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The property is within a larger area mapped by the Colorado <br />Geological Survey as "A-2" on Plate 2 in the report "Mineral <br />Resources Survey of Mesa County". The symbol A-2 is described <br />as "alluvial fan, gravel, significant fines, decomposed or weak <br />rock, and/or calcium carbonate". A drawing adapted from this <br />Survey map is attached to this report. <br />Western Slope Flagstone Quarry No. 2 <br />Mr. Rudy Fontanari of Clifton, Colorado presently operates a <br />quarry on his nearby property to produce primarily gravel, <br />cobbles, and boulders in the southwest corner of Section 35, <br />T 10 S, R 98 W, Sixth Principal Meridian. This quarry is about <br />0.5 mile east of the subject Powder Mountain Ranch property. <br />The existing Western Slope F1agsLOne Quarry No. 2 operates under <br />current permits for an area of 9.55 acres from the Colorado <br />Mined Land Reclamation Board, Mesa County, and other authorities. <br />The materials from the quarry have commercial value, after <br />separation, for uses such as riprap, roadfill, landscaping stone, <br />and other construction needs. <br />Description of the Alluvial Fan Materials <br />Based on exposures in nearby roadcuts and excavation at Quarry <br />No. 2, the materials in the alluvial fans are generally an <br />unsorted mixture of all sizes from silt and clay up to 10-foot <br />boulders. The high fraction of very large rock sizes and the <br />large amount of fines (silt and clay) indicate that the material <br />was transported in a very high energy, debris-choked stream <br />that could move giant boulders. The gradient of the present <br />Rapid Creek is about 600 feet per mile, as the drainage descends <br />from its head at 10,000-foot elevation on Grand Mesa down to <br />its confluence with the Colorado River at about elevation 4,800 <br />feet. The large volume of stream flow that would have been <br />necessary to move such a volume of material is believed to have _ <br />resulted from the melting of an ice cap on Grand Mesa in <br />Pleistocene times. The debris-laden stream moved down the steep <br />gradient of Rapid Creek and deposited its load as alluvial fans <br />as the stream gradient lessened near the Colorado River. <br />The fan materials in the exposures near the Powder Mountain <br />Ranch property are estimated visually to be approximately 50 <br />percent passing the No. 4 screen size (approximately < inch) <br />and 50 percent that would be retained on a No. 4 screen. No <br />samples have been screened to determine the exact gradings. <br />The coarser fraction contains all sizes of gravel, cobbles, <br />and boulders but seems to consist of a large amount of 6-inch <br />to 36-inch rocks with some boulders up to 10 feet across. The <br />rocks are almost entirely of hard, dense basalt which has <br />originated from the lava capping on Grand Mesa, with a few <br />sandstone clasts. The fragments range from angular to subrounded <br />and are generally unweathered with varying amounts of vesicles <br />2 <br />