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1~ <br />N <br />N <br />Mr. 4l)ly Frank <br />September 23, I9B6 <br />Sanm comments specific to the E15 Lollar: <br />Page 1-3, Dera. 3. In of ew of the less controllable method of solution <br />mining, mining to rlthln 50 Teet of a lease boundary seems much too lenient ~ 22 <br />If the o11 shill! aM nshcolite On ad3olning Federal lanOS 1s tmpet rcd, are <br />there any provisions for lndemnl/f cation for loss of oil shale, nahcolite, end <br />ground water resources on these lands by the lessee? <br />Page 2-8, pare. 2.2.12.3. If substantial subsidence occurs, Mat steps wu~ <br />De taken by BLM to correct the prbblemi provisions for Daymm~t by the lessee 45 <br />far damage Lo oil shale am the sodium leases that might be caused by solution <br />mining of nahcolite should be included 1n this EIS. <br />Pa 9e }6, Dara. 3.2.3. The EIS states that the oi) shale fn the leached zone <br />is too incompetent t0 mine by conrentlenal Beans. Nhat about MI5 methods? <br />Most o! the oil shale on the C-a and C-b tracts has been leached of nahcolite <br />anO can be considered Dart of the leached zone, On the C-b tract, mining <br />plans Include retorting ail shale by an MIS method in parts of the Mahogany <br />Zone, B-groove, aiM R-6 oil-shale zones. On the C-a tract, the MI5 retort <br />No.l, Mich vas sucessfully burned, extends rerticelly from the middle oT the 3~ <br />R-5 through the R-6 to nearly the top of the Mahogany Zone. These o71 shales <br />contain ruDbll zones and solution breccias. 4lthout a comparison o! the rock <br />properties of the leached oil shale on the C-b and C-a tracts with the <br />properties of the oil shale 1n the leached zone on the sodium lease lands, the <br />conclusion that the leached zone on the sodium lands cannot De mined fs <br />untenable. The oil shale to the leached zone on the sodium leases should De <br />considered as recoreraDie resources that could be ferioutly impaired or lost <br />by solution ml ni ng of the Bales bed. <br />Page 3-7, fig. 3-111. The serattgraphy Ls too generals xed to clearly see the <br />relationships between oil shale, nahcolite, antl darsanlte. Profiles of <br />Fischer assays, nahcolite, and dewsonlte for one of the Intlustrlal Resouces <br />core holes on the sodium lease lands should De shorn to gl re the reader some <br />Idea of the vertical disLrf butlon and abundances of these resources on the 43 <br />sodium lease lands, Slmllar to that published by Cale, Oeub, and Yelchnan <br />(1982, Ceolo9y of the Norse Draw nahcolite end oil-shale mine, Ptceance Creek <br />Basin, Colorado Iln] ]5th 011 Shale Symposium Proceedings: Colo. Sch, Nines, <br />p, 15-28). <br /> <br />Mr. tally crank 3 <br />Septer~er 23, 1986 <br />Page }e, pare. 3.3.2. The trcetmenL of oil shale resources 1n this section <br />fs not adequate. Estimates oT the total tonnages of o11 shale--principal ly fn <br />the R-6 and Mahogany zones--that could Oe adversely affected by solution <br />mining should be included In a table. Tne total amount of nahcolite that would <br />be recovered Dy the proposed solution mining plan should also be included. 33 <br />The amount of 1n-piece shale-o11 resources far the Mahogany and R-6 zones on <br />the 219-acre .ell-field area under the Proposed Actfon is estimated at 140 <br />million barrels that could be adversely affected Dy solution mining as <br />opposed to production o/ an estimated 4 mf llfon tons of nah<olite (330 <br />cavities a 12,000 tons of nahcolite per cavity), <br />Sincerely yours, <br />~..G..A.&~;, <br />John R. Oynt, Geologist ono <br />i / <br />>~.-...aJ'r~a el- I.. ~] <br />Thomas Gooch, BrenrJr Cfilef7 <br />