| | A Find of Rare Pseudo-Cubic Quartz Crystals in Maine. Frank C. Perham, geologist West Paris, Maine. 1960
This find of quartz oddities was made at the Tamminen Mine, Greenwood, Maine, in the heart of Oxford County. The owner, Mr. Nestor Tamminen, and the author had suspected the location of these crystals, but due to drainage conditions, the area was difficult to work in. (ed. note: Then) Some work for feldspar in the pit during the summer of 1960 changed the water level and made the area workable.
This mine has long been recognized by collectors who come to Maine as one of the choice locations for rare and unusual minerals. The mine is located within a highly mineralized, lithia-rich pegmatite containing about fifteen separate mineral families and over forty varieties. The mineralizing solutions followed the hangingwall contacts of the pegmatite and the greater percent of the exotic minerals are found within twenty feet of the contact. The secondary mineralization was terminated with the permeating of the pegmatite by silica solutions causing pockets and vugs to form at random. Literally hundreds of pockets have been discovered in the course of mining, but rarely does any one pocket have many good quartz crystals. These crystals are unique in that rarely do you find a "common" crystal with single termination and long prisms. The crystals tend to be doubly terminated with short prisms, or to form in parallel groupings along the face of a larger crystal. Some very fine peduncled crystals have also been found in various pockets. One fact in the collectors favor is that in this location, most of the pockets were filled with a wet, sticky clay and during mining more crystals went over the dumps than were ever recovered.
The pseudo-cubic quartz crystals are not actually cubic, as the angle is not a right angle (ed note: 90°), but 85 degrees, 45 minutes (ed note: 89° 45'). When the crystals are oriented properly, it is easy to see all the faces and the side prisms, even though they are very small with respect to the enlarged faces. Until one gets the proper orientation though, it is difficult to see anything but a generally cubic block.
The actual removal of the pocket area had to be undertaken with great care because until we actually reached an opening, it was difficult to tell if one was there. The area of the crystals finally turned out to be a little over four feet long, with about twelve crystal-bearing pockets along the length of it. The mineralized area was bounded on one side by a huge block of feldspar with most of the pockets being contained in etched portions of the feldspar. The other side was solid massive quartz. For most of the four foot length, the pocket zone was lined with a light blue cleavelandite and we knew that if there were crystals, they would be in this cleavelandite zone. To remove the rock, we drilled short holes about two feet from the cleavelandite and blasted lightly. With a pinch bar, we pried out the rock hoping for a cavity of quartz crystals. |
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