Terrene Investments, Ltd., Deerbrook Construction, Inc., Tax Matters Partner - Page 11




                                       - 11 -                                         
               Terrene contends that the FMV on November 15, 1998 was                 
          $1,801,618.  Terrene first argues that no comparable sales exist,           
          so we must use only the DCF method.  Terrene also argues--                  
          crucially as it turns out--that the type of interest to which we            
          should be applying that method is a royalty interest, not an                
          operating interest.  Terrene’s expert, Gerald Ebanks, began with            
          the field logs and samples that were part of a Geotest report               
          that wasn’t contested by either party.  Based on these soil                 
          borings, Ebanks created an isopach map3 of the aggregate across             
          the property.  He then subtracted a 25-foot nonminable setback              
          next to Hamblen Road, multiplied the remainder by 12% to reflect            
          the increase in the volume of sand and gravel once they’re                  
          brought to the surface, and finally determined that the total               
          minable deposits were 3,973,149 tons.  He estimated that a                  
          prudent slope of the pit walls and the usual operations of a mine           
          would reduce the total tons of minable aggregate to 3,637,000.              
          Unlike Moritz, Ebanks did not include a work area in his                    
          calculation because he assumed that the operator would build a              
          workplant somewhere on the 24-acre parcel still owned by Terrene            
          that was sand-and-gravel-free.  Ebanks’s hypothetical mine                  
          operator would produce at a much higher rate than Moritz’s--                


               3 An isopach map depicts the thickness of deposits (in this            
          case, sand and gravel deposits) as contour lines, called                    
          isopachs.  Think of it as a topographic map, except that the                
          contour lines are subterranean.  Ebanks’s isopach map assumes               
          that changes in the thickness of sand and gravel deposits between           
          boreholes are linear.                                                       





Page:  Previous  4  5  6  7  8  9  10  11  12  13  14  15  16  17  18  Next 

Last modified: November 10, 2007