Laserfiche WebLink
<br />Mount Carbon Metropolitan District <br />Job No. 1-1107-6292-00 <br />-2- <br />records indicating that 20 tons of coal were removed between 1934 and 1936. <br />The Bluebird Maps seem to include the workings of the previous Satanic and <br />Sharon Mines. The Bluebird workings are mapped for more than 1,800 feet <br />southeast along strike from the location of the shaft, shown on figure 1, <br />attached. The workings are up to 950 feet in depth. <br />five pit-like subsidence features were noted south of Alameda Parkway on the <br />City of Lakewood park property in the southwest corner of Section 24. The <br />pits are linearly oriented, generally along strike. The two southernmost <br />depressions are thought to correspond to the locations of the Bluebird hoist <br />shaft and portal. Evidence of surface workings of the Rooney-White Ash Mine is <br />visible north of Alameda on the same bearing. No distress was noted in the <br />Alameda Roadway. These subsidence depressions were the only ones noted on the <br />parcel and are almost certainly related to the various shafts necessary to <br />service the mines. No evidence of large-scale collapse of underground work- <br />ings was noted, although some of the maps indicate that mining took place <br />within 50 feet of the surface near Alameda Parkway. <br />The theoretical subsidence trough profile on the parcel would start at the <br />western edge of the coal seams in the Laramie and extend far to the east <br />under the park property. The areas of maximum possible subsidence would <br />be over the strike trace of the coals and for several hundred feet just to the <br />east of the known depressions. The probability of mesurable subsidence to the <br />west of the coal seam from mining within the seam is exceedingly remote. Any <br />possible subsidence at the surface would be mast likely from the shallow <br />workings of the mines and very much less likely from the deep workings <br />due to bridging effects of deep overlying hard sedimentary layers and bulking <br />effects as voids fill in from below. For example, subsidence expected from a <br />` :00 foot deep extracted seam would be much more than the same thickness of <br />extraction much deeper. <br />As further regards the alignment of McIntyre Street onto the park parcel as <br />shown on maps supplied to this office, a further concern is brought forth. <br />The mesa associated with the Chieftain Clay Surface Mine is quite steep-sided <br />and during the spring of this year, a significant landslide mass has moved <br />off the hill, nearly into the proposed alignment. We recommend that if the <br />roadway is to pass close to the toe of the mesa, the mesa be cut back in <br />benches to a safer overall slope. <br />We have found that Alameda Parkway was originally built by the City of Denver <br />as an access road to Red Rocks Park in the 1930's. It is doubtful if special <br />considerations were taken in its design as it crosses the Rooney-White Ash <br />However, it can be assumed that for a proposed alignment of a major atertial <br />such as McIntyre Street to cross an area known to contain obvious subsidence <br />features and subject to the most probable future subsidence, a very high <br />level investigation would be recommended to show how the roadway could be <br />built over the shallow workings and continue to be safe for travel. We are of <br />the opinion that such a detailed investigation would be expensive and may <br />