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2- <br /> from the SE1/4 of section 18 , through the NW1/4 of section <br /> 18 and into the SW1/4 of section 7 , T. 10 S . , R. 89 W. , near <br /> the ridgeline at the southeast end of the meadow. These <br /> features were described in my report of August 30 , 1990 . <br /> The area was examine again on October 9 , 1991 , by Lew Ron <br /> Thompson, Environmen al Coordinator, and myself. The cracks <br /> first described in t e fall of 1988 had not enlarged, and in <br /> fact lesser portions of them could be found than in 1990 , <br /> much of their original extent having been filled in by <br /> surface wash or frost heaving . The pond located in the <br /> ancient slump block between the larger crack and the nearest <br /> mined-out area was full , again indicating no additional <br /> cracking toward thes old works . <br /> The single break down and away from the ridge top described <br /> in last year' s report had both deepened and widened, to up <br /> to two feet and one foot , respectively. In addition an <br /> offset of several inches had developed along short portions <br /> of this crack, which ''is parallel to the long direction and <br /> near the stoplines of longwalls 208 and 210 in the M bed and <br /> additionally is parallel to and above the startlines of <br /> longwalls 101 and 10 in the B bed. Both the direction, <br /> parallel to the pane instead of to the faces , and the <br /> offset , down on the idge-top side , are opposite of what <br /> might be expected of a subsidence-induced feature , and we <br /> remain of the opinion that these are ridgeline slumpage <br /> features . In spite of this crack' s enlargement in some <br /> places , mending by in-wash of soil material had obliterated <br /> it in others, and it was no longer than when discovered in <br /> 1990 . Other cracks in this area described in the 1990 <br /> report had not changed except for continued in-filling . <br /> A very similar crack was noted virtually on the ridge line <br /> extending northwesterly a couple hundred feet from the peak <br /> in the north center of section 18 ( highest point on Huntsman <br /> Ridge ) , parallel to the ridge and at nearly a 450 <br /> angle to <br /> the underlying longwall 208 and 101 panels . This area had <br /> been examined in 1990 and this crack was not discovered <br /> then, although it must be noted that we stood within 20 feet <br /> of it , examining the bowl below us for any signs of <br /> subsidence (none were noted) for at least 15 minutes before <br /> observing it . <br />