Laserfiche WebLink
-4- <br /> scale and nature of the slump itself, the sediment load of <br /> the south fork of Coal Creek might be temporarily <br /> increased . No other significant effects can be projected . <br /> It should be noted that the memorandum from Mr . Jim <br /> Pendleton to Ms . Candace Thompson dated January 14, 1986, <br /> and upon which the Technical Revision approved February 3, <br /> 1986, was based, contains a misinterpretation of data <br /> presented by MCR to establish an angle of draw of 180 for <br /> the Coal Basin Mines area. Mr . Pendleton interpreted the <br /> report written by the writer while acting as consultant to <br /> MCR as demonstrating " . . .that observed angles of draw have <br /> varied from 13 degrees to 21 degrees . . . " . In fact, the <br /> report established, given the data available at its writing, <br /> that 210 was the min mum adjusted angle between a mined-out <br /> area and a monitoring point that had not moved, given the <br /> monitoring point density. Thus the actual maximum angle of <br /> draw was less than 2 °, and based on the calculations made <br /> at the time was estimated at 180; this was intended as an <br /> approximate maximum, and not an average . MCR makes this <br /> point only for clari6ication and future reference, and does <br /> not dispute the 20 . 5 reference angle now included in the <br /> permit . <br /> In summary, local surface cracking in the general area of <br /> mining operations wa detected during the subsidence survey <br /> conducted as require; during the late summer of 1988 . All <br /> observed features we a on surface under which no coal has <br /> been mined, both wit in and outside of the maximum projected <br /> angle of draw of 20 . °. The major feature parallels <br /> topography rather th n mined-out area boundaries, is <br /> apparently related t an existing ancient slump block, and <br /> has its major develo ment at its greatest distance from <br /> mined-out area, dyin out at both ends as mined-out areas <br /> are approached . Bas d on the available data, the features <br /> are thus assumed to a natural ridge-line slumpage cracks, <br /> with movement trigge ed by natural processes, including <br /> excessive precipitation and possibly reactivation of old <br /> slippage plans related to the existing slump block . Worst- <br /> case effects of continued movement would be limited to <br /> resumption of slumping and possible increase of upper Coal <br /> Creek silt load, depending on scale and nature of slumpage . <br /> In reference to Stipulation No . 1 of its approved Technical <br /> Revision, MCR proposes to monitor the area by visual <br /> observation during subsequent summer field seasons; full- <br /> scale resumption of the subsidence monitoring program would <br /> be meaningless as th re are no subsidence monitoring points <br /> or control points in the area of concern. <br /> A sketch map showing the area discussed, the approximate <br /> location and extent of the two cracks discussed, subsidence <br /> monitoring and control points and subjacent mine workings is <br /> attached . Please note that weather conditions prohibited <br /> accurate mapping of these features . Specifically, the <br />