To: jerry janko  who wrote (108 ) 11/18/1999 11:27:00 AM From: Len Hynes     Respond to    of 123  
FOR FURTHER INFORMATION PLEASE CONTACT: COPPER HILL CORPORATION 709-739-4780 709-739-4785 (FAX) copperhillcorp.com NEWS RELEASE TRANSMITTED BY CANADIAN CORPORATE NEWS FOR:  COPPER HILL CORPORATION SHARES OUTSTANDING:16,647,140 (FULLY DILUTED: 17,751,140) CANADIAN DEALING NETWORK SYMBOL:  CUHL NOVEMBER 18, 1999 COPPER HILL CORPORATION ("COPPER HILL") DISCOVERY HOLE PN-99-01 INTERSECTED BANDED SILICATES-POLYMETALLIC BASE METAL SULPHIDES WITH UP TO 7.4% Zn HOSTED IN ROBERTS ARM BELT ST. JOHN'S, NEWFOUNDLAND--Copper Hill is pleased to report very  encouraging assay results from the vertically drilled borehole  PN-99-01 on its North Powderhorn Lake property, Central Mineral  Belt of Newfoundland. The property is situated 40 km south of  Springdale and 40 km west of the Central Newfoundland community of Grand Falls-Windsor, adjacent to the Trans-Canada Highway.   As previously reported (Press Release 99-07) the sulphides are  dominantly stritiform/stratibound and are hosted by variably  silicious lithologies (sediments/tuffs/rhyolites). Similar  mineralization has been observed in outcrops and boulders  dispersed throughout the property. These host lithologies are  geologically equivalent (L. Dickson, Dept. of Mines and Energy,  Government of Newfoundland and Labrador) to the Roberts Arm Belt  which hosted the Buchans VMS deposits (17.8 million tonnes  averaging 14.88% Zn, 7.7% Pb, 1.3% Cu, 3.7 opt Ag and 0.045 opt  Au; Zn:Cu ratio of approximately 11:1).  The analytical results  from borehole PN-99-01 (given as ranges) tabled below are arranged in order of increasing in hole and stratigraphic depth.  /T/ ------------------------------------------------------------------------ Zone/Interval         Cu             Zn               Pb  (in meters)          (%)            (%)              (ppm)  ------------------------------------------------------------------------ Lean Zn   facies 6.4 - 19.0       .003 - .039      .010 - .043        6 - 25   ------------------------------------------------------------------------ Zn facies 19.0 - 24.5      .015 - .125      .109 - 1.10      292 - 1503  ------------------------------------------------------------------------ Zn facies 24.5 - 26.8      .115 - .262       .34 - 7.40       28 - 376  ------------------------------------------------------------------------ Lean "Cu facies" 26.8 - 33.8      .007 - .037      .009 - .067        2 - 19  ------------------------------------------------------------------------ Zone/Interval        Au               Ag              Cd  (in meters)        (ppb)            (ppm)            (ppm) ------------------------------------------------------------------------ Lean Zn   facies 6.4 - 19.0          5 - 13         0.3 - 0.8       0.5 - 1.3 ------------------------------------------------------------------------ Zn facies 19.0 - 24.5         9 - 111        1.3 - 9.0       1.4 - 49.8 ------------------------------------------------------------------------ Zn facies 24.5 - 26.8        58 - 182        2.6 - 4.1     11.4 - greater than 110 ------------------------------------------------------------------------ Lean "Cu facies" 26.8 - 33.8         5 - 40         0.2 -0.8        0.5 - 10.6 ------------------------------------------------------------------------ /T/ The results suggest the following:  1.   The presence of a primary metal zoning with a zinc-facies  (6.4 to 26.8 m) variably rich in Pb-Au-Ag-Cd, and a Zn:Cu ratio of approximately 10:1 overlying a Cu facies (26.8 to 33.8 m) with a  Zn:Cu ratio of 1:1 to 1:10.  2.   The primary metal zoning agrees with stratigraphic "tops"  being uphole, which in turn, would agree with a structural  location on the east limb of the regionally-identified anticline.  3.   Within the zinc facies (17.0 to 26.8 m) the relative  concentrations of Pb and Ag decreases with depth, whereas the  relative concentrations of Cu and Zn increase with depth.  4.   The higher grade Au mineralization (250 - 2540 ppb)  encountered on surface at the Lake Zone and the Road Zone (Press  Release 99-03) was apparently not intersected at the depth  penetrated.  It remains to be proven that vectoring of mineralization will in  turn assist in identifying variations in the intensity of  alteration and cordierite development in the footwall lithologies. Also, PN-99-01 being randomly located and drilled to a depth of 36 m will greatly assist in the data interpretation from future  geophysical surveys. The drill rig remains on site.   All analyses were performed by Eastern Analytical Ltd., Springdale Newfoundland. Copper Hill which trades on the CDN holds a number  of mineral exploration projects in Newfoundland and Labrador. For  further information, please call 709-739-4780; fax: 709-739-4785,  or visit our web site home page at copperhillcorp.com to view  project location maps and other data.   On behalf of the Board of Directors,  Earl R. Benson, President.         -30-