite of a rich blue color. The best pieces were locked within the hard lepidolite lining the bottom of the pocket. There was only limited amount of loose cookeite in pocket 5 though. In it Mary found the best elbaite. It was broken into 3 clean sections each a slightly different shade of blue . Each piece was 15 carats or more of gem.

Pocket 5
Pocket 5: Lepidolite rimmed books form the ceiling. The back is lined with coarse lepidolite
Blue Elbaite
Blue elbaite locked in the lepidolite of pocket 5

As Richard and I continued expanding our advance to the left we found another small series of interconnected vugs. For all of these pockets small was the dominant theme. After pocket 11-05 they appeared tiny yet each hadMMP6-6 Best Xtal a small offering.  A blast revealed a small vug that regurgitated this fine crystal. The 2 upper sections were substantially gemmy. This elbaite had the good fortune of not being encased in lepidolite.

We continued working to the left and soon intercepted another pocket. Once we have drilled into a pocket we often used our blow pipe  to see what might be ejected from the pocket through the drill hole. This time a small gem piece of green tourmaline came out with the mica flakes and quartz chips... a most promising sign.  By careful blasting we were able to remove the pegmatite such that we could again open the pocket using our chipping hammer. This pocket proved to be much like all of the others. Lepidolite rimmed micas formed the roof. A few fractured but gemmy BOP MMP7-06smoky quartz crystals lined the walls. The floor was coated with lepidolite but this time rather than being a bright lavender it was a pale gray. Like pocket 5, within this lepidolite some fine elbaite crystals had become entrapped.( see image at the top of the page).  Only by careful chisel work could they be liberated.  The best crystal from this pocket was very reminiscent of some of the classical Mount Mica material.

The abundance of mica in the mineralized zone of  step 'D'  is unlike anything we have so far encountered. Each blast pours out huge transparent mica books up to .6 m long and .4 m thick.  Another observation piquing our curiosity...why where the pockets we were finding now so tightly packed together?  We were use to more distributed and perhaps larger pockets. It struck me as I was examining the Loren Merrill picture in which the pockets had been flagged as to how tightly bunched the flags were. This was now our experience. In Hamlin's History of Mount Mica it was noted how abundantly mica littered the ground around the site of the initial tourmaline discovery.  Had Loren Merrill and Hamlin and others before them been working the trend we have labeled step 'D'? My projection of step 'D' led up dip to  the base of the Merrill dumps. 

Figure 4: Loren Merrill and Oliver Stone pose at Mount Mica with each of their early pockets marked with small flags

Merrill Dumps
Figure 5: By the early 1900s Merrill had expanded their workings considerably. Using a stiff legged derrick, the muck was stacked behind as the pit was advanced down dip.

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