Laserfiche WebLink
• <br />Table 2.04.6 - 3 Stratigraphy from Drillhole Log of Monitor Well <br />No. 296519-1 <br />Depth (FT) Description <br />0 - 5 Soil, brown and sandy <br />5 - 10 Sand, unconsolidated, fine grained; some <br /> interbeds of brown shale <br />10 - 35 Shale, chocolate brown, dark green, <br /> yellowish, grey and black with bright <br /> orange stained partings; shale is <br /> sandy with thin lenses of sandstone, <br /> carbonaceous at the bottom with thin beds <br /> of impure coal. <br />35 - 52 Sandstone, white, fine grained with <br /> carbonaceous lenses and streaks <br />52 - 56 Coal and streaks of carbonaceous shale <br />56 - 69 Shale and coal; carbonaceous shale and coal <br /> with pyrite overly dark grey to black <br /> hard shale. <br /> <br />69 - 74 Coal - the Cameron seam - with vitreous <br />luster, dry <br />74 - 77 Shale and impure coal; shale is black <br />and carbonaceous <br />77 - 85 Trinidad Sandstone, white, fine grained <br />with carbonaceous specks and streaks. <br />The beds strike at 170° and dip 6° to the southwest. This attitude seems <br />to be consistent throughout the permit area except where the beds have been <br />disturbed by faulting. One normal fault was observed in the existing mine pit <br />at the foot of the ridge north of the reclaimed Pryor Canyon channel (see <br />Revised Map 3). The beds are downthrown to the west with an offset of 29 <br />feet. The same fault was encountered at the mine pit inside the Pryor Canyon <br />and it is expected to extend further south into the southeast corner of the <br />permit area (Revised Map 3). Drillhole logs and sections in the Permit <br />Application under 2.04.6 also indicate that there is a fault running close to <br />the inside of the western boundary of the 1982(2) partial permit area. Other <br />faults were interpreted from aerial photographs under the stereoscope but <br />these were not always easy to verify on the ground. Some of the lineations <br />JPSA-19 <br />1 E SAIQ & ASSQCIAgS„ WC. <br />