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Tue 27 Dec 2005, 8:37 sxr Uranium One Inc - Waterfound Project Drilling
SXR
 SXR                                                                             
sxr Uranium One Inc - Waterfound Project Drilling Results                       
sxr Uranium One Inc                                                             
(Formerly Southern Cross Resources Inc.)                                        
(Incorporated in Canada)                                                        
(Registration number: 15096422420)                                              
Share code on the JSE: SXR    ISIN: CA8429021089                                
Share code on the TSX: SXR   ISIN: CA8429021089                                 
("SXR")                                                                         
WATERFOUND  PROJECT  DRILLING  RESULTS                                          
* Expanded drilling program completed                                           
* Initial analytical results encouraging                                        
* Uranium at unconformity confirmed                                           
  * Strong enrichment of other metals normally associated with                  
    uranium                                                                     
  * Strong boron halo present that is also an indicator of uranium              
* Additional drilling warranted                                                 
sxr Uranium One Inc. (SXR) is pleased to announce results from                  
drilling recently completed by Pitchstone Exploration Ltd.                      
("Pitchstone") at the Waterfound Project.  Significant uranium                  
mineralization was encountered from this initial diamond drilling               
program.  A total of 2,714 m of drilling was completed in five holes            
and initial analytical results are available for 27 samples taken               
from radioactive zones in holes WF02 and WF03.  sxr Uranium One is              
funding the Waterfound Project and is earning a 50% interest in five            
of Pitchstone"s seven Athabasca Basin projects.                                 
Anomalous Mineralization                                                        
In hole WF02, a 2.8 m core interval straddling the unconformity                 
averages 94 ppm uranium including 338 ppm (0.04 % U3O8) over a 0.39             
m interval of sandstone immediately above the unconformity, which is            
at a depth of 441.3 m.  The background uranium content in basal                 
Athabasca Group sandstone is typically 5.0 ppm or less.  Uranium in             
WF02 is accompanied by a strong enrichment in other metals,                     
including cobalt to 26 ppm, copper to 135 ppm, nickel to 189 ppm and            
vanadium to 161 ppm.  Analytical results also indicate strong boron             
enrichment, both within the uraniferous zone (to 910 ppm) and higher            
in the hole (to 295 ppm).  Anomalous uranium (to 22 ppm), nickel (to            
87 ppm) and boron (to 136 ppm) were also reported in samples in                 
proximity to the unconformity from hole WF03.                                   
Holes WF02 and WF03 were drilled 700 m apart along the strike of a              
six kilometer long conductive zone (see News Release 05.05, Nov. 23,            
2005).  Considering the small size of Athabasca uranium deposits,               
the extremely wide spacing between these holes indicates an                     
extensive zone of alteration and metal enrichment.  In addition to              
boron enrichment, alteration noted during core logging includes                 
chloritization, silicification, bleaching, hematitization and                   
moderate clay alteration.                                                       
Analytical results for samples collected in all holes for                       
geochemical study, as well as samples from a 0.2 m radioactive zone             

in WF05, are not yet available.  No radioactivity was detected in               
holes WF01 or WF04.                                                             
Significant Waterfound Features                                                 
The coincidence of anomalous geological and geochemical features in             
proximity to the basal Athabasca Group unconformity is considered               
important due to a similar association at many Athabasca uranium                
deposits.  Important features documented at Waterfound include:                 
1. significant uranium enrichment                                             
  2. anomalous copper, nickel, cobalt and vanadium                              
  3. an alteration halo that includes boron enrichment,                         
     chloritization, silicification, bleaching, hematitization and              
moderate clay alteration                                                   
  4. a thick sequence of graphite-pyrite-garnet-cordierite pelitic              
     rocks immediately below Athabasca Group sandstone in four of               
     five holes drilled.                                                        
Future Exploration                                                              
Strong metal enrichment and favorable alteration intersected over a             
large area has significantly upgraded the Waterfound Project and                
additional drilling is warranted.                                               
The Waterfound project is situated in the eastern Athabasca Basin,              
Saskatchewan.  The drilling at Waterfound is the first phase of an              
8,600 m program by Pitchstone and sxr Uranium One that will test                
targets at the Darby and Candle Projects beginning in January .                 
E.A.G. (Ted) Trueman, P.Eng., P.Geo., is the Qualified Person for               
the purposes of NI 43-101 with respect to the technical information             
in this news release.  Sample preparation and analyses were done by             
SRC Geoanalytical Laboratories of Saskatoon.  A partial digestion               
with chemical analyses (fluorimetry) was used for uranium                       
determinations.                                                                 
sxr Uranium One                                                                 
sxr Uranium One began trading on the JSE and the TSX on 19th                    
December 2005.  sxr Uranium One was formed through the reverse take             
over of  Southern Cross Resources Inc by Aflease Gold and Uranium               
Resources Ltd.                                                                  
Forward-looking statements                                                      
This announcement contains certain forward-looking statements.                  
These forward-looking statements are subject to a variety of risks              
and uncertainties which are beyond SXR Uranium One"s ability to                 
control or predict (including among others regulatory and                       
shareholder approval and market fluctuations), which could cause                
actual events or results to differ materially from those anticipated            
in such forward-looking statements.  Readers should not place undue             
reliance on forward-looking statements.                                         
Notice to Investors                                                             
This announcement does not constitute an offer to sell or an                    
invitation to purchase or subscribe for any securities.                         
For more information call:                                                      
Don Falconer     + 1 416 6713341                                                
John Fraser        + 27 82 331 7330                                             
Date: 27/12/2005 08:37:51 AM Produced by the JSE SENS Department                
                                                                                
                                                                                
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